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Ulysses Tholus

Coordinates:2°53′N121°33′W / 2.89°N 121.55°W /2.89; -121.55
From Wikipedia, the free encyclopedia
Martian volcano
Ulysses Tholus
THEMIS daytime IR mosaic of Ulysses Tholus. Much of the caldera floor is covered by deposits from landslides triggered by the formation of adjacentimpact craters.
Coordinates2°53′N121°33′W / 2.89°N 121.55°W /2.89; -121.55

Ulysses Tholus is aMartianvolcano. It is located in theTharsis quadrangle at 2.89° north latitude and 121.55° west longitude. It is 58 km across and is named after a classical albedo feature.[1] Ulysses Tholus is immediately east and slightly north of another volcano,Biblis Tholus. The name of the mountain itself was changed on September 19, 2007. The former terminology,Ulysses Patera, now applies only (and more accurately) to the centralcaldera, whereas formerly it had applied to the whole edifice.[1]Tholus describes a volcanic edifice somewhat smaller than would be implied bymons.

  • Location of Ulysses Tholus in relation to other volcanoes (photo by THEMIS).
    Location of Ulysses Tholus in relation to other volcanoes (photo byTHEMIS).
  • Map of Tharsis quadrangle with major features indicated, Ulysses Tholus is on the bottom-left
    Map ofTharsis quadrangle with major features indicated, Ulysses Tholus is on the bottom-left
  • Crater at the top of Ulysses Patera, as seen by HiRISE under HiWish program Note the lack of a rim. Volcanic craters do not usually have a rim, as most impact craters do.
    Crater at the top ofUlysses Patera, as seen by HiRISE underHiWish program Note the lack of a rim. Volcanic craters do not usually have a rim, as most impact craters do.
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References

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  1. ^ab"Ulysses Tholus".Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.

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