{"type":"FeatureCollection","features":[{"type":"Feature","properties":{"id":1492,"name":"A typical ligurian ophiolitic sequence","description":"

The alpine Chenaillet ophiolite is characteristic of an oceanic crust created at a low spreading ridge. The sequence is discontinuous and differs from the classical sequence of the Penrose conference.
\nFrom the bottom to the top of the SW ridge of the Chenaillet, we have the sequence : serpentinized mantle, isotropic gabbro and pillows lavas. The dyke complex is missing. Only a few dykes crosscut the serpentinite or the gabbro. Sometimes, the sediments directly lie on the serpentinized mantle.
\nView towards the NE from the Sommet des Anges.
\nPhotoID306<\/p>\n

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

Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/chenaillet\/chenaillet.html<\/p>\n","modified":"2018-10-10T18:48:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-typical-ligurian-ophiolitic-sequence-768x512.jpg","taxonomy":{"webmapp_category":[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\/1492","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1492&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-typical-ligurian-ophiolitic-sequence\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.71565055847168,44.893214870201454]}},{"type":"Feature","properties":{"id":960,"name":"Affioramento 1","description":"

Prova .<\/p>\n","modified":"2018-10-10T18:59:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/03\/Boudinage_near_Kangerlussuaq-e1522400693889-768x432.jpeg","taxonomy":{"webmapp_category":[228,234]},"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\/960","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=960&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/affioramento-1\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.44679641,43.76837132]}},{"type":"Feature","properties":{"id":1187,"name":"Andalusite bearing micaschist","description":"

Cm-size andalusite crystals in micaschist of the Medium Grade Metamorphic Complex; Varisca orogeny (Asinara Island, Italy). Usually andalusite grows during a HT-LP metamorphic event after staurolite. PhotoID157<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:55:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Andalusite-bearing-micaschist-300x225.jpg","taxonomy":{"webmapp_category":[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\/1187","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1187&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/andalusite-bearing-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.259208679199219,41.05718945133737]}},{"type":"Feature","properties":{"id":1353,"name":"Baviaanskloof gneisses","description":"

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

Photograph: JF Moyen<\/p>\n","modified":"2018-09-04T14:55:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Baviaanskloof-gneisses-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1353","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1353&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/baviaanskloof-gneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[29.74589,-23.4441]}},{"type":"Feature","properties":{"id":2200,"name":"Bradshaw Mountains Garnetite (Close-up)","description":"

Close-up of garnet crystals in the garnetite layer.
\nPhotoID762<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-09-04T11:26:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bradshaw-Mountains-Garnetite-Close-up-768x576.jpg","taxonomy":{"webmapp_category":[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\/2200","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2200&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bradshaw-mountains-garnetite-close-up\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.35401,34.18239]}},{"type":"Feature","properties":{"id":2098,"name":"Cm-size andalusite crystals","description":"

Cm-size andalusite crystals in micaschist of the Medium Grade Metamorphic Complex; Varisca orogeny (Asinara Island, Italy). HT-LP metamorphic overprint on Variscan Barrovian metamorphism.
\nPhotoID690<\/p>\n

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

Reference: CAROSI R, DI PISA A., IACOPINI D., MONTOMOLI C, OGGIANO G. (2004) – The structural evolution of the Asinara Island (NW Sardinia, Italy). Geodinamica Acta, 17, 5 309-329. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-07-30T16:30:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cm-size-andalusite-crystals-768x576.jpg","taxonomy":{"webmapp_category":[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\/2098","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2098&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cm-size-andalusite-crystals\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.2641,41.0624]}},{"type":"Feature","properties":{"id":6192,"name":"Conctac schist, Calabria","description":"

 <\/p>\n

Contact schist with porphyroblasts of cordierite, Mammola, Calabria (Italy)<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-03-04T10:53:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Cordierite-schist-Mammola-225x300.jpg","taxonomy":{"webmapp_category":[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\/6192","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6192&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/conctac-schist-calabria\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[16.251052899456113,38.372216711762405]}},{"type":"Feature","properties":{"id":6201,"name":"Contact metamorphism around Monte Capanne pluton, Elba island, Italy","description":"

Contact metamorphism around Monte Capanne pluton, Elba island, Italy. Garnet-bearing marble with grossular: sedimentary covers of the Liguride Units affected by contact metamorphism of the Monte Capanne intrusion.<\/p>\n","modified":"2019-01-28T11:21:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/IMG_5180-768x1024.jpg","taxonomy":{"webmapp_category":[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\/6201","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6201&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/contact-metamorphism-around-monte-capanne-pluton-elba-island-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.104346722364426,42.766734740563045]}},{"type":"Feature","properties":{"id":1799,"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. The pavements show banded Dalgaringa gneiss cut by several generations of granite and pegmatite veins, possibly of Wooramel and Moorarie age. West at the top. S 178-82; Lstr 253-32<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T12:18:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[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\/1799","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1799&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57327894973753,-25.5128364991]}},{"type":"Feature","properties":{"id":1341,"name":"Deformed veins (Rainy Lake)","description":"

