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Papeschi<\/p>\n<p>Reference: RAU A., TONGIORGI M. 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Usually andalusite grows during a HT-LP metamorphic event after staurolite. PhotoID157<\/p>\n<p>Photograph: R. 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(Find it on ngmdb.usgs.gov)<\/p>\n","modified":"2018-09-04T15:53:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cleator-Exhalites-768x576.jpg","taxonomy":{"webmapp_category":[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\/2188","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2188&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cleator-exhalites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.2131,34.27324]}},{"type":"Feature","properties":{"id":1343,"name":"COLUMNAR JOINTING IN BASALT","description":"<p>Basalt columns and columnar joints converge upwards in a Tertiary volcanic vent with an age about 14.07\u00b10.37 Ma (K-Ar age, whole rock), north of Jijiazhuang village in the Chnagle area, Shandong province, China. 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Photo ID 657<\/p>\n<p>Photograph: S. 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The so-called stone mushrooms<br \/>\nDronero-Cuneo<\/p>\n<p>Colonne di erosione, dette funghi di pietra<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-12-22T10:26:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/erosion-protected-columns-768x576.jpg","taxonomy":{"webmapp_category":[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\/1915","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1915&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/erosion-protected-columns\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.383842468261719,44.48970924356387]}},{"type":"Feature","properties":{"id":1636,"name":"Finero peridotite","description":"<p>Finero Peridotite (Olivine, Phlogopite, Cr-Diopside); Lithosferic mantel afffected by metasomatism.<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T12:28:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Finero-peridotite-768x576.jpg","taxonomy":{"webmapp_category":[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\/1636","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1636&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/finero-peridotite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.536205291748047,46.10192339248404]}},{"type":"Feature","properties":{"id":1941,"name":"flattened xenoliths","description":"<p>Ca-alkaline granitoid with flattened xenoliths. Rio Urubu<br \/>\nPhotoID559<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T15:51:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/flattened-xenoliths-768x492.jpg","taxonomy":{"webmapp_category":[232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1941","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1941&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/flattened-xenoliths\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-60.488888,2.4825]}},{"type":"Feature","properties":{"id":1961,"name":"Fluvial Channel, Trias","description":"<p>Arenitic level in metaconglomerates: probably a fluvial channel in an alluvial fan or braided river systems.<\/p>\n<p>Anageniti Fm. (Verrucano)<br \/>\nAnageniti Grossolane Mb.<br \/>\nPhotoID570<\/p>\n<p>Photograph: S. Papeschi<\/p>\n","modified":"2018-06-30T12:20:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fluvial-Channel-Trias-768x576.jpg","taxonomy":{"webmapp_category":[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\/1961","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1961&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fluvial-channel-trias\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.568614304065704,43.734718438850855]}},{"type":"Feature","properties":{"id":6417,"name":"Flysch Monte Cassio","description":"<p>Impressively parallel bedded basin-plain deposits mainly consisting of resedimented pelagic and hemipelagic biogenic oozes; subordinate, fine-grained sandstone forms darker and considerably thinner, more resistent units. These sediments, which are interpreted as a trench-fill, are thought to be a classic example of stacked megaturbidites triggered by seismic activity (seismoturbidites of Mutti et al., 1984). Thin-bedded sandstones and dark mudstones represent the background sedimentationof the basin plain.<br \/>\nMonte Cassio Flysch, late Cretaceous, northern Appennines<\/p>\n","modified":"2019-01-29T17:15:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/2016-10-29-Flysch-Cassio_02-768x514.jpg","taxonomy":{"webmapp_category":[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\/6417","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6417&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/flysch-monte-cassio\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.094345457668965,44.58982326981736]}},{"type":"Feature","properties":{"id":1100,"name":"Fold interference pattern","description":"<p>Refolded isoclinal F1 folds in cherty metalimetsones of the Alpi Apuane metamorphic complex (Northern Appennines, Italy)<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:52:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fold-interference-pattern-768x532.