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Deskripsyon 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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Gigikanan http://pubs.usgs.gov/publications/text/slabs.html
Tagsulat USGS; cropped by Beyond My Ken (talk) 10:06, 27 February 2010 (UTC)
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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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kasamtangan14:56, 19 Abril 2020Thumbnail sa bersyon sa 14:56, 19 Abril 20201,440 × 1,423 (699 KB)Beyond My KenNew version without unattributed arrows added by User Scott Nash
10:06, 27 Pebrero 2010Thumbnail sa bersyon sa 10:06, 27 Pebrero 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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