The massif of anorthosite (black on the drawing) is 10 km in diameter. It is wrapped by a NNE-SSW vertical foliation S2, like a giant porphyroclast. East of the massif, a early foliation S1 is preserved and folded in a megalithon. PhotoID316<\/p>\n
Photograph: j.e.martelat & c.nicollet<\/p>\n
Reference: Martelat, J. E., Nicollet, C., Lardeaux, J. M., Vidal, G., Rakotondrazafy, R. (1997) – Lithospheric tectonic structures developed under High-grade metamorphism in the southern part of Madagascar. Geodinamica Acta, 10, 94-114.<\/p>\n","modified":"2018-06-30T11:08:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-giant-porphyroclast-768x1093.jpg","taxonomy":{"webmapp_category":[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\/1508","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1508&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-giant-porphyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[44.905242919921875,-24.4908978153]}},{"type":"Feature","properties":{"id":2214,"name":"Amalaoulaou","description":"
Metagabbro from the root of the Amalaoulaou Neoproterozoic oceanic arc. The rock has been subject to partial dehydration-melting (900\u00b0C, ~10 kbar) during the maturation stage of the arc. It has leaded to the formation of coarse peritectic garnet, dark garnet clinopyroxenite restites and incomplete extraction of an anorthositic melt.
\nThe high temperature deformation post dating the partial melting event has been acquired during partial exhumation of the arc (intra-oceanic rifting). PhotoID769<\/p>\n
Photograph: Julien Berger<\/p>\n
Reference: Berger J, Caby R, Li\u00e9geois J-P, Mercier J-C, Demaiffe D (2011) Deep inside a neoproterozoic intra-oceanic arc: growth, differentiation and exhumation of the Amalaoulaou complex (Gourma, Mali). Contributions to Mineralogy and Petrology 162(4):773-796 doi:10.1007\/s00410-011-0624-5<\/p>\n","modified":"2018-06-28T18:07:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Amalaoulaou-768x576.jpg","taxonomy":{"webmapp_category":[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\/2214","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2214&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/amalaoulaou\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.319485015869077,15.437590271133272]}},{"type":"Feature","properties":{"id":1845,"name":"Augengneiss","description":"
Weakly deformed porphyritic granite of unknown age, showing a dextral shear sense. Yilgarn craton<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T15:56:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Augengneiss-768x502.jpg","taxonomy":{"webmapp_category":[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\/1845","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1845&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/augengneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.671333,-25.9215]}},{"type":"Feature","properties":{"id":1098,"name":"Bermagui","description":"
coastal outcrops of slate in Bermagui – this is a classical site to study the development of foliations in slates and sandstones. PhotoID171<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:14:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bermagui-768x481.jpg","taxonomy":{"webmapp_category":[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\/1098","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1098&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bermagui\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[150.08198082447052,-36.4227522334]}},{"type":"Feature","properties":{"id":1775,"name":"Bertibubba Gneiss","description":"
Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Leucocratic augengneiss with strong subvertical EW planar fabric, gently E-plunging stretching lineation and good dextral shear sense indicators on horizontal surfaces. Dominant D1, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite.
\nPhotoID473<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:52:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-768x503.jpg","taxonomy":{"webmapp_category":[232,230,231]},"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\/1775","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1775&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.575333,-25.609167]}},{"type":"Feature","properties":{"id":1779,"name":"Bertibubba gneiss","description":"
Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Leucocratic augengneiss with strong subvertical planar fabric and gently E-plunging stretching lineation. Dominant D1-deformation, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite; it shows a strong EW foliation, and good dextral shear sense indicators on horizontal surfaces. Weakly deformed pegmatite veins probably belong to the Moorarie granites (1830-1780 Ma)
\nPhotoID474<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:45:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-gneiss-768x501.jpg","taxonomy":{"webmapp_category":[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\/1779","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1779&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57562267857361,-25.6091573251]}},{"type":"Feature","properties":{"id":1781,"name":"Bertibubba Gneiss","description":"
Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Augengneiss with strong steeply NNW-dipping foliation and subhorizontal lineation with mantled porphyroclasts that indicate dextral shear sense; dominant D1-deformation, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite. Width of view 30 cm
\nPhotoID475<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:46:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[232,230,231]},"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\/1781","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1781&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.573003,-25.593833]}},{"type":"Feature","properties":{"id":1534,"name":"Big Penn slate quarry","description":"
Asymmetric anticline in Big Penn slate quarry. Slatedale, PA.
\nThe slate is mined by cutting it with cables and carborundum (the curved lines). The slate is then polished on rotating tables, again using carborundum as the abrasive. The best pieces are used for pool tables, but most is now used for ornamental paving.
