{"type":"FeatureCollection","features":[{"type":"Feature","properties":{"id":5985,"name":"A meso-scale faulted multi-detachment fold, Khabr area, Kerman, Iran","description":"

Fault-related folding is an important process in compressive belts (Mukherjee et al. 2015). This horizontal section photograph shows a textbook example of a detachment horizon, which has developed asymmetric detachment fold (\u201cA\u201d in Fig. 1), fault-propagation fold (\u201cB\u201d in Fig. 1), and a box-fold (\u201cC\u201d in Fig. 1). The structure in the middle of the photo (\u201cB\u201d in Fig. 1) is plausibly a fold-propagation fold, where white thin beds of laminated marble is sitting as an intermediate detachment horizon (Fig. 1). The fold geometry (\u201cB\u201d in Fig. 1) is usually tighter structure than asymmetric detachment fold with a long, gently dipping backlimb and a shorter, steeply dipping forelimb. The larger fold structure in the right side (\u201cC\u201d in Fig. 1) is more complex, with multiple sharp hinges separating straight limbs as a box lift-off anticline (e.g. McClay 1992; Mitra 2002, 2003) and small scale offsets due to penetrative strain (Burberry 2015). This fold is tighter in the core. See Mukherjee (2012) for a similar kind of fold in micro-scale.
\nThese structures are well developed within the sequence of Devonian alternating layers of calcschist, meta-limestone turbidite (brown) and thin bands of laminated marble (white) and affected by east trending dextral Khabr shear zone with moderate dip to the north. This photo is taken from the Khabr Mountain (height: 3845m) (Geographic coordinates: 28\u00b052\u00b404\u02baN, 56\u00b023\u00b456\u02baE), Structural zone of Sanandaj-Sirjan metamorphic-ophiolitic Complex, southwest of the city of Baft, Kerman province, Iran.<\/span><\/p>\n

A meso-scale faulted multi-detachment fold, Khabr area, Kerman, Iran, Photo by Seyed Tohid Nabavi<\/p>\n","modified":"2018-12-12T15:07:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Picture1-1-768x434.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5985","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5985&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-meso-scale-faulted-multi-detachment-fold-khabr-area-kerman-iran\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[56.43751508107118,28.802959234513224]}},{"type":"Feature","properties":{"id":1436,"name":"A-type flanking folds","description":"

Flanking fold showing antithetic displacement in high-grade quartzites and schists (Priestely Schists); Simpson Cgraggs, Norhern Victoria Land (Ross Orogen, Antarctica). The cross-cutting element is a granite vein related to the Cambrian-Ordovician Granite Harbour Intrusives.
PhotoID233<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: R. Carosi – Unipi<\/p>\n","modified":"2018-06-15T10:21:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-type-flanking-folds-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1436","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1436&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-type-flanking-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.9713,-74.43736]}},{"type":"Feature","properties":{"id":2017,"name":"Als\u00f3telekes, gypsum open pit","description":"

Folds in laminar gypsum.
\nThe mine is located on a gypsum-anhydrite dome structure with sheath folds and other flow structures in a regional strike-slip fault zone (Darn\u00f3 Zone) Photo ID 612<\/p>\n

Photograph: N\u00e9meth Norbert<\/p>\n

Reference: ZELENKA T. \u2013 KAL\u00d3 J. \u2013 N\u00c9METH N. 2005: Az als\u00f3telekesi gipsz-anhidrit d\u00f3m szerkezete. F\u00f6ldtani K\u00f6zl\u00f6ny 135\/4, pp. 493-511. (in Hungarian)<\/p>\n","modified":"2018-06-30T19:17:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Als\u00f3telekes-gypsum-open-pit-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2017","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2017&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/alsotelekes-gypsum-open-pit\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[20.6565,48.423621]}},{"type":"Feature","properties":{"id":1269,"name":"Angular fold train","description":"

Angular fold train in a multilayer sequence (chert-limestone) at Agios Pavlos (Crete, Greece).<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-10-10T18:52:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Angular-fold-train-768x576.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1269","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1269&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/angular-fold-train\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[24.562339782714844,35.10178922694953]}},{"type":"Feature","properties":{"id":1929,"name":"Annapurna North","description":"

Km-scale North-verging F2 fold. Black shale and limestone of the Sombre Formation (Silurian-Devonian); Tibetan Sedimentary Sequence.<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Godin, L. (2003). Journal of Asian Earth Sciences, v. 22 pp. 307-328<\/p>\n","modified":"2018-09-04T13:24:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Annapurna-North-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1929","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1929&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/annapurna-north\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.71385,28.62859]}},{"type":"Feature","properties":{"id":1448,"name":"Anticlinal de La Tete de Bostan","description":"

Giant anticline known as La Tete de Bostan in thick Urgonian limestones.
PhotoID290<\/p>\n

Photograph: ch.nicollet<\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/divers\/ObjetsGeol.html#bostan<\/p>\n","modified":"2018-06-15T10:17:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Anticlinal-de-La-Tete-de-Bostan-768x319.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1448","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1448&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/anticlinal-de-la-tete-de-bostan\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.786986589431763,46.13450461045325]}},{"type":"Feature","properties":{"id":1199,"name":"antiform","description":"

asymmetric tectonic antiform in a sandstone sequence (Upper Carboniferous). PhotoID164<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-06-28T14:49:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/antiform-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1199","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1199&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/antiform\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.863488674163818,50.458854987663635]}},{"type":"Feature","properties":{"id":7128,"name":"Antiform, Pania di Corfino (Northern Apennines)","description":"

Panoramic view of the kilometric large-scale F2\u00a0 fold (open antiform) in the Corfino area involving the Tuscan Nappe (Calcare massiccio\u201d formation on top and \u201cCalcari & Marne a Rhaetavicula contorta\u201d formation below with eviedence of bedding). Mount La Bandita view to the west.<\/p>\n

Ref. Carosi et al 2004 Geodinamica Acta 17 (2004) 253\u2013273<\/p>\n","modified":"2019-08-29T10:18:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/IMG_4503-300x225.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7128","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7128&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/antiform-pania-di-corfino-northern-apennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.408263900061002,44.18231481013327]}},{"type":"Feature","properties":{"id":1572,"name":"Antiformal stack","description":"

Antiformal stack of 3 folds (remp-flat system) at the beginning of Cimoliana Valley, Cimolais – Italy
\nPhotoID668<\/p>\n

Photograph:<\/p>\n

Reference: Geological map of Friuli region<\/p>\n","modified":"2018-06-30T11:17:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Antiformal-stack-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1572","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1572&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/antiformal-stack\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[12.474889755249023,46.3439651268241]}},{"type":"Feature","properties":{"id":1979,"name":"asymmetric fold","description":"

Asymmetric NW-facing fold with some thrusting along the upper limb, producing an antithetic deflection in the steep limb . Schuld, Germany
\nPhotoID583<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T18:09:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/asymmetric-fold-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1979","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1979&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/asymmetric-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.889445246696482,50.447324520500544]}},{"type":"Feature","properties":{"id":1353,"name":"Baviaanskloof gneisses","description":"

Migmatitic, granulite-facies Baviaanskloof orthogneisses of the Southern Marginal zone of the Limpopo belt.
\nPhotoID259<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-09-04T14:55:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Baviaanskloof-gneisses-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1353","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1353&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/baviaanskloof-gneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[29.74589,-23.4441]}},{"type":"Feature","properties":{"id":1209,"name":"Bermagui Fold","description":"

This is a historic site for structural geology where generations of scientits have wondered about apparently simple folds in low grade sandstone and slate, which are more complex than they should be. Here, folations are not simply axial planar; in some cases there seem to be two axial planar crenulations overprinting each other within thier parent fold closure. Williams 1971. J geol Soc Australia 18, 215-228; Powell and Rickard 1985 JSG 7, 385-400. PhotoID170<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:38:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bermagui-Fold-768x481.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1209","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1209&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bermagui-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[150.07447063922882,-36.4220270543]}},{"type":"Feature","properties":{"id":2216,"name":"Bhuban Mohan Behera","description":"

Migmatitic Fold in Hornblende-Biotite gneiss in precambrian rock of Southern Granulite Terrane in Pallakapalayam, Tamil Nadu (India). PhotoID808<\/p>\n

Photograph: Bhuban Mohan Behera<\/p>\n","modified":"2018-09-04T11:11:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bhuban-Mohan-Behera-768x508.jpeg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2216","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2216&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bhuban-mohan-behera\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[77.75680892419814,11.448546937418941]}},{"type":"Feature","properties":{"id":1534,"name":"Big Penn slate quarry","description":"

Asymmetric anticline in Big Penn slate quarry. Slatedale, PA.
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\nPhotoID321<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T14:37:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Big-Penn-slate-quarry-768x503.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1534","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1534&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/big-penn-slate-quarry\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-75.660408,40.749519]}},{"type":"Feature","properties":{"id":1560,"name":"Box fold","description":"

Box fold. Northcott Mouth, North of Bude, Devon, England
\nPhotoID336<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:12:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Box-fold-768x503.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1560","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1560&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/box-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.555493,50.848006]}},{"type":"Feature","properties":{"id":6094,"name":"Bunglass Point, Carrick Co. Donegal, Ireland","description":"

Near Slieve League, highest sea-cliffs in west Europe.<\/p>\n","modified":"2018-12-14T11:08:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Bunglass-Point-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6094","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6094&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bunglass-point-carrick-co-donegal-ireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.686220171948662,54.62705267588337]}},{"type":"Feature","properties":{"id":1807,"name":"Camel Hills folded metapelite","description":"

Metapelite alternating with quartzite , looking West (north at the right). There is a strong stretching lineation on steeply N dipping foliation surfaces; Lstr 167-79. Camel Hills metasediments, (ca 2000 Ma).<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T16:14:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Camel-Hills-folded-metapelite-196x300.jpg","taxonomy":{"webmapp_category":[229,232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1807","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1807&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/camel-hills-folded-metapelite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.384,-25.601167]}},{"type":"Feature","properties":{"id":6083,"name":"Cashelgolan, Co. Donegal, Ireland","description":"","modified":"2018-12-14T11:09:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Fold-8JPG-768x1024.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6083","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6083&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cashelgolan-co-donegal-ireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.397561575920463,54.84407671782797]}},{"type":"Feature","properties":{"id":6025,"name":"Cashelgolan, Co. Donegal,Ireland","description":"","modified":"2018-12-14T19:49:11","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Fold-3-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6025","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6025&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cashelgolan-co-donegalireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.6846923828125,54.62740048383535]}},{"type":"Feature","properties":{"id":2184,"name":"Chamanbid Anticline","description":"

This is view of a open anticline. Inner part of the fold is Chamanbid Fm. and outer part is Mozdooran Fm.. These layers are belong to late Jurassic of Kopehdagh structural zone of Iran.
\nPhotoID754<\/p>\n

Photograph: Masoud Mirzaei<\/p>\n","modified":"2018-06-28T14:54:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Chamanbid-Anticline-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2184","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2184&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/chamanbid-anticline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[59.859812,36.593886]}},{"type":"Feature","properties":{"id":1442,"name":"Chapeau du Gendarme fold","description":"

Large and famous fold known as the Chapeau du Gendarme in limestone of the Jura Mountains
PhotoID286<\/p>\n

Photograph: ch.nicollet<\/p>\n","modified":"2018-06-15T10:17:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Chapeau-du-Gendarme-fold-768x463.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1442","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1442&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/chapeau-du-gendarme-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.905945301055908,46.35895364547408]}},{"type":"Feature","properties":{"id":1412,"name":"Chenaillet Ophiolite","description":"

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Altitude is 2400 m, so access is only possible in summer months (may-october); early summer is normally packed with french students groups.
PhotoID279<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-15T10:17:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Chenaillet-Ophiolite-225x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1412","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1412&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/chenaillet-ophiolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.7333,44.89788]}},{"type":"Feature","properties":{"id":2296,"name":"chevron fold","description":"

chevron fold present in pithoragarh district uttrakhand, India PhotoID817<\/p>\n

Photograph: vibha katiyar<\/p>\n

Reference: chevron fold present in pithoragarh district uttrakhand, India<\/p>\n","modified":"2018-07-24T16:15:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/chevron-fold-300x225.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2296","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2296&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/chevron-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[80.1149,29.33185]}},{"type":"Feature","properties":{"id":6425,"name":"Chevron Fold -Scabiazza sandstone","description":"","modified":"2019-01-29T17:14:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/2012-08-12-Piega-Chevron-Corchia-768x514.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6425","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6425&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/chevron-fold-scabiazza-sandstone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.933840831405291,44.511510663660715]}},{"type":"Feature","properties":{"id":6016,"name":"Cilindro de Marbor\u00e9","description":"

Monte Perdido, in the Central Pyrenees, constitutes the highest limestone massif in Europe, rising to the maximum height of 3355 m.a.s.l. of Monte Perdido peak. Looking west from the summit a spectacular anticlinal fold can be observed below the nearby Cilindro de Marbor\u00e9 peak (3328 m.a.s.l.). The fold is developed in a stacked Cretaceous-Paleogene sequence (Marbor\u00e9, Salarons and Gallinera Formations) deformed by thin-skinned tectonics in the imbricated thrust system of Monte Perdido unit. Later emplacement of the major Gavarnie basement thrust was accompanied by refolding of the Meso-Cenozoic sedimentary cover of its hangingwall (Flach\u00e8re, 1977. Th\u00e8se 3 cycle, Toulouse), of which this anticlinal is an extraordinary example. A paired syncline, mostly covered by scree, is located left of the main structure. The height difference between the Cilindro de Marbor\u00e9 summit and the Ib\u00f3n Helado, the lake just below it is of 350m.<\/p>\n

de Paz-\u00c1lvarez, M.I., Fl\u00f3rez-Rodr\u00edguez, A.G. (2018). Photograph of the month. Journal of Structural Geology<\/em>, 111, iii.<\/p>\n

 <\/p>\n","modified":"2018-12-12T10:05:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/23613466591_5e44b769b5_k-1-768x416.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6016","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6016&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cilindro-de-marbore\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.032573312104659635,42.67723635993417]}},{"type":"Feature","properties":{"id":1737,"name":"Col Ombert and diapiric anticline","description":"

Permian Bellerophon FM forming a diapiric antickline plus Col Ombert thrsts – San Nicol\u00f2 Valley – Dolomites
\nView from Magnifici 4 Via ferrata
\nPhotoID669<\/p>\n

Photograph: Max Scarpa<\/p>\n

Reference: – Bosellini A. Geology of Dolomites AA. VV. Geologia del Sudalpino – Geological SOc. of Italy SGI<\/p>\n","modified":"2018-06-30T12:40:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Col-Ombert-and-diapiric-anticline-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1737","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1737&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/col-ombert-and-diapiric-anticline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.790035963058472,46.42219483079669]}},{"type":"Feature","properties":{"id":1548,"name":"Concentric fold","description":"

Brecciated core of concentric fold. Grosses Roches, Quebec
\nPhotoID328<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-30T11:24:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Concentric-fold-211x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1548","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1548&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/concentric-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-67.172692,48.940749]}},{"type":"Feature","properties":{"id":1550,"name":"Concentric fold","description":"