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1100","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1100&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fold-interference-pattern\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.214435,44.122228]}},{"type":"Feature","properties":{"id":1153,"name":"folded metasediments","description":"<p>Typical example of the S-shaped folds with many ptygmatically folded quartz veins&lt;br \/&gt;. PhotoID111<\/p>\n<p>Photograph: Paul Bons, T\u00fcbingen<\/p>\n","modified":"2018-10-10T18:58:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/folded-metasediments-300x225.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1153","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1153&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-metasediments\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.315942585468292,42.319467553072116]}},{"type":"Feature","properties":{"id":1225,"name":"Folded Ribbon Cherts","description":"<p>Spectacularly folded ribbon cherts, Monterey formation, part of accreted material from the extinct subduction zone of the Farallon plate. Photo ID 711<\/p>\n<p>Photograph: David Manaker<\/p>\n","modified":"2018-10-10T18:44:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-Ribbon-Cherts-768x509.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1225","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1225&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-ribbon-cherts\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.497993,37.82822]}},{"type":"Feature","properties":{"id":1235,"name":"Folding in a ductile shear zone","description":"<p>Folded layering in the Deh Vazir ductile shear zone, Iran. This is a structure as described by vanderPluijm and Marshak (1997); folding accompanies shearing and occurs where a sequence of interlayered weak and strong rock layers is caught between the opposing boundaries of a shear zone. In such circumstances, displacement of the rigid shear zone boundaries with respect to each other causes the intervening rock to fold. The Deh Vazir shear zone mainly consists of foliated and lineated marble and greenschist. Metamorphic grade is generally low grade (Sarkarinejad et al., 2010). The photograph shows how strong marble layers act as a shear zone boundary and weak greenschist layers between the marble layers have been subject of shearing. Location: Deh Vazir shear zone in the Southwest of the HP-LT Sanandaj-Sirjan metamorphic belt, Iran. PhotoID190<\/p>\n<p>Sarkarinejad, K., Samani, B., Faghih, A., Grasemann, B., Moradipoor, M., 2010. Implications of strain and vorticity of flow analyses to interpret the kinematics of an oblique convergence event (Zagros Mountains, Iran). Journal of Asian Earth Sciences 38, 34-43<\/p>\n<p>van der Pluijm, B.A., Marshak, S., 1997. Earth Structure: an Introduction to Structural Geology and Tectonics, McGraw-Hill, New York.<\/p>\n<p>This is a photograph of the month in the Journal of Structural Geology<\/p>\n<p>Photograph: Babak Samani<\/p>\n","modified":"2018-10-10T18:54:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folding-in-a-ductile-shear-zone-768x576.jpg","taxonomy":{"webmapp_category":[229,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1235","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1235&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folding-in-a-ductile-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.793333,29.342222]}},{"type":"Feature","properties":{"id":2037,"name":"Folds in comendites","description":"<p>Mesoscopic folds in S. Pietro Island comendite lava flows. Locality Cala Fico, Carloforte. Photo ID 629<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: Cioni R. &amp; Funedda A. -2005- Structural geology of crystal-rich, silicic lava flows: a case study from San Pietro Island (Sardinia, Italy) &#8211; in M. Manga and G. Ventura (Eds.) Kinematics and dynamics of lava flows, GSA Special Paper 396, 1-14.<\/p>\n","modified":"2018-09-04T11:40:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-comendites-300x202.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2037","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2037&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-in-comendites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.227013,39.15635]}},{"type":"Feature","properties":{"id":6894,"name":"Foliated gabbro cross cut by an amphibole rich-vein","description":"<p>Foliated gabbro cross cut by an amphibole (hornblende) rich-vein (Internal Luguride Units), Bonassola, Italy<\/p>\n<p>For more info see Geological Field Trips and Maps, Societ\u00e0 Geologica Italiana:<\/p>\n<p>https:\/\/gftm.socgeol.it\/296\/issue-13\/the-ligurian-ophiolites-a-journey-through-the-building-and-evolution-of-slow-spreading-oceanic-lithosphere.html<\/p>\n","modified":"2019-06-07T16:47:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/04\/IMG_3016-1-768x576.jpg","taxonomy":{"webmapp_category":[219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6894","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6894&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/foliated-gabbro-cross-cut-by-an-amphibole-rich-vein\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.584197416671714,44.180837602423956]}},{"type":"Feature","properties":{"id":2224,"name":"Fossil Tree","description":"<p>Fossil tree trapped in lava flows. 