\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":6153,"name":"Bookshelf sliding structure","description":"
Bookshelf sliding structure. Alternance of mylonitic microaugen gneiss of Aspromonte Unit and of the mylonitic phyllites of the Mandaci Unit<\/p>\n","modified":"2018-12-21T14:18:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSC_0637-768x509.jpg","taxonomy":{"webmapp_category":[228,232,231]},"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\/6153","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6153&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bookshelf-sliding-structure\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[15.29620337206984,37.96975104375447]}},{"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":1843,"name":"Camel Hills metasediments","description":"
Wooramel mylonites with EW steep foliation<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:44:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Camel-Hills-metasediments-768x498.jpg","taxonomy":{"webmapp_category":[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\/1843","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1843&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/camel-hills-metasediments\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.75588813757327,-25.5524658466]}},{"type":"Feature","properties":{"id":1592,"name":"Capo Bianco","description":"
tourmaline spots (Eurite) in Capo Bianco Aplite
\nPhotoID372<\/p>\n
Photograph: Alessandro Da Mommio<\/p>\n
Reference: Sooty sweat stains or tourmaline spots. The Argonauts on the Island of Elba (Tuscany) and the spread of Greek trading in the Mediterranean Sea ANDREA DINI, ALESSANDRO CORRETTI, FABRIZIO INNOCENTI, SERGIO ROCCHI,& DAVID SCOTT WESTERMAN.<\/p>\n","modified":"2018-06-28T14:35:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Capo-Bianco-768x573.jpg","taxonomy":{"webmapp_category":[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\/1592","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1592&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/capo-bianco\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.315389633178711,42.82055653548981]}},{"type":"Feature","properties":{"id":2140,"name":"Clast in breccia with algae","description":"
Algae (Dyploporae) in carbonatic clast within the Middle Trias metabreccias of Massa Unit, Punta Binaca locality.
\nPhotoID721<\/p>\n
Photograph: R. Carosi<\/p>\n","modified":"2018-12-12T13:14:18","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Clast-in-breccia-with-algae-300x191.jpg","taxonomy":{"webmapp_category":[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\/2140","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2140&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/clast-in-breccia-with-algae\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.975747,44.035887]}},{"type":"Feature","properties":{"id":1110,"name":"Cleavage Refraction","description":"
Cleavage Refraction visible on the right of this fold in the verrucano Fm. (Complex II; Elba Island)<\/p>\n
the refracted cleavage is the axial plane foliation of the fold visible in this photo.
\nPhotoID596<\/p>\n
Photograph: S. Papeschi<\/p>\n","modified":"2018-06-30T11:55:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cleavage-Refraction-768x576.jpg","taxonomy":{"webmapp_category":[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\/1110","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1110&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cleavage-refraction\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.432389,42.82941]}},{"type":"Feature","properties":{"id":1991,"name":"Cleavage refraction – geovandalism","description":"
Cleavage refraction in graded bedding in Devonian sandstone. The cleavage was reactivated as joint planes at a later stage and filled with quartz veins. Cleavage refraction, accentuated by the veins, indicates that the layering is in normal position. In the 1970s the outcrop was unfortunately vandalised by sample drilling. The samples were never investigated since the student project was cancelled…
\nPhotoID590<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2019-01-28T12:14:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cleavage-refraction-geovandalism-768x576.jpg","taxonomy":{"webmapp_category":[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\/1991","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1991&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cleavage-refraction-geovandalism\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.202704,50.002027]}},{"type":"Feature","properties":{"id":1488,"name":"Cm-size staurolite","description":"
Cm-size Staurolite crystals in garnet+staurolite bearing micaschist partly reoriented on the S2 foliation. Variscan Basement of northern Sardinia.
\nPhotoID304<\/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. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-30T12:58:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cm-size-staurolite-300x225.jpg","taxonomy":{"webmapp_category":[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\/1488","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1488&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cm-size-staurolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.582494,40.601903]}},{"type":"Feature","properties":{"id":1997,"name":"Crenulation cleavage","description":"
Sub-vertical crenulation cleavage (S2) in Varicolured Sericitic Schists of the epimetamoprhic Tuscan succession (tectonic complex n. 3) at Cala dell\u2019Alga, Elba Island (Italy).
\nPhotoID594<\/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":"2018-09-04T13:25:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Crenulation-cleavage-768x1023.jpg","taxonomy":{"webmapp_category":[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\/1997","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1997&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/crenulation-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.421874,42.866019]}},{"type":"Feature","properties":{"id":2094,"name":"Crenulation cleavage","description":"
S2 spaced crenualtion cleavage in the low grade metamorphic basement of Nurra peninsula, Sardinia, Italy.
\nPhotoID688<\/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":"2018-06-28T14:58:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Crenulation-cleavage-1-768x1023.jpg","taxonomy":{"webmapp_category":[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\/2094","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2094&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/crenulation-cleavage-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.1618,40.7614]}},{"type":"Feature","properties":{"id":6228,"name":"Crenulation cleavage Chenaillet, France","description":"
Crenulation cleavage in marbles, Chenaillet, France. It is on sedimentary cover of ophiolites<\/p>\n","modified":"2019-01-26T19:18:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/cren-cleavage-Chenaillet-300x225.jpg","taxonomy":{"webmapp_category":[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\/6228","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6228&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/crenulation-cleavage-chenaillet-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.726630920532216,44.896993396879076]}},{"type":"Feature","properties":{"id":1801,"name":"Dalgaringa gneiss","description":"
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\nThe pavements show banded gneiss rafts in younger less deformed granite pegmatite veins. North at the top<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:45:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[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\/1801","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1801&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.573,25.512333]}},{"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":2146,"name":"Deformed breccia","description":"
Flattened and stretched calcareous clasts along S1 foliation in Middle Trias metasediments; Massa Unit at Punta Bianca locality.
