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A normal fault
PhotoID312<\/p>\n

Photograph: c.nicollet<\/p>\n","modified":"2018-06-15T10:18:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-normal-fault-Malaga-300x198.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1506","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1506&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-normal-fault-malaga\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.37715053558,36.736141388028194]}},{"type":"Feature","properties":{"id":1775,"name":"Bertibubba Gneiss","description":"

Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Leucocratic augengneiss with strong subvertical EW planar fabric, gently E-plunging stretching lineation and good dextral shear sense indicators on horizontal surfaces. Dominant D1, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite.
\nPhotoID473<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:52:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-768x503.jpg","taxonomy":{"webmapp_category":[232,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1775","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1775&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.575333,-25.609167]}},{"type":"Feature","properties":{"id":1779,"name":"Bertibubba gneiss","description":"

Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Leucocratic augengneiss with strong subvertical planar fabric and gently E-plunging stretching lineation. Dominant D1-deformation, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite; it shows a strong EW foliation, and good dextral shear sense indicators on horizontal surfaces. Weakly deformed pegmatite veins probably belong to the Moorarie granites (1830-1780 Ma)
\nPhotoID474<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:45:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-gneiss-768x501.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1779","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1779&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57562267857361,-25.6091573251]}},{"type":"Feature","properties":{"id":1781,"name":"Bertibubba Gneiss","description":"

Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Augengneiss with strong steeply NNW-dipping foliation and subhorizontal lineation with mantled porphyroclasts that indicate dextral shear sense; dominant D1-deformation, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite. Width of view 30 cm
\nPhotoID475<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:46:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[232,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1781","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1781&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.573003,-25.593833]}},{"type":"Feature","properties":{"id":1807,"name":"Camel Hills folded metapelite","description":"

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

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T16:14:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Camel-Hills-folded-metapelite-196x300.jpg","taxonomy":{"webmapp_category":[229,232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1807","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1807&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/camel-hills-folded-metapelite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.384,-25.601167]}},{"type":"Feature","properties":{"id":1628,"name":"civita di bagnoregio","description":"

ghost town built on a pyroclastic deposit.
PhotoID373<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:23:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/civita-di-bagnoregio-768x576.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1628","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1628&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/civita-di-bagnoregio\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[12.105817794799805,42.62243364300101]}},{"type":"Feature","properties":{"id":1578,"name":"CONTACT FELSIC- MAFIC GRANULITE","description":"

CONTACT BETWEEN FELSIC AND MAFIC GRANULITE.
Mylonitized contact between Garnet-bearing felsic granulite and gabbroic granulite of Permian age. Shear bands in the felsic portion indicate sinistral shear sense (base of photo: 50 cm)
PhotoID343<\/p>\n

Photograph: Ivan Zibra<\/p>\n

Reference: Zibra I, Kruhl JH, Braga R (2010). Late Palaeozoic deformation of post-Variscan lower crust: shear zone widening due to strain localization during retrograde shearing. Int J Earth Sci (Geol Rundsch) DOI 10.1007\/s00531-009-0441-5<\/p>\n","modified":"2018-06-15T10:18:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/CONTACT-FELSIC-MAFIC-GRANULITE-768x576.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1578","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1578&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/contact-felsic-mafic-granulite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.211220741271973,42.317998952837506]}},{"type":"Feature","properties":{"id":1789,"name":"Double stretching lineations","description":"

Vertical E-W trending foliation surface of Yarweelor bi-granite gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga) showing two lineations: one stretching lineation (vague striping) plunging gently (14\u00b0) to the east (left) and one biotite mineral lineation plunging steeply ( 60\u00b0) to the east (left). The latter lineation is parallel to elliptical aggregates of biotite which may represent pseudomorphs after another mineral (garnet?). In that case, this unknown mineral must have predated the steep lineation, which would therefore be the younger one of the two. The gently lineation is interpreted as D1: the steep one as D2. The D1-lineation is best visible at the top and bottom of the photograph. Vertical outcrop surface. The two lineations are thought to represent the two phases of activity of the Erabiddy shear zone.<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:10:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Double-stretching-lineations-768x502.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1789","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1789&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/double-stretching-lineations\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381667,-25.585667]}},{"type":"Feature","properties":{"id":2242,"name":"Elba Quartzite","description":"

