File:Plates tect2-sv.svg

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Description The key principle of plate tectonics is that the lithosphere exists as separate and distinct tectonic plates, which float on the fluid-like (visco-elastic solid) asthenosphere. The relative fluidity of the asthenosphere allows the tectonic plates to undergo motion in different directions. This map shows 15 of the largest plates. Note that the Indo-Australian Plate may be breaking apart into the Indian and Australian plates, which are shown separately on this map.
Date 2010-01-21 22:17 (UTC)
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Applications-graphics.svg This is a retouched picture, which means that it has been digitally altered from its original version. The original can be viewed here: Plates_tect2_en.svg.

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I, the copyright holder of this work, hereby publish it under the following license:
Public domain This image is in the public domain because it contains materials that originally came from the United States Geological Survey, an agency of the United States Department of Interior. For more information, see the official USGS copyright policy

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[edit] Original upload log

This image is a derivative work of the following images:

  • File:Plates_tect2_en.svg licensed with PD-USGov-USGS
    • 2009-04-20T02:06:16Z Octane 4217x3169 (466632 Bytes) couple fixes
    • 2006-12-26T21:54:44Z AzaToth 4217x3169 (460986 Bytes) if it's small, and it's an svg, lets then resize it :)
    • 2006-01-26T00:42:41Z Scott Nash 682x462 (461282 Bytes) Tectonic plate map with its relative movements. Translated from [[Image:Placas_tect2_pt_BR.svg]].

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current22:18, 21 January 2010Thumbnail for version as of 22:18, 21 January 20104,217 × 3,169 (455 KB)Inteloutside2 (talk | contribs){{Information |Description=The key principle of plate tectonics is that the lithosphere exists as separate and distinct tectonic plates, which float on the fluid-like (visco-elastic solid) asthenosphere. The relative fluidity of th

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