\nPhotoID724<\/p>\n
Photograph: R. Carosi<\/p>\n","modified":"2018-06-30T12:31:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-breccia-300x202.jpg","taxonomy":{"webmapp_category":[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\/2146","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2146&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-breccia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.97676,44.03593]}},{"type":"Feature","properties":{"id":2138,"name":"Deformed breccias","description":"
Sedimentary bedding marked by alternances of siltstones and breccias with mainly carbonatic clasts (white). Clasts are strongly deformed along S1 foliation at small angle to the bedding. Middle Trias, Massa Unit.
\nPhotoID720<\/p>\n
Photograph: R. Carosi<\/p>\n","modified":"2018-06-30T16:21:18","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-breccias-300x201.jpg","taxonomy":{"webmapp_category":[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\/2138","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2138&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-breccias\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.976055,44.035922]}},{"type":"Feature","properties":{"id":1217,"name":"deformed conglomerate","description":"
Deformed congloemrate in a small sedimentary basin overlying a core complex of Neoproterozoic age
\nPhotoID176<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:54:18","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/deformed-conglomerate-768x576.jpg","taxonomy":{"webmapp_category":[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\/1217","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1217&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-conglomerate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[36.71579360961914,26.588066624976207]}},{"type":"Feature","properties":{"id":1689,"name":"deformed conglomerate","description":"
deformed conglomerate, Wrangle Island
\nPhotoID419<\/p>\n
Photograph: Vicky Pease<\/p>\n","modified":"2018-06-30T12:24:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/deformed-conglomerate-1-768x524.jpg","taxonomy":{"webmapp_category":[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\/1689","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1689&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-conglomerate-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[179.2428,71.0972]}},{"type":"Feature","properties":{"id":1767,"name":"Deformed conglomerate","description":"
Mt James formation conglomerate of facetted quartzite pebbles in a schist matrix; the Formation is dated at ca. 1800Ma. North is at the top
\nPhotoID469<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:56:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-conglomerate-768x502.jpg","taxonomy":{"webmapp_category":[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\/1767","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1767&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-conglomerate-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[115.973354,-25.153833]}},{"type":"Feature","properties":{"id":1771,"name":"Deformed conglomerate","description":"
Mt James formation conglomerate of facetted quartzite pebbles in a schist matrix; the Formation is dated at ca. 1800Ma. North is at the top
\nPhotoID471<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:46:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-conglomerate-1-768x502.jpg","taxonomy":{"webmapp_category":[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\/1771","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1771&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-conglomerate-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[115.969591,-25.152245]}},{"type":"Feature","properties":{"id":2242,"name":"Elba Quartzite","description":"
Base of Elba Quartzite, Clear Creek, Raft River Mountains, Idaho-Utah
\nPhotoID786<\/p>\n
Photograph: Elizabeth L. Miller<\/p>\n","modified":"2018-10-10T18:34:14","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Elba-Quartzite-768x1033.jpg","taxonomy":{"webmapp_category":[232,230,219]},"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\/2242","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2242&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/elba-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-113.328952789,41.95572429954907]}},{"type":"Feature","properties":{"id":1634,"name":"Finero","description":"
Layered Peridotite in Finero
\nPhotoID376<\/p>\n
Photograph:<\/p>\n","modified":"2018-06-28T18:10:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Finero-768x576.jpg","taxonomy":{"webmapp_category":[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\/1634","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1634&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/finero\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.532428741455078,46.10216144429074]}},{"type":"Feature","properties":{"id":1941,"name":"flattened xenoliths","description":"
Ca-alkaline granitoid with flattened xenoliths. Rio Urubu
\nPhotoID559<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T15:51:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/flattened-xenoliths-768x492.jpg","taxonomy":{"webmapp_category":[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\/1941","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1941&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/flattened-xenoliths\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-60.488888,2.4825]}},{"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":1969,"name":"folded foliation","description":"
Folded foliation in Devonian slates, Malpas, Spanish Pyrenees. The foliation is Variscan in age, the folds are probably formed during the Pyrenean (Late Cretaceous to earliest Miocene) deformation in the Pyrenees
\nPhotoID578<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:51:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/folded-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\/1969","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1969&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-foliation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.800705394195575,42.42711238402593]}},{"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":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":1167,"name":"Foliation boudinage","description":"
Foliation boudinage in micaschist of the Urseren zone. PhotoID121<\/p>\n
Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-09-04T14:52:18","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Foliation-boudinage-225x300.jpg","taxonomy":{"webmapp_category":[228,232]},"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\/1167","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1167&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/foliation-boudinage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.388117849826813,46.57723943852251]}},{"type":"Feature","properties":{"id":1195,"name":"Geologist on Elephant Island","description":"
Typical coastal cliff of micaschist on Elephant Island with overhaning glacier. The cliffs are due to recent uplift of the island. Sampling is only possible by quickly slipping below the glacier and hoping that no piece will break off at that time. Notice size of geologist dressed in yellow at the foot of the cliff. PhotoID162<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2019-01-28T15:17:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Geologist-on-Elephant-Island-768x1166.jpg","taxonomy":{"webmapp_category":[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\/1195","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1195&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/geologist-on-elephant-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-55.10039786054688,-61.19143055411936]}},{"type":"Feature","properties":{"id":841,"name":"Granulites, Corsica","description":"
Granulites, Corsica
\n<\/i><\/p>\n","modified":"2018-09-04T13:31:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/03\/Screenshot-2018-03-30-09.36.22-e1522395922804-768x432.png","taxonomy":{"webmapp_category":[232,234]},"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\/841","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=841&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/corse-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.139251708,42.54751604]}},{"type":"Feature","properties":{"id":1759,"name":"II_31","description":"
Yarweelor gneiss, reworked Yilgarn basement deformed by the Glenburgh Orogeny. Augengneiss with subvertical E-W trending foliation and and gently E-plunging lineation. Dextral D1-shear bands on a pavement. Dominant D1-deformation (Glenburgh Orogeny)<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:54:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/II_31-768x502.jpg","taxonomy":{"webmapp_category":[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\/1759","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1759&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ii_31\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.596667,-25.528167]}},{"type":"Feature","properties":{"id":6387,"name":"Intertectonic cm-size staurolite porhyroblasts","description":"
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Staurolite grew after D1 deformation and is wrapped around by an S2 foliation. Details in: Real et al., 2018 Italian Journal of Geosciences<\/p>\n
Photo by R. Carosi<\/p>\n","modified":"2019-01-28T18:41:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/staurolite-colico-768x1024.jpg","taxonomy":{"webmapp_category":[232,234]},"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\/6387","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6387&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/intertectonic-cm-size-staurolite-porhyroblasts\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.402963039422616,46.1124186025169]}},{"type":"Feature","properties":{"id":1717,"name":"ivan zibra","description":"
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\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":1719,"name":"ivan zibra","description":"
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Photograph: Ivan Zibra<\/p>\n
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\nPhotoID440<\/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":"2018-06-30T12:17:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-2-768x535.jpg","taxonomy":{"webmapp_category":[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\/1721","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1721&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ivan-zibra-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.211821556091309,42.30519757469809]}},{"type":"Feature","properties":{"id":1727,"name":"ivan zibra","description":"
Layered gabbro sheared under granulite-facies conditions. The tectonic foliation is nearly parallel to the primary compositional layering. White layers are anorthositic; dark layers are hornblenitic and layers with intermediate color index are gabbroic to gabbro-noritic. A brown-weathered Opx porphyroclast occur in the central hornblendite layer.
\nPhotoID443<\/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":"2018-09-16T10:32:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-5-768x552.jpg","taxonomy":{"webmapp_category":[232,234]},"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\/1727","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1727&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ivan-zibra-6\/","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":2068,"name":"Kyanite bearing micascists","description":"
Cm-size kyanite crystals in micaschist. Variscan basement of Sardinia island, Italy. Photo ID 675<\/p>\n
Photograph: R. Carosi – Unipi<\/p>\n
Reference: CAROSI R., PLAMERI R. (2202)- Orogen-parallel tectonic transport in the Variscan belt of northeastern Sardinia (Italy): implications for the exhumation of medium-pressure metamorphic rocks. Geological Magazine, 139, 497-511. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-28T14:33:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kyanite-bearing-micascists-300x227.jpg","taxonomy":{"webmapp_category":[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\/2068","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2068&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kyanite-bearing-micascists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.587852,40.607705]}},{"type":"Feature","properties":{"id":1566,"name":"Layered intrusion","description":"
Layered kakortokites, Kangerdluarsuk, Ilimaussaq intrusion
\nPhotoID338<\/p>\n
Photograph: Tim Ivanic<\/p>\n","modified":"2018-06-30T11:35:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Layered-intrusion-768x576.jpg","taxonomy":{"webmapp_category":[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\/1566","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1566&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/layered-intrusion\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-45.8500671387,60.87099222956163]}},{"type":"Feature","properties":{"id":2114,"name":"Limestone Cap","description":"