Faulted core of a concentric fold. Notre Dame du Portage, Quebec.
\nPhotoID329<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-09-04T11:43:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Concentric-fold-1-768x536.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1550","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1550&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/concentric-fold-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-69.596701,47.793588]}},{"type":"Feature","properties":{"id":1333,"name":"Cordilleran orogenic base","description":"

Thin vein (grey layer) of the 1.9 Ga Bourne granite suite crosscutting a fold train of orthogneiss and amphibolite layers. Located a few meters below the Cordilleran orogenic base mapped in the northern Monashee Complex of the southeastern Canadian Cordillera.<\/p>\n

Crowley, J.L., Brown, R.L., Gervais, F., Gibson, H.D. (2008). Assessing zircon and monazite inheritance in granitic rocks; an example from the Monashee Complex, Canadian Cordillera. Journal of Petrology 49, 1915-1929.
Gervais, F., Brown, R.L., Crowley, J.L. (2010). Tectonic implications for a Cordilleran orogenic base in the Frenchman Cap dome, southeastern Canadian Cordillera. Journal of Structural Geology 32, 941-959.<\/p>\n

PhotoID237<\/p>\n

Photograph: F\u00e9lix Gervais<\/p>\n","modified":"2018-06-15T10:16:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cordilleran-orogenic-base-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1333","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1333&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cordilleran-orogenic-base\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.588399887,51.3353977950284]}},{"type":"Feature","properties":{"id":7161,"name":"Coriscao syncline","description":"

The eastern face of the Coriscao peak (2235m) in the Cantabrian Mountains, (NW Spain) shows the deformation associated with the external nappes of the Cantabrian Zone (NW Iberian Massif) during the Variscan Orogeny. The Panda Fm. limestones (Moscovian) were thrust on top of the Coriscao Fm. olistrostrome (Moscovian), and subsequently folded by the Coriscao syncline.<\/p>\n","modified":"2019-09-26T11:22:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/09\/3_El-sinclinal-nevado-del-Coriscao2-768x511.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7161","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7161&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/coriscao-syncline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.778738389639102,43.090446431918664]}},{"type":"Feature","properties":{"id":1480,"name":"Coronitic eclogite of Sifah","description":"

The centimetric garnet of the eclogite is surrounded by a corona of glaucophane. It indicates a retrogression from the eclogite conditions to the blueschists conditions during the exhumation of the rock. Yellow epidote and dark blue glaucophane constitute the matrix of rock. PhotoID302<\/p>\n

Photograph: ch.nicollet<\/p>\n","modified":"2018-06-15T10:17:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Coronitic-eclogite-of-Sifah-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1480","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1480&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/coronitic-eclogite-of-sifah\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[58.7794303894043,23.454900281161684]}},{"type":"Feature","properties":{"id":842,"name":"Corse 5","description":"

Sheath fold in metacherts, Locality: Accendipipa, Corse, france
\n<\/i><\/p>\n

Photo by R.Carosi, University of Torino<\/p>\n","modified":"2018-07-01T11:24:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/03\/Screenshot-2018-03-30-09.35.52-e1522395952493-768x432.png","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/842","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=842&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/corse-5\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.187788963,42.54084461]}},{"type":"Feature","properties":{"id":1803,"name":"Dalgaringa gneiss","description":"

Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations.
\nThe pavements show banded gneiss intruded by less deformed granite pegmatite veins. North at the top<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:27:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-2-768x496.jpg","taxonomy":{"webmapp_category":[229,232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1803","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1803&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57345061111448,-25.5129526909]}},{"type":"Feature","properties":{"id":1341,"name":"Deformed veins (Rainy Lake)","description":"

Photographic mosaic of a subhorizontal outcrop of four consecutive sets of differently deformed granitoid veins within foliated metavolcanic rocks. Rainy Lake transpressional zone (Ontario, Canada). PhotoID150<\/p>\n

Photograph: Elena Druguet\/Jordi Carreras<\/p>\n

Reference: Druguet, E., Czeck, D.M., Carreras, J., Casta\u00f1o, L.M., 2008. Emplacement and deformation features of syntectonic leucocratic veins from Rainy Lake zone (Western Superior Province, Canada). Precambrian Research 163, 384-400.<\/p>\n","modified":"2018-07-24T12:22:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-veins-Rainy-Lake-768x348.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1341","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1341&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-veins-rainy-lake\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-93.2719516754,48.67541938037722]}},{"type":"Feature","properties":{"id":1253,"name":"Detachment folding","description":"

Detachment folding in lower Cretaceous coal-bearing strata of the Luscar Group as exposed by mining in the AN pit of the Cardinal River Coal Mine near Hinton, Alberta, Canada. The dragline at the bottom of the pit provides a scale. The Jewel Coal Seam, which has a stratigraphic thickness of 10 m, is structurally thickened in the cores of chevron-type folds, providing enhanced mining situations. There are various detachment horizons. The one visible in the picture is at the contact of the Jewel Coal Seam (black in the centre of the picture) and the underlying sandstone of the Torrens Member. On a larger scale there is detachment along the underlying Folding Mountain\/Mystery Lake Thrust, which in places follows shale horizons in the Nikanassin and Fernie formations. These folds form part of the Cadomin Syncline, which is a footwall syncline of the Nikanassin\/Drinnan Thrust.<\/p>\n

Lebel, D., Langenberg, C.W. and Mountjoy, E.W. (1996). Bulletin of Canadian Petroleum Geology 44, 282-298<\/p>\n

This is a Journal of Structural Geology Photograph of the Month (JSG 30, 547). Photo ID 201<\/p>\n

Photograph: Willem Langenberg<\/p>\n","modified":"2018-07-24T12:28:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Detachment-folding-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1253","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1253&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/detachment-folding\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-117.44258,53.06469]}},{"type":"Feature","properties":{"id":2180,"name":"Detail of Col Ombert Thrust","description":"

A detail of previous pic. Basal Col Ombert thrust and folded strata.
\nPhotoID752<\/p>\n

Photograph: Max Scarpa<\/p>\n

Reference: A. Castellarin F. Guy, L. Selli Geologia dei dintorni di Passo San Nicol\u00f2 e della Valle del Contrin – Mem. Soc. Geol. Guida alla geologia del Sudalpino centro-orientale<\/p>\n","modified":"2018-07-28T18:17:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Detail-of-Col-Ombert-Thrust-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2180","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2180&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/detail-of-col-ombert-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.797492504119873,46.419280805842625]}},{"type":"Feature","properties":{"id":1233,"name":"Disharmonic folds, Marble Point","description":"

Disharmonic folds in marbles deformed during the Ross Orogeny, Marble Point, Victoria Land (Antarctica). PhotoID187<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:53:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Disharmonic-folds-Marble-Point-300x192.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1233","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1233&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/disharmonic-folds-marble-point\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.833,-77.433]}},{"type":"Feature","properties":{"id":1504,"name":"Ecum Secum","description":"

Folded crossbedded sandstone in slate, Ecu Secum. The outcrops are also famous for deformed burrows
\nPhotoID284<\/p>\n

Photograph:<\/p>\n","modified":"2018-09-04T15:52:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ecum-Secum-768x518.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1504","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1504&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ecum-secum\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-61.156132,44.967428]}},{"type":"Feature","properties":{"id":1377,"name":"F1 fold, Argentiera","description":"

South-west facing F1 fold in Paleozoic quartzites involved in the Variscan Orogeny; Nurra Peninsula (Sardinia, Italy).
\nPhotoID180<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2019-01-07T12:51:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/F1-fold-Argentiera-300x202.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1377","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1377&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/f1-fold-argentiera\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.137432849838206,40.73386788922788]}},{"type":"Feature","properties":{"id":1393,"name":"F1 fold, Scaglia Toscana","description":"

Urpight F1 folds in pelites and limestones of the Scaglia Toscana Formation and refraction of S1 continuos foliation. Sassorosso, Lucca (Northern Appennines, Italy). PhotoID189<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CAROSI R., MONTOMOLI C., PERTUSATI P.C. (2004) – Late tectonic evolution of the Northern Apennines: the role of contractional tectonics in the exhumation of the Tuscan Units. Geodinamica Acta, 17, 4, 253-273, Lovoisier Parigi.<\/p>\n","modified":"2018-06-15T10:20:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/F1-fold-Scaglia-Toscana-209x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1393","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1393&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/f1-fold-scaglia-toscana\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.405371,44.184598]}},{"type":"Feature","properties":{"id":1223,"name":"F2 folds, Tukuche Peak","description":"

Overturned F2 folds on the south-eastern slope of Tukuche Peak (6950 m) affecting Ordovician to Devonian succession of the Tethyan Sedimentary Sequence (Kali Gandaki valley, Nepal). Height of the slope is >3000 m. PhotoID179<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2019-01-07T12:53:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/F2-folds-Tukuche-Peak-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1223","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1223&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/f2-folds-tukuche-peak\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.7661927947388,28.79535103893526]}},{"type":"Feature","properties":{"id":6672,"name":"Farini d\u2019Olmo Flysch (Paleocene-Early Eocene). Fold. Nure Valley. Piacenza (Italy)","description":"","modified":"2019-03-01T08:04:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/2017-07-30-Flysch-Farini-commentata-768x514.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6672","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6672&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/farini-dolmo-flysch-paleocene-early-eocene-fold-nure-valley-piacenza-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.579472883329117,44.71969867792041]}},{"type":"Feature","properties":{"id":7029,"name":"Fault and fold in calcschist of Giens near Hy\u00e8res, France","description":"

\"\"<\/p>\n

Giens peninsula (near Hy\u00e8res, France) has beautiful outcrops of metamorphic rocks. Some are folded and faulted like on this picture on the western side of the peninsula.<\/p>\n","modified":"2019-06-16T19:45:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-768x1024.jpg","taxonomy":{"webmapp_category":[220,229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7029","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7029&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-and-fold-in-calcschist-of-giens-near-hyeres-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.096309,43.028767]}},{"type":"Feature","properties":{"id":6849,"name":"Fault and folds in Calanques, close to Marseille","description":"

Normal N140 fault (that will form the Grande Candelle) and associated folds in the upper Berriasian and lower Valanginian in the Calanques, near Marseille.<\/p>\n","modified":"2019-04-22T08:45:59","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/04\/P4140136-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6849","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6849&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-and-folds-in-calanques-close-to-marseille\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.450431311500552,43.21679260993947]}},{"type":"Feature","properties":{"id":2236,"name":"Faulted fold with quartz veins","description":"

Irregular brittle fault splay cutting small anticline in Neoproterozoic-Cambrian Malmesbury Formation sandstone on Robben Island. Table Mountain in the background.
\nPhotoIF783<\/p>\n

Photograph: Christie Rowe<\/p>\n

Reference: Rowe, C. D., *Backeberg, N., *van Rensburg, T., *Maclennan, S., *Faber, C., *Curtis, C. and *Viglietti, P. (2010) Structural geology of Robben Island: Implications for the tectonic environment of Saldanian deformation, South African Journal of Geology 113.1 57-72. (Download geologic map eps.mcgill.ca\/~crowe\/publications)<\/p>\n","modified":"2018-09-04T11:21:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Faulted-fold-with-quartz-veins-768x512.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2236","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2236&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/faulted-fold-with-quartz-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[18.371931,-33.820772]}},{"type":"Feature","properties":{"id":1409,"name":"Flanking folds and boudins","description":"

This photograph shows modified boudin structures from Wilson Bluff in the Southern Prince Charles Mountains, East Antarctica. There is an impressive flanking-fold structure situated between the torn mafic boudins, that presumably formed by ductile flow of the overlying host grey gneiss into a low-pressure sink during the boudin separation. Subsequent reworking and shortening is indicated by numerous folded boudin structures in the leucocratic pegmatite material. The timing of the structures is uncertain but the host rock is of Precambrian age. The exposure is southwest facing. PhotoID200<\/p>\n

Photograph: Adrian F Corvino<\/p>\n

Reference: This is a photograph of the Month in the Journal of Structural geology (JSG 32, 1)<\/p>\n","modified":"2018-06-15T10:21:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Flanking-folds-and-boudins-768x509.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1409","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1409&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/flanking-folds-and-boudins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[66.78333,-70.3]}},{"type":"Feature","properties":{"id":1687,"name":"fold and cleavage","description":"

fold and cleavage, Ellesmere Island
\nPhotoID418<\/p>\n

Photograph: Vicky Pease<\/p>\n","modified":"2018-06-28T14:41:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/fold-and-cleavage-768x576.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1687","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1687&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fold-and-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-82.02,70.1506]}},{"type":"Feature","properties":{"id":1869,"name":"Fold at Rio Marina","description":"

Stretched and folded vein at Rio Marina, Elba Island<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T19:27:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sigma-object-at-Rio-Marina-768x576.jpg","taxonomy":{"webmapp_category":[228,229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1869","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1869&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sigma-object-at-rio-marina\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.428192615509033,42.80568148315707]}},{"type":"Feature","properties":{"id":2116,"name":"Fold BIF","description":"

Spectacular folds in Banded Iron Formation of the Hamersley Group (2.6-2.45 Ga). Pascal Philippot and Patrice Rey for scale. Photo ID 702<\/p>\n

Photograph: Joel Brugger (2003)<\/p>\n

Reference: Pilbara- Hamersley Gorge<\/p>\n","modified":"2018-07-24T16:02:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fold-BIF-225x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2116","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2116&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fold-bif\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[118.14111109999999,-22.6080556]}},{"type":"Feature","properties":{"id":6237,"name":"Fold in marble, Apuan Alps","description":"

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Photograph: R. Carosi, University of Torino<\/p>\n

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 <\/p>\n

\"\"<\/p>\n","modified":"2019-03-05T23:11:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/03\/DSC_3389-768x334.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6749","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6749&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-marbles-apuan-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.250156602128868,44.075119106339244]}},{"type":"Feature","properties":{"id":1153,"name":"folded metasediments","description":"

Typical example of the S-shaped folds with many ptygmatically folded quartz veins<br \/>. PhotoID111<\/p>\n

Photograph: Paul Bons, T\u00fcbingen<\/p>\n","modified":"2018-10-10T18:58:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/folded-metasediments-300x225.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1153","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1153&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-metasediments\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.315942585468292,42.319467553072116]}},{"type":"Feature","properties":{"id":6469,"name":"Folded migmatites, Antarctica","description":"

Folded migmatites and leucosomes of the Ross Orogen, Lichen Hills, Antarctica<\/p>\n

Photo by Chiara Montomoli<\/p>\n

 <\/p>\n","modified":"2019-01-31T17:26:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/migmatiti-lichen-hills_n-768x345.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6469","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6469&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-migmatites-antarctica\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.00544236913947,-73.27132581745721]}},{"type":"Feature","properties":{"id":2053,"name":"Folded migmatites, Punta ainu","description":"

folded Sillimanite migmatites. Photo ID 637<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n

Reference: Anatexis in the Hercynian basement of NE Sardinia, Italy: a case study of the migmatite of Porto Ottiolu (G. Cruciani, M. Franceschelli, A. M. Caredda, and G. Carcangiu)<\/p>\n","modified":"2019-02-05T22:05:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Punta-ainu-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2053","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2053&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/punta-ainu\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.73864495754242,40.69441536211751]}},{"type":"Feature","properties":{"id":1620,"name":"folded mylonites","description":"