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On the picture, you&#8217;ll see on the left, Garlaban and its famous fold. On the right, You&#8217;ll see the Sainte-Baume with a change in dip.<\/p>\n<div id=\"attachment_6272\" style=\"width: 1034px\" class=\"wp-caption alignnone\"><img class=\"size-large wp-image-6272\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Panorama_Garlaban_Sainte-Baume-1024x252.jpg\" alt=\"\" width=\"1024\" height=\"252\" srcset=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Panorama_Garlaban_Sainte-Baume-1024x252.jpg 1024w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Panorama_Garlaban_Sainte-Baume-300x74.jpg 300w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Panorama_Garlaban_Sainte-Baume-768x189.jpg 768w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Panorama_Garlaban_Sainte-Baume-1080x266.jpg 1080w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><p class=\"wp-caption-text\">Anne-Sabine Grosjean and Baptiste 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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":1683,"name":"Neptunian dyke","description":"<p>In the M. Sagro area the Marmi carbonate platform is cut by fractures, often karstified. In the Castelbaito quarry a wide neptunian dyke filled by carbonate and cherty clasts lies in a marly-matrix of Dogger age. The fill of this mega-fracture indicates a strong tectonic activity during the Middle Jurassic. The height of the cut is about 7-8 m. From Campocecina, northern Alpi Apuane.<\/p>\n<p>Boccaletti M., Gosso G., Moratti G., (1981): Indizi di paleocarsismo nel Marmo delle Alpi Apuane Settentrionali. Rend. Soc. Geol. It., 4, 315-316<\/p>\n<p>Coli M., Fazzuoli M. (1994): New data on the lithostatigraphy of the Morlungo Monte Sagro area, a preliminary data. Mem. Soc. Geol. It., 48, 67-70<\/p>\n<p>Molli G., Meccheri M. (2008): Eredit\u00e0 paleotettoniche e stili di riattivazione a livelli medio-crostali: un esempio dalle Alpi Apuane occidentali. Rend. Soc. Geol. It., 3, 564-565<\/p>\n<p>PhotoID414<\/p>\n<p>Photograph: D. 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Carosi<\/p>\n","modified":"2018-06-30T12:27:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Overturned-pillow-lavas-768x516.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1420","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1420&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/overturned-pillow-lavas\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.202813,42.806814]}},{"type":"Feature","properties":{"id":1919,"name":"paleo river","description":"<p>In the background: Paleo-riverbed with tractive structures (megaripples and ripples). 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Cuadernos de Geologica Iberica, v. 10, p. 9-30<\/p>\n<p>Photograph: F.Milazzo<\/p>\n","modified":"2018-06-28T18:14:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/paleo-river-768x575.jpg","taxonomy":{"webmapp_category":[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\/1919","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1919&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/paleo-river\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.701537132263184,42.1555457945941]}},{"type":"Feature","properties":{"id":1664,"name":"pegmatite vein","description":"<p>Tourmaline bearing pegmatite vein. 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This is the so called Geotimes Outcrop. 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PhotoID194<\/p>\n<p>Photograph: Chiara Montomoli<\/p>\n","modified":"2018-10-10T18:54:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Tibetan-Detachment-768x576.jpg","taxonomy":{"webmapp_category":[219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1243","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1243&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-tibetan-detachment\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.739616,28.189158]}},{"type":"Feature","properties":{"id":1281,"name":"South-verging folds (Samaria Gorge)","description":"<p>Metre-scale south-verging folds in the Plattenkalk nappe. 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Papeschi<\/p>\n","modified":"2018-07-24T12:27:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Subaerial-deposits-of-Vulcanello-768x1023.jpg","taxonomy":{"webmapp_category":[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\/1359","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1359&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/subaerial-deposits-of-vulcanello\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.961297512054443,38.42602947616809]}},{"type":"Feature","properties":{"id":1311,"name":"Sublimated Sulphur","description":"<p>Sublimated Sulphur in fumaroles. 