Base of Elba Quartzite, Clear Creek, Raft River Mountains, Idaho-Utah
\nPhotoID786<\/p>\n

Photograph: Elizabeth L. Miller<\/p>\n","modified":"2018-10-10T18:34:14","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Elba-Quartzite-768x1033.jpg","taxonomy":{"webmapp_category":[232,230,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2242","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2242&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/elba-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-113.328952789,41.95572429954907]}},{"type":"Feature","properties":{"id":1602,"name":"Fold mullions","description":"

Classic locality resolving the problem of strong lineation and folds parallel to the movement on the Moine Thrust. These are sheath folds. Oykel Bridge
PhotoID357<\/p>\n

Photograph: Jim Talbot<\/p>\n

Reference: More photos at: http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Localities\/Sheath.html#Oykell<\/p>\n","modified":"2018-06-15T10:18:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fold-mullions-768x493.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1602","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1602&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fold-mullions\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.730087,57.967111]}},{"type":"Feature","properties":{"id":1670,"name":"Kyanite crystals","description":"

Posada. Kyanite crystals in a quarz vein
PhotoID399<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:19:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kyanite-crystals-768x576.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1670","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1670&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kyanite-crystals\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.625997543334961,40.650103777363256]}},{"type":"Feature","properties":{"id":1102,"name":"Linear fabric in orthogneiss","description":"

Constrictional fabric seen in the XY plane (foliation plane). Photo ID 709<\/p>\n

Photograph: Patrice Rey<\/p>\n","modified":"2018-09-04T11:24:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Linear-fabric-in-orthogneiss-768x576.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1102","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1102&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-fabric-in-orthogneiss\/","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":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":2128,"name":"Linear fabric in orthogneiss","description":"

Constrictional fabric in the core of the Caroux dome in an Ordovician orthogneiss. Photo ID 708<\/p>\n

Photograph: Patrice Rey<\/p>\n","modified":"2018-06-28T14:32:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Linear-fabric-in-orthogneiss-2-768x576.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2128","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2128&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-fabric-in-orthogneiss-3\/","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":2122,"name":"Linear fabric in rhyolite","description":"

Steeply dipping constrictional fabric in 3.3 Ga old Wyman formation (Rhyolite, Warrawoona Syncline). Photo ID 705<\/p>\n

Photograph: Patrice Rey<\/p>\n","modified":"2018-06-28T14:30:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Linear-fabric-in-rhyolite-768x576.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2122","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2122&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-fabric-in-rhyolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.83571290969849,-21.3249782343]}},{"type":"Feature","properties":{"id":7200,"name":"Lochsite","description":"

The Glarus Thrust: In Switzerland\u2019s most famous geological outcrop at the Lochsite, 250-300 million-year-old Verrucano rocks rest on younger, 35-50 million-year-old Flysch rocks. Since the 19th century, fundamental insights into the formation of the Alps have been gained here. Specifically, scientists understood the way mountains form as a result of overthrusts. Previously, earth scientists had assumed that mountains were formed due to the shrinkage of the earth in connection with the mantle cooling.<\/p>\n

After visiting the Lochsite, it is clear to everyone that \u201calpine folding\u201d never happened!<\/p>\n","modified":"2019-10-02T12:47:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Strukturen_Lochsite_3D_Buckingham-768x543.jpg","taxonomy":{"webmapp_category":[220,224,230,231]},"accessibility":{"mobility":{"check":true,"description":"

Access by public transport<\/strong>: Train to “Glarus S\u00fcd”<\/strong> and after bus to “Wart”<\/strong> (8762 Glarus S\u00fcd)<\/span><\/p>\n

Public transport Switzerland https:\/\/www.sbb.ch\/en\/home.html<\/a><\/p>\n

Access by car<\/strong> from Glarus S\u00fcd: follow Sernftalstrasse in direction ELm, after 6 minutes you will see the installation of “Lochsite” and a parking lot<\/p>\n"},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"related_url":["https:\/\/unesco-sardona.ch\/erlebnis\/lochsite"],"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7200","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7200&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/lochsite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"+41 81 723 59 20","contact:email":"info@unesco-sardona.ch","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.091614036983856,46.997288304920126]}},{"type":"Feature","properties":{"id":1656,"name":"Melfi","description":"