Folded mylonites above the Roman temple of the Sikeit Emerald mines. The mylonites define the decollement of the Wadi Sikeit core complex.
\nPhotoID365<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:49:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/folded-mylonites-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1620","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1620&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[34.79671061038971,24.63022903917177]}},{"type":"Feature","properties":{"id":1530,"name":"Folded radiolarites in Corsica","description":"

At the pass of San Colombano, in the nappe of Balagne, thin, folded levels of red radiolarite and white quarzite lie on pillows lavas. The folds reversed towards the West are contemporaneous of the thrusting of alpine corsica on the hercynian basement. PhotoID315<\/p>\n

Photograph: c.nicollet<\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/Corse\/balagne\/balagne.html<\/p>\n","modified":"2019-05-16T12:24:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-radiolarites-in-Corsica-768x535.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1530","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1530&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-radiolarites-in-corsica\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.077174663543701,42.579551093890814]}},{"type":"Feature","properties":{"id":1225,"name":"Folded Ribbon Cherts","description":"

Spectacularly folded ribbon cherts, Monterey formation, part of accreted material from the extinct subduction zone of the Farallon plate. Photo ID 711<\/p>\n

Photograph: David Manaker<\/p>\n","modified":"2018-10-10T18:44:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-Ribbon-Cherts-768x509.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1225","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1225&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-ribbon-cherts\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.497993,37.82822]}},{"type":"Feature","properties":{"id":2100,"name":"Folded strata","description":"

View of the Asmari Formation in the backlimb of the Khaviz Anticline.
\nPhotoID693<\/p>\n

Photograph: Stefano Tavani<\/p>\n","modified":"2018-06-30T12:28:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-strata-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2100","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2100&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-strata\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.36956787109375,30.700515832683973]}},{"type":"Feature","properties":{"id":2158,"name":"Folded veins","description":"

Folded calcite veins showing stretching parallel to the fold axis in west-facing recumbent F1 fods in Scaglia Formation (Tuscan Nappe). The space between stretched vein fragments is filled by quartz (yellow-orange)
\nPhotoID738<\/p>\n

Photograph: C. Montomoli, R. Carosi<\/p>\n

Reference: Montomoli C., Ruggeri G., Boiron M. C., Cathelineau M. (2001) – Pressure fluctuation during uplift of the Northern Apennines (Italy): a fluid inclusion study. Tectonophysics, 314, 121-139. Montomoli C. (2002) – Vein development and fluid inclusion data: insight on the evolution of the Tuscan Nappe in the Northern Apennines. Boll. Soc. Geol. It.\/Italian Journal of Geoscience, 801-817. Carosi R., Leoni L., Montomoli C., Sartori F. (2003) – Very low-grade metamorphism in the Tuscan Nappe, Northern Apennines, Italy: relationships between deformation and metamorphic indicators in the La Spezia mega-fold. Schweiz. Schweiz. Mineral. und Petrogr, Mitteinl., 83, 15-32.<\/p>\n","modified":"2018-06-28T14:40:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-veins-300x202.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2158","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2158&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.8034894523621,44.06415033211528]}},{"type":"Feature","properties":{"id":1339,"name":"Folded zigzagging vein (Rainy Lake)","description":"

Leucocratic vein with an intrusion-related zig-zag pattern and incipient post-emplacement folding. The vein is emplaced in foliated Archean metasedimentary rocks. The oblique stripes are glacial striae. PhotoID149<\/p>\n

Photograph: Elena Druguet<\/p>\n

Reference: Druguet, E., Czeck, D.M., Carreras, J., Casta\u00f1o, L.M., 2008. Emplacement and deformation features of syntectonic leucocratic veins from Rainy Lake zone (Western Superior Province, Canada). Precambrian Research 163, 384-400.<\/p>\n","modified":"2018-06-15T10:20:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-zigzagging-vein-Rainy-Lake-200x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1339","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1339&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-zigzagging-vein-rainy-lake\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-93.0834728479,48.75059182757777]}},{"type":"Feature","properties":{"id":1235,"name":"Folding in a ductile shear zone","description":"

Folded layering in the Deh Vazir ductile shear zone, Iran. This is a structure as described by vanderPluijm and Marshak (1997); folding accompanies shearing and occurs where a sequence of interlayered weak and strong rock layers is caught between the opposing boundaries of a shear zone. In such circumstances, displacement of the rigid shear zone boundaries with respect to each other causes the intervening rock to fold. The Deh Vazir shear zone mainly consists of foliated and lineated marble and greenschist. Metamorphic grade is generally low grade (Sarkarinejad et al., 2010). The photograph shows how strong marble layers act as a shear zone boundary and weak greenschist layers between the marble layers have been subject of shearing. Location: Deh Vazir shear zone in the Southwest of the HP-LT Sanandaj-Sirjan metamorphic belt, Iran. PhotoID190<\/p>\n

Sarkarinejad, K., Samani, B., Faghih, A., Grasemann, B., Moradipoor, M., 2010. Implications of strain and vorticity of flow analyses to interpret the kinematics of an oblique convergence event (Zagros Mountains, Iran). Journal of Asian Earth Sciences 38, 34-43<\/p>\n

van der Pluijm, B.A., Marshak, S., 1997. Earth Structure: an Introduction to Structural Geology and Tectonics, McGraw-Hill, New York.<\/p>\n

This is a photograph of the month in the Journal of Structural Geology<\/p>\n

Photograph: Babak Samani<\/p>\n","modified":"2018-10-10T18:54:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folding-in-a-ductile-shear-zone-768x576.jpg","taxonomy":{"webmapp_category":[229,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1235","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1235&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folding-in-a-ductile-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.793333,29.342222]}},{"type":"Feature","properties":{"id":1971,"name":"Folding in salt","description":"

Folding in rock salt, salt dome of Cardona, Spain
\nPhotoID579<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:16:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folding-in-salt-768x493.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1971","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1971&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folding-in-salt\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.677736,41.906732]}},{"type":"Feature","properties":{"id":1985,"name":"Folds and foliation","description":"

Folded bedding and steep foliation in Devonian slates. Bunte Kuh, Ahrtal, Germany
\nPhotoID586<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T12:20:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-and-foliation-768x576.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1985","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1985&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-and-foliation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.06944207675167,50.53097394425512]}},{"type":"Feature","properties":{"id":6933,"name":"Folds and metasomatized, retrogressed ex garnet peridotite (now serpentinized) boudins within amphibole-bearing migmatitic gneiss, Borgo outcrop Darengo Valley, Adula nappe","description":"

Interference patterns in metric refolded folds described by layering foliation traces in Adula nappe crystalline basement with , Borgo outcrop at the confluence Darengo – Led\u00f9 streams, southern steep zone of Adula nappe (ex) “roots zone” (Southern Steep Belt), Adula nappe ancient southern paleoeuropean continental margin, Penninic domain, Darengo Valley, “Costiera dei Muncech”, Mesolcina Range, Eastern Lepontine Alps. Central Alps, Lombardy region, northern Italy.<\/span><\/p>\n

(Photo by Lorusso Angelo)<\/p>\n

 <\/p>\n","modified":"2019-05-05T22:32:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/val_darengo_II-407-PDT-boudins-in-AG-amph-bearing-migmatitic-gneiss-F-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6933","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6933&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-and-metasomatized-retrogressed-ex-garnet-peridotite-now-serpentinized-boudins-within-amphibole-bearing-migmatitic-gneiss-borgo-outcrop-darengo-valley-adula-nappe\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.299345345603342,46.214173658796085]}},{"type":"Feature","properties":{"id":1108,"name":"Folds in bedding","description":"

Small folds in bedding in Devonian slate
\nPhotoID591<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T14:51:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-bedding-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1108","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1108&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-bedding\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.973081,50.486241]}},{"type":"Feature","properties":{"id":2037,"name":"Folds in comendites","description":"

Mesoscopic folds in S. Pietro Island comendite lava flows. Locality Cala Fico, Carloforte. Photo ID 629<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Cioni R. & Funedda A. -2005- Structural geology of crystal-rich, silicic lava flows: a case study from San Pietro Island (Sardinia, Italy) – in M. Manga and G. Ventura (Eds.) Kinematics and dynamics of lava flows, GSA Special Paper 396, 1-14.<\/p>\n","modified":"2018-09-04T11:40:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-comendites-300x202.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2037","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2037&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-comendites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.227013,39.15635]}},{"type":"Feature","properties":{"id":1361,"name":"Folds in Kaligandaki","description":"

Second phase overurned folds in the Triassic-Jurassic succession of the Tethyan Sedimentary Sequence in the Kali Gandaki valley, between Jomsom and Kagbeni villages (central Nepal). PhotoID166<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Godin L. (2003) – Structural evolution of the Tethyan sedimentary sequence in the Annapurna area, central Nepal Himalaya. Journal of Asian Earth Sciences, 22, 307-328.<\/p>\n","modified":"2018-06-15T10:20:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-Kaligandaki-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1361","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1361&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-kaligandaki\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.77796173095703,28.83098970381284]}},{"type":"Feature","properties":{"id":6328,"name":"Folds in marbles and stretched dykes, Elba Island","description":"

Folds in marbles and stretched dykes, Elba Island, Italy. Folds related to the emplacement of the Monte Capanne pluton and sub-horizontally stretched dyke (upper part of the photo).<\/p>\n

Photo by R. Carosi<\/p>\n","modified":"2019-01-28T13:34:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/SPartaiaElba-225x300.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6328","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6328&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-marbles-and-stretched-dykes-elba-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.234650693640106,42.788866799946256]}},{"type":"Feature","properties":{"id":1231,"name":"Folds in marbles, Dry Valleys","description":"

Tight folds with stretched limbs in quartz-feldspatic layer in high-grade marbles, Roos Orogen. Nussbaun Riegel, Taylor Valley, Victoria Land (Antarctica). PhotoID186<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-09-03T14:16:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-marbles-Dry-Valleys-225x300.jpg","taxonomy":{"webmapp_category":[228,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1231","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1231&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-marbles-dry-valleys\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.76666,-77.66666]}},{"type":"Feature","properties":{"id":7227,"name":"Folds in metalimestone (Northen Apennines, Italy)","description":"

Folds in metalimestone (Northen Apennines, Italy) Photo by Chiara Montomoli<\/p>\n","modified":"2019-10-06T20:42:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/IMG_0529-768x512.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7227","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7227&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-metalimestone-northen-apennines-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.790677596818114,42.7740764940183]}},{"type":"Feature","properties":{"id":1973,"name":"Folds in Pegmatite","description":"

D2 folds deforming pegmatite veins which intruded parallel to an S1 foliation in Ordovician micaschist. This famous outcrop, known as the Barrados pegmatite was saved from destruction by Henk Zwart when he noticed a road crew buldozing a track straight to the outcrop in the 1960s; he convinced them to put the road a bit lower, so that the outcrop was saved for posterity
\nPhotoID580<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T18:06:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-Pegmatite-768x502.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1973","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1973&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-pegmatite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.787484,42.776286]}},{"type":"Feature","properties":{"id":6492,"name":"Folds in salt mine, Realmonte, Sicily","description":"

Folds in salt mine, Realmonte, Sicily, Italy<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-02-01T17:14:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/folds-realmonte-mine-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6492","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6492&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-salt-mine-realmonte-sicily\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.473952174535953,37.29885740775526]}},{"type":"Feature","properties":{"id":6533,"name":"Folds in the Annapurna Yellow Formation, Kaligandaki, Nepal","description":"

Road cliff just south of Larjung village; (a) banded marbles of the Annapurna Yellow Formation; b) F2 metric folds in the marble just below the road cut in a) folding the S1 foliation, c) asymmetric F2 fold in the marble with gently dipping to the North D2 axial planes; d) thin section of the marbles showing a SPO of calcite crystals along the S2 foliation.<\/p>\n

Locality: south of Larjung village (N 20\u00b0 40\u2019 57.33\u2019\u2019 E 83\u00b0 36\u2019 41.70\u2019\u2019).<\/p>\n

More Information on: Carosi, R. Gemignani, L. Godin, Iaccarino S., Larson K. P., Montomoli C., Rai S. M. (2014) – A geological journey in the deepest canyon of the earth: the Kali Gandaki section Rodolfo. . In: (Eds.) Chiara Montomoli, Rodolfo Carosi, Rick Law, Sandeep Singh, and Santa Man Rai, Journal of the Virtual Explorer, volume 47, paper 9, 1-31.<\/p>\n","modified":"2019-02-04T21:21:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/Larjung-composizione-foto-768x514.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6533","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6533&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-the-annapurna-yellow-formation-kaligandaki-nepal\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.59598293989393,28.67216703851193]}},{"type":"Feature","properties":{"id":6262,"name":"Folds in the Helvetic Wildhorn nappe","description":"

Sanetsch dam: folds in the frontal part of the Helvetic Wildhorn nappe, Switzeerland<\/p>\n","modified":"2019-01-29T07:22:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/folds-Wildhorn-300x225.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6262","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6262&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-the-helvetic-wildhorn-nappe\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.298998772582991,46.362943017467984]}},{"type":"Feature","properties":{"id":6651,"name":"Folds on Fm. Trubi (Southern Sicily)","description":"","modified":"2019-03-01T08:08:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/13-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6651","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6651&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-on-fm-trubi-southern-sicily\/","addr:street":"","addr:housenumber":"","addr:postcode":"92020","addr:city":"Palma di Montechiaro","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.688814668709256,37.18500938847492]}},{"type":"Feature","properties":{"id":6796,"name":"Folds on Fm. Trubi (Southern Sicily)","description":"

Folds on Pliocene limestone. Photo by Giuseppe Ruffino<\/p>\n","modified":"2019-03-25T16:30:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/03\/71-768x461.jpg","taxonomy":{"webmapp_category":[229,235]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6796","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6796&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-on-fm-trubi-southern-sicily-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.661628127508948,37.19440102171752]}},{"type":"Feature","properties":{"id":809,"name":"Folds, Corsica","description":"

Folds in metacherts, Corsica (France)
\n<\/i><\/p>\n","modified":"2018-09-04T13:26:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/03\/Screenshot-2018-03-30-09.34.24-e1522396012575-768x432.png","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/809","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=809&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/outcrop-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.69570541,46.19046715]}},{"type":"Feature","properties":{"id":1544,"name":"Folds, Dorset","description":"

Folds in Liassic limestone. Lulworth Cove, Dorset. Photo taken from west of the cove.
\nPhotoID326<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-09-04T11:04:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-Dorset-209x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1544","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1544&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-dorset\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-2.25203,50.61901]}},{"type":"Feature","properties":{"id":6271,"name":"Garlaban and Sainte-Baume from Ruissatel","description":"

Almost from Ruissatel’s cross, looking North (left) and West (right). On the picture, you’ll see on the left, Garlaban and its famous fold. On the right, You’ll see the Sainte-Baume with a change in dip.<\/p>\n

\"\"

Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p><\/div>\n","modified":"2020-05-04T18:21:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Panorama_Garlaban_Sainte-Baume-768x189.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6271","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6271&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garlaban-and-sainte-baume-from-ruissatel\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.530409508754815,43.31441300936813]}},{"type":"Feature","properties":{"id":1466,"name":"Giant sheath folds in Wadi Mayh","description":"

