{"type":"FeatureCollection","features":[{"type":"Feature","properties":{"id":1141,"name":"1944 quake fault","description":"

Outcrop of La Laja backthrust in Pleistocene gravels. A 7.4 magnitude earthquake on the fault destroyed the city of San Juan in 1944. PhotoID104<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-09-04T14:55:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/1944-quake-fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1141","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1141&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/1944-quake-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-68.4679341316,-31.3651621906]}},{"type":"Feature","properties":{"id":5985,"name":"A meso-scale faulted multi-detachment fold, Khabr area, Kerman, Iran","description":"

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

A meso-scale faulted multi-detachment fold, Khabr area, Kerman, Iran, Photo by Seyed Tohid Nabavi<\/p>\n","modified":"2018-12-12T15:07:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Picture1-1-768x434.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5985","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5985&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-meso-scale-faulted-multi-detachment-fold-khabr-area-kerman-iran\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[56.43751508107118,28.802959234513224]}},{"type":"Feature","properties":{"id":1494,"name":"A reverse fault – Djebel Akhdar","description":"

A reverse fault in the Djebel Akhdar – Oman<\/p>\n

PhotoID308<\/p>\n

Photograph: c.nicollet<\/p>\n","modified":"2018-09-03T17:45:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-reverse-fault-Djebel-Akhdar-768x462.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1494","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1494&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-reverse-fault-djebel-akhdar\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[57.398441433906555,23.19427475983768]}},{"type":"Feature","properties":{"id":1293,"name":"Arkitsa fault","description":"

One of the largest fresh fault surfaces in the world with very well preserved striations.<\/p>\n

Jackson J. & McKenzie D. (1999). DOI: 10.1016\/S0191-8141(98)00091-1
\nJones R.R. et al. (2009). DOI: 10.1130\/GES00216.1
\nResor P.G. & Meer V.E. (2009). DOI: 10.1016\/j.epsl.2009.10.010<\/p>\n

Photograph: Alex CHATZIPETROS<\/p>\n","modified":"2018-06-28T14:38:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Arkitsa-fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1293","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1293&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/arkitsa-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.00759732723236,38.732150592296996]}},{"type":"Feature","properties":{"id":1460,"name":"Arkitsa Fault","description":"

Segment of the Arkitsa Fault zone with corrugations and open tension fractures on the exposed fault surface.
\nPhotoID250<\/p>\n

Photograph: Sotiris Kokkalas<\/p>\n

Reference: Jones et al. (2009) Geosphere v.5, n.6, p. 1-18<\/p>\n","modified":"2018-06-28T14:57:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Arkitsa-Fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1460","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1460&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/arkitsa-fault-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.00662636756897,38.732410041502824]}},{"type":"Feature","properties":{"id":2270,"name":"Bhuban Mohan Behera","description":"

Pseudotachylyte with tentacle veins (almost Octopus shape) in quartzofeldspathic gneiss from Southen Granulite Terrane in Tamil Nadu (India). PhotoID811<\/p>\n

Photograph: Bhuban Mohan Behera<\/p>\n","modified":"2018-06-30T12:55:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bhuban-Mohan-Behera-3-768x508.jpeg","taxonomy":{"webmapp_category":[220,231]},"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\/2270","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2270&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bhuban-mohan-behera-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[78.64164680242538,11.489894677904124]}},{"type":"Feature","properties":{"id":2218,"name":"Calaveras fault active creep","description":"

Active fault creep on the Calaveras fault in central Hollister has displaced this concrete retaining wall, sidewalk, and curb. The fault has multiple strands creeping through the town at rates of 7 to 10 mm\/yr, with the overall slip rate for the fault at 15 – 18 mm\/yr of right-lateral slip, trending roughly NW-SE.
\nPhotoID771<\/p>\n

Photograph: David Manaker<\/p>\n

Reference: Manaker et al. (2003), Distribution of interseismic slip rates and the potential for significant earthquakes on the Calaveras fault, Central California, Journal of Geophysical Research, v. 108, no. B6.<\/p>\n","modified":"2018-09-04T15:48:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Calaveras-fault-active-creep-300x196.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2218","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2218&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/calaveras-fault-active-creep\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-121.406652,36.850604]}},{"type":"Feature","properties":{"id":2061,"name":"Capraia","description":"

Surge deposits. Photo ID 641<\/p>\n

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

Reference: The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea. Massimo Gasparona, Gideon Rosenbauma, Jan Wijbransb, Piero Manetti<\/p>\n","modified":"2018-06-15T10:27:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Capraia-2-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2061","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2061&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/capraia-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.846229702234268,43.04711155959075]}},{"type":"Feature","properties":{"id":1923,"name":"Carboneras Fault","description":"

Carboneras Fault Zone, a strike-slip fault system which runs NE-SW across the Almeria region of southeast Spain. Movement on the fault juxtaposed disparate slices of basement and sedimentary rocks, creating the spectacular striped colouration exposed at this dry river bed near the coast, halfway between the towns of Carboneras and Mojacar. Grinding and crushing of the rock during faulting facilitated chemical alteration of the rocks, giving rise to the vivid colours. Some of the lithologies caught up in the fault zone pictured include pale purple basement phyllite, red Triassic mudstone, yellow to pale green Miocene marls, dark blue-grey basement schist, and purplish red sandstone.<\/p>\n

Photograph: Fionnuala Sheehan<\/p>\n","modified":"2018-06-15T10:27:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Carboneras-Fault-300x201.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1923","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1923&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/carboneras-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-1.87750339508,37.04993685476495]}},{"type":"Feature","properties":{"id":6108,"name":"Carboneras Fault","description":"

Tectonic melange of metamorphic basement, post-orogenic sediments (marls, sandstones) and volcanic rocks, mainly andesites. NE-SW oriented left lateral stike-slip zone, estimated offset >15 to possibly 40km<\/p>\n","modified":"2018-12-14T11:10:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Carboneras-fault-zone-300x201.jpg","taxonomy":{"webmapp_category":[220,231]},"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\/6108","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6108&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/carboneras-fault-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-1.8777535918429749,37.04998132312124]}},{"type":"Feature","properties":{"id":2260,"name":"Carua\u00e7u Member – Maracangalha Formation","description":"

Succession of fine to medium sandstone showing hummocky cross stratification, tool marks and parts of Bouma sequence. There are also normal and reverse faults in the outcrop. This member is the register of turbidity flow in a lacustre system
\nPhotoID795<\/p>\n

Photograph: Guilherme Duarte<\/p>\n

Reference: Magnavita et al 2005 – Guia de Campo da Rec\u00f4ncavo, NE do Brasil<\/p>\n","modified":"2018-10-10T18:33:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Carua\u00e7u-Member-Maracangalha-Formation-768x1362.jpg","taxonomy":{"webmapp_category":[220,219]},"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\/2260","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2260&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/caruacu-member-maracangalha-formation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-38.6162862182,-12.9298916864]}},{"type":"Feature","properties":{"id":2162,"name":"Champlain Thrust","description":"

Cambrian Dunham dolomite thrust over the Ordovician Iberville shales during the Taconic Orogeny. Outcrop at Lone Rock Point (private property) in Burlington, VT
\nPhotoID781<\/p>\n

Photograph: James Kirkpatrick<\/p>\n","modified":"2018-06-30T12:52:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Champlain-Thrust-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2162","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2162&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/champlain-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-73.248882,44.490956]}},{"type":"Feature","properties":{"id":1149,"name":"Chicago Pass Normal fault","description":"

Spectacular normal fault. PhotoID109<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-06-28T18:03:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Chicago-Pass-Normal-fault-768x508.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1149","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1149&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/chicago-pass-normal-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-116.218893528,35.99678361167792]}},{"type":"Feature","properties":{"id":6016,"name":"Cilindro de Marbor\u00e9","description":"