Hauyne crystal
PhotoID391<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:19:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Melfi-768x572.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1656","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1656&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/melfi\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[15.659079551696777,40.99523697414175]}},{"type":"Feature","properties":{"id":1518,"name":"Mini graben of Gandaillat","description":"

The mini graben of Gandaillat is a reduced version of the rift of Limagne
PhotoID287<\/p>\n

Photograph: <\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/Figures\/Limagne\/Limagne.html<\/p>\n","modified":"2018-06-15T10:21:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mini-graben-of-Gandaillat-768x501.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1518","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1518&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mini-graben-of-gandaillat\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.154771327972412,45.773420143839864]}},{"type":"Feature","properties":{"id":1558,"name":"Mitre fold","description":"

Tight fold, known as Mitre fold. Belleville, New Brunswick, Canada
PhotoID334<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-15T10:22:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mitre-fold-199x300.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1558","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1558&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mitre-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-67.704628,46.203814]}},{"type":"Feature","properties":{"id":1185,"name":"Mullions at Dedenborn, Germany","description":"

Small roadside outcrop near the village of Dedenborn in the N-Eifel, the type example of mullions.<\/p>\n

The outcrop is situated in the steep to overturned limb of a regional series of upright folds with well-developed axial planar cleavage. The rocks consist of alternating psammite-pelite layers.<\/p>\n

Janos Urai, G. Spaeth, Wouter van der Zee, Christoph Hilgers (2001). Evolution of mullion (boudin) structures in the Variscan of the Ardennes and Eifel. Journal of the Virtual Explorer online, 3,1
\n*Ilse Kenis, Janos Urai, Wouter van der Zee, Christoph Hilgers, Manuel Sintubin (2005). Rheology of fine-grained siliciclastic rocks in the middle crust \u2013 evidence from a combined structural and numerical analysis. Earth and Planetary Science Letters, 233,351-360<\/p>\n

http:\/\/www.ged.rwth-aachen.de\/index.php?cat=Research&subcat=Fractures_and_veins&page=Mullions_and_Boudins PhotoID156<\/p>\n

Photograph: Heijn van Gent<\/p>\n","modified":"2018-06-28T18:05:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mullions-at-Dedenborn-Germany-225x300.jpg","taxonomy":{"webmapp_category":[220,232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1185","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1185&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mullions-at-dedenborn-germany\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.352341,50.581511]}},{"type":"Feature","properties":{"id":1588,"name":"Niguelas normal fault","description":"

This striated fault scarp belongs to the NW-SE-trending Pad\u00edl-Nig\u00fcelas late Neogene to present high-angle extensional front, dipping to the SW and separating the Sierra Nevada uplifted metamorphic core complex to the E and the Pad\u00fal Cenozoic basin to the E. <\/p>\n

Photograph: Miguel Doblas <\/p>\n

Reference: Doblas, M. & Oyarzun, R., 1989, Geology, 17, 430-433; Doblas, M., et al., 1997, Journal of Structural Geology, 19, 2, 159-170<\/p>\n","modified":"2018-06-15T10:18:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Niguelas-normal-fault-768x512.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1588","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1588&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/niguelas-normal-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-3.536802,36.982455]}},{"type":"Feature","properties":{"id":1809,"name":"Pencil cleavage","description":"

Pencil cleavage in wm-chl phyllite. Camel Hills metasediments, (ca. 2000 Ma).<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:23:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pencil-cleavage-768x502.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1809","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1809&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pencil-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.654667,-25.533]}},{"type":"Feature","properties":{"id":1512,"name":"Penrhyn slate","description":"

Fence of Ordovician slate from the Penrhyn quarries. The light-coloured spots, up to five cm by two cm on the cleavage, and <1cm thick, were spherical spots in mud before the rocks deformed during the Caledonian collision.
PhotoID318<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-15T10:18:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Penrhyn-slate-200x300.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1512","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1512&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/penrhyn-slate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.045215,53.158315]}},{"type":"Feature","properties":{"id":1570,"name":"Rodaderos non-planar slickensides","description":"

Curious curved slickenside fault surface with striations, which seems to be folded. Possibly, a granite intruded into soft sediment along a fault surface which was folded in the still liquid granite to the present shape
\nPhotoID340<\/p>\n