Cross section (YZ) perpendicular to the lineation through hectometric sheath folds staked on top of each other. The road gives the scale.
PhotoID294<\/p>\n

Photograph: ch.nicollet<\/p>\n

Reference: Searle and Alsop (2007). Eye-to-eye with a mega\u2013sheath fold: A case study from Wadi Mayh, northern Oman Mountains. Geology, 35, 1043\u20131046<\/p>\n","modified":"2018-06-15T10:17:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Giant-sheath-folds-in-Wadi-Mayh-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1466","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1466&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/giant-sheath-folds-in-wadi-mayh\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[58.53699088096619,23.42836263603364]}},{"type":"Feature","properties":{"id":1277,"name":"Hasan-Robat","description":"

The Precambrian Basement of the Hasan-Robat Region, north Isfahan, in the Sanandaj-Sirjan Metamorphic Belt of Iran preserves evidence of multiple orogenic events. The Sanandaj-Sirjan Zone is the inner crystalline zone of the Zagros Orogen, which has been highly deformed and exhumed during continental collision between the Arabian Plate and Central Iran. The Hasan-Robat Region is an example of the exhumed Precambrian basement complexes.<\/p>\n

In the photo, deformed Precambrian grey marbles contain metamorphosed chert (cream folded layers) which, record a complex shortening and shearing history. This lead to the development of disharmonic ptygmatic folds with vertical axes during the Pan-African Orogeny and later phases.
\nLocation: The photo has taken in the southeast Hasan-Robat Village in the north Isfahan, Iran PhotoID222<\/p>\n

Nadimi, A., 2010, Journal of Structural Geology, Vol. 32, 263<\/p>\n

Photograph: Alireza Nadimi<\/p>\n","modified":"2018-10-10T18:51:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hasan-Robat-768x576.jpg","taxonomy":{"webmapp_category":[228,229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1277","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1277&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/hasan-robat\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.91407775878906,33.40253396866421]}},{"type":"Feature","properties":{"id":1432,"name":"Hasan-Robat","description":"

The Precambrian Basement of the Hasan-Robat Region, north Isfahan, in the Sanandaj-Sirjan Metamorphic Belt of Iran preserves evidence of multiple orogenic events. The Sanandaj-Sirjan Zone is the inner crystalline zone of the Zagros Orogen, which has been highly deformed and exhumed during continental collision between the Arabian Plate and Central Iran. The Hasan-Robat Region is an example of the exhumed Precambrian basement complexes.<\/p>\n

In the photo, deformed Precambrian grey marbles contain metamorphosed chert (cream folded layers) which, record a complex shortening and shearing history. This lead to the development of disharmonic ptygmatic folds with vertical axes during the Pan-African Orogeny and later phases.
Location: The photo has taken in the southeast Hasan-Robat Village in the north Isfahan, Iran and at latitude: N 33, 24, 05 and longitude: E050, 54, 50.
PhotoID223<\/p>\n

Photograph: Alireza Nadimi<\/p>\n

Reference: Nadimi, A., 2010, doi: 10.1016\/j.jsg.2008.01.016.<\/p>\n","modified":"2018-06-15T10:21:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hasan-Robat-1-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1432","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1432&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/hasan-robat-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.91624766588211,33.40224399551489]}},{"type":"Feature","properties":{"id":2252,"name":"Hercinian folds in Ballota Beach","description":"

Fold propagation and fautt bend folds in red mudastones from the Tournaisian- Visean Alba Formation in Ballota Beach, Llanes, Asturias, Northern Spain.
\nPhotoID791<\/p>\n

Photograph: Enrique Bern\u00e1rdez Rodr\u00edguez<\/p>\n","modified":"2018-09-04T11:12:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hercinian-folds-in-Ballota-Beach-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2252","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2252&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/hercinian-folds-in-ballota-beach\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.71158981323,43.411844042307344]}},{"type":"Feature","properties":{"id":6970,"name":"Interference of F1 and F2 folds, Orto di Donna, Lucca, Italy","description":"

Tyoe 3 interference pattern of folds in Selcifero limestone, Orto di Donna, Lucca, Italy.<\/p>\n

Layers of Selcifero limestone and F1 steeply diping axial planes are refolded by F2 folds with shallowly dipping axial planes giving rise to type 3 interference pattern (Ramsay, 1967). A F1 fold hinge is observable close to the center of the photo highlighted by withish cherts layers with M secondary folds.<\/p>\n","modified":"2019-06-07T16:45:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/Orto-di-Donna-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6970","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6970&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/interference-of-f1-and-f2-folds-orto-di-donna-lucca-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.19580936438524,44.13535574040764]}},{"type":"Feature","properties":{"id":6397,"name":"interference pattern figure, sheath folds “Paina Marble” mylonite","description":"

Tectonic & metaphysics : “lobated arrow” or “head+fishbone” like interference pattern figure, 20 cm approx, offered by sheath folds in dolocarbonatic (ex european triassic cover, pre-rift sediments) mylonite labeled “Paina Marble”: the ductile shear zone that is the tectonic boundary between upper “Bellinzona-Dascio Zone” (B.D.Z. frontal accretionary prism at lithospheric levels) and structural lower Adula nappe (ex southern paleoeuropean continental thinned lithospheric subducted margin), Penninic Domain, Southern Steep Belt, Livo Valley, “Costiera dei Muncech”, “Alto Lario”, Eastern Lepontine Alps, Lombardy, Italy.<\/p>\n

(Photo by Lorusso Angelo).<\/p>\n","modified":"2019-01-29T13:41:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/BD_III-543-F-768x576.jpg","taxonomy":{"webmapp_category":[229,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6397","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6397&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/interference-pattern-figure-sheath-folds-paina-marble-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.31133165069673,46.191203645751116]}},{"type":"Feature","properties":{"id":2092,"name":"Isoclinal fold","description":"

Tight to isoclinal SW verging F1 fold in the low-grade metamorphic basement of Sardinia develped during the Lower Carbonifeorus collisional stage.
\nPhotoID686<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CAROSI R. & OGGIANO G. (2002) – Transpressional deformation in northwestern Sardinia (Italy): insights on the tectonic evolution of the Variscan belt. Comptes Rendus Geoscience, 334, 287-294, Elsevier, Paris 2002. MONTOMOLI C. (2002) – Zone di taglio fragili-duttili nel basamento Varisico metamorfico di basso grado della Nurra meridionale (Sardegna nord-occidentale). Atti della Societ\u00e0 Toscana di Scienze Naturali, Memorie seria A, 108, 23-29. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-30T11:29:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Isoclinal-fold-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2092","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2092&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/isoclinal-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.1619,40.7612]}},{"type":"Feature","properties":{"id":1450,"name":"Isoclinal fold in the LAC","description":"

In the leptyno-amphibolitic complex (LAC) which represents portions of metamorphised hercynian oceanic crust, the two main lithologies, amphibolites and leptynites are interlayed at all scales, from cm to hectometer.
PhotoID291<\/p>\n

Photograph: ch.nicollet<\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/enseignement\/HautAllier\/HA.html<\/p>\n","modified":"2018-06-15T10:17:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Isoclinal-fold-in-the-LAC-242x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1450","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1450&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/isoclinal-fold-in-the-lac\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.409785032272339,45.1621521018405]}},{"type":"Feature","properties":{"id":1679,"name":"Isoclinal folds in limestone","description":"

Isoclinal Folds in cherty limestones. These folds were generated during a first deformation event D1 (underthrusting of tectonic units)
\nPhotoID410<\/p>\n

GEOLOGY OF THE ALPI APUANE METAMORPHIC COMPLEX (ALPI APUANE, CENTRAL ITALY)
\nL. Carmignani, P. Conti, M. Meccheri, G. Molli
\nField Trip Guide Book p 38
\nVolume 5 – p37 to 54<\/p>\n

Photograph: Flavio Milazzo<\/p>\n","modified":"2018-06-30T11:53:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Isoclinal-folds-in-limestone-768x575.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1679","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1679&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/isoclinal-folds-in-limestone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.119623243808746,44.11379982390481]}},{"type":"Feature","properties":{"id":6486,"name":"Isoclinal folds in marbles, Ross Orogen, Antarctica","description":"

Isoclinal folds in marbles, Ross Orogen, Antarctica<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-01-31T19:25:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/DSCN01781-225x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6486","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6486&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/isoclinal-folds-in-marbles-ross-orogen-antarctica\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.7677081800781,-77.67115825816413]}},{"type":"Feature","properties":{"id":1717,"name":"ivan zibra","description":"

Parallel fold in the Cretaceous Tralonca Flysch. This fold belongs to the D3 local deformation event, occurring after the main greenschist-facies metamorphic peak. Axial-plane spaced cleavage is well-developed in shale layers, while it is nearly absent in limestone-rich layers.
\nPhotoID438<\/p>\n

Photograph: Ivan Zibra<\/p>\n

Reference: Zibra (2006). Late-Hercynian granitoid plutons emplaced along a deep crustal shear zone. A case study from the S. Lucia nappe (Alpine Corsica, France). PhD. thesis<\/p>\n","modified":"2018-06-30T13:01:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-768x483.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1717","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1717&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ivan-zibra\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.227056503295898,42.30986302053201]}},{"type":"Feature","properties":{"id":1725,"name":"ivan zibra","description":"

Isclinal fold in granulite-facies, garnet-bearing metasediments.The fold is truncated by a compositionally layered flaser gabbro of Permian age.
\nPhotoID442<\/p>\n

Photograph: Ivan Zibra<\/p>\n

Reference: Reference: Zibra I, Kruhl JH, Braga R (2010). Late Palaeozoic deformation of post-Variscan lower crust: shear zone widening due to strain localization during retrograde shearing. Int J Earth Sci (Geol Rundsch) DOI 10.1007\/s00531-009-0441-5<\/p>\n","modified":"2018-06-30T13:04:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-4-768x468.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1725","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1725&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ivan-zibra-5\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.212851524353027,42.31287792063872]}},{"type":"Feature","properties":{"id":1554,"name":"Kink folds","description":"

Kink folded crenulation cleavage. Any planar structure will fold. Narooma, New South Wales, Australia.
\nPhotoID332<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:06:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kink-folds-768x514.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1554","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1554&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kink-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[150.141292,-36.220436]}},{"type":"Feature","properties":{"id":1556,"name":"Kink folds","description":"

Kink Folds in Carboniferous Culm facies. Hartland Quay, Devon, England
\nPhotoID333<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-07-30T16:29:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kink-folds-1-768x499.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1556","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1556&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kink-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.531395,50.995643]}},{"type":"Feature","properties":{"id":5746,"name":"Kinked augen gneiss, Lod\u00e8","description":"

Kinked augen gneiss (F3 fold). Kinks affect theS2 mylonitic foliation. Lod\u00e8.<\/p>\n","modified":"2018-08-07T12:27:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Kinked-augen-gneiss-300x213.png","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5746","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5746&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kinked-augen-gneiss-lode\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.544945999999982,40.593203]}},{"type":"Feature","properties":{"id":1104,"name":"Kinked foliation","description":"

Kinked foliation. Boscastle, Cornwall. UK
\nPhotoID335<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-30T12:37:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kinked-foliation-197x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1104","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1104&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kinked-foliation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.698765,50.691844]}},{"type":"Feature","properties":{"id":5967,"name":"Kinked schist, Malfatano beach","description":"

Kinked folds in the Bithia Schists (Cambrian) (Malfatano beach, southern Sardinia).<\/p>\n","modified":"2018-12-21T14:19:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSC_0490-768x509.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5967","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5967&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kinked-schist-malfatano-beach\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.800785620799502,38.89166278326032]}},{"type":"Feature","properties":{"id":1777,"name":"K\u00f6z\u00e9p-sz\u00e9k, B\u00fckk Mts","description":"

Folds in cherty limestone with boudinage and interference patterns. Photo ID 714<\/p>\n

Photograph: N\u00e9meth Norbert<\/p>\n","modified":"2018-10-23T13:42:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/K\u00f6z\u00e9p-sz\u00e9k-B\u00fckk-Mts-768x360.jpg","taxonomy":{"webmapp_category":[228,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1777","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1777&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kozep-szek-bukk-mts\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[20.54168701171875,48.052840971122784]}},{"type":"Feature","properties":{"id":1122,"name":"Kreuzberg","description":"

Open fold in bedding in Devonian slates, Kreuzberg, Germany This fold is part of the Eiffel fold and thrust belt.
\nPhotoID80<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T19:23:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kreuzberg-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1122","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1122&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kreuzberg\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.00927734375,50.708634400828224]}},{"type":"Feature","properties":{"id":1502,"name":"Leptyno-amphibolitic group","description":"

The Leptyno-amphibolitic Complex (local name) corresponds to bimodal plutonic rocks that may represent remnants of early Hercynian ophiolites within the Massif Central thrust stack in central France. Here, it shows several phases of partial melting, folding and granitic dyke intrusions in and around the locality depicted here (esp. in the disused road curve some 100m to the North).
\nPhotoID273<\/p>\n

Photograph: JF Moyen<\/p>\n

Reference: Outcrop courtesy of V. Gardien, Univ. Lyon I<\/p>\n","modified":"2018-09-16T10:30:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Leptyno-amphibolitic-group-225x300.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1502","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1502&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/leptyno-amphibolitic-group\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.75931,45.06425]}},{"type":"Feature","properties":{"id":2114,"name":"Limestone Cap","description":"

Mississippian to Middle Triassic Buttle Lake Group Limestone. Strathcona Provincial Park, Vancouver Island, Canada. Photo ID 701<\/p>\n

Photograph: Stewart Butler<\/p>\n","modified":"2018-06-28T14:42:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Limestone-Cap-768x1023.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2114","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2114&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/limestone-cap\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-125.678958893,49.679070062652194]}},{"type":"Feature","properties":{"id":1981,"name":"Major fold","description":"

Open syncline in slates, Schuld, Germany
\nPhotoID584<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:32:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Major-fold-768x1023.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1981","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1981&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/major-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.880679787635813,50.44734501645746]}},{"type":"Feature","properties":{"id":2234,"name":"Malmesbury Group syncline Robben Island","description":"

Open plunging syncline in Neoproterozoic-Cambrian Malmesbury Fm. shales on Robben Island, Cape Town, South Africa.
\nPhotoID782<\/p>\n

Photograph: Christie Rowe<\/p>\n

Reference: Rowe, C. D., Backeberg, N., van Rensburg, T., Maclennan, S., Faber, C., Curtis, C. and Viglietti, P. (2010) Structural geology of Robben Island: Implications for the tectonic environment of Saldanian deformation, South African Journal of Geology 113.1 57-72. (Download geologic map eps.mcgill.ca\/~crowe\/publications)<\/p>\n","modified":"2018-09-04T11:20:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Malmesbury-Group-syncline-Robben-Island-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2234","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2234&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/malmesbury-group-syncline-robben-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[18.360006,-33.795977]}},{"type":"Feature","properties":{"id":1329,"name":"Marble Bar","description":"

Strip of Archaean banded iron formation that gave its name to the town of Marble Bar. PhotoID144<\/p>\n