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

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

Reference: Druguet, E., Czeck, D.M., Carreras, J., Casta\u00f1o, L.M., 2008. Emplacement and deformation features of syntectonic leucocratic veins from Rainy Lake zone (Western Superior Province, Canada). Precambrian Research 163, 384-400.<\/p>\n","modified":"2018-07-24T12:22:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-veins-Rainy-Lake-768x348.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1341","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1341&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-veins-rainy-lake\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-93.2719516754,48.67541938037722]}},{"type":"Feature","properties":{"id":7289,"name":"Dyke in the migmatitic gneiss at St Tropez","description":"

Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-12-04T09:53:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/12\/PB010085-768x576.jpg","taxonomy":{"webmapp_category":[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\/7289","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7289&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dyke-in-the-migmatitic-gneiss-at-st-tropez\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.678109,43.278828]}},{"type":"Feature","properties":{"id":2015,"name":"Exotic Metamorphic Block, Ring Mountain","description":"

One of many high grade exotic metamorphic blocks embedded in Franciscan Melange on Ring Mountain in Tiburon California.
\nPhoto ID 610<\/p>\n

Photograph: Brenor Brophy<\/p>\n","modified":"2018-07-24T12:26:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Exotic-Metamorphic-Block-Ring-Mountain-768x576.jpg","taxonomy":{"webmapp_category":[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\/2015","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2015&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/exotic-metamorphic-block-ring-mountain\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.485253,37.911811]}},{"type":"Feature","properties":{"id":7029,"name":"Fault and fold in calcschist of Giens near Hy\u00e8res, France","description":"

\"\"<\/p>\n

Giens peninsula (near Hy\u00e8res, France) has beautiful outcrops of metamorphic rocks. Some are folded and faulted like on this picture on the western side of the peninsula.<\/p>\n","modified":"2019-06-16T19:45:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-768x1024.jpg","taxonomy":{"webmapp_category":[220,229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7029","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7029&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-and-fold-in-calcschist-of-giens-near-hyeres-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.096309,43.028767]}},{"type":"Feature","properties":{"id":1638,"name":"Finero","description":"

Finero Peridotite (Olivine, Phlogopite, Cr-Diopside); Lithosferic mantel affected by metasomatsm.
\nPhotoID379<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-09-04T15:55:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Finero-1-768x576.jpg","taxonomy":{"webmapp_category":[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\/1638","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1638&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/finero-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.531227111816406,46.102637544820595]}},{"type":"Feature","properties":{"id":6778,"name":"fold in the most external portion of the”Eclogitic Micaschist Complex” (Sesia-Lanzo Unit)","description":"

Alpine deformations. Huge pluridecametric F4 folds in the most external portion of the EMC “Eclogitic Micaschist Complex” (retrogressed eclogites with greenshist facies imprint) of the Sesia-Lanzo Zone Unit (nappe of the Australpine domain),\u00a0adriatic (paleoafrican) subducted ex continental margin. Outcrop exposed along the Roman consular road from Donnas to Bard (AO) spur, Aosta Valley region. Outcrop related to “Fig. 8 \u2013 (a) View of the outcrops exposed along the Roman consular road at Bard, not far from Stop 4.” outcrop described at page 32 of the paper “Valle d\u2019Aosta section of the Sesia Zone: multi-stage HP metamorphism and assembly of a rifted continental margin” – 10th International Eclogite Conference – Courmayeur (Aosta, Italy), Compagnoni, Engi, Regis – Geol.F.Trips, Vol.6 No.1.2 (2014), Periodico semestrale del Servizio Geologico d’Italia – ISPRA e della Societ\u00e0 Geologica Italiana.<\/p>\n

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

 <\/p>\n","modified":"2019-03-16T20:28:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/03\/SL-1.Bard-2.Mellier-153-F-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6778","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6778&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fold-in-the-most-external-portion-of-theeclogitic-micaschist-complex-sesia-lanzo-unit\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.750706418415575,45.60468243847165]}},{"type":"Feature","properties":{"id":6338,"name":"Folded leucosome, Punta Ottiolu, Sardinia","description":"

Folded leucosomes in Variscan migmatite, Punta Ottiolu, Sardinia, Italy<\/p>\n","modified":"2019-01-28T13:35:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/migmatiti-ottiolu-225x300.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6338","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6338&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-leucosome-punta-ottiolu-sardinia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.714694446093745,40.742290346143335]}},{"type":"Feature","properties":{"id":6469,"name":"Folded migmatites, Antarctica","description":"