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Papeschi<\/p>\n","modified":"2019-02-22T13:16:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sublimated-Sulphur-768x576.jpg","taxonomy":{"webmapp_category":[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\/1311","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1311&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sublimated-sulphur\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.961276054382324,38.40622016528014]}},{"type":"Feature","properties":{"id":1313,"name":"Sulphur and Borates in fumaroles","description":"<p>Minerals precipitated from the gas rising from fumaroles. Photo ID 647<\/p>\n<p>Photograph: S. Papeschi<\/p>\n","modified":"2018-06-30T13:00:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sulphur-and-Borates-in-fumaroles-768x576.jpg","taxonomy":{"webmapp_category":[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\/1313","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1313&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sulphur-and-borates-in-fumaroles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.96063232421875,38.40605201718267]}},{"type":"Feature","properties":{"id":1905,"name":"Sulphur crystals","description":"<p>Sulphur crystals, Larderello geotermal field.<\/p>\n<p>Larderello<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T19:32:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sulphur-crystals-768x576.jpg","taxonomy":{"webmapp_category":[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\/1905","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1905&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sulphur-crystals\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.7940673828125,43.17463764270234]}},{"type":"Feature","properties":{"id":7005,"name":"syntectonic granite sheets","description":"<div id=\"attachment_7002\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img class=\"size-medium wp-image-7002\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-300x225.jpg 300w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-768x576.jpg 768w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-1024x768.jpg 1024w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-510x382.jpg 510w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p class=\"wp-caption-text\">Syntectonic granite sheets Salknappen, Antarctica.<\/p><\/div>\n<div id=\"attachment_7006\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img class=\"size-medium wp-image-7006\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-300x225.jpg 300w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-768x576.jpg 768w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-1024x768.jpg 1024w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-510x382.jpg 510w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p class=\"wp-caption-text\">Syntectonic granite sheets at Salknappen, Antarctica<\/p><\/div>\n<p>Steeply dipping discordant pegmatite veins are crosscut by layering parallel granite sheets along which extensional top to South syntectonic displacement has occurred at ~490Ma. Person at bottom for scale. Extensional shears parallel to the pegmatite veins are evident.<\/p>\n","modified":"2019-06-07T22:53:34","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[224,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7005","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7005&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/syntectonic-granite-sheets\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.00582449859985,-72.323492195148]}},{"type":"Feature","properties":{"id":1496,"name":"The K\/T boundary in the Basque coast.","description":"<p>The Cretaceous-Tertiary boundary is well exposed on the beach of Bidart (4km south of Biarritz). A 20cm thick Iridium rich level of black shales separates the grey Maestrichian limestone (on the bottom) and the white Danian limestones (on the top). The K-T transition seems to be continuous. PhotoID309<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/limiteK-T\/KT.html<\/p>\n","modified":"2018-06-28T14:38:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/The-KT-boundary-in-the-Basque-coast-768x576.jpg","taxonomy":{"webmapp_category":[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\/1496","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1496&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/the-k-t-boundary-in-the-basque-coast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-1.58585071564,43.450247382932425]}},{"type":"Feature","properties":{"id":1498,"name":"The pillows lavas of the Collet Vert","description":"<p>In the Collet Vert, the cliff of 200m high is composed of the stacking of pillows lavas. Ophiolite Massif of Chenaillet<br \/>\nPhotoID310<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/chenaillet\/chenaillet.html<\/p>\n","modified":"2018-07-24T11:10:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/The-pillows-lavas-of-the-Collet-Vert-768x530.jpg","taxonomy":{"webmapp_category":[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\/1498","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1498&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/the-pillows-lavas-of-the-collet-vert\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.750755310055796,44.90974370958705]}},{"type":"Feature","properties":{"id":6678,"name":"The Upper Eocene-Oligocene Montepiano Marl and Ranzano Sandstone formations. 