Photograph: C. W. Passchier<\/p>\n

Reference: Uni Mainz<\/p>\n","modified":"2018-06-15T10:20:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Marble-Bar-300x197.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1329","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1329&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/marble-bar\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.7115159034729,-21.186402506]}},{"type":"Feature","properties":{"id":2202,"name":"Mazatzal Mountains Chevron Folds 1","description":"

Chevron folds in the Mazatzal Peak Quartzite of the Proterozoic Mazatzal Group.
\nPhotoID763<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-06-30T11:38:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mazatzal-Mountains-Chevron-Folds-1-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2202","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2202&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mazatzal-mountains-chevron-folds-1\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-111.43886,34.09354]}},{"type":"Feature","properties":{"id":2206,"name":"Mazatzal Mountains Chevron Folds 2","description":"

Chevron folds in the Mazatzal Peak Quartzite of the Proterozoic Mazatzal Group.
\nPhotoID765<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-09-04T11:39:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mazatzal-Mountains-Chevron-Folds-2-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2206","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2206&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mazatzal-mountains-chevron-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-111.4395,34.0909]}},{"type":"Feature","properties":{"id":2204,"name":"Mazatzal Mountains Mullions","description":"

Mullions within the Maverick shale of the Proterozoic Mazatzal Group.
\nPhotoID764<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-06-28T15:00:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mazatzal-Mountains-Mullions-768x576.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2204","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2204&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mazatzal-mountains-mullions\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-111.43811,34.09143]}},{"type":"Feature","properties":{"id":1321,"name":"melt-filled conjugate shear zones","description":"

Melt-filled, conjugate shear zones developed in granitic orthogneisses of the Grenville Province along the shore of the St-Lawrence River (Quebec). The orientation of these shear zones was used to derived the spatial distribution of the principal directions of the strain ellipsoid. The radial distribution of maximal stretching directions around km-scale domes is one of the arguments for the model of diapiric rise of partially molten orthogneisses induced by the sagduction of the heavy Davy synform. The 3-10 km wide domes and the adjacent (NW) ca. 50 X 100 km, north plunging synform are clearly visible on the Google image. <\/p>\n

Gervais, F., Nadeau, L., Malo, M., 2004. Migmatitic structures and solid-state diapirism in orthogneiss domes, Eastern Grenville Province, Canada. In Hodges, K., Whitney, D. and Teyssier, C. (eds). Gneiss domes in Orogeny: Geological Society of America Special Paper 380, p. 359-378.<\/p>\n

PhotoID235<\/p>\n

Photograph: F\u00e9lix Gervais<\/p>\n","modified":"2018-06-15T10:16:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/melt-filled-conjugate-shear-zones-768x510.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1321","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1321&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/melt-filled-conjugate-shear-zones\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-62.4802780151,50.26147330918773]}},{"type":"Feature","properties":{"id":1827,"name":"Migmatic gneiss","description":"

Migmatitic gneiss with melt veins parallel to folds. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). North at the top<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-03T17:46:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Migmatic-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1827","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1827&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatic-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381667,-25.582667]}},{"type":"Feature","properties":{"id":1829,"name":"migmatic gneiss","description":"

Folded layered grey gneiss with steep E-W trending foliation (S 160-70) N is at the top of the image. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T13:06:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/migmatic-gneiss-197x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1829","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1829&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatic-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.794031,-25.542606]}},{"type":"Feature","properties":{"id":2057,"name":"Monte Albo","description":"

Fold in Sandstone. Photo ID 639<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n

Reference: THE VARISCAN BASEMENT OF NORTHERN SARDINIA (ITALY): FIELD GUIDE TO THE EXCURSION IN THE BARONIE REGION R. CAROSI (*), C. FRASSI (*), C. MONTOMOLI (*)<\/p>\n","modified":"2018-07-28T09:09:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Monte-Albo-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2057","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2057&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/monte-albo\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.523596167564392,40.482401161134334]}},{"type":"Feature","properties":{"id":6597,"name":"Monte Cassio Flysch syncline, late Cretaceous, northern Appennines","description":"

Impressively syncline made of\u00a0 parallel bedded basin-plain deposits mainly consisting of resedimented pelagic and hemipelagic biogenic oozes; subordinate, fine-grained sandstone forms darker and considerably thinner, more resistent units. These sediments, which are interpreted as a trench-fill, are thought to be a classic example of stacked megaturbidites triggered by seismic activity (seismoturbidites of Mutti et al., 1984). Thin-bedded sandstones and dark mudstones represent the background sedimentationof the basin plain.
\nMonte Cassio Flysch, late Cretaceous, northern Appennines<\/p>\n","modified":"2019-02-12T11:41:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/2019-02-10-Ravarano_01-768x254.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6597","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6597&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/monte-cassio-flysch-syncline-late-cretaceous-northern-appennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.053761312902793,44.58136899811507]}},{"type":"Feature","properties":{"id":1319,"name":"More pseudoboudins","description":"

A string of spaced pseudo-boudins adjacent to a shear zone, amongst them one intreaging squarish one
See fig. 5 of Bons et al. 2004. PhotoID114<\/p>\n

Photograph: Paul Bons, T\u00fcbingen<\/p>\n

Reference: Bons et al. 2004. Apparent boudinage in dykes. J. Structural Geology 26, 625-636.<\/p>\n","modified":"2018-06-15T10:20:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/More-pseudoboudins-300x200.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1319","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1319&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/more-pseudoboudins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.319272547960281,42.316948798364244]}},{"type":"Feature","properties":{"id":1747,"name":"Mount Everest","description":"

The most magnificent outcrop on Earth; Mount Everest. Notice the isoclinal folds
\n(caption to be expanded)<\/p>\n

Photograph taken from the south<\/p>\n

Photograph: David Iacopini<\/p>\n","modified":"2018-07-24T11:42:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mount-Everest-768x1020.jpg","taxonomy":{"webmapp_category":[229,232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1747","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1747&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mount-everest\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.92498663494871,27.9877885755318]}},{"type":"Feature","properties":{"id":1895,"name":"Mylonitic granite & pegmatite","description":"

Mylonitized monzogranite from the Youanmi dextral shear zone. An isoclinally folded pegmatite occurs in the center of the image. Photo ID 673<\/p>\n

Photograph: I.Zibra<\/p>\n

Reference: Geological Survey of Western Australia. http:\/\/www.dmp.wa.gov.au\/371.aspx<\/p>\n","modified":"2018-09-04T11:39:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-granite-amp-pegmatite-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1895","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1895&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitic-granite-pegmatite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.01024723052979,-28.4270734464]}},{"type":"Feature","properties":{"id":1118,"name":"Namibia Boudins","description":"

Metaturbidites of Neoproterozoic age from the junction of the Cambrian Kaoko and Damara Mobile Belts, Lower Ugab area, Namibia. A sandstone layer in the centre is boudinaged during a first phase of regional deformation in the Cambrian, associated with activity of the NS trending Kaoko Belt between the Rio de la Plata and Congo cratons. Boudin necks were filled with blocky calcite. The layers above and below this structure are folded by regional D3, associated with activity in the EW trending Damara Belt. Boudinage predates folding, since boudin necks can be seen to be folded as well. Width of view 1.5m. North is to the left in this photograph. PhotoID78<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-16T10:33:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Namibia-Boudins-768x505.jpg","taxonomy":{"webmapp_category":[228,229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1118","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1118&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/namibia-boudins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.644775390625,-20.879342972]}},{"type":"Feature","properties":{"id":1315,"name":"Nerotal","description":"

Type III refolded isoclinal folds in phyllite. PhotoID107<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-06-15T10:20:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Nerotal-768x1024.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1315","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1315&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/nerotal\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.22200059890747,50.1035907071083]}},{"type":"Feature","properties":{"id":1347,"name":"Neyriz Ophiolite area","description":"

Folded, thrusted and sheared Radiolarite and pelagic rock units of the Neyriz Ophiolite Sequence.<\/p>\n

Nadimi, A., and Nadimi, H., 2006, Thrusts and Folds in the Neyriz Ophiolite and Associated Rocks,
Iran. Geolines Journal, 20, G20-67, 97-98.
PhotoID253<\/p>\n

Photograph: Alireza Nadimi<\/p>\n","modified":"2018-06-15T10:16:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Neyriz-Ophiolite-area-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1347","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1347&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/neyriz-ophiolite-area\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.196929931640625,29.177044469781038]}},{"type":"Feature","properties":{"id":1309,"name":"Nilgiril Anticline","description":"

View to the east across the Kali Gandaki from the trail leading toward Hidden Valley and Dhaulagiri basecamp to the Nilgiri Peaks (7061m, 6940m, 6839m respectively from north to south). Overturned anticlinal closure of Cambro-Ordovician (Annapurna Formation) and Ordovician (Nilgiri Formation) sedimentary rocks (Godin, 2003).<\/p>\n

Godin, L. (2003) Structural evolution of the Tethyan sedimentary sequence in the Annapurna area, central Nepal Himalaya. Journal of Asian Earth Sciences, v. 22 pp. 307-328<\/p>\n

PhotoID234<\/p>\n

Photograph: K. Larson<\/p>\n","modified":"2018-06-28T18:13:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Nilgiril-Anticline-768x527.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1309","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1309&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/nilgiril-anticline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.726806640625,28.66769613249295]}},{"type":"Feature","properties":{"id":1931,"name":"North verging F2 fold","description":"

Km-scale North-verging F2 fold. Black shale and limestone of the Sombre Formation (Silurian-Devonian); Tibetan Sedimentary Sequence.<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Godin, L. (2003). Journal of Asian Earth Sciences, v. 22 pp. 307-328<\/p>\n","modified":"2018-06-30T12:51:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/North-verging-F2-fold-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1931","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1931&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/north-verging-f2-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.6788,28.732]}},{"type":"Feature","properties":{"id":1379,"name":"Oldest rocks in Africa","description":"

Outcrop of the oldest-dated rocks in Africa near Piggs Peak, Swaziland. Zircons from this outcrop of the Ngwane gneisses of the Ancient Gneiss Complex gave an age of 3.644 Ga (upper intercept).<\/p>\n

Compston, W., Kroner, A., 1988. Multiple zircon growth within early Archean tonalitic gneiss from the Ancient Gneiss Complex, Swaziland. Earth.Plan.Sci.Lett. 87, 13-28.
\nPhotoID267<\/p>\n

Photograph:<\/p>\n","modified":"2018-06-30T12:17:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Oldest-rocks-in-Africa-768x576.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1379","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1379&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/oldest-rocks-in-africa\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[31.30301,-25.90973]}},{"type":"Feature","properties":{"id":811,"name":"Outcrop 4","description":"

Lorem ipsum dolor sit amet, consectetur adipisci elit, sed eiusmod tempor incidunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrum exercitationem ullam corporis suscipit laboriosam, nisi ut aliquid ex ea commodi consequatur. Quis aute iure reprehenderit in voluptate velit esse cillum dolore eu fugiat nulla pariatur. Excepteur sint obcaecat cupiditat non proident, sunt in culpa qui officia deserunt mollit anim id est laborum.<\/i><\/p>\n","modified":"2018-10-10T18:59:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/03\/Screenshot-2018-03-30-09.58.53-e1522396842281-768x432.png","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/811","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=811&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/outcrop-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.66025733,46.21161569]}},{"type":"Feature","properties":{"id":2144,"name":"Overturned F1 fold","description":"

Alternances of black metapelites and metasiltites\/metasandstones of the Middle Trias (Massa Unit, Punta Bianca locality). F1 tight fold with thickened hinges and stretched limbs .
\nS1 axial plane foliation shows refraction in brown layers (metasiltites and metasandstones)
\nPhotoID723<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2019-02-19T22:59:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Overturned-F1-fold-300x202.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2144","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2144&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/overturned-f1-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.975957,44.035983]}},{"type":"Feature","properties":{"id":2178,"name":"Overturned Fold","description":"

This folding is located in Eocene setting (Karaj Fm.) of Alborz (Northen Iran); and it refers to Alpine orogeny.
\nPhotoID751<\/p>\n

Photograph: Masoud Mirzaei<\/p>\n","modified":"2018-06-28T18:05:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Overturned-Fold-768x575.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2178","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2178&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/overturned-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[51.05969154365539,35.88172264085996]}},{"type":"Feature","properties":{"id":1420,"name":"Overturned pillow lavas","description":"

Overturned pillow lavas in the Ligurid Units of Elba island (tectonic complex n. 4). Marciana Marina village, locality Il Cotone.<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: R. Carosi<\/p>\n","modified":"2018-06-30T12:27:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Overturned-pillow-lavas-768x516.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1420","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1420&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/overturned-pillow-lavas\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.202813,42.806814]}},{"type":"Feature","properties":{"id":1699,"name":"Pania di Corfino Anticline","description":"

The structure consist of liassic massive limestones (Calcare Massiccio Formation) that outcrop in the upper part of the mountain.
\nThe bottom of the mountain is composed by well stratified rhetic limestone (Calcari e marne a Rhaetavicula Contorta Formation)
\nPhotoID425<\/p>\n

Photograph: F.Milazzo<\/p>\n

Reference: Fazzuoli M., Fois E. & Turi A. (1988) Stratigarfia e sedimentologia dei Calcari e marne a Rhaetavicula contorta Auctt. (Norico-Retico) della Toscana Nord occidentale. Nuova suddivisione formazionale. Riv. It. Paleont. Strat., 94(4), 561-618. Fazzuoli M. & Turi A. (1981) – Ricerche stratigrafiche, sedimentologiche e petrografiche sulla sequenza triassica della Pania di Corfino (Appennino settentrionale). Boll. Soc. Geol. It., 100 (4), 541-553.<\/p>\n","modified":"2018-07-30T16:28:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pania-di-Corfino-Anticline-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1699","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1699&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pania-di-corfino-anticline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.393613128662082,44.18887256768503]}},{"type":"Feature","properties":{"id":2282,"name":"Passo Valles","description":"

The lower part of the Bellerophon Formation (Upper Permian) includes thin dolomite layers (grey), marls (dark grey) and anhydrites (white) allowing plastic deformation (Neogene compressional folds with southern vergence). The marl layers show pervasive white veins of gypsum at high angle to the bedding, due to remobilization of the anhydrite prior to and during the folds development (Passo Valles, Dolomites, Italy). PhotoID806<\/p>\n

Photograph: Dario Zampieri<\/p>\n

Reference: MASSIRONI M., PRETO N., ZAMPIERI D., Note illustrative della Carta Geologica della Provincia di Trento, scala 1:25.000. Tavola 45 III – S. Martino di Castrozza. Provincia Autonoma di Trento, Servizio Geologico, Firenze: S.EL.CA., 2007.<\/p>\n","modified":"2018-06-30T11:52:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Passo-Valles-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2282","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2282&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/passo-valles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.79995,46.33582]}},{"type":"Feature","properties":{"id":1385,"name":"Pillows in the Br\u00e9venne unit","description":"

Remnants of pillow-lavas in the Visean Br\u00e9venne unit of the French Hercynian Belt.
PhotoID271<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-15T10:17:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pillows-in-the-Br\u00e9venne-unit-225x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1385","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1385&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pillows-in-the-brevenne-unit\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.64573,45.85135]}},{"type":"Feature","properties":{"id":1444,"name":"Pli de St Cl\u00e9ment","description":"