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

Photo by Chiara Montomoli<\/p>\n

 <\/p>\n","modified":"2019-01-31T17:26:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/migmatiti-lichen-hills_n-768x345.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6469","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6469&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-migmatites-antarctica\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.00544236913947,-73.27132581745721]}},{"type":"Feature","properties":{"id":6933,"name":"Folds and metasomatized, retrogressed ex garnet peridotite (now serpentinized) boudins within amphibole-bearing migmatitic gneiss, Borgo outcrop Darengo Valley, Adula nappe","description":"

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

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

 <\/p>\n","modified":"2019-05-05T22:32:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/val_darengo_II-407-PDT-boudins-in-AG-amph-bearing-migmatitic-gneiss-F-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6933","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6933&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-and-metasomatized-retrogressed-ex-garnet-peridotite-now-serpentinized-boudins-within-amphibole-bearing-migmatitic-gneiss-borgo-outcrop-darengo-valley-adula-nappe\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.299345345603342,46.214173658796085]}},{"type":"Feature","properties":{"id":6328,"name":"Folds in marbles and stretched dykes, Elba Island","description":"

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

Photo by R. Carosi<\/p>\n","modified":"2019-01-28T13:34:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/SPartaiaElba-225x300.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6328","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6328&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-marbles-and-stretched-dykes-elba-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.234650693640106,42.788866799946256]}},{"type":"Feature","properties":{"id":5743,"name":"Garnet + staurolite bearing micaschist","description":"

On the road from<\/span> Torp\u00e8<\/span> village<\/span> to<\/span> Lod\u00e8<\/span> (S. Anna villages<\/span>) there<\/span> is<\/span> an<\/span> outcorp<\/span> of<\/span> staurolite and garnet<\/span> bearing<\/span> micaschist<\/span>: near<\/span> the gate<\/span> at the entrance<\/span> of<\/span> a small<\/span> forest<\/span> track<\/span>, we<\/span> see<\/span> cm-size<\/span>staurolite and garnet<\/span> porphyroclasts<\/span> on the S2 foliation<\/span> of<\/span> the micaschist. Garnet and staurolite grew after the D1 and from pre-to syn-D2 deformation phase.<\/span> <\/span><\/p>\n","modified":"2018-09-03T18:03:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Garnetstaurolite-bearing-micaschist-300x300.png","taxonomy":{"webmapp_category":[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\/5743","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5743&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garnetstaurolite-bearing-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.579414000000043,40.6018154]}},{"type":"Feature","properties":{"id":7305,"name":"Garnet and biotite in micaschist of Rayol le Canadel","description":"

By Le Canadel beach, the micaschist hosts garnet, staurolite, biotite and quartz veins. The garnet are locally more concentrated, the biotite in concentrated around a quartz vein making the black surroundings. Staurolite can be also observed in this rock beach.<\/p>\n

Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-12-11T14:48:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/12\/PB010106-768x576.jpg","taxonomy":{"webmapp_category":[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\/7305","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7305&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garnet-and-biotite-in-micaschist-of-rayol-le-canadel\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.463840813491856,43.1576273019213]}},{"type":"Feature","properties":{"id":7308,"name":"Garnet and muscovite in micaschist of Rayol le Canadel","description":"

On the eastern side of Le Canadel beach, the micaschist hosts garnet and muscovite with quartz.<\/p>\n

Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-12-11T14:47:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/12\/PB010117-768x576.jpg","taxonomy":{"webmapp_category":[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\/7308","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7308&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garnet-and-muscovite-in-micaschist-of-rayol-le-canadel\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.4656008515205485,43.1574795424012]}},{"type":"Feature","properties":{"id":2074,"name":"Garnet and sillimanite gneiss","description":"

Cm-size garnets in garnet- and sillimanite- bearing gneiss of the Hgher Himalayan Crystallines, Sikkim. Photo ID 678<\/p>\n

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

Reference: Searle M. & Szulc A. (2005) – Channel flow and ductile extrusion of the high Himalayan slab-the Kangchenjunga\u2013Darjeeling profile, Sikkim Himalaya. J Asian Earth Sciences, 25, 173-185.<\/p>\n","modified":"2018-09-04T13:28:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Garnet-and-sillimanite-gneiss-768x575.jpg","taxonomy":{"webmapp_category":[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\/2074","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2074&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garnet-and-sillimanite-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[88.70980765075683,27.371519717248823]}},{"type":"Feature","properties":{"id":7302,"name":"Garnet and staurolite in micaschist of Rayol le Canadel","description":"

In the Canadel beach, beautiful outcrop of micaschist with garnets and staurolite<\/p>\n

Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-12-11T14:46:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/12\/PB010099-768x576.jpg","taxonomy":{"webmapp_category":[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\/7302","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7302&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garnet-and-staurolite-in-micaschist-of-rayol-le-canadel\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.463890396329816,43.157639779322956]}},{"type":"Feature","properties":{"id":1933,"name":"Garnet rock","description":"