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

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

 <\/p>\n","modified":"2018-12-12T10:05:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/23613466591_5e44b769b5_k-1-768x416.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6016","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6016&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cilindro-de-marbore\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.032573312104659635,42.67723635993417]}},{"type":"Feature","properties":{"id":2272,"name":"Cm-scale graben, Khabr mountain","description":"

Caption: Graben is the downthrown part of rock within extensional tectonics such as rifts.
\nGrabens are commonly bound by horsts and can be formed in a linear,
\nnon-linear or radial (as collapse crater) style at different geological scales. The
\nphotograph shows two oppositely dipping normal faults forming a spectacular cm-scale graben.
\nThis structure formed within the sequence of Devonian alternating layers of calc-schist, metalimestone
\nturbidite (brown) and thin bands of laminated marble (white). Metamorphic units is
\nresult from Early Cimmerian orogeny. No drag of the faulted unit characterizes it as a specific
\ntype of flanking structure. The throw (vertical displacement) on the fault is ~2 cm (follow the marker layer).
\nExtensional faulting within compressional orogeny is a crux and attracts geologists.
\nExtensional tectonism and its related structures may occur during as well as after the
\ncontractional history of a collisional orogeny. It is important in structural analysis and tectonic
\nmodelling to know which structures are synorogenic and which formed during the postcontractional stage. Synorogenic extensional structures are related to orogeny-internal
\nfeatures that cause relatively local instabilities in an overall contractional regime. By contrast
\nsignificant postorogenic extensional deformation implies true extension at the scale of the
\norogenic belt and crust. Accordingly, orogeny can be affected by
\ncontractional and extensional deformations overprinting each other and producing complex
\nstructural architectures (such as type-II superposed folds). Small-scale extension is commonly
\nrelated to local thrust faults and brittle-ductile shear zones. From the Khabr Mountain.
\nStructural zone of Sanandaj-Sirjan metamorphic-ophiolitic Complex, SW of the city of Baft,
\nKerman province, Iran (Location 28\u00b052\u00b404\u02baN, 56\u00b023\u00b456\u02baE). The coin radius is 1.25 cm. PhotoID800<\/p>\n

Photograph: Seyed Tohid Nabavi<\/p>\n","modified":"2018-06-30T13:04:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cm-scale-graben-Khabr-mountain-768x439.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2272","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2272&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cm-scale-graben-khabr-mountain\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[56.41699215397239,28.83986196550162]}},{"type":"Feature","properties":{"id":1381,"name":"Col du Lautaret","description":"

View, looking North, from the Col du Lautaret showing multiple thrusts of the Alpine internal zones over the external zones (to the left).
\nPhotoID269<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-30T19:12:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Col-du-Lautaret-768x248.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1381","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1381&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/col-du-lautaret\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.40562,45.03562]}},{"type":"Feature","properties":{"id":1847,"name":"Conjugate normal faults","description":"

Conjugate normal faults in Rosso Ammonitico Limestone in a quarry close to Sassorosso village (Lucca).
\nPhotoID601<\/p>\n

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

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The Cordelia fault is part of the San Andreas fault system in Northern California. It is a right-lateral, strike-slip fault. The outcrop exposure shows the preferential weathering of the fault gouge create by cataclasis in the active fault zone. Fault slip rates are estimated at 1 mm\/yr. Photo ID 698<\/p>\n

Photograph: David Manaker<\/p>\n

Reference: Moores, E., Wakabayashi, J., Unruh, J.R., Waechter, S., A Transect Spanning 500 Million Years of Plate Margin History: Outline and Field Trip Guide, in 1906 San Francisco Centennial Field Guides, Geological Society of America, Field Guide 7, 2006.<\/p>\n","modified":"2018-06-28T13:30:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cordelia-fault-fault-gouge-768x1023.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2108","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2108&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cordelia-fault-fault-gouge\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.136207,38.253617]}},{"type":"Feature","properties":{"id":7161,"name":"Coriscao syncline","description":"

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Brecciated Precambrian dolomite and shale, cemented with carbonate and abundant ironstone. A small amount of uranium mineralisation was found within the fault, near Corona homestead, in 1953.
\nPhotoID366<\/p>\n

Photograph:<\/p>\n

Reference: Gilligan, L.B., 1972. Geochemical sampling of the ironstone at Corona, Broken Hill District. Geological Survey of New South Wales Quarterley Notes 9, 1st October 1972<\/p>\n","modified":"2018-06-30T11:17:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Corona-Fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1622","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1622&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/corona-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[141.4534,-31.3292]}},{"type":"Feature","properties":{"id":838,"name":"Corse 1","description":"

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Millimeter wide zones of cataclasis in the Navajo Sandstone, associated with faulting. Photo ID 713<\/p>\n

Photograph:<\/p>\n","modified":"2018-10-10T18:47:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformation-bands-in-Eolian-sandstone-768x576.jpg","taxonomy":{"webmapp_category":[220,219]},"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\/1273","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1273&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformation-bands-in-eolian-sandstone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-108.510292,38.739657]}},{"type":"Feature","properties":{"id":1967,"name":"deformed slope breccia","description":"

Deformed slope breccia of mainly foliated fragments of Devonian slate; the foliated fragments show a crenulation cleavage, with a Variscan and Pyrenean (Late Cretaceous to earliest Miocene) foliation; the matrix has only the Pyrenean foliation
PhotoID577<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:25:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/deformed-slope-breccia-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1967","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1967&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-slope-breccia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.800142130302447,42.426712455977174]}},{"type":"Feature","properties":{"id":2180,"name":"Detail of Col Ombert Thrust","description":"

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

Photograph: Max Scarpa<\/p>\n

Reference: A. Castellarin F. Guy, L. Selli Geologia dei dintorni di Passo San Nicol\u00f2 e della Valle del Contrin – Mem. Soc. Geol. Guida alla geologia del Sudalpino centro-orientale<\/p>\n","modified":"2018-07-28T18:17:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Detail-of-Col-Ombert-Thrust-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2180","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2180&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/detail-of-col-ombert-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.797492504119873,46.419280805842625]}},{"type":"Feature","properties":{"id":2013,"name":"Diabase intrusion with Greenstone","description":"

Diabase intrusion into greenstone with some greenstone clasts along side trail out to Point Bonita. Photo ID 609<\/p>\n

Photograph: Brenor Brophy<\/p>\n","modified":"2018-06-15T10:26:11","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Diabase-intrusion-with-Greenstone-225x300.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2013","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2013&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/diabase-intrusion-with-greenstone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.53028,37.819484]}},{"type":"Feature","properties":{"id":1207,"name":"Domino faults","description":"

The photograph shown antitetic domino-microfaults in the so called Parvenets two-mica plagiogneisses which consitute the basement of the Trakia unit, northern Central Rhodopes, Bulgaria. The antitetic domino-microfaults indicate top-o-the-left (top-to-the southeast) sense of shear. These faults are formed during the third deformation phase in the tectonic evolution of the area \u2013 a stage of brittle to brittle-ductile strike-slip faulting and south-vergent trusting. During this stage some parts of the Trakia unit overtrusted the Late Oligocene sediments from the northernmost slopes of the Central Rhodopes. Near Parvenets village in the area of Plovdiv. PhotoID169<\/p>\n

Photograph: Kalin V. Naydenov<\/p>\n","modified":"2019-01-28T15:16:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Domino-faults-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1207","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1207&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/domino-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[24.57416699999999,41.601111]}},{"type":"Feature","properties":{"id":2132,"name":"Duplex structure in Eocene flysch","description":"

Duplex structure caused by underthrusting of Adriatic microplate under Euroasian plate. Photo ID 717<\/p>\n