Large fold known as the Pli de St Cl\u00e9ment in the nappe of the helmintho\u00efd flysch (nappe de Parpaillon), French Alps
PhotoID288<\/p>\n

Photograph: ch.nicollet<\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/StClement.jpg<\/p>\n","modified":"2018-06-15T10:17:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pli-de-St-Cl\u00e9ment-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1444","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1444&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pli-de-st-clement\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.59153938293457,44.6484599032109]}},{"type":"Feature","properties":{"id":1430,"name":"Prefolding quartz veins (Rursee)","description":"

Beautiful Eschaulerberg cliffs showing an overturned secondary fold with late burial bedding-normal quartz veins and early tectonic bedding-parallel quartz veins continuously present across the anticlinal and synclinal fold hinge. Both vein-types are folded passively during Variscan contraction. Bedding-normal veins formed as a result of high fluid pressures during extension, while bedding-parallel veins reflect bedding-normal uplift and bedding-parallel thrusting at the onset of Variscan compression, prior to the main Variscan fold-and-cleavage development.<\/p>\n

Outcrop only accessible by boat.<\/p>\n

Photograph: Koen Van Noten<\/p>\n

Reference: Van Noten, K., Muchez, Ph. & Sintubin, M. (in press). Stress-state evolution of the brittle upper crust during compressional tectonic inversion as defined by successive quartz vein-types (High-Ardenne slate belt, Germany). Journal of the Geological Society, London 168, (2011) DOI: 10.1144\/0016-76492010-112.<\/p>\n","modified":"2018-06-28T18:02:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Prefolding-quartz-veins-Rursee-768x520.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1430","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1430&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/prefolding-quartz-veins-rursee\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.414194405078888,50.641481868567205]}},{"type":"Feature","properties":{"id":1552,"name":"Ptygmatic folds","description":"

Linear ptygmatic folded quartz veins. Weekeroo, South Australia.
\nPhotoID331<\/p>\n

Photograph: Jim Talbot<\/p>\n

Reference: Other photos of folds with enveloping surfaces may be seen at: http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Structure\/Fold\/Folds1\/Fold_styles.html#ptygmatic<\/p>\n","modified":"2018-06-30T11:14:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ptygmatic-folds-768x497.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1552","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1552&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ptygmatic-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[140.07076,-32.19229]}},{"type":"Feature","properties":{"id":1181,"name":"quartz veins and mullions","description":"

Metasandstone-metapelite multilayer sequence with regularly spaced layer-perpendicular quartz veins and buckled interfaces, Carri\u00e8re Mardasson, Bastogne.PhotoID152
\nThis is one of the localities where in 1908 the terms boudin and boudinage were coined.
\nThis quarry can only be visited by appointment.<\/p>\n

Photograph: Manuel Sintubin<\/p>\n

Reference: Sintubin, M. 2008. Photograph of the month: Boudin centennial. Journal of Structural Geology 30, 1315-1316 (doi: 10.1016\/j.jsg.2008.06.003)<\/p>\n","modified":"2018-10-23T13:50:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/quartz-veins-and-mullions-768x576.jpg","taxonomy":{"webmapp_category":[228,229,224,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1181","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1181&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/quartz-veins-and-mullions\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.742212533950806,50.01537834744035]}},{"type":"Feature","properties":{"id":1197,"name":"quartz veins and mullions","description":"

layer-parallel multilayer buckling (mullion development) pinned by pre-existing layer-perpendicular quartz veins.
\nPhotoID163
\n– Kenis, I. & Sintubin, M. 2007. About boudins and mullions in the Ardenne-Eifel area (Belgium, Germany). Geologica Belgica 10(1-2), 79-91 (and references therein).
\n– Sintubin, M. 2008. Photograph of the month: Boudin centennial. Journal of Structural Geology 30, 1315-1316 (doi: 10.1016\/j.jsg.2008.06.003).<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-10-10T18:54:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/quartz-veins-and-mullions-1-768x516.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1197","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1197&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/quartz-veins-and-mullions-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.84072470664978,50.090705354465136]}},{"type":"Feature","properties":{"id":1685,"name":"Quartzite","description":"

Asymptotic current bedding on a folded limb of a quartzite bed, which helps decipher the younging direction. See Naha (1965) for detailed analysis.
\nPhotoID416<\/p>\n

Photograph: M.A. Mamtani<\/p>\n","modified":"2018-06-28T14:58:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Quartzite-768x576.jpg","taxonomy":{"webmapp_category":[229,232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1685","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1685&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.41141891479492,22.657581403130564]}},{"type":"Feature","properties":{"id":1428,"name":"Radicofani","description":"

Block lava flow from Radicofani Volcano. Photo ID 659<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n

Reference: The Tuscan Magmatic Province ANGELO PECCERILLO and CARMELITA DONATI (Per. MineraI. (2003), 72, SPECIAL ISSUE: Miocene fo Recent … , 27-39)<\/p>\n","modified":"2018-06-15T10:16:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Radicofani-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1428","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1428&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/radicofani\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.768331527709961,42.89876083768572]}},{"type":"Feature","properties":{"id":2156,"name":"Recumbent fold","description":"

West-facing recumbent F1 fods in Scaglia Formation (Tuscan Nappe) defrming both sedimentary bedding and calcite veins.
\nPhotoID737<\/p>\n

Photograph: C. Montomoli, R. Carosi<\/p>\n

Reference: Montomoli C., Ruggeri G., Boiron M. C., Cathelineau M. (2001) – Pressure fluctuation during uplift of the Northern Apennines (Italy): a fluid inclusion study. Tectonophysics, 314, 121-139. Montomoli C. (2002) – Vein development and fluid inclusion data: insight on the evolution of the Tuscan Nappe in the Northern Apennines. Boll. Soc. Geol. It.\/Italian Journal of Geoscience, 801-817. Carosi R., Leoni L., Montomoli C., Sartori F. (2003) – Very low-grade metamorphism in the Tuscan Nappe, Northern Apennines, Italy: relationships between deformation and metamorphic indicators in the La Spezia mega-fold. Schweiz. Schweiz. Mineral. und Petrogr, Mitteinl., 83, 15-32.<\/p>\n","modified":"2018-06-28T18:15:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Recumbent-fold-300x202.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2156","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2156&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/recumbent-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.806,44.064]}},{"type":"Feature","properties":{"id":1562,"name":"Recumbent Fold on a Ramp-Flat System","description":"

Recumbent fold in Civetta Ramp-Flat systems along Van delle Sasse, Civetta Bassa, Dolomites – Italy
\nPhotoID667<\/p>\n

Photograph: Max Scarpa<\/p>\n

Reference: C. Doglioni, various papers.<\/p>\n","modified":"2018-06-28T13:37:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Recumbent-Fold-on-a-Ramp-Flat-System-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1562","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1562&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/recumbent-fold-on-a-ramp-flat-system\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[12.040328979492188,46.36232993806045]}},{"type":"Feature","properties":{"id":2166,"name":"Recumbent folds","description":"

Minor recumbent F1 west-facing folds in the hinge zone of La Spezia megafold affecting the Tuscan Nappe. Red layers are in Diaspri Formation (cherts) whereas withish layers are in the Maiolica Formation (limestone).
\nPhotoID741<\/p>\n

Photograph: C. Montomoli, R. Carosi<\/p>\n

Reference: Montomoli C., Ruggeri G., Boiron M. C., Cathelineau M. (2001) – Pressure fluctuation during uplift of the Northern Apennines (Italy): a fluid inclusion study. Tectonophysics, 314, 121-139. Montomoli C. (2002) – Vein development and fluid inclusion data: insight on the evolution of the Tuscan Nappe in the Northern Apennines. Boll. Soc. Geol. It.\/Italian Journal of Geoscience, 801-817. Carosi R., Leoni L., Montomoli C., Sartori F. (2003) – Very low-grade metamorphism in the Tuscan Nappe, Northern Apennines, Italy: relationships between deformation and metamorphic indicators in the La Spezia mega-fold. Schweiz. Schweiz. Mineral. und Petrogr, Mitteinl., 83, 15-32.<\/p>\n","modified":"2018-06-28T13:33:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Recumbent-folds-300x202.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2166","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2166&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/recumbent-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.806439882278482,44.0643064458309]}},{"type":"Feature","properties":{"id":1540,"name":"Red Dome fold","description":"

Red dome, an open fold. Red Dome, Bridger, MT. PhotoID324<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-30T19:33:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Red-Dome-fold-768x506.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1540","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1540&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/red-dome-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-108.856373,45.314084]}},{"type":"Feature","properties":{"id":6758,"name":"Red-pelite fold in calcschists, Apuan Alps","description":"

Red-pelite fold in calcschists, Apuan Alps<\/p>\n

Photograph: A. Petroccia<\/p>\n

 <\/p>\n","modified":"2019-03-09T12:23:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/03\/DSC_3343-768x509.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6758","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6758&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/red-pelite-fold-in-calcschists-apuan-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.245803119464767,44.079060566282934]}},{"type":"Feature","properties":{"id":1259,"name":"refolded crenulation cleavage","description":"

This outcrop of micaschist shows a tightly folded spaced foliation of light quartz rich and dark mica rich bands. The regularity of the alternation of the bands suggests that this is not bedding but a tectonic layering. In the quartz-rich layers, a foliation can be seen at a high angle to the layering. If the layering is tectonic, this foliation could be S1 and the layering S2. The foliation S1 is folded (with the layering S2) in the central folds, which must therefore be D3 structures.<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T18:11:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-crenulation-cleavage-768x500.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1259","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1259&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-crenulation-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.62569475174,53.27978996944675]}},{"type":"Feature","properties":{"id":1733,"name":"refolded D1 structure","description":"

Interference of mesoscale folds: the first-phase structures deform the contact between the Rhetic Chloritoid Schists and Breccia of Seravezza PhotoID449
\nThe contact is characterized by isoclinal folds anticlines and synclines that shows a M geometry.
\nThe first deformation event (D1) is related to the phase of underthrusting of the tectonics units.
\nThe second deformation event (D2) refolds the previous structures and gives rise to open folds with sub-horizontal axial plane foliation.
\nD2 deformation event is related to the exhumation of the the Alpi Apuane metamorphic complex.
\nPhotoID449<\/p>\n

Photograph: F.Milazzo<\/p>\n

Reference: Franceschelli M. , Puxeddu M. ,Carcangiu G. ,Gattiglio M. ,Pannuti F. (1996) \u2013 Breccia-hosted manganese-rich minerals of Alpi Apuane, Italy : A marine, redoxgenerated deposits; Franceschelli M. , Puxeddu M. , Memmi I. (1998) – Li, B-rich Rhaetian metabauxite, Tuscany, Italy : reworking of older bauxites and igneous rocks Chemical Geology 144, 221-242; Franceschelli M. & Memmi I. (1999) \u2013 Zoning of chloritoid from kyanite-facies metapsammites, Alpi Apuane, Italy, Mineralogical Magazine, 63, 105-110; Franceschelli M. , Puxeddu M. ,Gattiglio M. (2003) – Geochemistry and origin of chloritoid schist from the Alpi Apuane, Italy: evidence of a prevailing lateritic signature Eur. J. Mineral. 15, 575-588<\/p>\n","modified":"2018-09-04T11:44:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-D1-structure-768x1274.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1733","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1733&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-d1-structure\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.292569398880005,44.03759642369555]}},{"type":"Feature","properties":{"id":1741,"name":"refolded D1 structure","description":"

Interference of mesoscale folds: the first-phase structures
\ndeform the contact between the Rhetic Chloritoid Schists and Breccia of Seravezza.
\nPhotoID453
\nThe contact is characterized by isoclinal folds anticlines and synclines that shows a M geometry.
\nThe first deformation event (D1) is related to the phase of underthrusting of the tectonics units.
\nThe second deformation event refolds the previous structures (D2) and gives rise to open folds with sub-horizontal axial plane foliation.
\nD2 deformation event is related to the exhumation of the the Alpi Apuane metamorphic complex.<\/p>\n

Photograph: F.Milazzo<\/p>\n

Reference: Franceschelli M. , Puxeddu M. ,Carcangiu G. ,Gattiglio M. ,Pannuti F. (1996) \u2013 Breccia-hosted manganese-rich minerals of Alpi Apuane, Italy : A marine, redoxgenerated deposits; Franceschelli M. , Puxeddu M. , Memmi I. (1998) – Li, B-rich Rhaetian metabauxite, Tuscany, Italy : reworking of older bauxites and igneous rocks Chemical Geology 144, 221-242; Franceschelli M. & Memmi I. (1999) \u2013 Zoning of chloritoid from kyanite-facies metapsammites, Alpi Apuane, Italy, Mineralogical Magazine, 63, 105-110; Franceschelli M. , Puxeddu M. ,Gattiglio M. (2003) – Geochemistry and origin of chloritoid schist from the Alpi Apuane, Italy: evidence of a prevailing lateritic signature Eur. J. Mineral. 15, 575-588.<\/p>\n","modified":"2019-02-02T07:23:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-D1-structure-1-768x575.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1741","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1741&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-d1-structure-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.292526483535767,44.03723392161239]}},{"type":"Feature","properties":{"id":1422,"name":"Refolded folds","description":"

Upright F2 folds refolded by F3 more open folds with shallowly dipping axial planes. Type 3 interference pattern (Ramsay, 1967).
Varicolured Sericitic Schists of the epimetamoprhic Tuscan succession (tectonic complex n. 3) at Cala dell\u2019Alga, Elba Island (Italy).<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Benvenuti et al. (2001) \u2013 B Eastern Elba (field trip). Ofioliti, 26 (2a), 331-346.<\/p>\n","modified":"2018-06-15T10:21:14","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-folds-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1422","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1422&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.421267,42.865852]}},{"type":"Feature","properties":{"id":1959,"name":"Refolded Folds","description":"

Refolded Fold in the Variscan Basement of Monti Pisani.
\nPhotoID569<\/p>\n

Photograph: S. Papeschi<\/p>\n","modified":"2018-06-28T14:34:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-Folds-768x1023.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1959","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1959&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.568144917488098,43.734584714924154]}},{"type":"Feature","properties":{"id":1424,"name":"Refolded folds in marbles","description":"

Refolded folds in grey marbles of the Koettlitz Group (Ross Orogen). DIsmal Ridge, Southern Vitcoria Land, Antarctica.<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Talarico et al. (2005) – Terra Antarctica, 12 (1), 3-23.<\/p>\n","modified":"2018-06-30T19:11:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-fold-in-marbles-225x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1424","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1424&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-fold-in-marbles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[163.04061,-78.251206]}},{"type":"Feature","properties":{"id":1307,"name":"Refolded isoclinal fold","description":"

Isoclinal F1 synform refolded by F2 open folds (type 3 interference pattern) in white quartzites containing phengite, glaucophane and garnet. F1 folds developed under high-pressure metamorphic conditions. Morteda-Farinole eclogite Unit.
Locality Accendipipa, Corse (France)
PhotoID232<\/p>\n