Garnets and flakes of gold in metamorphic basement.
\nPhotoID555<\/p>\n

Photograph: Bernd Andeweg VU University Amsterdam<\/p>\n","modified":"2018-09-04T15:57:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Garnet-rock-768x576.jpg","taxonomy":{"webmapp_category":[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\/1933","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1933&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/garnet-rock\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-50.5182266235,66.96931216090262]}},{"type":"Feature","properties":{"id":7268,"name":"Gneiss with quartz lenses","description":"

Gneiss (locally micaschiste) with abundant quartz lenses on the c\u00f4te d’Azur close to Sainte-Maxime.<\/p>\n

Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n

 <\/p>\n","modified":"2019-11-14T22:10:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/11\/PA290018-768x576.jpg","taxonomy":{"webmapp_category":[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\/7268","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7268&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/gneiss-with-quartz-lenses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.711333542327907,43.34493832027594]}},{"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":7054,"name":"Intense ductile deformation","description":"

Ex feldspar crystals developed in mantled \u03b4-type porphyroclasts affecting mylonitic texture orthogneiss (“augengneiss”).\u00a0 Dextral sense of shear (top-to-right ductile shear zone).\u00a0 Outcrop photo originally vertical, from the Engadine valley (outcrops probably associated to Engadine Line), near St. Moritz (20km south of St.Moritz towards Como lake), Rhetic Alps, central Alps, Switzerland.<\/p>\n","modified":"2019-06-21T11:20:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/46-768x551.jpg","taxonomy":{"webmapp_category":[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\/7054","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7054&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/intense-ductile-deformation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.69975255446218,46.39600241775577]}},{"type":"Feature","properties":{"id":6397,"name":"interference pattern figure, sheath folds “Paina Marble” mylonite","description":"

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

(Photo by Lorusso Angelo).<\/p>\n","modified":"2019-01-29T13:41:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/BD_III-543-F-768x576.jpg","taxonomy":{"webmapp_category":[229,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6397","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6397&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/interference-pattern-figure-sheath-folds-paina-marble-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.31133165069673,46.191203645751116]}},{"type":"Feature","properties":{"id":6387,"name":"Intertectonic cm-size staurolite porhyroblasts","description":"

Intertectonic cm-size staurolite porhyroblasts in the basement of Como Lake, Colico, Italy.<\/p>\n

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":1719,"name":"ivan zibra","description":"

Magmatically foliated, Opx-bearing granodiorite of Perrmian Age, intruded by Opx-bearing pegmatite.
\nPhotoID439<\/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":"2018-07-24T11:35:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-1-768x474.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\/1719","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1719&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ivan-zibra-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.182939529418945,42.34446221439218]}},{"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":5746,"name":"Kinked augen gneiss, Lod\u00e8","description":"

Kinked augen gneiss (F3 fold). Kinks affect theS2 mylonitic foliation. Lod\u00e8.<\/p>\n","modified":"2018-08-07T12:27:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Kinked-augen-gneiss-300x213.png","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5746","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5746&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kinked-augen-gneiss-lode\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.544945999999982,40.593203]}},{"type":"Feature","properties":{"id":5745,"name":"Kyanite","description":"

Kyanite bearing micaschist, Bruncu Nieddu.<\/p>\n

About<\/span> 0.5 km further<\/span> north<\/span> along<\/span> the track<\/span> we<\/span> reach<\/span> the kyanite+biotite<\/span> isograd<\/span> with<\/span>mm- to<\/span> cm-size<\/span> bluish<\/span> kyanite<\/span> crystals<\/span> in the matrix<\/span> of<\/span> the mylonites<\/span> and in quartz-rich<\/span> veins<\/span> (Fig. 1). The kyanite+biotite<\/span> isograd<\/span> is<\/span> marked<\/span> by<\/span> the first appearance<\/span> of<\/span>kyanite<\/span> crystals<\/span>. The rocks<\/span> consist<\/span> of<\/span> porphyroblasts<\/span> of<\/span> staurolite, kyanite<\/span>, andplagioclase<\/span> enveloped<\/span> in a mylonitic<\/span> matrix<\/span> of<\/span> muscovite, biotite, chlorite<\/span>, and ilmenite.<\/span> Temperatures<\/span> up to<\/span> 595 \u00b0C and pressures<\/span> up to<\/span> 0.67 GPa<\/span> have<\/span> been<\/span> reported<\/span> by<\/span>Franceschelli<\/span> et<\/span> al. (1989), and pressures<\/span> over<\/span> 0.9 GPa<\/span> by<\/span> Carosi<\/span> & Palmeri<\/span> (2002) for <\/span>the metamorphic<\/span> peak<\/span><\/span>.<\/p>\n","modified":"2018-09-03T17:41:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/ky-2-768x768.jpg","taxonomy":{"webmapp_category":[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\/5745","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5745&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kyanite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.579414000000043,40.6018154]}},{"type":"Feature","properties":{"id":1502,"name":"Leptyno-amphibolitic group","description":"