Photograph: BlazV<\/p>\n

Reference: L. Placer, 1981, Geological structure of southwestern Slovenia, Geologija 24\/1, 27 60<\/p>\n","modified":"2018-07-01T11:24:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Duplex-structure-in-Eocene-flysch-768x310.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2132","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2132&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/duplex-structure-in-eocene-flysch\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.639343976974487,45.533153600425386]}},{"type":"Feature","properties":{"id":1211,"name":"Earthquake damage to dam","description":"

Damage to the Shih-Kang dam, the first dam in the world ever to be directly deformed by a earthquake surface rupture. This damage was caused by thrust motion on the Che-Lung Pu fault during the 21 September 1999 Chi Chi earthquake (Ml 7.3). Uplift of the hanging wall is in the order of 4 metres. PhotoID172<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-10T18:54:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Earthquake-damage-to-dam-768x576.jpg","taxonomy":{"webmapp_category":[220,219]},"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\/1211","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1211&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/earthquake-damage-to-dam\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[120.76859307289124,24.28271066985509]}},{"type":"Feature","properties":{"id":2005,"name":"Eddie Lynch","description":"

Inverted cross bedding in Beinn na Seamraig Formation sandstones (Sleat Group) on the upper overturned limb of the Lochalsh Syncline, Moine Thrust Belt, Scotland.
PhotoID 604<\/p>\n

Photograph: Eddie Lynch<\/p>\n","modified":"2018-06-15T10:26:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Eddie-Lynch-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2005","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2005&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/eddie-lynch\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-5.6783,57.2908]}},{"type":"Feature","properties":{"id":2007,"name":"Eddie Lynch","description":"

Kinloch Formation sandstones (Sleat Group) younging to the left (west) as indicated by injection structure on the upper overturned limb of the Lochalsh Syncline, Scotland
PhotoID 605<\/p>\n

Photograph: Eddie Lynch<\/p>\n","modified":"2018-06-15T10:26:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Eddie-Lynch-1-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2007","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2007&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/eddie-lynch-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-5.693,57.2864]}},{"type":"Feature","properties":{"id":1137,"name":"Ephesus fault scarp","description":"

Major scarp of an extensional fault with polished breccia. PhotoID102<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-10-10T18:58:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ephesus-fault-scarp-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1137","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1137&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ephesus-fault-scarp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[27.344541549682617,37.93059116662753]}},{"type":"Feature","properties":{"id":1917,"name":"erosion-protected column","description":"

Ciciu del villar (Children of the village), erosion column. The so-called stone mushrooms
Dronero-Cuneo<\/p>\n

Colonne di erosione, dette funghi di pietra<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:26:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/erosion-protected-column-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1917","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1917&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/erosion-protected-column\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.389121055603027,44.489280634920476]}},{"type":"Feature","properties":{"id":7029,"name":"Fault and fold in calcschist of Giens near Hy\u00e8res, France","description":"

\"\"<\/p>\n

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

Normal N140 fault (that will form the Grande Candelle) and associated folds in the upper Berriasian and lower Valanginian in the Calanques, near Marseille.<\/p>\n","modified":"2019-04-22T08:45:59","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/04\/P4140136-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6849","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6849&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-and-folds-in-calanques-close-to-marseille\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.450431311500552,43.21679260993947]}},{"type":"Feature","properties":{"id":1604,"name":"Fault damage to basin","description":"

Qasr el Telah- Toloana; Wall of a Roman water basin, displaced by a branch of the dead Sea transform fault, the Wadi es Sidre fault. The damage was probably caused by a 363 AD earthquake.
\nPhotoID358<\/p>\n

Photograph: Cees Passchier<\/p>\n

Reference: Galli and Galadini, Tectonophysics 335, 291-312<\/p>\n","modified":"2018-07-24T16:13:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fault-damage-to-basin-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1604","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1604&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-damage-to-basin\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[35.41193962097168,30.829600063147787]}},{"type":"Feature","properties":{"id":1532,"name":"Fault line scarp","description":"

Mt Goodenough and the Mackenzie River delta, NWT, Canada. Mt Goodenough is part of an uplift hanging wall block.
\nPhotoID320<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:16:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fault-line-scarp-768x501.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1532","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1532&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-line-scarp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-135.445862,67.940206]}},{"type":"Feature","properties":{"id":6910,"name":"Fault mirror at Le Tholonet, south flank of Sainte Victoire mountain","description":"

Fault mirror at Le Tholonet, south flank of Sainte Victoire mountain<\/p>\n

Picture from Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-05-05T21:57:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/Le-Tholonet_miroir_faille2-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6910","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6910&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-mirror-at-le-tholonet-south-flank-of-sainte-victoire-mountain\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.523718139881112,43.524214613777986]}},{"type":"Feature","properties":{"id":1731,"name":"Fault Plane","description":"

Fault plane with cataclasite in Liassic marbles. Pania della Croce, Alpi Apuane
\nPhotoID445<\/p>\n

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

Reference: Maxwell J. C. ,(1956) \u2013 Tectonics of Pania della Croce \u2013 Pania Secca area, Alpi; Apuane Bol. Soc. Geol. It. , 75 (2), 57-78 Mem. Soc. Geol. It., 28, 549-576. Raffaello Nardi, GEOLOGIA DELLA ZONA TRA LA PANIA DELLA CROCE, GALLICANO E CASTELNUOVO GARFAGNANA (ALPI APUANE). 1961<\/p>\n","modified":"2018-10-23T13:53:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fault-Plane-768x1024.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1731","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1731&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-plane\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.32154530286789,44.03834263110903]}},{"type":"Feature","properties":{"id":1859,"name":"fault plane","description":"

Fault Plane, Avane
\nPhotoID515<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2019-01-28T15:20:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/fault-plane-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1859","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1859&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fault-plane-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.388250704077109,43.809107992575704]}},{"type":"Feature","properties":{"id":2236,"name":"Faulted fold with quartz veins","description":"

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

Photograph: Christie Rowe<\/p>\n

Reference: Rowe, C. D., *Backeberg, N., *van Rensburg, T., *Maclennan, S., *Faber, C., *Curtis, C. and *Viglietti, P. (2010) Structural geology of Robben Island: Implications for the tectonic environment of Saldanian deformation, South African Journal of Geology 113.1 57-72. (Download geologic map eps.mcgill.ca\/~crowe\/publications)<\/p>\n","modified":"2018-09-04T11:21:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Faulted-fold-with-quartz-veins-768x512.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2236","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2236&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/faulted-fold-with-quartz-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[18.371931,-33.820772]}},{"type":"Feature","properties":{"id":1865,"name":"faults with opposite shear sense","description":"

horst and graben type faults with opposite shear sense, Rio Marina<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-28T14:47:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/faults-with-opposite-shear-sense-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1865","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1865&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/faults-with-opposite-shear-sense\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.428085327148438,42.811206920241304]}},{"type":"Feature","properties":{"id":2246,"name":"Fazenda Capit\u00e3o – Sergipano Belt","description":"

Outstanding outcrop of thrust of Neoproterozoic carbonate sediments of the Vaza-Barris Domain in the Sergipano Belt (a Brasiliano-Pan-African orogen system) over clastic sediments.PhotoID788<\/p>\n

Photograph: Felipe Guadagnin<\/p>\n","modified":"2018-06-30T11:20:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fazenda-Capit\u00e3o-Sergipano-Belt-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2246","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2246&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fazenda-capitao-sergipano-belt\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-37.5745725632,-10.7252126229]}},{"type":"Feature","properties":{"id":6583,"name":"Flysch Monte Cassio Northern Appenninies Italy – Reverse fault","description":"