Field Trip Guidebook vol. 4, P27, ISPRA (2004) – 32nd INTERNATIONAL GEOLOGICAL CONGRESS, Florence, Italy.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-06-15T10:16:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-isoclinal-fold-201x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1307","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1307&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-isoclinal-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.32627,42.50975]}},{"type":"Feature","properties":{"id":1586,"name":"Refolded isoclinal fold","description":"

Refolded isoclinal fold in Dalradian schists, Kinlochleven.<\/p>\n

Photograph: Tim Ivanic<\/p>\n","modified":"2018-06-30T13:03:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-isoclinal-fold-1-768x1023.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1586","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1586&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-isoclinal-fold-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.99929428101,56.71958015055486]}},{"type":"Feature","properties":{"id":1426,"name":"Refolded isoclinal folds","description":"

Refolded F1 isoclinal folds in cherty metalimestones of the Alpi Apuane metamorphic complex (Northern Appennines, Italy)<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: R. Carosi – Unipi<\/p>\n","modified":"2018-06-15T10:21:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-isoclinal-folds-768x532.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1426","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1426&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-isoclinal-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.214435,44.122228]}},{"type":"Feature","properties":{"id":1584,"name":"refolded marble breccia","description":"

Highly deformed Carrara marble from the central Alpi Apuane.
\nJurassic sedimentary breccias (the original protolith) were deformed during the main deformation of the Alpi Apuane complex (D1) at mid-crustal depths and then refolded during exhumation.<\/p>\n

Kligfield, R., Carmignani, L., and Owens, W. H., 1981. Strain analysis of a Northern Apennine shear zone using deformed marble breccias. Journal of Structural Geology, v. 3, p. 421\u2013436.<\/p>\n

Carmignani, L., Decandia, F.A., Fantozzi, P.L., Lazzarotto, A., Liotta, D., and Meccheri, M., 1994. Tertiary extensional tectonics in Tuscany (Northern Apennines, Italy). Tectonophysics, v. 238, p. 295-315.<\/p>\n

Molli G, Vaselli L 2006. Structures, interference patterns and strain regime during mid-crustal deformation in the Alpi Apuane (Northern Apennines, Italy). Geological Society of America Special Paper, 414, 79-94.
\nPhotoID348<\/p>\n

Photograph: G.Molli<\/p>\n","modified":"2019-01-31T10:17:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-marble-breccia-200x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1584","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1584&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/refolded-marble-breccia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.24692894458771,44.077207360382424]}},{"type":"Feature","properties":{"id":1301,"name":"Revenue","description":"

Folded high grade foliation in the Revenue pluton, Duchess, Australia. The Revenue granite contains an olded planar to linear fabric that is folded into opene to tight folds. In this case, a flattend enclave is deformed into a boomerang shaped geometry. PhotoID85<\/p>\n

Photograph: Cees Passchier<\/p>\n

Reference: Passchier, C.W. (1991) Deformation in the Revenue granite pluton, Mt Isa Inlier, Australia. Geologie<\/p>\n","modified":"2018-06-15T10:20:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Revenue-300x199.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1301","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1301&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/revenue\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[139.7021484375,-21.4530686331]}},{"type":"Feature","properties":{"id":2084,"name":"Reverse fault and folded quartz vein","description":"

Small-scale reverse fault and folded quartz-vein. The vein developed perpendicular to sedimentary bedding and S1 foliation and underwent initial stretching. Paleozoic metasediments involved in Variscan Orogeny; Nurra peninsula, Sardinia, Italy.
\nPhotoID683<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: MONTOMOLI C. (2002) – Zone di taglio fragili-duttili nel basamento Varisico metamorfico di basso grado della Nurra meridionale (Sardegna nord-occidentale). Atti della Societ\u00e0 Toscana di Scienze Naturali, Memorie seria A, 108, 23-29. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-07-24T11:33:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Reverese-fault-and-folded-quartz-vein-300x225.jpg","taxonomy":{"webmapp_category":[220,229,224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2084","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2084&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/reverese-fault-and-folded-quartz-vein\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.161822,40.761442]}},{"type":"Feature","properties":{"id":1743,"name":"Rheomorfic folds","description":"

Reomorfic folds in Komenditic lava flows (peralkalyne rhiolyte). From San Pietro island, SW Sardinia.
\nPhotoID455<\/p>\n

Photograph: D. Pieruccioni<\/p>\n

Reference: Cioni R., Funedda A. (2005): Structural geology of crystal-rich, silicic lava flows: A case study From San Pietro Island (Sardinia, Italy).Geological Society or America Special Paper 396; Cioni R., Salaro L., Pioli L. (2001): The Cenozoic volcanism of San Pietro Island (Sardinia, Italy). Rendiconti Seminario Facolt\u00e0 Scienze Universit\u00e0 Cagliari Supplemento Vol. 71 Fasc. 2<\/p>\n","modified":"2018-06-28T13:37:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rheomorfic-folds-768x576.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1743","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1743&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rheomorfic-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.226571083068848,39.15644601929688]}},{"type":"Feature","properties":{"id":1275,"name":"Rhinowash","description":"

Major fold in Neoproterozoic limestone and clastic metaturbidites. The fold is Cambrian in age and is part of the local D1 deformation sequence affecting the Zerissene turbidite sequence. PhotoID77<\/p>\n

Photograph: C. Passchier<\/p>\n

Reference: Passchier, C.W. , Trouw, R.A.J., Ribeiro, A, Paciulo, F (20<\/p>\n","modified":"2018-09-04T11:38:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rhinowash-300x212.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1275","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1275&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rhinowash\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.043102264404297,-20.9605579556]}},{"type":"Feature","properties":{"id":1126,"name":"Roveredo","description":"

Metasediments showing polyphase folding and boudinage. This small outcrop underneath the footbridge to the church shows very nice examples of type III fold interference. Take care, the outcrop is slippery and can only be reached along a narrow path! PhotoID83<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T13:35:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Roveredo-768x486.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1126","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1126&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/roveredo\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.173583984375,46.164614496897094]}},{"type":"Feature","properties":{"id":1438,"name":"Saint-Cl\u00e9ment fold","description":"

The often photographed Saint-Cl\u00e9ment fold occurs in the NW facing cliff on the other side of the road. This recumbent fold is actually part of a system of asymetric (S\/Z folds) within the Helminthoids flysh nappe (upper cretaceous), indicating a transport direction to the West (right on the photo).
PhotoID281<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-15T10:17:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Saint-Cl\u00e9ment-fold-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1438","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1438&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/saint-clement-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.5859,44.65131]}},{"type":"Feature","properties":{"id":1287,"name":"San Andreas folds and faults","description":"

Contractional deformation near Palmdale along the San Andreas fault zone, representing a complex hard-linked restraining stepover structure. Complexly folded and faulted rocks of the Anaverde Formation (lower to middle Pliocene) are unconformably overlain by Pleistocene sediments.<\/p>\n

Fife, D. L. & Minch, J. A. 1982. In: Geology and mineral wealth of the California Traverse Ranges. South Coast Geological Society, 78-93.<\/p>\n

http:\/\/strike-slip.geol.ucsb.edu\/KESSEL\/palmdaleroadcut.html<\/p>\n

Photograph: Haakon Fossen<\/p>\n","modified":"2018-06-28T18:13:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/San-Andreas-folds-and-faults-768x404.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1287","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1287&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/san-andreas-folds-and-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.13379,34.563255]}},{"type":"Feature","properties":{"id":1695,"name":"Sardic Angular Unconformity","description":"

Cambrian-Early Ordovician shale (Cabitza Shists) are separated from overlying Upper Ordovician-lower Carfoniferous
\nsedimentary cycle by sharp angular unconformity (Sardic phase) and overlain by trasgressive polygenic
\nmetaconglomerate, the Puddinga Auct.
\nPhotoID422<\/p>\n

Photograph: F.Milazzo<\/p>\n

Reference: Luigi CARMIGNANI, Giacomo OGGIANO, Sebastiano BARCA, Paolo CONTI, Antonio ELTRUDIS, Antonio FUNEDDA, Sandro PASCI e Ilio SALVADORI GEOLOGY OF SARDINIA (Explanatory notes of the Geologic map of Sardinia at 1:200,000 scale) Martini, I.P., Tongiorgi, M., Oggiano, G. and Cocozza, T. 1991. Ordovician alluvial fan to marine shelf transition in SW Sardinia, Western Mediterranean Sea: tectonically (Sardic phase) influenced clastic sedimentation. Sedimentary Geology, 72: 97-115.<\/p>\n","modified":"2018-06-28T18:15:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sardic-Angular-Unconformity-768x576.jpg","taxonomy":{"webmapp_category":[229,232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1695","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1695&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sardic-angular-unconformity\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.440471887588501,39.30623512847013]}},{"type":"Feature","properties":{"id":2043,"name":"Sassalbo","description":"

Spectacularly exposed higly deformed Triassic Evaporites. Photo ID 632<\/p>\n

Photograph: Chiara Del Ventisette<\/p>\n

Reference: Del Ventisette C., 2005. Modalit\u00e0 di deformazione dei livelli duttili e record sintettonico nella copertura in relazione all\u2019attivit\u00e0 di strutture compressive (o riattivate in compressione) nel basamento: integrazione tra dati di campagna, linee sismiche e modellizzazione analogical sperimentale. PhD THesis<\/p>\n","modified":"2019-01-29T01:13:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sassalbo-768x411.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2043","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2043&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sassalbo\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.192295014858246,44.29529428212541]}},{"type":"Feature","properties":{"id":1135,"name":"Seedorf Quarry","description":"

Giant Chevron folds in flysch – the quarry can only be visited by appointment. PhotoID101<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:23:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Seedorf-Quarry-300x225.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1135","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1135&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/seedorf-quarry\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.609397411346436,46.87439196893145]}},{"type":"Feature","properties":{"id":1580,"name":"sheared subcontinental mantle","description":"

Isoclinally folded websterite layer in a mylonitic mantle lherzolite. The fold axis is gently dipping northward (i.e. toward the left).
\nPhotoID344<\/p>\n

Zibra I (2006) Late-Hercynian granitoid plutons emplaced along adeep crustal shear zone. A case study from the S. Lucia Nappe (Alpine Corsica, France). Ph.D. thesis, University of Pisa (Italy); p 204. The complete manuscript is available from: http:\/\/etd.adm.unipi.it\/theses\/available\/etd-09142006-171856\/<\/p>\n

Photograph: Ivan Zibra<\/p>\n","modified":"2018-09-04T11:25:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheared-subcontinental-mantle-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1580","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1580&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheared-subcontinental-mantle\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.219543635845184,42.3099264936029]}},{"type":"Feature","properties":{"id":1297,"name":"sheath fold","description":"

Sheath fold, view in a section peprendicular to the stretching lineation, in white quartzites containing phengite, glaucophane and garnet. The fold developed under high-pressure metamorphic conditions. Morteda-Farinole eclogite Unit.
\nLocality Accendipipa, Corse (France)
\nPhotoID231<\/p>\n

Field Trip Guidebook vol. 4, P27, ISPRA (2004) – 32nd INTERNATIONAL
\nGEOLOGICAL CONGRESS, Florence, Italy.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T14:46:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheath-fold-300x201.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1297","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1297&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.32594,42.50907]}},{"type":"Feature","properties":{"id":1600,"name":"Sheath fold – eye fold","description":"

Eye folds. Port Vasgo, Scotland
\nPhotoID356<\/p>\n

Photograph: Jim Talbot<\/p>\n

Reference: See more photos at: http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Localities\/Sheath.html#Portvasgo<\/p>\n","modified":"2018-06-30T11:20:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-eye-fold-768x495.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1600","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1600&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-eye-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.433548,58.550813]}},{"type":"Feature","properties":{"id":1205,"name":"Sheath fold in mylonite","description":"

The sheath fold in the photograph formed during dextral, southeast-side-up shear along the Assean Lake shear zone. The shear zone dips steeply to the southeast. In general, moderately ENE-plunging lineations in the shear zone are folded by drag folds that have commonly developed into non-cylindrical folds. The lineations and the folds are interpreted as having formed during dextral, southeast-side-up, thinning flow. In this photograph, the lineation on the ESE limb of the fold plunges moderately to the E, and the fold hinge lines plunge steeply to the SSW and shallowly to the NNE. The top of this photograph is towards the WNW. The lineation and fold hinge lines are thought to have partially rotated towards the direction of the maximum principal strain rate of the pure shear component, which may or may not be parallel to the shear direction (cf. Kuiper et al., JSG, 2007). PhotoID168<\/p>\n

This is a Photograph of the Month in the Journal of Structural Geology<\/p>\n

Photograph: Yvette D. Kuiper, Boston College<\/p>\n","modified":"2018-10-10T18:55:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-in-mylonite-768x576.jpg","taxonomy":{"webmapp_category":[229,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1205","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1205&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-in-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-94.347,56.111]}},{"type":"Feature","properties":{"id":1249,"name":"Sheath fold in mylonite","description":"

The sheath fold in the photograph formed during dextral, southeast-side-up shear along the Assean Lake shear zone. The shear zone dips steeply to the southeast. In general, moderately ENE-plunging lineations in the shear zone are folded by drag folds that have commonly developed into non-cylindrical folds. The lineations and the folds are interpreted as having formed during dextral, southeast-side-up, thinning flow. In this photograph, the lineation on the ESE limb of the fold plunges moderately to the E, and the fold hinge lines plunge steeply to the SSW and shallowly to the NNE. The top of this photograph is towards the WNW. The lineation and fold hinge lines are thought to have partially rotated towards the direction of the maximum principal strain rate of the pure shear component, which may or may not be parallel to the shear direction (cf. Kuiper et al., JSG, 2007)<\/p>\n

This is a photograph of the month in JSG
\nPhotoID198<\/p>\n

Photograph: Yvette D. Kuiper<\/p>\n","modified":"2018-06-30T12:57:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-in-mylonite-1-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1249","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1249&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-in-mylonite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-96.347,56.111]}},{"type":"Feature","properties":{"id":1157,"name":"sheath folds","description":"

Sheath folds developed in strongly sheared quartz and pegmatite veins. PhotoID116<\/p>\n

Photograph: Paul Bons, T\u00fcbingen<\/p>\n","modified":"2018-06-30T12:23:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheath-folds-300x200.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1157","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1157&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.317535817623138,42.317161012295884]}},{"type":"Feature","properties":{"id":1590,"name":"Sheath folds","description":"

Cross sections of sheath folds — eye folds. Skullomie cove, near Tongue, Scotland.
\nPhotoID352<\/p>\n

Photograph: Jim Talbot<\/p>\n

Reference: See more photos at http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Localities\/Sheath.html<\/p>\n","modified":"2018-06-30T11:43:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-folds-768x507.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1590","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1590&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.378385,58.519003]}},{"type":"Feature","properties":{"id":1793,"name":"sheath folds in quartzite","description":"

Strongly mylonitised vein-quartzite with D2-sheath folds. Foldaxes are strongyl curved and both vertical and horizontal orientations are visible. A strong stretching lineation is folded over the sheath folds, probably formed earlier during D2 in the Erabiddy shear zone.<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:36:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheath-folds-in-quartzite-196x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1793","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1793&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-folds-in-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381333,-25.6015]}},{"type":"Feature","properties":{"id":2268,"name":"Slump folding in the Karaj Formation","description":"