Photograph:<\/p>\n

Reference: Spencer 1999. Geologic continuous casting below continental and deep-sea detachment faults and at the striated extrusion of Sacsayhuam\u00e1n, Peru. Geology 27, 327-330<\/p>\n","modified":"2018-06-28T18:05:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rodaderos-non-planar-slickensides-300x225.jpg","taxonomy":{"webmapp_category":[220,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1570","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1570&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rodaderos-non-planar-slickensides\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-71.9820034504,-13.5067277437]}},{"type":"Feature","properties":{"id":1546,"name":"Rootless fold","description":"

Rootless concentric folds of dolomite in slate. Belvidere, NJ.
PhotoID327<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-15T10:18:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rootless-fold-768x524.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1546","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1546&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rootless-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-75.094156,40.835411]}},{"type":"Feature","properties":{"id":1644,"name":"Rosignano cpx crystals","description":"

Clinopyroxene megacrystals in the Rosignano Gabbro (Theralite)
PhotoID384<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:19:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rosignano-cpx-crystals-768x576.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1644","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1644&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rosignano-cpx-crystals\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.435638427734375,43.43696596521823]}},{"type":"Feature","properties":{"id":1646,"name":"San Venanzo","description":"

Venanzite (Leucite Olivin Melilitite)<\/p>\n

Pegmatite and venanzite lava flow
PhotoID385<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:19:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/San-Venanzo-768x1030.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1646","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1646&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/san-venanzo\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[12.296973466873169,42.79518415471335]}},{"type":"Feature","properties":{"id":1594,"name":"Sheath fold","description":"

Curved lineation around nose of a sheath fold. Skullomie Cove, near Tongue, Scotland
PhotoID353<\/p>\n

Photograph: Jim Talbot<\/p>\n

Reference: Holdsworth, R. E. 1989. The geology and structural evolution of a Caledonian fold and ductile thrust zone, Kyle of Tongue region, Sutherland, northern Scotland. Journal of the Geological Society of London 146, 809-823. See more photos at http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Localities\/Sheath.html<\/p>\n","modified":"2018-06-15T10:18:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-202x300.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1594","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1594&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.37829378441,58.51870159962132]}},{"type":"Feature","properties":{"id":1674,"name":"Sideling Hill roadcut","description":"

mega-syncline in folded Devonian-Mississipian. A local exhibition center explains the structure.<\/p>\n

See:
\nhttp:\/\/www.mgs.md.gov\/esic\/features\/sidel.html<\/p>\n

PhotoID405<\/p>\n

Photograph:<\/p>\n","modified":"2018-12-13T17:26:44","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1674","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1674&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sideling-hill-roadcut\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-78.283752,39.719189]}},{"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":1576,"name":"Slickenslide fault plane","description":"

A slickenside fault plane in a cataclasite. It is exposed in the core zone of the NASZ, defining the border between the Carboniferous Ploun\u00e9our-M\u00e9nez granite in the south and the Silurian-devonian Plougastel Formation in the north.
\nPhotoID342<\/p>\n

Photograph: Isaac Berwouts<\/p>\n","modified":"2018-09-04T11:45:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Slickenslide-fault-plane-768x583.jpg","taxonomy":{"webmapp_category":[220,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1576","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1576&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/slickenslide-fault-plane\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-3.82992625237,48.49632099933981]}},{"type":"Feature","properties":{"id":6333,"name":"Slikenlines on Zuccale Fault, Elba Isand","description":"

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Strongly mylonitised vein-quartzite in the Erabiddy shear zone, with steeply south-dipping foliation and very strong subvertical D2-stretching lineation<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T13:05:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/stretching-lineation-in-quartzite-768x500.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1791","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1791&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/stretching-lineation-in-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381,-25.6015]}},{"type":"Feature","properties":{"id":2120,"name":"Warrawoona rod schists","description":"

Mafic schists and cherts with a strong, steeply dipping, linear fabrics. Geologits for scale: Pascal Philippot, Florence Lehebel, Patrice Rey and Nicolas Th\u00e9baud. Photo ID 704<\/p>\n

Photograph: Joel Brugger (2003)<\/p>\n","modified":"2018-06-28T13:35:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Warrawoona-rod-schists-768x576.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2120","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2120&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/warrawoona-rod-schists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.85069563865659,-21.3110617816]}}]}