Flysch Monte Cassio Northern Appenninies Italy – Reverse fault<\/p>\n","modified":"2019-02-11T14:34:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/2019-02-10-Ravarano_05-768x1147.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6583","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6583&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/flysch-monte-cassio-northern-appenninies-italy-reverse-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.05862438968336,44.581639663862994]}},{"type":"Feature","properties":{"id":2082,"name":"Folds and stretched dykes","description":"

Tight folds in low-grade metamorphic rocks of the Tibetan Sedimentary Sequence intruded by stretched leucogranitiic dykes.
Wetstern Nepal. Photo ID 682<\/p>\n

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

Reference: CAROSI R., MONTOMOLI C., VISONA\u2019 D. (2007) – A structural transect in the Lower Dolpo: Insights on the tectonic evolution of Western Nepal. J. Asian Earth Sciences, 29, 407-423.<\/p>\n","modified":"2018-06-15T10:28:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-and-stretched-dykes-300x201.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2082","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2082&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folds-and-stretched-dykes\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[82.4079,29.4189]}},{"type":"Feature","properties":{"id":1957,"name":"Foliated leucogranite","description":"

Foliated basal portion of the recently discovered Tertiary Bura Buri leucogranite (nearly 110 kmq) intruding the Tibetan Sedimentary Sequence in Western Nepal. The foliated portion is composed of a two-mica and tourmaline granite rich in giant muscovite crystals (1-10cm), tourmaline aggregates or giant white K-feldspar crystal.<\/p>\n

BERTOLDI L., MASSIRONI M., VISONA\u2019 D., CAROSI R., MONTOMOLI C., GUBERT F., NALETTO G., PELIZZO M.G. – Mapping the Buraburi granite in the Himalaya of Western Nepal: remote sensing analysis in a collisional belt with vegetation cover and extreme variation of topography. Remote Sensing of Environment, in press.
PhotoID567<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-06-15T10:27:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Foliated-leucogranite-300x201.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1957","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1957&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/foliated-leucogranite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[82.3826,29.3886]}},{"type":"Feature","properties":{"id":1947,"name":"foliations boudinage","description":"

foliation boudinage in garnet-micaschist. Boudin axes trend normal to a mineral lineation of kyanite, which was later statically replaced by sillimanite. E-side of Praia de Geriba, Buzios
PhotoID562<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:25:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/foliations-boudinage-300x197.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1947","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1947&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/foliations-boudinage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-41.90390892,-22.7809634777]}},{"type":"Feature","properties":{"id":2070,"name":"Granite of Mt. Nuptse","description":"

Granite of Mt. Nuptse, intruded in Everest series within the ductile portion of the South Tibetan Detachment System. Emplacement age is 23-24 Ma (Jessup et al., 2008). View from West to East. Photo ID 676<\/p>\n

Photograph: R. Carosi – Unipi<\/p>\n

Reference: Carosi R., Lombardo B., Musumeci G. & Pertusati P.C. (1999) – Geology of the Higher Himalayan Crystalline in Eastern Nepal (Khumbu Himal). In: Advances on the geology of the Himalaya. Focus on Nepal (P. Le Fort and B. N. Upreti eds.), Journal of Asian Earth Science, Elsevier (Great Britain), 17 (5-6), 785-803. Jessup, M.J., Cottle, J.M., Searle, M.P., Law, R.D., Tracy, R.J., Newell, D.L. & Waters, D.J. (2008) P-T-t-D paths of the Everest Series schist, Nepal. Journal of Metamorphic Geology, 26, 717-739.<\/p>\n","modified":"2018-06-15T10:28:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Granite-of-Mt.-Nuptse-207x300.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2070","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2070&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/granite-of-mt-nuptse\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.8102,27.9477]}},{"type":"Feature","properties":{"id":2222,"name":"Great Smoky Thrust at White Oak Sink","description":"

Within Great Smoky Mountain National Park, this beautiful waterfall can be found after a fairly easy ~1 mile hike. The small creek tumbles over the cliff and enters an underground passage here at White Oak Sink. Behind the waterfall, the Great Smoky Thrust fault can be easily seen as the horizontal line going across the middle of the rocks. The Great Smoky Thrust fault brings up Precambrian metamorphic rocks and places them on top of much younger Ordovician Knox group carbonate sedimentary rocks.
\nPhotoID773<\/p>\n

Photograph: Charles W. Carrigan<\/p>\n","modified":"2018-07-24T16:07:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Great-Smoky-Thrust-at-White-Oak-Sink-768x1023.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2222","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2222&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/great-smoky-thrust-at-white-oak-sink\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-83.74505,35.63585]}},{"type":"Feature","properties":{"id":1520,"name":"Half graben of Lac Besson","description":"

Many hectometric half-grabens of the margin of the alpine ocean are visible near the Lac Besson.
\nUnder the foot of Mireille, the escarpment of the normal fault consists of hercynian gneisses. The half graben is filled with red triassic dolomites which rest unconformably on the Hercynian basement on the right side of the photography (to the East). PhotoID296<\/p>\n

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

Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/ornon\/besson.html<\/p>\n","modified":"2018-06-30T11:07:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Half-graben-of-Lac-Besson-768x288.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1520","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1520&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/half-graben-of-lac-besson\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.089880466461182,45.121665339526665]}},{"type":"Feature","properties":{"id":2252,"name":"Hercinian folds in Ballota Beach","description":"

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

Photograph: Enrique Bern\u00e1rdez Rodr\u00edguez<\/p>\n","modified":"2018-09-04T11:12:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hercinian-folds-in-Ballota-Beach-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2252","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2252&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/hercinian-folds-in-ballota-beach\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.71158981323,43.411844042307344]}},{"type":"Feature","properties":{"id":1975,"name":"Historic Image: Soulsem striations","description":"

Glacial striations on a rockface of Cambro-Ordovician micaschist and pegmatite. This photograph was made during construction of the Soulsem dam in the 1970s. The outcrop is now largely destroyed and covered by the Soulsem dam
PhotoID581<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:28:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Historic-Image-Soulsem-striations-193x300.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1975","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1975&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/historic-image-soulsem-striations\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.452328512939403,42.67614435141624]}},{"type":"Feature","properties":{"id":1303,"name":"Kusadasi","description":"

Fault scarp in Cretaceous marbles, associated with a major EW trending fault NE of Kusadasi, Turkey. PhotoID86<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-03T14:16:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kusadasi-300x205.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1303","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1303&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/kusadasi\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[27.283000946044922,37.86895884124672]}},{"type":"Feature","properties":{"id":2276,"name":"LAND of Plage de Tamarone","description":"

That is a LANF (Low Angle Normal Fault) of Plage de Tamarone.
\nFootwall: Schistes Lustr\u00e9s
\nHangingwall: Balagne Nappe
\nPhotoID802<\/p>\n

Photograph: Sara Marrone<\/p>\n","modified":"2018-06-28T13:38:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/LAND-of-Plage-de-Tamarone-768x410.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2276","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2276&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/land-of-plage-de-tamarone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.454207420349121,42.97297258930983]}},{"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":2102,"name":"Longitudinal normal faults","description":"

Longitudinal normal faults in the crest of the Khaviz Anticline, Asmari Formation.
\nPhotoID694<\/p>\n

Photograph: Stefano Tavani<\/p>\n","modified":"2018-06-28T14:50:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Longitudinal-normal-faults-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2102","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2102&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/longitudinal-normal-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.33266067504883,30.700183726181734]}},{"type":"Feature","properties":{"id":1191,"name":"McConnel Thrust","description":"

McConnel thrust; Mount Yamnuska. Cambrian limestone (Eldon Formation; grey rocks) on top of Upper Cretaceous rocks (Belly River Formation). Southern Canadian Cordillera.<\/p>\n

