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Marte_Vallis Latitude and Longitude:

15°00′N 176°30′W / 15°N 176.5°W / 15; -176.5
From Wikipedia, the free encyclopedia
Marte Vallis
Marte Vallis based on THEMIS day-time image
Coordinates 15°00′N 176°30′W / 15°N 176.5°W / 15; -176.5
Columnar jointing in basalt, Marte Vallis. Image courtesy High Resolution Imaging Science Experiment, University of Arizona. [1]

Marte Vallis is a valley in the Amazonis quadrangle of Mars, located at 15 North and 176.5 West. It is 185 km long and was named for the Spanish word for "Mars". [2] It has been identified as an outflow channel, carved in the geological past by catastrophic release of water from aquifers beneath the Martian surface. [3] The surface material is thought to have been created out of 'a'ā and pāhoehoe lava flows from the Elysium volcanic province in the west. [4]

Marte Vallis is the site of the first discovery of columnar jointing on Mars. [1] Columnar jointing often forms when basalt lava cools. [5]

References

  1. ^ a b Milazzo, M.P., Keszthelyi, L.P., Jaeger, W.L. Rosiek, M., Mattson, S., Verba, C., Beyer, R.A., Geissler, P.E., McEwen, A.S., and the HiRISE Team. (2009) Discovery of columnar jointing on Mars. Geology. 37(2), 171–174. Abstract
  2. ^ "Home". planetarynames.wr.usgs.gov.
  3. ^ Carr, M.H. (2006), The Surface of Mars. Cambridge Planetary Science Series, Cambridge University Press.
  4. ^ Voigt, Joana R. C.; Hamilton, Christopher W. (2018-07-15). "Investigating the volcanic versus aqueous origin of the surficial deposits in Eastern Elysium Planitia, Mars". Icarus. 309: 389–410. Bibcode: 2018Icar..309..389V. doi: 10.1016/j.icarus.2018.03.009. ISSN  0019-1035. S2CID  125918565.
  5. ^ Bates, R. and J. Jackson (eds.) 1976. Dictionary of Geological Terms. Doubleday, New York.

See also