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Fasciculus:Orogenic wedge.jpg

Orogenic_wedge.jpg(580 × 213 elementa imaginalia, magnitudo fasciculi: 53 chiliocteti, typus MIME: image/jpeg)

Hic fasciculus apud Vicimedia Communia iacet; in aliis inceptis adhiberi potest. Contenta paginae descriptionis fasciculi subter monstrantur.

Summarium

Descriptio
English: An illustration of the collision between two tectonic plates. One plate goes under the other, and the result is the buildup of a critical wedge of material. This orogenic wedge, or mountain-building wedge, maintains its slope by a stress balance between failures along the décollment, or main basal fault, and the faults inside the wedge.
Datum
Fons U.S. Geological Survey Professional Paper 1624 - Online version 1.0: Migration of the Acadian Orogen and Foreland Basin Across the Northern Appalachians of Maine and Adjacent Areas: http://pubs.usgs.gov/pp/pp1624/
Auctor Dwight C. Bradley, Robert D. Tucker, Daniel R. Lux, Anita G. Harris, and D. Colin McGregor
This geology image could be re-created using vector graphics as an SVG file. This has several advantages; see Commons:Media for cleanup for more information. If an SVG form of this image is available, please upload it and afterwards replace this template with ((vector version available|new image name)).
It is recommended to name the SVG file “Orogenic wedge.svg”—then the template Vector version available (or Vva) does not need the new image name parameter.

Potestas usoris

Public domain
This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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Dies/TempusMinutioDimensionesUsorSententia
recentissima20:16, 30 Ianuarii 2009Minutum speculum redactionis 20:16, 30 Ianuarii 2009 factae580 × 213 (53 chiliocteti)Awickert((Information |Description=((en|1=An illustration of the collision between two tectonic plates. One plate goes under the other, and the result is the buildup of a critical wedge of material. This orogenic wedge, or mountain-building wedge, maintains its s

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Fasciculus:Orogenic wedge.jpg
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