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

Reference: Price R. A., Monger J.W.H. (2003) \u2013 A transect of the Southern Canadian Cordillera from Calgary to Vancouver. A filed trip guidebook. Geological Association of Canada, Cordilleran Section, 165 pp.<\/p>\n","modified":"2018-06-28T13:28:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/McConnel-Thrust-768x516.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1191","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1191&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mcconnel-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-115.065366,51.085712]}},{"type":"Feature","properties":{"id":2112,"name":"Moab fault outcrop","description":"

Moab fault outcrop near Arches National Park Visitor Center. The Moab fault is a complex normal fault zone resulting from salt tectonics in the valley below. This is an excellent example of fault zone cataclasis, as well as the formation of slickensides that indicate fault slip direction. Photo ID 700<\/p>\n

Photograph: David Manaker<\/p>\n","modified":"2018-06-30T12:33:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Moab-fault-outcrop-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2112","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2112&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/moab-fault-outcrop\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-109.621403,38.614766]}},{"type":"Feature","properties":{"id":2300,"name":"Monte Testo","description":"

The south cliff face of the Monte Testo in the Pasubio massif shows a prominent negative flower structure of early Jurassic age, when the Southern Alps experienced an extensional tectonics related to the development of the Adriatic passive margin of the Ligurian ocean. This structure is due to an oblique movement along a NNW-trending fault set experiencing transtension. In the lower part of the slope the Dolomia principale Fm (upper Triassic) crops out. The Dolomia principale is overlain by the well-stratified M. Zugna Fm (Hettangian-Sinemurian) and the Loppio oolitic lms (upper Sinemurian), which corresponds to the white layer poorly stratified. Since this layer is offset by (oblique-) normal faults and the subsequent marly Rotzo Fm (Pliensbachian) shows sharp thickness variations, the tectonic activity responsible for the M. Testo structure can be constrained to be Pliensbachian. In the upper part of the slope the Rotzo Fm shows an increase of the biohermal \u201cLithiotis\u201d mounds (white layers). PhotoID819<\/p>\n

Photograph: Dario Zampieri<\/p>\n

Reference: Tobaldo M., Zandonai F., Avanzini M., Miorandi R., Zampieri D., 2004. Note illustrative della carta geologica del settore nord occidentale del Monte Pasubio (Trentino, Italia). Studi Trentini di Scienze Naturali \u2013 Acta Geologica, v. 79 (2002), 161-180. Zampieri D., Massironi M., 2007. Evolution of a poly-deformed relay zone between fault segments in the eastern Southern Alps, Italy. In: Cunningham D. & Mann P. (eds), Tectonics of Strike-slip Restraining and Releasing Bends, Geol. Soc., London, Special Publication 290, 351-366. Martinelli, M., Franceschi, M., Massironi, M., Rizzi, A., Salvetti, G., Zampieri, D., 2017.An extensional syn-sedimentary structure in the Early Jurassic Trento Platform (Southern Alps, Italy) as analogue of potential hydrocarbon reservoirs developing in rifting-affected carbonate platforms. Marine and Petroleum Geology, 79, 360-371.<\/p>\n","modified":"2018-06-28T14:41:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Monte-Testo-300x202.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2300","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2300&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/monte-testo\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.13981,45.81772]}},{"type":"Feature","properties":{"id":1151,"name":"Mosaic Canyon sheared marble","description":"

Late normal faults cutting s strong ductile fabric in marble of Mosaic Canyon. Approximate location.PhotoID110<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-07-30T16:30:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mosaic-Canyon-sheared-marble-300x188.jpg","taxonomy":{"webmapp_category":[220,231]},"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\/1151","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1151&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mosaic-canyon-sheared-marble\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-117.143440247,36.57016580620263]}},{"type":"Feature","properties":{"id":2090,"name":"Mt. Kidd","description":"

Flexural slip folding in the Canadian Rockies of Alberta, west of Calgary. The Canadian Rockies are part of the North American Cordillera, a mountain belt that extends southward from Alaska along the plate margin. Uplift of this range occurred from late Jurassic through early Cenozoic. Deformed rocks are Carboniferous carbonates. Photo ID 697<\/p>\n

Photograph: David Manaker<\/p>\n

Reference: Eyles & Miall, 2007, Canada Rocks, 512 pages.<\/p>\n","modified":"2018-06-15T10:29:12","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Kidd-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2090","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2090&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mt-kidd\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-115.200076,50.872116]}},{"type":"Feature","properties":{"id":1500,"name":"Mt. Lhotse","description":"

Southwest face of Mt. Lhotse. The height of th exposed face is nearly 2 km. In the lower part: Miocene leucogranites with high grade schists (Rongbuck Formation); they are overlying by light colored, banded calc-silicate rocks (North Col Formation). North-northeast trending normal faults are highlighted by displacement of calc-silicate rocks
\nPhotoID311<\/p>\n

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

Reference: Carosi R. et al., 1999. Geol. Soc. America Special Papers n. 328, 211-223<\/p>\n","modified":"2018-06-28T14:45:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Lhotse-300x198.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1500","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1500&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mt-lhotse\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.8779,27.9114]}},{"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":1201,"name":"Nojima fault","description":"

The surface rupture along the Nojima fault, following the January 17, 1995 Kobe (Great Hanshin) earthquake, preserved in the Nojima Fault Preservation Museum. PhotoID165<\/p>\n

http:\/\/www.nojima-danso.co.jp\/nojimafaultpreservationmuseum.php<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-06-30T12:36:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Nojima-fault-768x513.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1201","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1201&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/nojima-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[134.93711292743683,34.54931946255584]}},{"type":"Feature","properties":{"id":1139,"name":"normal fault","description":"

Normal fault in road cut
\nPhotoID103<\/p>\n

Photograph:<\/p>\n","modified":"2018-06-28T18:04:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/normal-fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1139","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1139&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/normal-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[35.472986698150635,30.014669095574146]}},{"type":"Feature","properties":{"id":6669,"name":"Normal fault in upper pliocenic formations. Monte Giogo, Northern Appennines- Piacenza – Italy","description":"","modified":"2019-03-12T18:41:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/DSC_6598_02-768x514.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6669","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6669&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/normal-fault-in-pliocenic-upper-pliocenic-formations-monte-giogo-northern-appennines-piacenza-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.765498945654258,44.81442909865889]}},{"type":"Feature","properties":{"id":2302,"name":"Normal faulting, Zanjan-Tabriz highway","description":"

Extensional structures (such as horst, graben, tilted blocks, syn- and antithetic faults, drag folds) on the Zanjan-Mianeh-Tabriz highway, (WNW IRAN), in Pliocene-Quaternary sequences of Zanjan subsidence. PhotoID820<\/p>\n

Photograph:<\/p>\n","modified":"2018-06-30T16:20:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Normal-faulting-Zanjan-Tabriz-highway-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2302","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2302&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/normal-faulting-zanjan-tabriz-highway\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[47.64337919885293,37.120632612208595]}},{"type":"Feature","properties":{"id":6643,"name":"Normal faults in the Moenkopi Formation","description":"

Normal faults in the Early Triassic Moenkopi Formation near the entrance to Arches National Park. The Moenkopi Formation is sandstone, silty sandstone, to siltstone. Normal faults may be the result of extension due to salt anticlines.<\/p>\n","modified":"2019-02-26T09:20:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/P5300273-768x575.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6643","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6643&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/normal-faults-in-the-moenkopi-formation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"kincare1@cs.com","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-109.61925360361857,38.61532357794154]}},{"type":"Feature","properties":{"id":6957,"name":"Ophicalcite, Montaretto, La Spezia","description":"

Block of ophicalcite in the quarry of Monteretto, La Spezia, Italy.<\/p>\n

The typical brittle deformation of mantle ophicalcite.<\/p>\n

 <\/p>\n

\"\"<\/p>\n

 <\/p>\n

\"\"<\/p>\n","modified":"2019-06-07T16:46:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/blocco-levanto-Montaretto-300x225.jpg","taxonomy":{"webmapp_category":[220,231]},"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\/6957","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6957&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ophicalcite-montaretto-la-spezia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.58892429176285,44.19776670828329]}},{"type":"Feature","properties":{"id":1939,"name":"orthogneiss with pseudotachylyte","description":"

