Arsinoes Chaos
Arsinoes Chaos is in the Margaritifer Sinus quadrangle on Mars. It is 200.08 km in diameter. Its location is 7.66 S and 332.08 E. Arsinoes Chaos was named after the daughter of Ptolemy Lagun and Bernice and the name was approved in 1982.[1] [2]
Chaos terrain on Mars is distinctive; nothing on Earth compares to it. Chaos terrain generally consists of irregular groups of large blocks, some tens of kilometres across and a hundred or more meters high. The tilted and flat topped blocks form depressions hundreds of metres deep.[3] A chaotic region can be recognized by a rat's nest of mesas, buttes, and hills, chopped through with valleys which in places look almost patterned.[4][5][6] Some parts of this chaotic area have not collapsed completely—they are still formed into large mesas, so they may still contain water ice.[7] <templatestyles src="Module:Hatnote/styles.css"></templatestyles>
Some buttes and mesas in Arsinoes display layering. Many places on Mars show rocks arranged in layers. Rock can form layers in a variety of ways. Volcanoes, wind, or water can produce layers.[8] Layers can be hardened by the action of groundwater. Martian ground water probably moved hundreds of kilometers, and in the process it dissolved many minerals from the rock it passed through. When ground water surfaces in low areas containing sediments, water evaporates in the thin atmosphere and leaves behind minerals as deposits and/or cementing agents. Consequently, layers of dust could not later easily erode away since they were cemented together. On Earth, mineral-rich waters often evaporate forming large deposits of various types of salts and other minerals. <templatestyles src="Module:Hatnote/styles.css"></templatestyles>
A detailed discussion of layering with many Martian examples can be found in Sedimentary Geology of Mars.[9]
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Boundaries of Arsinoes Chaos represented by dark green in the center.
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Butte in Arsinoes Chaos with some light-toned layers, as seen by HiRISE under HiWish program.
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Light-toned deposit in Arsinoes Chaos, as seen by CTX camera (on Mars Reconnaissance Orbiter).
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Light-toned deposit in Arsinoes Chaos, as seen by HiRISE under HiWish program. Note: this field can be found in the previous wide image of Arsinoes Chaos, as seen by CTX camera (on Mars Reconnaissance Orbiter).
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Yardangs formed in light-toned material and surrounded by dark, volcanic basalt sand, as seen by HiRISE under HiWish program.
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Close-up image of yardangs, as seen by HiRISE under HiWish program. Arrows point to transverse aeolian ridges, TAR's, a type of dune. Note this is an enlargement of the previous image from HiRISE.
References
- ↑ http://planetarynames.wr.usgs.gov
- ↑ http://www.google.com/mars/
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Carr, M. 2006. The Surface of Mars. Cambridge University Press. ISBN 978-0-521-87201-0
- ↑ Forget, F., et al. 2006. Planet Mars Story of Another World. Praxis Publishing, Chichester, UK. ISBN 978-0-387-48925-4
- ↑ http://themis.asu.edu/features/aramchaos
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Grotzinger, J. and R. Milliken (eds.). 2012. Sedimentary Geology of Mars. SEPM.