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

Photograph: JF Moyen<\/p>\n

Reference: Outcrop courtesy of V. Gardien, Univ. Lyon I<\/p>\n","modified":"2018-09-16T10:30:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Leptyno-amphibolitic-group-225x300.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1502","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1502&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/leptyno-amphibolitic-group\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.75931,45.06425]}},{"type":"Feature","properties":{"id":2126,"name":"Linear fabric in orthogneiss","description":"

Constriction in the core of the Caroux dome. Picture plane is perpendicular to the stretching lineation. Photo ID 707<\/p>\n

Photograph: Patrice Rey<\/p>\n","modified":"2018-09-04T13:29:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Linear-fabric-in-orthogneiss-1-768x576.jpg","taxonomy":{"webmapp_category":[230,234]},"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\/2126","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2126&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-fabric-in-orthogneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[2.96231746673584,43.58381046177999]}},{"type":"Feature","properties":{"id":1955,"name":"melt in shear zone","description":"

melt-accumulation along a ductile shear zone. Praia das Conchas
\nPhotoID566<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:33:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/melt-in-shear-zone-300x197.jpg","taxonomy":{"webmapp_category":[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\/1955","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1955&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/melt-in-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-41.980555,-22.8675]}},{"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":1464,"name":"Metagabbro of the Oman ophiolite","description":"

Thanks to a still important hydrothermalism at this depth, the varitextured gabbros, just below the dyke complex, can be metamorphized. A black corona of amphibole surrounds the clinopyroxene. The amphibole, from brown to green under the microscope, records the different steps of the cooling of the gabbro since the tardi-magmatic conditions until the conditions of the Greenschists facies. Wadi Abyad.
\nPhotoID293<\/p>\n

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

Reference: http:\/\/christian.nicollet.free.fr\/page\/oman\/metamRide\/omanMetamRide.html<\/p>\n","modified":"2018-09-04T13:37:53","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Metagabbro-of-the-Oman-ophiolite-768x576.jpg","taxonomy":{"webmapp_category":[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\/1464","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1464&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/metagabbro-of-the-oman-ophiolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[57.684748470783234,23.487186627010345]}},{"type":"Feature","properties":{"id":1462,"name":"Metagranite of Monte Mucrone","description":"

The Metagranite of Monte Mucrone, eclogitized during the HP alpine metamorphism, preserves magmatic textures and minerals: biotite is surrounded by a garnet corona. Only in decimeter thick shear zones, the metamorphic reaction goes to completion: black patches of biotite have disappeared and the light- green color of jadeite is dominant.
\nPhotoID292<\/p>\n

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

Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/Mucrone\/mucrone.html<\/p>\n","modified":"2018-09-04T13:27:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Metagranite-of-Monte-Mucrone-768x576.jpg","taxonomy":{"webmapp_category":[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\/1462","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1462&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/metagranite-of-monte-mucrone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.94727,45.62353]}},{"type":"Feature","properties":{"id":1827,"name":"Migmatic gneiss","description":"

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

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-03T17:46:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Migmatic-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1827","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1827&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatic-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381667,-25.582667]}},{"type":"Feature","properties":{"id":1813,"name":"migmatic veins","description":"

Migmatitic gneiss with melt veins axial planar to older melt veins which have been folded; the last veins are deformed by the Errabiddy shear zone mylonites. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T11:43:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/migmatic-veins-768x493.jpg","taxonomy":{"webmapp_category":[224,234]},"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\/1813","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1813&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatic-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.7945,-25.544333]}},{"type":"Feature","properties":{"id":1831,"name":"migmatite","description":"

Migmatite with S 353-78, Lstr 16-62. 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":"2018-09-04T15:50:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/migmatite-768x494.jpg","taxonomy":{"webmapp_category":[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\/1831","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1831&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.794667,-25.474167]}},{"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":7285,"name":"Migmatitic gneiss at St Tropez","description":"

 <\/p>\n

By the coast, from the cap St Pierre to the cap de St Tropez, intensively folded migmatitic gneiss are exposed.
\nPicture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-12-04T09:54:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/12\/PB010078-768x576.jpg","taxonomy":{"webmapp_category":[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\/7285","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7285&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/migmatitic-gneiss-at-st-tropez\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.669392,43.276128]}},{"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":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":1295,"name":"Mt. Makalu south face","description":"

Kilometre scale thick sill of Makalu granite (top of Mt.Makalu) and migmatitic Barun gneiss and Black gneiss with abundant granites (Grater Himalayan Sequence) on the southern slope of Mt. Makalu (8485 m). Photograph from Makalu base camp nearly 4900 m. Makalu granite emplaced age is between 24 and 21 Ma. PhotoID230<\/p>\n

References: Streule et al. 2010 Tectonics, in press.
\nLombardo et al. 1993. Geol Soc. London Sepc. Publ., 74, 341-355.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-07-25T08:46:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Makalu-south-face-768x516.jpg","taxonomy":{"webmapp_category":[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\/1295","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1295&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mt-makalu-south-face\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.076445,27.837501]}},{"type":"Feature","properties":{"id":1118,"name":"Namibia Boudins","description":"