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

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:35:53","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/orthogneiss-with-pseudotachylyte-768x499.jpg","taxonomy":{"webmapp_category":[220,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1939","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1939&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/orthogneiss-with-pseudotachylyte\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-60.106111,2.46222]}},{"type":"Feature","properties":{"id":1921,"name":"Pillow lava","description":"

Basalt Pillow Lava in a reversed sequence, inferred from the inverted geometry of one of the pillows. Collesalvetti, Livorno
PhotoID547
Marroni M., 1990. Le ofioliti di Poggio Caprone (Monti Livornesi). Quaderni del Museo di Storia
Naturale di Livorno, vol. 11: 87-93.<\/p>\n

Bortolotti V. (1983) Stratigrafia, tettonica ed evoluzione geodinamica delle ofioliti della Toscana. Mem. Soc. Geol. It., 25, 63-74.<\/p>\n

Photograph: F.Milazzo<\/p>\n","modified":"2018-06-15T10:27:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pillow-lava-768x575.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1921","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1921&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pillow-lava\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.46924114227295,43.5693224350409]}},{"type":"Feature","properties":{"id":1171,"name":"Pissia fault scarp","description":"

Pissia fault scarp. PhotoID142<\/p>\n

Photograph: AChanou<\/p>\n","modified":"2018-10-10T18:57:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pissia-fault-scarp-768x574.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1171","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1171&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pissia-fault-scarp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[22.98811912536621,38.01656569516094]}},{"type":"Feature","properties":{"id":1193,"name":"Pseudotachylyte","description":"

Pseudotachylyte at teh base of the Perry Sound Allochthone
\nFresh rock cuts created recently during selective upgrading of Highway 522 in Golden Valley village and its vicinity facilitate the detailed study of Grenvillian structures. In western outskirts of Golden Valley village, pseudotachylite veins and breccias are discernible on clean outcrop surfaces of highly strained granodiorite-tonalite gneiss marking the basal contact of the Parry Sound allochthon (Davidson et al., 1982; Culshaw et al., 1997; Wodicka et al., 2000). As at various localities along the Georgian Bay shore, eastern Lake Huron (Tony Davidson and Rebecca Jamieson, written communications), the presence of pseudotachylite veins and breccias attests to seismic failure and friction melting near the basal contact of the Parry Sound allochthon, at middle to shallow crustal levels<\/p>\n

Davidson, A., Culshaw, N.G., Nadeau, L., 1982. A tectono-metamorphic framework for part of the Grenville Province, Ontario. Geological Survey of Canada Paper 82-1A, 275 \u2013 290.
\nCulshaw, N.G., Jamieson, R.A., Ketchum, J.W.F., Wodicka, N., Corrigan, D., Reynolds, P.H., 1997. Transect across the southwestern Grenville Orogen, Georgian Bay, Ontario: polystage convergence and extension in the lower orogenic crust. Tectonics 16, 966 \u2013 982.
\nJSG Photograph of the Month<\/p>\n

Wodicka, N., Ketchum, J.W.F., Jamieson, R.A., 2000. Grenvillian metamorphism of
\nmonocyclic rocks, Georgian Bay, Ontario, Canada: implications for convergence
\nhistory. Canadian Mineralogist 38, 471 \u2013 510. PhotoID161<\/p>\n

Photograph: Fried Schwerdtner<\/p>\n","modified":"2018-09-03T17:28:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pseudotachylyte-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1193","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1193&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pseudotachylyte\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-79.819633,45.920616]}},{"type":"Feature","properties":{"id":1965,"name":"reduction spots","description":"

Slightly deformed reduction spots in Permian shale. Malpas, Spain
PhotoID576<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:28:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/reduction-spots-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1965","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1965&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/reduction-spots\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.794997653411883,42.420665708156776]}},{"type":"Feature","properties":{"id":2084,"name":"Reverse fault and folded quartz vein","description":"

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

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

Reference: MONTOMOLI C. (2002) – Zone di taglio fragili-duttili nel basamento Varisico metamorfico di basso grado della Nurra meridionale (Sardegna nord-occidentale). Atti della Societ\u00e0 Toscana di Scienze Naturali, Memorie seria A, 108, 23-29. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-07-24T11:33:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Reverese-fault-and-folded-quartz-vein-300x225.jpg","taxonomy":{"webmapp_category":[220,229,224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2084","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2084&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/reverese-fault-and-folded-quartz-vein\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.161822,40.761442]}},{"type":"Feature","properties":{"id":1279,"name":"Reverse faults (Samaria Gorge, Crete)","description":"

Centimetre-scale reverse faults cross-cutting alternating dolomites and silica layers of the Plattenkalk nappe. Faults (photo) and asymmetric south-verging folds reflect Oligocene compression and are exposed in the Samaria Gorge, which developed as a result of contemporaneous (Pleistocene) continent uplift and erosion.<\/p>\n

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

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

Reference: Fassoulas C. (2004). Field Guide to the Geology of Crete. Natural History Museum of Crete, Publ., 104p, Heraklio (3th edition)<\/p>\n","modified":"2018-09-04T13:20:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Reverse-faults-Samaria-Gorge-Crete-768x531.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1279","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1279&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/reverse-faults-samaria-gorge-crete\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.954752385616302,35.29608394976411]}},{"type":"Feature","properties":{"id":1143,"name":"Rio de las Pe\u00f1as thrust","description":"

Thrust front of the Sierra de las Pe\u00f1as, where Miocene-Pliocene deposits override quarternary alluvial fan gravels. PhotoID105<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-10-10T18:58:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rio-de-las-Pe\u00f1as-thrust-768x576.jpg","taxonomy":{"webmapp_category":[220,219]},"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\/1143","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1143&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rio-de-las-penas-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-68.7980926037,-32.4878185652]}},{"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":1287,"name":"San Andreas folds and faults","description":"

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

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

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

Photograph: Haakon Fossen<\/p>\n","modified":"2018-06-28T18:13:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/San-Andreas-folds-and-faults-768x404.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1287","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1287&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/san-andreas-folds-and-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.13379,34.563255]}},{"type":"Feature","properties":{"id":1241,"name":"Serpentine along Hayward fault","description":"

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

Photograph: David Manaker<\/p>\n","modified":"2018-09-04T13:23:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Serpentine-along-Hayward-fault-768x513.jpg","taxonomy":{"webmapp_category":[220,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1241","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1241&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/serpentine-along-hayward-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.178909,37.805243]}},{"type":"Feature","properties":{"id":1993,"name":"Shear zone in Granite","description":"

Shear zone (magmatic) in Malanjkhand Granite (central India).
PhotoID592<\/p>\n

Photograph: M.A. Mamtani<\/p>\n

Reference: Majumder, S. and Mamtani, M.A. (2009). Magnetic fabric in the Malanjkhand Granite (Central India)\u2014Implications for regional tectonics and Proterozoic Suturing of the Indian shield. PHYSICS OF THE EARTH & PLANETARY INTERIORS, 172, 310-323. (doi:10.1016\/j.pepi.2008.10.007)<\/p>\n","modified":"2018-06-15T10:28:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zone-in-Granite-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1993","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1993&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zone-in-granite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[80.74710845947266,21.890013564114792]}},{"type":"Feature","properties":{"id":2029,"name":"Sheath fold","description":"

Textbook example of a sheath fold (Ile de Groix, Brittany, France) PhotoID 619<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven)<\/p>\n