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This valley,\u00a0 is commonly interpreted as a submarine fan-valley.<\/p>\n<p>&nbsp;<\/p>\n","modified":"2019-03-01T14:50:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/03\/DSC_1231dis-768x514.jpg","taxonomy":{"webmapp_category":[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\/6678","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6678&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/the-upper-eocene-oligocene-montepiano-marl-and-ranzano-sandstone-formations-val-mozzola-parma-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.828322089980475,44.592639987380664]}},{"type":"Feature","properties":{"id":1355,"name":"Theespruit pluton","description":"<p>Intrusive breccias of the ca. 3.45 Ga Theespruit pluton into amphibolites from the Lower Onverwacht Group of the Barberton Greenstone Belt. Photo on an horizontal surface (YZ plane); on a vertical plane the breccia is stretched, probably by the ca. 3.2 Ga deformation.<\/p>\n<p>Kisters, A.F.M., Anhaeusser, C.R., 1995. Emplacement features of Archaean TTG plutons along the Southern margin of the Barberton greenstone belt, South Africa. Precamb.Res. 75, 1-15.<br \/>\nPhotoID260<\/p>\n<p>Photograph: JF Moyen<\/p>\n","modified":"2018-06-28T14:44:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Theespruit-pluton-768x576.jpg","taxonomy":{"webmapp_category":[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\/1355","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1355&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/theespruit-pluton\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[30.80072,-26.04062]}},{"type":"Feature","properties":{"id":6607,"name":"Tilted layers of Dolomia and Limestone. 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Near Monte Cimone Northern Appenninies. Aquitanian- Burdigaglian (Miocene)<br \/>\nPhotoID813<\/p>\n<p>Photograph: Marco Mazzotta<\/p>\n<p>Reference: Carta Geologica D?italia. Foglio 236 Pavullo nel Frignano. 1:50.000<\/p>\n","modified":"2018-06-30T11:37:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Torrente-Scoltenna-Sandstone-768x515.jpg","taxonomy":{"webmapp_category":[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\/2288","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2288&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/torrente-scoltenna-sandstone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.720338821411133,44.22232188545298]}},{"type":"Feature","properties":{"id":2290,"name":"Torrente Scoltenna Sandstone","description":"<p>Cervarola Group. Near Monte Cimone Northern Appenninies. Aquitanian- Burdigaglian (Miocene) PhotoID814<\/p>\n<p>Photograph: Marco Mazzotta<\/p>\n<p>Reference: Carta Geologica D?italia. Foglio 236 Pavullo nel Frignano. 1:50.000<\/p>\n","modified":"2018-07-24T11:43:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Torrente-Scoltenna-Sandstone-1-768x515.jpg","taxonomy":{"webmapp_category":[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\/2290","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2290&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/torrente-scoltenna-sandstone-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.720338821411133,44.22232188545298]}},{"type":"Feature","properties":{"id":6827,"name":"Torrente Scoltenna Sandstones &#8211; Cervarola Unit &#8211; Middle Miocene","description":"","modified":"2019-04-13T08:58:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/04\/2017-06-12-Pian-Del-Falco_02-768x514.jpg","taxonomy":{"webmapp_category":[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\/6827","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6827&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/torrente-scoltenna-sandstones-cervarola-unit-middle-miocene\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.763602564276084,44.22140925894826]}},{"type":"Feature","properties":{"id":6687,"name":"Tortonian sedimentary cycles on Fm. Licata (Southern Sicily)","description":"","modified":"2019-03-07T19:20:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/20150902_182015-768x461.jpg","taxonomy":{"webmapp_category":[235,219]},"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\/6687","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6687&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tortonian-sedimentary-cycles-on-fm-licata-southern-sicily\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.778549476349212,37.14735453586975]}},{"type":"Feature","properties":{"id":6475,"name":"Trassic conglomerate, Verrucano sequence, Monti Pisani","description":"<p>Bedding in Trassic