Shalbatana Vallis

Summary

Shalbatana Vallis is an ancient water-worn channel on Mars, located in the Oxia Palus quadrangle at 7.8° north latitude and 42.1° west longitude. It is the westernmost of the southern Chryse outflow channels. Beginning in a zone of chaotic terrain, at 0° latitude and 46° W longitude, it ends in Chryse Planitia.[1]

Shalbatana Vallis
Coordinates7°48′N 42°06′W / 7.8°N 42.1°W / 7.8; -42.1
NamingWord for "Mars" in Akkadian.

Shalbatana Vallis contains the first definitive evidence of a Martian shoreline. This shoreline was part of an ancient lake 80 square miles (210 km2) in size and 1,500 feet (460 m) deep. The study carried out with HiRISE images indicates that water formed a 30 miles (48 km) long canyon that opened up into a valley, deposited sediment, and created a delta. This delta and others around the basin imply the existence of a large, long-lived lake. Of special interest is evidence that the lake formed after the warm, wet period was thought to have ended. So, lakes may have been around much longer than previously thought. [2][3]

It is the word for "Mars" in Akkadian.[4]

See also edit

References edit

  1. ^ Baker, Victor R. (1982). The Channels of Mars. University of Texas Press. ISBN 0-292-71068-2.
  2. ^ "CU Researchers Find First Definitive Evidence for Ancient Lake on Mars | News Center | University of Colorado at Boulder". Archived from the original on 2011-12-29. Retrieved 2009-06-18.
  3. ^ "SPACE.com -- Evidence Found for Ancient Mars Lake". www.space.com. Archived from the original on 2009-06-19.
  4. ^ "Gazetteer of Planetary Nomenclature". Astrogeology Research Program. United States Geological Survey. Retrieved 20 March 2022.

Further reading edit

  • Baker, V.R.; Carr, M.H.; Gulick, V.C.; Williams, C.R. & Marley, M.S. "Channels and Valley Networks". In Kieffer, H.H.; Jakosky, B.M.; Snyder, C.W. & Matthews, M.S. (eds.). Mars. Tucson, AZ: University of Arizona Press.
  • Carr, M.H. (11 January 2007). "Channels, Valleys and Gullies". The Surface of Mars. Cambridge University Press. ISBN 978-0-521-87201-0.