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Thaumasia Plateau information


The Thaumasia Plateau is a vast sloping volcanic plain in the western hemisphere of Mars, and is the most extensive component of the Tharsis Rise by area.[1][2][3] Syria Planum, Solis Planum, Sinai Planum, and Thaumasia Planum are the constituent sectors of the plateau, which sits between 8 km and 4 km above the surrounding southern highlands. It is bounded by vestigial basement terrains that predate the formation of Tharsis. This area has been proposed to be a drainage basin that sourced the floodwaters forming the outflow channels surrounding Chryse Planitia.

  1. ^ Dohm, J.M.; Tanaka, K.L. (1999). "Geology of the Thaumasia region, Mars: Plateau development, valley origins, and magmatic evolution". Planetary and Space Science. United States: United States Geological Survey. p. 21. Retrieved 2019-01-25.
  2. ^ "Geologic Map of the Thaumasia Region, Mars". pubs.usgs.gov. United States: United States Geological Survey. Retrieved 2019-01-25.
  3. ^ "Geology of the Thaumasia region, Mars: Plateau development, valley origins, and magmatic evolution". ResearchGate. Retrieved 2019-01-25.

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Thaumasia Plateau

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Plateau on Mars...

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Coprates quadrangle

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