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

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-16T10:33:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Namibia-Boudins-768x505.jpg","taxonomy":{"webmapp_category":[228,229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1118","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1118&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/namibia-boudins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.644775390625,-20.879342972]}},{"type":"Feature","properties":{"id":1999,"name":"Ophiolitic Breccias","description":"

Ophiolitic breccias on the contact between Pillow lavas and Radiolaran Charts (Complex IV, Elba Island)<\/p>\n

A Huge pillow lava block trapped in the breccias is visible.
\nPhotoID595<\/p>\n

Photograph: S. Papeschi<\/p>\n","modified":"2018-10-10T18:45:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ophiolitic-Breccias-768x576.jpg","taxonomy":{"webmapp_category":[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\/1999","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1999&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ophiolitic-breccias\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.40531,42.788505]}},{"type":"Feature","properties":{"id":5741,"name":"Orthogneiss","description":"

Deformed mafic microgranular enclave in the sheared Ordovician granodioritic orthogneiss.<\/p>\n","modified":"2018-12-12T09:38:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Ortogneiss-768x578.png","taxonomy":{"webmapp_category":[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\/5741","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5741&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.53913799999998,40.591026]}},{"type":"Feature","properties":{"id":1939,"name":"orthogneiss with pseudotachylyte","description":"

pavement of weakly mylonitised orthogneiss, cut by undeformed pseudotachylyte. The pseudotachylyte has a steep movement component
\nPhotoID558<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:35:53","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/orthogneiss-with-pseudotachylyte-768x499.jpg","taxonomy":{"webmapp_category":[220,234]},"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\/1939","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1939&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/orthogneiss-with-pseudotachylyte\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-60.106111,2.46222]}},{"type":"Feature","properties":{"id":1414,"name":"Pebbles of metagabbros","description":"

While most of the Brian\u00e7onnais zone of the Western Alps has been through blueschist facies conditions, it is not always easy to find good rocks to look at. Some of the best (and most accessible) metagabbros are found as pebbles in the Gul river downstream of Chateau-Queyras; the gabbros here are only partly transofrmed into blueschist, such that the glaucophane forming reaction (at the expense of hornblende) can be seen in the rocks.<\/p>\n

Bruand, E., Nicollet, C., Goncalves, P., Schwartz, S., Chamorro-Perez, E., 2010. Petrology of metagabbros and Schistes Lustr\u00e9s through the Queyras accretionary wedge (Western Alps), EGU General Assembly 2010, Vienna, p. 11983.
\nPhotoID280<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-09-04T15:54:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pebbles-of-metagabbros-225x300.jpg","taxonomy":{"webmapp_category":[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\/1414","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1414&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pebbles-of-metagabbros\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.78427,44.75404]}},{"type":"Feature","properties":{"id":1159,"name":"pegmatite boudin","description":"

spectacular pegmatite boudin in mylonitised schist. The boudin is almost completely exposed in 3D due to erosion of the surrounding mylonite. PhotoID117<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-10-10T18:57:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/pegmatite-boudin-768x576.jpg","taxonomy":{"webmapp_category":[228,234]},"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\/1159","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1159&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pegmatite-boudin\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.317587450146675,42.3171272961114]}},{"type":"Feature","properties":{"id":2009,"name":"Pillow Basalt at Tennessee Point","description":"

As mentioned in Streetcar to Subduction, trip 5b (Marin Headlands). An excellent exposure of pillow basalt from the Marin Headlands Terrane. Photo ID 607<\/p>\n

Photograph: Brenor Brophy<\/p>\n","modified":"2018-10-10T18:46:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pillow-Basalt-at-Tennessee-Point-768x576.jpg","taxonomy":{"webmapp_category":[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\/2009","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2009&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pillow-basalt-at-tennessee-point\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.548286,37.834227]}},{"type":"Feature","properties":{"id":2142,"name":"Pillow Lavas","description":"

Deformed pillow lavas in low-grade metamorphic sequence of Massa Unit at Punta Bianca locality. Each pillow is nearly 40-60 in thickness. Age: Middle Trias.
\nPhotoID722<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:44:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pillow-Lavas-300x202.jpg","taxonomy":{"webmapp_category":[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\/2142","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2142&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pillow-lavas\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.973118,44.036885]}},{"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":6291,"name":"Pseudotachylyte","description":"

Pseudotachylyte veins\u00a0inject granulitic metagabbros referred to “Ivrea-Verbano Zone” (southalpine continental inferior crust) outcrops on the slopes between Vogogna – Premosello towns, Southalpine basement next to Insubric Line, from Verbano – Cusio – Ossola province, Piedmont, \u00a0Italy.\u00a0<\/span><\/p>\n