conglomerate, Verrucano sequence, Monti Pisani, Italy<\/p>\n<p>Photo by Rodolfo Carosi<\/p>\n","modified":"2019-01-31T17:40:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Anageniti-grossolane-Verrucano-768x515.jpg","taxonomy":{"webmapp_category":[232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6475","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6475&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/trassic-conglomerate-verrucano-sequence-monti-pisani\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.560105667731477,43.73486265497749]}},{"type":"Feature","properties":{"id":7040,"name":"Travertine of the Huveaune source, France","description":"<p><img class=\"alignnone size-large wp-image-7041\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1024x768.jpg\" alt=\"\" width=\"1024\" height=\"768\" srcset=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1024x768.jpg 1024w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-300x225.jpg 300w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-768x576.jpg 768w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-510x382.jpg 510w, http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1080x810.jpg 1080w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/p>\n<p>Modern travertine of the Huveaune source in Sainte-Baume near Aubagne, France.<\/p>\n<p>Picture By Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-06-16T21:44:59","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-768x576.jpg","taxonomy":{"webmapp_category":[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\/7040","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7040&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/travertine-of-the-huveaune-source-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.764099,43.348645]}},{"type":"Feature","properties":{"id":1739,"name":"Turbidite deposits","description":"<p>The Turbidite deposits of the photo (Flysch of Solignano Fm.) consist of Maastrichtian alternations of sandstones and mudstones interbedded with marly limestones and silty marls.<br \/>\nThe Flysh of Solignano belongs to the Solignano Units (Ligure Domain )<br \/>\nPhotoID452<\/p>\n<p>Photograph: F.Milazzo<\/p>\n<p>Reference: 1983 D. Rio &amp; Villa G &#8211; I nannofossili calcarei del Cretacico superiore del Flysch di Solignano, media Val Taro &#8211; Appennino Settentrionale. Mem. Soc Geol. Padova , 36, 239-282; G. PLESI , L. BIANCHI , S. CHICCHI &amp; G. DANIELE THE LIGURIAN AND EMILIAN UNITS OF THE MIDDLE TARO VALLEY (NORTHERN APENNINES) AND THEIR STRUCTURAL EVOLUTION Atti Tic. Sc. Terra 36 (1993), 183-229; C1 &#8211; FONTANA D., STEFANI C., ZUFFA G.G. e TATEO F., 1990, Il Flysch di Solignano nel quadro dei Flysch ad Elmintoidi (Maastrichtiano inferiore, Appennino settentrionale: Giornale di Geologia, v. 52\/1-2, p.99-120. ZANZUCCHI G. (1967) &#8211; Osservazioni preliminari sulla tettonica della media Val di Taro (Carta Geologica 1:50.000 e sezioni). 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The Vale da<br \/>\nLua is well preserved and to keep this condition it is necessary to increase the information to the visitors about<br \/>\nthe rocks conditions formation (including depositional and sedimentary processes), once there is great confusion<br \/>\nby part of the public, and many believe in volcanic origin to the local rocks. It is important to emphasize in<br \/>\nwarning plates, the importance of the area preservation, the prohibition of getting rock samples and the general<br \/>\nmaintenance of the place. PhotoID801<\/p>\n<p>Photograph:<\/p>\n<p>Reference: Campos,J.E.G.; Monteiro,C.F.; Dardenne,M.A. 2005. S\u00e3o Miguel Conglomerate in the Vale da Lua valley, South of the Chapada dos Veadeiros Park, State of Goi\u00e1s, Brazil &#8211; Beautiful exotic scenario modeled by fluvial erosion. In: Winge,M.; Schobbenhaus,C.; Berbert-Born,M.; Queiroz,E.T.; Campos,D.A.; Souza,C.R.G. ; Fernandes,A.C.S. (Edit.) Geological and Palaeontological Sites of Brazil. 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Rivista Italiana di Paleontologia e Stratigrafia 115: 269-274.<\/p>\n","modified":"2018-12-24T00:53:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Variscan-unconformity-300x197.jpg","taxonomy":{"webmapp_category":[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\/2148","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2148&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/variscan-unconformity\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.5153,39.2969]}},{"type":"Feature","properties":{"id":2039,"name":"Vena del Gesso","description":"<p>Panoramic view showing the typical features of the Vena del Gesso monocline. The \u201cVena del Gesso\u201d represents one of the most significant and well areas where primary evaporites related to the Messinian Salinity Crisis of the Mediterranean widely crop out. (Montanari et al.2007. Geological Journal, DOI 10.1002\/gj.1085). Photo ID 630<\/p>\n<p>Photograph: Domenico Montanari<\/p>\n<p>Reference: Montanari et al. 2007. Geological Journal, DOI 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