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Constrictional fabric seen in the XY plane (foliation plane). Photo ID 709<\/p>\n
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Constrictional fabric in the core of the Caroux dome in an Ordovician orthogneiss. Photo ID 708<\/p>\n
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Photograph: Patrice Rey<\/p>\n","modified":"2018-06-28T14:30:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Linear-fabric-in-rhyolite-768x576.jpg","taxonomy":{"webmapp_category":[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\/2122","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2122&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-fabric-in-rhyolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.83571290969849,-21.3249782343]}},{"type":"Feature","properties":{"id":1418,"name":"Magmatic foliation in a granodiorite","description":"
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Photograph: R. Carosi<\/p>\n
Reference: Dini et al. (2002) – Geological Magazine, 139, 257-279.<\/p>\n","modified":"2018-06-30T19:14:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Magmatic-foliation-in-a-granodiorite-768x516.jpg","taxonomy":{"webmapp_category":[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\/1418","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1418&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/magmatic-foliation-in-a-granodiorite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.140329,42.808823]}},{"type":"Feature","properties":{"id":7148,"name":"Magmatic foliation in a granodiorite, Elba island Italy","description":"
Magmatic foliation in the Monte Capanne granodiorite, S. Andrea locality, Elba island Italy<\/p>\n
The foliation is highlighted by cm-scale k-feldspar. Two rounded mafic enclaves occurrs on the right.<\/p>\n","modified":"2019-08-29T10:15:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/08\/IMG_4281-225x300.jpg","taxonomy":{"webmapp_category":[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\/7148","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7148&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/magmatic-foliation-in-a-granodiorite-elba-island-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.14093058483354,42.808671301450886]}},{"type":"Feature","properties":{"id":1371,"name":"Magmatic layering in granite","description":"
Magmatic layering in the Panafrican Cape Peninsula pluton of the Cape Granite suite at Llanduno, Cape Peninsula
\nPhotoID266<\/p>\n
Photograph: JF Moyen<\/p>\n","modified":"2018-09-04T15:55:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Magmatic-layering-in-granite-768x576.jpg","taxonomy":{"webmapp_category":[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\/1371","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1371&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/magmatic-layering-in-granite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[18.33739,-34.0094]}},{"type":"Feature","properties":{"id":2204,"name":"Mazatzal Mountains Mullions","description":"
Mullions within the Maverick shale of the Proterozoic Mazatzal Group.
\nPhotoID764<\/p>\n
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Strongly deformed metaconglomerate layer of the Phyllite-Quartzite unit (Lower high-pressure nappes, External Hellenides). The outcrop surface is parallel to the XZ-principal plane of the strain ellipsoid. The elongated pebbles are mainly quartzites. PhotoID 613<\/p>\n
Photograph: Paris Xypolias<\/p>\n
Reference: Xypolias, P., Kokkalas, S. 2006. Heterogeneous ductile deformation along a mid-crustal extruding shear zone: an example from the External Hellenides (Greece). In: Law, R.D., Searle, M., Godin, L. (eds) Channel flow, ductile extrusion and exhumation of lower-mid crust in continental collision zones. Geological Society, London, Special Publications, 268, 497-516.<\/p>\n","modified":"2018-06-30T11:36:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Metaconglomerate-768x576.jpg","taxonomy":{"webmapp_category":[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\/2021","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2021&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/metaconglomerate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[22.255174,37.090057]}},{"type":"Feature","properties":{"id":1446,"name":"Metagabbro of Chenaillet ophiolite","description":"
This gabbro of the Ligurian ophiolite of the Chenaillet is deformed and metamorphosed during cooling of the oceanic crust. The black corona around clinopyroxene (grey) consists of amphibole (from hornblende to actinolite).
\nPhotoID289<\/p>\n
Photograph: ch.nicollet<\/p>\n
Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/chenaillet\/MetamRide\/metamride.html<\/p>\n","modified":"2018-07-24T11:35:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Metagabbro-of-Chenaillet-ophiolite-768x576.jpg","taxonomy":{"webmapp_category":[232,234]},"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\/1446","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1446&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/metagabbro-of-chenaillet-ophiolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.731153726577759,44.90737296801133]}},{"type":"Feature","properties":{"id":1833,"name":"migmatite","description":"
Migmatite with schlieren of micaschist in a mainly granodioritic matrix. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:54:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/migmatite-1-768x501.jpg","taxonomy":{"webmapp_category":[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\/1833","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1833&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.794939,-25.473916]}},{"type":"Feature","properties":{"id":1835,"name":"migmatite","description":"
Migmatite with schlieren of micaschist in a mainly granodioritic matrix. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T12:29:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/migmatite-2-768x502.jpg","taxonomy":{"webmapp_category":[232,234]},"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\/1835","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1835&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatite-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.527246,-25.55963]}},{"type":"Feature","properties":{"id":1875,"name":"Migmatitic gneisses","description":"
Magmatic boundary between late varisican leucogranite and migmatitic gneisses of granulitic metamorphic complex. From Punta Chiappa, SE Corsica.