Folds caused by gravitational gliding in unconsolidated and soft-sediments are called slump folds. They can form by layer-parallel shear. Such folds reflect the orientation of the palaeoslope in ancient settings. PhotoID799
\nThe photograph was taken from the road section of Eocene Karaj Formation, near Karaj city (with a view to the WNW), 35\u00b0 50\u00b4 11\u02ddN, 51\u00b0 02\u00b4 40\u02ddE. Karaj Formation, ~ 3300 m thick, mainly composed of a heterogeneous assemblage of green tuff and tuffite, thin bands of marine shale, and igneous rocks. The thick turbidites with slump folding in the Karaj Formation may indicate a relatively deep water through and submarine fan. The Z-shaped asymmetric and overturned slump fold indicate northward palaeoslope. These conditions show stage 3 geometries (late translation of slump) of formation and develop of slump fold system by surging flow with flow accelerates and contraction increases downslope.<\/p>\n

Photograph: Seyed Tohid Nabavi<\/p>\n","modified":"2018-10-10T18:32:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Slump-folding-in-the-Karaj-Formation-768x441.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2268","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2268&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/slump-folding-in-the-karaj-formation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.966125490376726,35.85010031851634]}},{"type":"Feature","properties":{"id":1416,"name":"South border","description":"

Grey: deposits: ashes and bombs deposits from 1888-1890 and 1731-1739 eruptions.
Orange: surge deposits. Photo ID 658<\/p>\n

Photograph: S. Papeschi<\/p>\n","modified":"2018-06-15T10:15:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-border-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1416","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1416&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-border\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.960997104644775,38.40203736518958]}},{"type":"Feature","properties":{"id":1510,"name":"South Stack, Anglesey","description":"

Lighthouse with large second generation folds in schist. South Stack, Anglesey, Wales.
\nPhotoID317<\/p>\n

Photograph: Jim Talbot<\/p>\n

Reference: D.E.B. Bates and J.R. Davies, 1981. Anglesey. Geologists Association, London, guide #40<\/p>\n","modified":"2018-09-04T13:38:18","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Stack-Anglesey-768x493.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1510","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1510&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-stack-anglesey\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.69653,53.306728]}},{"type":"Feature","properties":{"id":1281,"name":"South-verging folds (Samaria Gorge)","description":"

Metre-scale south-verging folds in the Plattenkalk nappe. Several faults and these asymmetric south-verging folds (photo) reflect Oligocene compression and are exposed in the Samaria Gorge, which developed as a result of contemporaneous (Pleistocene) continent uplift and erosion.<\/p>\n

Approximate location of the outcrop.<\/p>\n

Photograph: Koen Van Noten<\/p>\n

Reference: Fassoulas C. (2004). Field Guide to the Geology of Crete. Natural History Museum of Crete, Publ., 104p, Heraklio (3th edition)<\/p>\n","modified":"2018-10-10T18:51:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-verging-folds-Samaria-Gorge-768x576.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1281","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1281&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-verging-folds-samaria-gorge\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.9693221449852,35.2549041839846]}},{"type":"Feature","properties":{"id":1389,"name":"Stretching lineation in metaconglomerate","description":"

Stretching lineation in an Ordovician metaconglomerate, VAriscan Orogeny (Mt. S. Vittoria, Sardinia, Italy). PhotoID183<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CARMIGNANI L., CAROSI R., DI PISA A., GATTIGLIO M., MUSUMECI G., OGGIANO G. and PERTUSATI P.C. (1994) – The Hercynian chain in Sardinia (Italy). Geodinamica Acta, 7, 1, 31-47, Paris, 1994.<\/p>\n","modified":"2018-06-15T10:20:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Stretching-lineation-in-metaconglomerate-768x512.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1389","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1389&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/stretching-lineation-in-metaconglomerate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.303735151481646,39.758925227298484]}},{"type":"Feature","properties":{"id":2019,"name":"Superposed folds in BIF","description":"

Two generations of superposed folds in c. 2.8Ga banded iron formation, creating a dome-and-basin pattern Photo ID 671<\/p>\n

Photograph: I. Zibra<\/p>\n

Reference: Geological Survey of Western Australia. http:\/\/www.dmp.wa.gov.au\/371.aspx<\/p>\n","modified":"2018-06-30T11:30:53","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Superposed-folds-in-BIF-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2019","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2019&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/superposed-folds-in-bif\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.79970169067383,-27.9943445701]}},{"type":"Feature","properties":{"id":1522,"name":"Superposed folds in marbles","description":"

Superposed folds in the Santa Catalina marbles ; east coast of the Alpine Corsica. On the right photography, the axes of the 2 generations of the folds are perpendicular ; they are parallel on the left photography.
\nPhotoID297<\/p>\n

Photograph: ch.nicollet<\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/Corse\/CapCorse\/CoteE.html<\/p>\n","modified":"2018-06-28T18:10:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Superposed-folds-in-marbles-768x353.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1522","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1522&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/superposed-folds-in-marbles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.486383199691772,42.82344849130125]}},{"type":"Feature","properties":{"id":1574,"name":"Swan fold","description":"

Migmatitic garnet-biotite gneiss in the east-central portion of the Zona Transversal Domain Borborema Province in northeastern of Brazil. In our point of view, the rock was affected by at least two phases of folding with axes subparallel. The first phase developed isoclinal folds that are responsible for bending the migmatitic banding generated in other oldest event of unknown genesis. The second phase of folding produced asymmetrical closed to tight folds with disharmonious character and steep axial surface that dips to SSE. The interference between the two phases of folding provided interference patterns of type 3 on a mesoscopic scale. The character of disharmonic folds generated in the second stage is coupled to irregular granitic garnet-leucosome and provides a curious swan-shape, as shown in the image.
\nPhotoID341<\/p>\n

Photograph: Alan Miranda<\/p>\n","modified":"2018-06-28T14:53:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Swan-fold-768x544.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1574","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1574&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/swan-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-36.152497,-7.571612]}},{"type":"Feature","properties":{"id":1542,"name":"Synclinal basin","description":"

A basin in upper Precambrian quartzite. Mookra Towers, South Australia.
\nPhotoID325<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-10-21T19:21:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Synclinal-basin-768x435.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1542","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1542&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/synclinal-basin\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[138.806648,-30.584549]}},{"type":"Feature","properties":{"id":2220,"name":"The Lovell Wash Syncline","description":"

A plunging syncline east of Las Vegas exposes Miocene age lacustrine units of the Horse Spring Formation. In the photo conglomerates that formed at a lake margin grade laterally (toward the observer) into stromatolitic limestones. A short hike around the fold to the north along Lovell Wash takes you to a beautifully exposed microbial limestone sequence in a slot canyon exposure reminiscent of 200 m of core. On the way you pass a borate mine and can collect borate minerals in the wash.
\nPhotoID772<\/p>\n

Photograph: Thomas Hickson<\/p>\n

Reference: Hickson, Thomas A., Anders J. Ness, and Melissa A. Lamb. 2010. Miocene tectonics and climate in the lake mead region recorded by horse spring formation carbonates. Special Paper – Geological Society of America 463, : 121-145<\/p>\n","modified":"2018-09-04T11:21:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/The-Lovell-Wash-Syncline-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2220","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2220&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/the-lovell-wash-syncline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-114.695657,36.20294]}},{"type":"Feature","properties":{"id":6448,"name":"Thrust in the Priestley Formation, Northern Victoria Land","description":"

Thrust fault in the Priestley Formation, O’Kane Canyon, Northern Victoria Land. The thrust cuts the hinge of an upright fold.<\/p>\n

Photo by Rodolfo Carosi (@PNRA)<\/p>\n","modified":"2019-01-30T18:54:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/piega-okane-canyon-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6448","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6448&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrust-in-the-priestley-formation-northern-victoria-land\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.40159831160247,-74.31535554773862]}},{"type":"Feature","properties":{"id":7015,"name":"thrusts intra-nappe double up australpine mesozoic cover (Ortles nappe) Rhetic Alps","description":"

Corne del Palone mount\u00a0thrusts intra-nappe thrusts double up australpine mesozoic cover (Ortles nappe) made of “Fraele formation” + “Dolomia del Cristallo formation” (Triassic), just under regional importance thrust (Alpisella Line), at the top of Corne del Palone mount, where Ortles nappe is overthrusted by<\/em>\u00a0“Dolomia dello Stelvio” belonging to Quattervals nappe, australpine domain. Southern slopes of\u00a0Corne del Palone mount, towards <\/span>Stelvio Pass,Braulio Valley, high eastern Valtellina,\u00a0Rhetic Alps, Lombardy.<\/em><\/span><\/h4>\n

\"\"\"\"<\/em><\/h4>\n

(Photo by Lorusso Angelo)<\/span><\/h4>\n","modified":"2019-06-15T13:19:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7015","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7015&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrusts-intra-nappe-double-up-australpine-mesozoic-cover-ortles-nappe-rhetic-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.368900560383395,46.51367560697147]}},{"type":"Feature","properties":{"id":7238,"name":"Tight fold in Jurassic marble (Apuane Alps, Northern Apennines)","description":"

Tight fold in Jurassic marble (Apuane Alps, Northern Apennines). Photo by Rodolfo Carosi<\/p>\n","modified":"2019-10-14T18:56:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/IMG_9306-768x1024.jpeg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7238","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7238&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tight-fold-in-jurassic-marble-apuane-alps-northern-apennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.231296649292858,44.06523680749263]}},{"type":"Feature","properties":{"id":1399,"name":"Tudela leucosomes","description":"

Leucosome pods in migmatitic schists from Tudela (former ClubMed) in the Cap de Creus tectonometamorphic belt. Notice the complex folding around the pods. PhotoID197<\/p>\n

Photograph: Elena Druguet<\/p>\n

Reference: Druguet, E., Carreras, J. 2006. Analogue modelling of syntectonic leucosomes in migmatitic schists. Journal of Structural Geology 28, 1734-1747.<\/p>\n","modified":"2018-09-04T15:56:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Tudela-leucosomes-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1399","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1399&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tudela-leucosomes\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.294842317700386,42.3270494869462]}},{"type":"Feature","properties":{"id":1713,"name":"Type-2 fold Interference","description":"

Type-2 fold interference pattern in banded gneiss (southern parts of Aravalli Mountain Belt, India)
\nPhotoID436<\/p>\n

Photograph: M.A. Mamtani<\/p>\n","modified":"2018-06-28T14:46:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Type-2-fold-Interference-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1713","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1713&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/type-2-fold-interference\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[74.13213729858398,22.49273302919317]}},{"type":"Feature","properties":{"id":1677,"name":"Type-3 fold Intereference","description":"

Type-3 fold intereference pattern in banded gneiss (southern parts of Aravalli Mountain Belt, India)
\nPhotoID408<\/p>\n

Photograph: M.A. Mamtani<\/p>\n","modified":"2018-06-30T12:06:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Type-3-fold-Intereference-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1677","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1677&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/type-3-fold-intereference\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[74.13299560546875,22.49225722008523]}},{"type":"Feature","properties":{"id":6480,"name":"Upright folds in the Priestley schists, Ross Orogen, Antarctica","description":"

Upright folds in the low-grade Priestley schists, Ross Orogen. Foolsmate glacier, Antarctica<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-01-31T19:15:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/foolsmate-300x201.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6480","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6480&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/upright-folds-in-the-priestley-schists-ross-orogen-antarctica\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[161.9894514238281,-74.06537543803805]}},{"type":"Feature","properties":{"id":1440,"name":"Usuaya slates","description":"

slate outcrops with nice folding and cleavage-bedding relations
PhotoID285<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:17:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Usuaya-slates-300x197.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1440","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1440&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/usuaya-slates\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-68.4015655518,-54.7882153087]}},{"type":"Feature","properties":{"id":1405,"name":"View of fumaroles and crater area","description":"

Photo shot from the South border of the crater. Photo ID 656<\/p>\n

Photograph: S. Papeschi<\/p>\n","modified":"2018-06-15T10:15:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/View-of-fumaroles-and-crater-area-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1405","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1405&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/view-of-fumaroles-and-crater-area\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.961512088775635,38.40506413920944]}},{"type":"Feature","properties":{"id":6130,"name":"Villaz\u00f3n-Reigada Syncline (Cantabrian Zone, NW Iberia)","description":"

The Cantabrian Zone (CZ) conforms the Variscan foreland fold and thrust belt, and is located in the core of the Ibero-Armorican arc of NW-Iberia. Deformation is characterized by thin-skinned thrusts and associated folds that accommodate frontal and lateral ramps. The Villaz\u00f3n-Reigada Syncline is located in the Somiedo Nappe, the most internal nappe of the CZ. It is associated with a paired fault-propagation anticline, and is characterised by an open interlimb angle and a subvertical axial plane. The erodibility of the Silurian shales of the Formigoso Fm. has allowed the syncline to be perfectly highlighted in the landscape by the Cambro-Ordovician quartzarenites of the Barrios Fm., as it can be appreciated in the picture. As an scale, the height of the left-hand side mountain over La Barca Reservoir is about 300 m.<\/p>\n

Reference: Guti\u00e9rrez-Alonso, G. (1992). The Narcea Antiform and its relation with the Western Nappes of the Cantabrian Zone. PhD Thesis. University of Oviedo.<\/p>\n","modified":"2018-12-14T20:00:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/8194706944_95d7a26409_k-768x359.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6130","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6130&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/villazon-reigada-syncline-cantabrian-zone-nw-iberia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-6.330373113396149,43.295568591194595]}},{"type":"Feature","properties":{"id":1387,"name":"VMS in the Br\u00e9venne unit","description":"

Gossan and alteration zone around a VMS lens in the Visean Br\u00e9venne unit, French Massif Central, Hercynian belt, in Carri\u00e8re Saint-Antoine near St-Pierre la Palud, France. PhotoID272<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-15T10:17:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/VMS-in-the-Br\u00e9venne-unit-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1387","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1387&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/vms-in-the-brevenne-unit\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.60869,45.78831]}},{"type":"Feature","properties":{"id":1373,"name":"West crater of Vulcanello","description":"

W crater of Vulcanello, partially covered by trees. Photo ID 653<\/p>\n

Photograph: S. Papeschi<\/p>\n","modified":"2018-06-15T10:28:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/West-crater-of-Vulcanello-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1373","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1373&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/west-crater-of-vulcanello\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.962069988250732,38.42665145016567]}},{"type":"Feature","properties":{"id":1773,"name":"Yarweelor Gneiss","description":"

Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). Gneissic layering (trending NS) is cut by an EW foliation associated with folds. The layering is probably an older Narryer direction and the folds are formed during D1-D2 in the Erabiddy shear zone.
\nPhotoID472<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:46:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-768x500.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1773","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1773&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.793833,-25.542833]}},{"type":"Feature","properties":{"id":1819,"name":"Yarweelor Gneiss","description":"

Grey gneiss that has strongly deformed mafic bands, several generations of granitic veins and sinistral shear bands with leucosome material. The deformation is of unknown age, but may be the steep deformation component of the Errabiddy shear zone. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T19:18:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1819","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1819&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.53487084788514,-25.5688242179]}}]}