Jezža (crater)

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Jezža
Jezza Crater.JPG
Jezža Crater,as seen by HiRISE. North wall (at top) has gullies. Dark lines are dust devil tracks. Scale bar is 500 meters long.
Planet Mars
Coordinates 48°48′S 38°00′W / 48.8°S 38°W / -48.8; -38Coordinates: 48°48′S 38°00′W / 48.8°S 38°W / -48.8; -38
Diameter 9.1 km
Eponym a town in Russia

Jezža Crater is a crater in the Argyre quadrangle of Mars, located at 48.8° S and 38° W. It is 9.1 km in diameter and was named after a town in Russia.[1] Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak.[2] The peak is caused by a rebound of the crater floor following the impact.[3]

Why are Craters important?[edit]

The density of impact craters is used to determine the surface ages of Mars and other solar system bodies. [4] The older the surface, the more craters present. Crater shapes can reveal the presence of ground ice.

The area around craters may be rich in minerals. On Mars, heat from the impact melts ice in the ground. Water from the melting ice dissolves minerals, and then deposits them in cracks or faults that were produced with the impact. This process, called hydrothermal alteration, is a major way in which ore deposits are produced. The area around Martian craters may be rich in useful ores for the future colonization of Mars. [5]

References[edit]

  1. ^ Blue, Jennifer. "Jezža (crater)". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. ^ http://www.lpi.usra.edu/publications/slidesets/stones/
  3. ^ Hugh H. Kieffer (1992). Mars. University of Arizona Press. ISBN 978-0-8165-1257-7. Retrieved 7 March 2011. 
  4. ^ http://www.lpi.usra.edu/publications/slidesets/stones/
  5. ^ http://www.indiana.edu/~sierra/papers/2003/Patterson.html.

See also[edit]