\nPhotoID523<\/p>\n
Photograph: D. Pieruccioni<\/p>\n
Reference: Giacomini et al. (2008): Exhumation of a Variscan orogenic complex: insights into the composite granulitic\u2013amphibolitic metamorphic basement of south-east Corsica (France). J. Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-06-30T12:24:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Migmatitic-gneisses-768x576.jpg","taxonomy":{"webmapp_category":[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\/1875","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1875&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatitic-gneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.374256134033203,41.67215850558213]}},{"type":"Feature","properties":{"id":1401,"name":"Migmatitic high-strain paragneisses","description":"
The Lower Gneiss Unit of the French Hercynian Massif Central is dominated by paragneisses, often partially molten (into the Velay complex). This outcrop is on the upper contact of the LGU, a tectonic contact with the overlying Upper Gneiss Unit (with the Leptyno-amphibolitic complex, a dismembered ophiolite, at its base);the gneisses are migmatitic and high strain.
\nPhotoID274<\/p>\n
Photograph: JF Moyen<\/p>\n","modified":"2018-09-04T14:54:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Migmatitic-high-strain-paragneisses-768x576.jpg","taxonomy":{"webmapp_category":[232,234]},"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\/1401","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1401&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatitic-high-strain-paragneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.76385902648925,45.065814819214815]}},{"type":"Feature","properties":{"id":1403,"name":"Miocene molasse","description":"
Pebbles in miocene molasse in the Chartreuse massif, external Alps. Some of the pebbles (above and right the pencil for instance) show dents, related to pressure dissolution by adjacent pebbles doing post-miocene deformation
\nPhotoID276<\/p>\n
Photograph: JF Moyen<\/p>\n","modified":"2018-06-28T14:31:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Miocene-molasse-768x576.jpg","taxonomy":{"webmapp_category":[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\/1403","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1403&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/miocene-molasse\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.69849,45.247193]}},{"type":"Feature","properties":{"id":1855,"name":"Monzogranite mylonite","description":"
Monzogranite mylonite intruded in the sinistral (top-to-the West) shear zone in the anphibolitic metamorphic complex. From Punta Chiappa, SE Corsica.<\/p>\n
Photograph: D. Pieruccioni<\/p>\n
Reference: Giacomini et al. (2008): Exhumation of a Variscan orogenic complex: insights into the composite granulitic\u2013amphibolitic metamorphic basement of south-east Corsica (France). J. Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-07-24T11:39:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Monzogranite-mylonite-768x1023.jpg","taxonomy":{"webmapp_category":[232,234,231]},"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\/1855","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1855&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/monzogranite-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.368183612823486,41.596148735352934]}},{"type":"Feature","properties":{"id":1681,"name":"Morlungo bank","description":"
Morlungo bank is a very thick level of metarudite with predominant quartzite clasts that crops out in the southern flank of the Monte Borla.
\nPhotoID413<\/p>\n
Photograph: Flavio Milazzo<\/p>\n
Reference: New data on the lithostatigraphy of the Morlungo Monte Sagro area, a preliminary data. Coli M., Fazzuoli M. (1994) Mem. Soc. Geol. It. 48, 67-70<\/p>\n","modified":"2018-09-03T16:54:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Morlungo-bank-768x576.jpg","taxonomy":{"webmapp_category":[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\/1681","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1681&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/morlungo-bank\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.13627976179123,44.11782443162595]}},{"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":1185,"name":"Mullions at Dedenborn, Germany","description":"
Small roadside outcrop near the village of Dedenborn in the N-Eifel, the type example of mullions.<\/p>\n
The outcrop is situated in the steep to overturned limb of a regional series of upright folds with well-developed axial planar cleavage. The rocks consist of alternating psammite-pelite layers.<\/p>\n
Janos Urai, G. Spaeth, Wouter van der Zee, Christoph Hilgers (2001). Evolution of mullion (boudin) structures in the Variscan of the Ardennes and Eifel. Journal of the Virtual Explorer online, 3,1
\n*Ilse Kenis, Janos Urai, Wouter van der Zee, Christoph Hilgers, Manuel Sintubin (2005). Rheology of fine-grained siliciclastic rocks in the middle crust \u2013 evidence from a combined structural and numerical analysis. Earth and Planetary Science Letters, 233,351-360<\/p>\n
http:\/\/www.ged.rwth-aachen.de\/index.php?cat=Research&subcat=Fractures_and_veins&page=Mullions_and_Boudins PhotoID156<\/p>\n
Photograph: Heijn van Gent<\/p>\n","modified":"2018-06-28T18:05:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mullions-at-Dedenborn-Germany-225x300.jpg","taxonomy":{"webmapp_category":[220,232,230]},"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\/1185","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1185&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mullions-at-dedenborn-germany\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.352341,50.581511]}},{"type":"Feature","properties":{"id":1787,"name":"Mylonitised calcsilicate","description":"
Mylonitised calcsilicate of the Camel Hills metasediments ( ca. 2000 Ma) in the Erabiddy shear zone. The fabric is a strong vertical stretching lineation parallel to foldaxes. The folds may be original D1-drag folds, stretched during D2. The lineation is interpreted as a D2-structure. These are two phases in the activity of the Erabiddy shear zone.<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:41:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitised-calcsilicate-192x300.jpg","taxonomy":{"webmapp_category":[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\/1787","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1787&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitised-calcsilicate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.809833,-25.495]}},{"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":2292,"name":"Palai, Malakand, Khyber Pakhtunkhwa","description":"