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

\"\"<\/p>\n

 <\/p>\n","modified":"2019-01-27T20:13:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/pseudotachiliti-Vogogna-Premosello-3-768x576.jpg","taxonomy":{"webmapp_category":[224,234]},"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\/6291","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6291&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pseudotachylyte-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.302449186461104,46.00610410571192]}},{"type":"Feature","properties":{"id":2055,"name":"Punta Sirenella","description":"

Sillimanite spot in Sillimanite Migmatites. Photo ID 638<\/p>\n

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

Reference: High-grade metamorphics from NE Sardinia, Italy. 85\u00b0 Congresso SIMP Fluminimaggiore Post-Session Field Trip Guide 29-30 september 2006 Field Leaders G. Cruciani, F.M. Elter, M. Franceschelli1, M. Puxeddu, D. Utzeri<\/p>\n","modified":"2018-09-04T11:25:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Punta-Sirenella-768x576.jpg","taxonomy":{"webmapp_category":[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\/2055","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2055&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/punta-sirenella\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.59329068660736,40.96816472029669]}},{"type":"Feature","properties":{"id":6516,"name":"Sapphirine bearing granulites from Gruf Compex, Penninic Domain, index of U.H.T. – “Ultra High Temperature” metamorphism in central (italian Rethic) Alps","description":"

Sapphirine bearing granulites from Gruf Compex, Penninic Domain, index of U.H.T. – “Ultra High Temperature” metamorphism in central (italian Rethic) Alps.These granulites (type A of Galli et al. 2011) are rare, dark, heavy and massive rocks normally occurred as relict enclaves in migmatitic orthogneisses and charnockites and represent restitic melanocratic refractory product as residue compliments originating through melt extraction from prepermian metapelitic sediments showing mineral assemblage made of orthopyroxene (honey light-brown), sapphirine (blue), biotite (dark brown), garnet (pink with opx\u2013cordierite symplectites inside), quartz (colourless), feldspar (grey). Stereomicroscope photo (horizontal FOV 6mm approx) of a sample from a detrital (not in situ) discovery on Punta di Bresciadega slopes, Alpe Coeder, medium Codera valley, Chiavenna valley, Rethic Alps, Lombardy, Italy. (Selfcollected)<\/span><\/p>\n

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

\"\"<\/span><\/p>\n","modified":"2019-02-02T07:21:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/gruf-granul-I-130-F-768x576.jpg","taxonomy":{"webmapp_category":[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\/6516","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6516&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sapphirine-bearing-granulites-from-gruf-compex-penninic-domain-index-of-u-h-t-ultra-high-temperature-metamorphism-in-central-italian-rethic-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.528751145359706,46.25998187696019]}},{"type":"Feature","properties":{"id":1363,"name":"Sea Point","description":"

Intrusive contact of the Panafrican Peninsula pluton of the Cape Granite Suite into metasediments from the Malmesbury Supergroup. This locality was famously described by Charles Darwin during the Beagle Voyage<\/p>\n

Master, S., 2009. Plutonism versus neptunism at the southern tip of Africa: the debate on the origin of granites at the Cape, 1776-1844. Trans. R. Soc. Edinb.-Earth Sci. 100, 1-13.<\/p>\n

PhotoID261<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-09-04T13:30:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sea-Point-225x300.jpg","taxonomy":{"webmapp_category":[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\/1363","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1363&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sea-point\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[18.37699,-33.92186]}},{"type":"Feature","properties":{"id":1241,"name":"Serpentine along Hayward fault","description":"

Masses of ophiolites, serpentinized mafic material that are remnants of ancient oceanic crust, outcrop along the Hayward fault zone. Photo ID 712<\/p>\n

Photograph: David Manaker<\/p>\n","modified":"2018-09-04T13:23:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Serpentine-along-Hayward-fault-768x513.jpg","taxonomy":{"webmapp_category":[220,234]},"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\/1241","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1241&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/serpentine-along-hayward-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.178909,37.805243]}},{"type":"Feature","properties":{"id":2208,"name":"Sierra Estrella Epidote + Quartz Rock","description":"

Epidote + quartz rock in a small, highly metasomatized rock unit in the Sierra Estrella Mountains. This unit has been mapped as a marble within the more pervasive gneiss of the Sierra Estrella, but extensive metasomatism has left dominantly calc-silicate rock comprised of grossular-andradite solid solution garnets, epidote, and wollastonite, among other minerals. Metasomatism was presumably due to intrusion of nearby pegmatites.
\nPhotoID766<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-09-04T13:22:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sierra-Estrella-Epidote-Quartz-Rock-768x576.jpg","taxonomy":{"webmapp_category":[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\/2208","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2208&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sierra-estrella-epidote-quartz-rock\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.26683,33.214]}},{"type":"Feature","properties":{"id":2210,"name":"Sierra Estrella Garnet","description":"

