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Summary

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.
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Source http://pubs.usgs.gov/publications/text/slabs.html
Author USGS; cropped by Beyond My Ken (talk) 10:06, 27 February 2010 (UTC)
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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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February 1996

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Date/TimeThumbnailDimensionsUserComment
current00:19, 1 September 2024Thumbnail for version as of 00:19, 1 September 20242,288 × 2,261 (1,005 KB)RXFADEZrestored Hispaniola to be a single island. Tried to preserve image format otherwise. Higher resolution
14:56, 19 April 2020Thumbnail for version as of 14:56, 19 April 20201,440 × 1,423 (699 KB)Beyond My KenNew version without unattributed arrows added by User Scott Nash
10:06, 27 February 2010Thumbnail for version as of 10:06, 27 February 2010588 × 579 (96 KB)Beyond My Ken== {{int:filedesc}} == {{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

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