Uranius Mons,[1] formerly Uranius Patera, is a volcano on Mars located in the Tharsis quadrangle, named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera.[2] It is 4,853 metres (15,922 ft) high[3] and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90×65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch.[4]
Feature type | mountain |
---|---|
Coordinates | 26°54′N 267°51′E / 26.90°N 267.85°E |
Peak | 4,853 metres (15,922 ft) |
References
editWikimedia Commons has media related to Uranius Mons.
- ^ "Uranius Mons". USGS planetary nomenclature page. USGS. Retrieved 2012-06-30.
- ^ "Uranius Patera". USGS planetary nomenclature page. USGS. Retrieved 2012-06-30.
- ^ Peter Grego (1 June 2012). Mars and How to Observe It. Springer. p. 63. ISBN 978-1-4614-2302-7. Retrieved 10 September 2019.
- ^ Lunar and Planetary Science XXX, Geology of Uranius Patera, Mars. J. B. Plescia, U. S. Geological Survey, 2255 N. Gemini Drive, Flagstaff, AZ 86001.