Reference: Quinquis, H., Audren, C., Brun, J.-P. & Cobbold, P. R. 1978. Intense progressive shear in Ile de Groix blueschists and compatibility with subduction or obduction. Nature 273, 43-45. doi:10.1038\/273043a0<\/p>\n","modified":"2018-06-15T10:26:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-1-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2029","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2029&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-3.46829473972,47.625126176625315]}},{"type":"Feature","properties":{"id":2264,"name":"Sibuti Formation Miri","description":"

The excellent field exposure of a large thrust fault observed in Sibuti Formation, Miri Sarawak Malaysia. Backthrust are beautifully preserved in the thrust-wedge on the hanging wall of the large fault. PhotoID797<\/p>\n

Photograph: Batmanathan Navakanesh<\/p>\n

Reference: Batmanathan Navakanesh, Mohammed Khalil, Nur Aqilah Safar, Praviandy Gustandika., Structural Analysis of Miri-Beluru region, Sarawak, Malaysia. Final Year Project for B.Sc. Applied Geology, 2015, Curtin Sarawak Malaysia. Advisor: Dr. Afroz Shah<\/p>\n","modified":"2018-06-30T19:56:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sibuti-Formation-Miri-768x567.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2264","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2264&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sibuti-formation-miri\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[113.94599,4.02422]}},{"type":"Feature","properties":{"id":2025,"name":"Silicified fault breccia\/gouge","description":"

Field photograph of a silicified fault breccia\/gouge zone in sheared granitoids of Gavilgarh-Tan shear zone, central India. The faults are roughly East-West and generally parallel to the mylonitic foliation in granitoids. Mylonitic foliation is clearly seen in the large fragments of host rock within the silicified zone. At places, such faults have displaced Deccan Trap lava flows, and therefore should be post-Mesozoic in age. Photo ID 615<\/p>\n

Photograph: A. Chattopadhyay, University of Delhi.<\/p>\n","modified":"2018-07-24T15:56:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Silicified-fault-brecciagouge-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2025","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2025&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/silicified-fault-breccia-gouge\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[76.46426169999995,21.04131989999999]}},{"type":"Feature","properties":{"id":2104,"name":"Slickenlines in Cenozoic conglomerates","description":"

Slickenlines in Cenozoic conglomerates, associated with right-lateral strike-slip tectonics in the Ubierna Fault System.
\nPhotoID695<\/p>\n

Photograph: Stefano Tavani<\/p>\n

Reference: Tavani S., Quinta A., Granado P., 2011. Cenozoic right-lateral wrench tectonics in the Western Pyrenees (Spain): The Ubierna Fault System. Tectonophysics, 510, 238-253.<\/p>\n","modified":"2018-09-04T15:51:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Slickenlines-in-Cenozoic-conglomerates-768x512.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2104","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2104&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/slickenlines-in-cenozoic-conglomerates\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.37075614929,42.771919950195944]}},{"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":1265,"name":"Small-scale thrust","description":"

Small-scale thrust in a sandstone sequence (Upper Carboniferous), expressing the Late Palaeozoic contraction at the northern Variscan front zone.<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-06-30T12:31:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Small-scale-thrust-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1265","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1265&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/small-scale-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.860624074935913,50.457387901484346]}},{"type":"Feature","properties":{"id":1897,"name":"Spiaggia di Barbarossa-Elba","description":"

Leucogranitic Dyke with Shist inclusion (Xenolithe).
PhotoID534<\/p>\n

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

Reference: The Porto Azzurro Unit (Mt. Calamita promontory, south-eastern Elba Island, Tuscany): stratigraphic, tectonic and metamorphic evolution NRICO PANDELI & GIANFRANCO PRINCIPI<\/p>\n","modified":"2018-06-15T10:26:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Spiaggia-di-Barbarossa-Elba-1-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1897","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1897&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/spiaggia-di-barbarossa-elba-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.405962467193604,42.76642251018375]}},{"type":"Feature","properties":{"id":6086,"name":"St John’s Point, Co. Donegal , Ireland","description":"","modified":"2018-12-14T11:07:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/St-Johns-Point-768x574.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6086","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6086&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/st-johns-point-co-donegal-ireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.451647994367022,54.57745957141567]}},{"type":"Feature","properties":{"id":2176,"name":"Syndepositional Faults","description":"

This photograph is a view of normal syndepositional faults in Shemshak Formation in Alborz mountain belt.
\nThis kind of faults is well exposed in Baladeh valley area of Shemshak Fm. outcrops, and refer to extensional tectonic regime during Norian-Bajocian.
\nPhotoID750<\/p>\n

Photograph: Masoud Mirzaei<\/p>\n

Reference: Alizade, F., Mirzaei, M., Shahidi, A.R. 2012. Paleostress reconstruction in Shemshak Group, Norian-lower Bajocian in Baladeh Valley (Central Alborz). In preparation.<\/p>\n","modified":"2018-06-30T12:50:12","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Syndepositional-Faults-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2176","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2176&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/syndepositional-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[51.9015,36.202472]}},{"type":"Feature","properties":{"id":2047,"name":"Synsedimentary breccia in Chert","description":"

Layer of monogenic chert breccia confined bewteen two unbrecciated chert layers of c. 2.8Ga deposition age. Photo ID 672<\/p>\n

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

Reference: Geological Survey of Western Australia. http:\/\/www.dmp.wa.gov.au\/371.aspx<\/p>\n","modified":"2018-06-15T10:25:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Synsedimentary-breccia-in-Chert-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2047","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2047&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/synsedimentary-breccia-in-chert\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.82274723052979,-27.996902384]}},{"type":"Feature","properties":{"id":1853,"name":"synsedimentary fault","description":"

Synsedimentary fault in Rosso Ammonitico Fm. The fault was active at the time of sedimentation (Lias). The dislocation of strata is greatest in the central part of the fault and decreases at the ends. (the height of the cut is about 6 m)<\/p>\n

Photograph: F.Milazzo<\/p>\n","modified":"2018-06-30T11:45:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/synsedimentary-fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1853","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1853&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/synsedimentary-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.394268035888672,44.181665379510186]}},{"type":"Feature","properties":{"id":1476,"name":"Synsedimentary graben","description":"

Synsedimentary graben in the Miocene StFlorent basin. Many small normal faults cut out the outcrop. They become inactive at the top of photography.
\nPhotoID300<\/p>\n

Photograph: ch.nicollet<\/p>\n","modified":"2018-07-30T16:25:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Synsedimentary-graben-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1476","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1476&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/synsedimentary-graben\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.338293075561523,42.72759575637386]}},{"type":"Feature","properties":{"id":1935,"name":"synvolcanic faulting in BIF","description":"

Small-scale faults at high-angle from the primary bedding in the c. 2.8 Ga banded iron formation near Mount Magnet. The gap created during faulting is filled by basaltic lava flows. Photo ID 670<\/p>\n

Photograph: ivan zibra<\/p>\n

Reference: Geological Survey of Western Australia. http:\/\/www.dmp.wa.gov.au\/371.aspx<\/p>\n","modified":"2018-06-15T10:22:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/synvolcanic-faulting-in-BIF-768x575.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1935","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1935&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/synvolcanic-faulting-in-bif\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.80030250549316,-28.0561130003]}},{"type":"Feature","properties":{"id":1963,"name":"Thrust duplex, normal & domino faults","description":"

A sample from the Breakaway Shale in the Lake Moondarra area north of Mt Isa with an Australian one dollar coin, 23 mm in diameter, as scale. The central part shows a thrust duplex comprising seven horses, some of them internally folded. The roof thrust is very well defined, separating the shortened layers from the upper layers that do not record any contractional deformation. The basal decollement, on the right side, becomes a low-angle normal fault toward the centre, whereas on the left, it is faulted by a right-dipping, high-angle normal fault that is partially overturned (rather than inverted) by contractional deformation. Together, these two faults define a graben. In the bottom right corner, a series of domino-style faults and two antithetic, low-angle faults are also accommodating extensional deformation.<\/p>\n

