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Statements

Subject Item
dbr:Thaumasia_Plateau
rdfs:label
Thaumasia Plateau
rdfs:comment
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. 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.
dcterms:subject
dbc:Surface_features_of_Mars
dbo:wikiPageID
59749321
dbo:wikiPageRevisionID
1049564017
dbo:wikiPageWikiLink
dbr:Pyroclastic_rock dbr:Northwestern_slope_valley dbr:Geology_of_Mars dbr:Precipitation dbr:Claritas_Rise dbr:Argyre_Planitia dbr:Claritas_Fossae dbr:Solis_Planum dbr:Hecates_Tholus dbr:Voeykov_(crater) dbr:Tharsis dbr:Tyrrhena_Patera dbr:Karnataka_Plateau dbr:Warrego_Valles dbr:Syria_Planum dbr:Outflow_channels dbc:Surface_features_of_Mars dbr:Elysium_(volcanic_province) dbr:Daedalia_Planum dbr:Arsia_Mons dbr:Chryse_Planitia dbr:Noachian dbr:Pavonis_Mons dbr:Apollinaris_Patera dbr:Hadriaca_Patera dbr:Terra_Sirenum dbr:Sinai_Planum dbr:Melas_Chasma dbr:Thaumasia_highlands dbr:Rhenish_shield dbr:Stratovolcano dbr:Deccan_Plateau dbr:Mars dbr:Impact_crater dbr:Valles_Marineris dbr:Germany dbr:Nectaris_Fossae dbr:Thaumasia_Planum dbr:Mantle_convection dbr:Lowell_(Martian_crater) dbr:List_of_plains_on_Mars dbr:Coprates_Rise dbr:Colorado_Plateau dbr:Ius_Chasma dbr:Coprates_Chasma dbr:Noctis_Labyrinthus dbr:Phreatomagmatic_eruption
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dbo:abstract
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. 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.
prov:wasDerivedFrom
wikipedia-en:Thaumasia_Plateau?oldid=1049564017&ns=0
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8303
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wikipedia-en:Thaumasia_Plateau