Grossular-andradite solid solution garnet within a calc-silicate pod that was metasomatized by the Sierra Estrella pegmatites.
\nPhotoID767<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-09-04T11:23:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sierra-Estrella-Garnet-768x576.jpg","taxonomy":{"webmapp_category":[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\/2210","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2210&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sierra-estrella-garnet\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.26681,33.21417]}},{"type":"Feature","properties":{"id":2045,"name":"Sillimanite nodules","description":"

Sillimanite nodules in the migmatites of Punta Ainu. High Grade Metamorphic Complex of the Variscan belt in Sardinia. Photo ID 634<\/p>\n

Photograph: R. Carosi – Unipi<\/p>\n

Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-09-04T11:38:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sillimanite-nodules-768x516.jpg","taxonomy":{"webmapp_category":[230,234]},"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\/2045","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2045&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sillimanite-nodules\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.738461,40.69532]}},{"type":"Feature","properties":{"id":6341,"name":"Sillimanite nodules, Punta Ainu, Sardinia","description":"

Sillimanite nodules in Variscan migmatites, Punta Ainu, Sardinia, Italy<\/p>\n

Photo by R. Carosi<\/p>\n","modified":"2019-01-28T13:17:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/sill-ottiolu-300x225.jpg","taxonomy":{"webmapp_category":[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\/6341","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6341&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sillimanite-nodules-punta-ainu-sardinia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.738252584375005,40.69513816034278]}},{"type":"Feature","properties":{"id":2190,"name":"Staurolite Porphyroblasts 1","description":"

Staurolite porphyroblasts in a Proterozoic metapelite.
\nPhotoID757<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-07-24T12:22:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Staurolite-Porphyroblasts-1-768x576.jpg","taxonomy":{"webmapp_category":[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\/2190","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2190&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/staurolite-porphyroblasts-1\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.27961,34.2766]}},{"type":"Feature","properties":{"id":2192,"name":"Staurolite Porphyroblasts 2","description":"

Close up of staurolite porphyroblasts.
\nPhotoID758<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-10-10T18:38:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Staurolite-Porphyroblasts-2-768x576.jpg","taxonomy":{"webmapp_category":[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\/2192","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2192&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/staurolite-porphyroblasts-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.27972,34.27656]}},{"type":"Feature","properties":{"id":7311,"name":"Staurolite with garnet and tourmaline in quartz rich micaschist of Rayol le Canadel","description":"

Staurolite with garnet and tourmaline in quartz rich micaschist of Rayol le Canadel. The staurolite are locally concentrated whereas the tourmaline forms small spines and the garnet are smaller than other formation forming Le Canadel beach.<\/p>\n

Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-12-11T14:47:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/12\/PB010118-768x576.jpg","taxonomy":{"webmapp_category":[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\/7311","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7311&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/staurolite-with-garnet-and-tourmaline-in-quartz-rich-micaschist-of-rayol-le-canadel\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.461853425760296,43.1574227613566]}},{"type":"Feature","properties":{"id":1399,"name":"Tudela leucosomes","description":"

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

Photograph: Elena Druguet<\/p>\n

Reference: Druguet, E., Carreras, J. 2006. Analogue modelling of syntectonic leucosomes in migmatitic schists. Journal of Structural Geology 28, 1734-1747.<\/p>\n","modified":"2018-09-04T15:56:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Tudela-leucosomes-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1399","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1399&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tudela-leucosomes\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.294842317700386,42.3270494869462]}},{"type":"Feature","properties":{"id":1114,"name":"veins in gneiss","description":"

Archaean gneiss with complex vein system<\/p>\n

Photograph: Sebastian Schr\u00f6der and Nils Suhr<\/p>\n","modified":"2018-09-03T17:56:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/veins-in-gneiss-768x576.jpg","taxonomy":{"webmapp_category":[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\/1114","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1114&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/veins-in-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[30.734671,-27.033955]}},{"type":"Feature","properties":{"id":1614,"name":"Wadi Rahma dykes","description":"

Three generations of dykes in Wadi Rahma. Cordierite bearing gneiss (800Ma) at the mountain top is intruded by granite (610-615Ma) with synintrusive gently dipping mafic veins (red arrow). This is in turn invaded by composite dykes (green arrow, 570-580Ma) and steep dolerite dykes (blue arrow, 550 Ma). Marker indicates viewpoint of photographer, looking east
\nPhotoID362<\/p>\n

Photograph: Cees Passchier, Ghaleb Jarrar<\/p>\n","modified":"2018-09-04T13:28:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Wadi-Rahma-dykes-1-768x576.jpg","taxonomy":{"webmapp_category":[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\/1614","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1614&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/wadi-rahma-dykes-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[35.15118598937988,29.90788738182232]}},{"type":"Feature","properties":{"id":1821,"name":"Yarweelor Gneiss","description":"

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

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:37:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-2-768x502.jpg","taxonomy":{"webmapp_category":[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\/1821","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1821&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.53419493121339,-25.5681515857]}}]}