Meta Sediments (Marble, Calcitic schist) embedded with granitic schist PhotoID815<\/p>\n
Photograph: Atique<\/p>\n","modified":"2018-06-28T18:08:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Palai-Malakand-Khyber-Pakhtunkhwa-768x225.jpg","taxonomy":{"webmapp_category":[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\/2292","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2292&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/palai-malakand-khyber-pakhtunkhwa\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[72.07920456246939,34.56778607530847]}},{"type":"Feature","properties":{"id":1809,"name":"Pencil cleavage","description":"
Pencil cleavage in wm-chl phyllite. Camel Hills metasediments, (ca. 2000 Ma).<\/p>\n
Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:23:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pencil-cleavage-768x502.jpg","taxonomy":{"webmapp_category":[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\/1809","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1809&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pencil-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.654667,-25.533]}},{"type":"Feature","properties":{"id":1524,"name":"Pillows lavas of the Monte Viso","description":"
Monte Viso is a portion of the ligurian oceanic crust subducted at more than 2 GPa. At the bottom of the mountain, blue pillows lavas are
\nundeformed.The blue color is due to fine needles of glaucophane. PhotoID307<\/p>\n
Photograph: c.nicollet<\/p>\n
Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/Viso\/viso.html<\/p>\n","modified":"2018-07-24T12:28:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pillows-lavas-of-the-Monte-Viso-768x576.jpg","taxonomy":{"webmapp_category":[232,234,219]},"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\/1524","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1524&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pillows-lavas-of-the-monte-viso\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.115278244018555,44.66346411852218]}},{"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":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":5744,"name":"S-C-C’ fabric in orthogneiss","description":"
S-C-C’ fabric in Ordovician orthogneiss, top-to-the NE sense of shear and thin section photo (II nicols).<\/p>\n
On the road near of \u00abCantoniera Mt. Tundu\u00bb we start to see outcorps of granodioritic orthogneiss with a prominent C-S fabric and C\u2019 structures pointing to a top-to-the NW sense of shear (\u201cdextral\u201d)<\/span>.<\/p>\n","modified":"2018-09-03T18:04:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/S-Cogn-768x576.jpg","taxonomy":{"webmapp_category":[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\/5744","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5744&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/s_c-fabric-in-orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.598055599999952,40.5950246]}},{"type":"Feature","properties":{"id":1695,"name":"Sardic Angular Unconformity","description":" Cambrian-Early Ordovician shale (Cabitza Shists) are separated from overlying Upper Ordovician-lower Carfoniferous 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":6158,"name":"Sheared augen gneiss","description":" Sheared augen gneiss with kinematic indicators showing a dextral sense of shear (top-to-the NW).<\/p>\n","modified":"2018-12-21T14:17:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSCN3631-1-768x576.jpg","taxonomy":{"webmapp_category":[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\/6158","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6158&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheared-augen-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.563704545777796,40.59894691161987]}},{"type":"Feature","properties":{"id":1624,"name":"Sheared Quartzite","description":" Whitworth Quartzite (~1770Ma), with a strongly developed tectonic fabric due to proximity to the Mount Isa Fault. Photograph: Ryan Eagle<\/p>\n","modified":"2018-09-04T15:59:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheared-Quartzite-768x564.jpg","taxonomy":{"webmapp_category":[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\/1624","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1624&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheared-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[139.4608,-20.6491]}},{"type":"Feature","properties":{"id":1596,"name":"Spaced cleavage","description":" Pressure solution cleavage. Note the narrow dark bands crossing the sandy mudstone beds. Quartz has been removed from these bands and deposited in quartz veins nearby. The more massive layers have fewer dark solution bands running across them. Ilfracombe Bay, Devon, UK. Photograph: Jim Talbot<\/p>\n Reference: See more photos at : http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Localities\/DevonCornwall.html<\/p>\n","modified":"2018-07-24T12:23:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Solution-cleavage-768x545.jpg","taxonomy":{"webmapp_category":[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\/1596","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1596&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/solution-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.112678,51.210233]}},{"type":"Feature","properties":{"id":1909,"name":"Stylolites","description":" Stylolites in rovigno carbonates. Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-09-04T11:41:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Stylolites-768x572.jpg","taxonomy":{"webmapp_category":[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\/1909","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1909&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/stylolites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.681325912475586,45.054909222208146]}},{"type":"Feature","properties":{"id":1237,"name":"stylolites in marbles","description":" Deformed marbles containing green metachert layers which are transected by multiple stylolites during oblique collision in the Zagros orogenic belt. Subhorizontal sylolites are overpinted by steep ones. It is unclear whether the displacement of layer fragments is solely due to dissolution on stylolites or if it is due to displacement in domino boudinage, with subsequent lateral shortening. PhotoID191<\/p>\n Faghih, A., 2008. Structural evolution of accretion and collision processes of the Zagros orogeny, Iran. Unpublished PhD thesis, Shiraz University,Shiraz , Iran. This is a Journal of Structural Geology Photograph of the Month<\/p>\n Photograph:<\/p>\n","modified":"2018-07-24T11:33:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/stylolites-in-marbles-768x575.jpg","taxonomy":{"webmapp_category":[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\/1237","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1237&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/stylolites-in-marbles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.221388,29.204444]}},{"type":"Feature","properties":{"id":6557,"name":"Stylolitic foliation in pelagic limestone","description":" Stylolitic foliation in pelagic limestone (Northern Apennines, Italy)<\/p>\n","modified":"2019-02-09T10:46:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/IMG_6054-768x576.jpg","taxonomy":{"webmapp_category":[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\/6557","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6557&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/stylolitic-foliation-in-pelagic-limestone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.640336373831815,43.0817697609449]}},{"type":"Feature","properties":{"id":1691,"name":"Taimyr spaced cleavage","description":" shale and sandstone with low grade cleavage (spaced cleavage), Taimyr Photograph: Vicky Pease<\/p>\n","modified":"2018-06-30T11:18:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Taimyr-fracture-cleavage-768x576.jpg","taxonomy":{"webmapp_category":[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\/1691","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1691&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/taimyr-fracture-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[111.8785,74.9463]}},{"type":"Feature","properties":{"id":1568,"name":"tonalite-monzogranite intrusion","description":" Neoarchean (ca. 2680 Ma) granites displaying a well-defined planar fabric due to the injection of tonalite to monzogranite sheets aligned parallel to the magmatic foliation, which is defined by aligned euhedral feldspars. No effect of important solid-state deformation is visible at outcrop-scale. The base of photo is about 1 meter. Photograph: Ivan Zibra<\/p>\n Reference: Geological Survey of Western Australia (GSWA)<\/p>\n","modified":"2018-09-04T13:34:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/tonalite-monzogranite-intrusion-768x1024.jpg","taxonomy":{"webmapp_category":[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\/1568","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1568&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tonalite-monzogranite-intrusion\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.50710487365723,-27.8917167699]}},{"type":"Feature","properties":{"id":6475,"name":"Trassic conglomerate, Verrucano sequence, Monti Pisani","description":" Bedding in Trassic conglomerate, Verrucano sequence, Monti Pisani, Italy<\/p>\n Photo by Rodolfo Carosi<\/p>\n","modified":"2019-01-31T17:40:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Anageniti-grossolane-Verrucano-768x515.jpg","taxonomy":{"webmapp_category":[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\/6475","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6475&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/trassic-conglomerate-verrucano-sequence-monti-pisani\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.560105667731477,43.73486265497749]}},{"type":"Feature","properties":{"id":1375,"name":"Variscan shear zone","description":" Sinistral (top-to-the West) shear zone in the granulitic metamorphic complex of Southern Corsica (France). The age is nearly 320 Ma. PhotoID174<\/p>\n Photograph: R Carosi<\/p>\n Reference: Giacomini et al. (2008) – Exhumation of a Variscan orogenic complex: insights into the composite granulitic\u2013amphibolitic metamorphic basement of south-east Corsica (France). J. Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-06-28T13:40:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Variscan-shear-zone-768x516.jpg","taxonomy":{"webmapp_category":[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\/1375","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1375&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/variscan-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.406158,41.739092]}},{"type":"Feature","properties":{"id":2120,"name":"Warrawoona rod schists","description":" Mafic schists and cherts with a strong, steeply dipping, linear fabrics. Geologits for scale: Pascal Philippot, Florence Lehebel, Patrice Rey and Nicolas Th\u00e9baud. Photo ID 704<\/p>\n Photograph: Joel Brugger (2003)<\/p>\n","modified":"2018-06-28T13:35:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Warrawoona-rod-schists-768x576.jpg","taxonomy":{"webmapp_category":[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\/2120","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2120&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/warrawoona-rod-schists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.85069563865659,-21.3110617816]}},{"type":"Feature","properties":{"id":1785,"name":"Yarweelor augengneiss","description":" Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). Augengneiss with subvertical E-W trending foliation and and gently E-plunging lineation. Dextral D1-shear bands.<\/p>\n Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:34:11","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-augengneiss-768x502.jpg","taxonomy":{"webmapp_category":[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\/1785","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1785&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-augengneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.596667,-25.528167]}},{"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. 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]}}]}
\nsedimentary cycle by sharp angular unconformity (Sardic phase) and overlain by trasgressive polygenic
\nmetaconglomerate, the Puddinga Auct.
\nPhotoID422<\/p>\n
\nPhotoID367<\/p>\n
\nPhotoID354<\/p>\n
\nRovigno<\/p>\n
\nSarkarinejad, K., Faghih, A., Grasemann, B., 2008. Transpressional deformations within the Sanandaj-Sirjan Metamorphic Belt (Zagros Mountains, Iran). Journal of Structural Geology 30, 818\u201382<\/p>\n
\nPhotoID420<\/p>\n
\nPhotoID339<\/p>\n
\nPhotoID472<\/p>\n