Published as Photograph of the Month in the Journal of Structural Geology. <\/p>\n

PhotoID573<\/p>\n

Photograph: Arne F. Scherrenberg<\/p>\n

Reference: For more information see: Scherrenberg, A. F., and Rosenbaum, G. (2009). Photograph of the Month: Thrust duplex, low-angle normal faults and domino-style faults in laminated shale, Mt Isa, Australia. Journal of Structural Geology 31, 475.<\/p>\n","modified":"2018-06-15T10:28:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Thrust-duplex-normal-amp-domino-faults-768x457.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1963","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1963&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrust-duplex-normal-domino-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[139.578719,-20.595531]}},{"type":"Feature","properties":{"id":6448,"name":"Thrust in the Priestley Formation, Northern Victoria Land","description":"

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

Photo by Rodolfo Carosi (@PNRA)<\/p>\n","modified":"2019-01-30T18:54:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/piega-okane-canyon-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6448","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6448&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrust-in-the-priestley-formation-northern-victoria-land\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.40159831160247,-74.31535554773862]}},{"type":"Feature","properties":{"id":6027,"name":"Thrust sheets in Via del’Amore","description":"

Mesoscale thrust sheets within the Tuscan nappe of the Apenninic fold-and-thrust belt. The<\/p>\n","modified":"2018-12-12T13:00:28","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6027","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6027&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrust-sheets-in-via-delamore\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.73427911819988,44.100079135876825]}},{"type":"Feature","properties":{"id":6064,"name":"Thrust sheets in Via del\u2019Amore","description":"

Mesoscale thrust sheets within the Tuscan nappe of the Apenninic fold-and-thrust belt.<\/p>\n

Photo by Adriana G. Fl\u00f3rez<\/p>\n","modified":"2018-12-12T15:28:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Thrust-sheets-01-768x507.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6064","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6064&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrust-sheets-in-via-delamore-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.73425112013615,44.100118437748634]}},{"type":"Feature","properties":{"id":7015,"name":"thrusts intra-nappe double up australpine mesozoic cover (Ortles nappe) Rhetic Alps","description":"

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

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

(Photo by Lorusso Angelo)<\/span><\/h4>\n","modified":"2019-06-15T13:19:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7015","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7015&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/thrusts-intra-nappe-double-up-australpine-mesozoic-cover-ortles-nappe-rhetic-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.368900560383395,46.51367560697147]}},{"type":"Feature","properties":{"id":1977,"name":"Tilted thrust ramp","description":"

Thrust ramps in Permian redbeds, later tilted to a steep position. Noales, Spain
PhotoID582<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:28:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Tilted-thrust-ramp-190x300.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1977","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1977&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tilted-thrust-ramp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.648473,42.468594]}},{"type":"Feature","properties":{"id":2031,"name":"tonalitic gneiss","description":"

Archaean tonalitic gneiss, strongly deformed with remains of mafic dykes, cut by several sets of pegmatite and granite veins, and ductile and brittle shear zones. This outcrop is ideal for teaching structural geology in the field<\/p>\n

Photograph: Sebastian Schr\u00f6der and Nils Suhr<\/p>\n","modified":"2018-06-15T10:26:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/tonalitic-gneiss-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2031","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2031&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tonalitic-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[31.425616,-26.819933]}},{"type":"Feature","properties":{"id":2086,"name":"Type-3 intereference pattern","description":"

Type-3 interference pattern between F1 southwest-facing F1 folds and F2 upright to north-verging F2 folds in Paleozoic quartzites and black shale involved in the Variscan Orogeny; Nurra Peninsula (Sardinia, Italy).
PhotoID683<\/p>\n

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

Reference: CAROSI R. & OGGIANO G. (2002) – Transpressional deformation in northwestern Sardinia (Italy): insights on the tectonic evolution of the Variscan belt. Comptes Rendus Geoscience, 334, 287-294, Elsevier, Paris 2002. MONTOMOLI C. (2002) – Zone di taglio fragili-duttili nel basamento Varisico metamorfico di basso grado della Nurra meridionale (Sardegna nord-occidentale). Atti della Societ\u00e0 Toscana di Scienze Naturali, Memorie seria A, 108, 23-29. CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-15T10:28:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Type-3-intereference-pattern-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2086","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2086&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/type-3-intereference-pattern\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.1381,40.7343]}},{"type":"Feature","properties":{"id":2041,"name":"Vena del Gesso, Mauro Mt.","description":"

Panoramic view of NW\u2013SE oriented back-thrusts affecting messinian evaporites, Vena del Gesso. Photo ID 631<\/p>\n

Photograph: Domenico Montanari<\/p>\n

Reference: Montanari et al. 2007 \u201cPassive roof thrusting in the Messinian Vena del Gesso Basin (Northern Apennines, Italy): constraints from field data and analogue models. Geological Journal, DOI 10.1002\/gj.1085.<\/p>\n","modified":"2018-06-15T10:26:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Vena-del-Gesso-Mauro-Mt-300x179.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2041","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2041&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/vena-del-gesso-mauro-mt\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.696834564208984,44.23671337567926]}},{"type":"Feature","properties":{"id":1907,"name":"Volterra","description":"

Volterra Bedlands (Calanchi di volterra)<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:25:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Volterra-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1907","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1907&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/volterra\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.881786346435547,43.41265458964098]}},{"type":"Feature","properties":{"id":1514,"name":"West Bay Fault, Yellowknife","description":"

West Bay fault. View south of Great Slave Lake, Yellowknife, Northwest Territories, Canada. The fault displaces the Giant Yellowknife ore body from the mine on the light colored peninsular on the left to the mine complex near the top of the photo to the right of the fault. This makes it a left lateral fault.
\nPhotoID319<\/p>\n

Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:04:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/West-Bay-Fault-Yellowknife-768x503.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1514","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1514&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/west-bay-fault-yellowknife\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-114.368763,62.479704]}},{"type":"Feature","properties":{"id":1478,"name":"Zimudang thrust","description":"

Reversed anticline in the hangingwall of a thrust fault in Permian \u2013Triassic limestone. The cataclasite hosts gold and cinnabar deposits. Zimudang mine (Guizhou Province, China) PhotoID301<\/p>\n

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

Reference: R. Carosi – Unipi<\/p>\n","modified":"2018-06-28T14:51:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Zimudang-thrust-300x203.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1478","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1478&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/zimudang-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[105.470596,25.572227]}},{"type":"Feature","properties":{"id":1995,"name":"Zuccale fault","description":"

View form distance of the Zuccale low-angle fault at punta Zuccale, Elba Island. Top down to-the East (left) sense of movement.
PhotoID593<\/p>\n

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

Reference: Collettini, C., Holdsworth, R.E., 2004. Fault zone weakening and character of slip along low-angle normal faults: Insights from the Zuccale fault, Elba, Italy. Journal of the Geological Society, 161 (6), 1039-1051.<\/p>\n","modified":"2018-06-15T10:28:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Zuccale-fault-1-768x546.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1995","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1995&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/zuccale-fault-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.357881,42.752075]}},{"type":"Feature","properties":{"id":1711,"name":"Zuccale low-angle normal fault","description":"

Shear band cleavage, Zuccale low-angle normal fault. Elba Island. Top down to-the East sense of movement.
\nPhotoID435<\/p>\n

Photograph: Rodolfo Carosi<\/p>\n

 <\/p>\n","modified":"2019-02-03T21:24:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Zuccale-fault-300x201.jpg","taxonomy":{"webmapp_category":[220,231]},"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\/1711","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1711&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/zuccale-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.35749,42.75207]}}]}