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- Arsinoes_Chaos abstract "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. 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. 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. Some parts of this chaotic area have not collapsed completely—they are still formed into large mesas, so they may still contain water ice. 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. 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. A detailed discussion of layering with many Martian examples can be found in Sedimentary Geology of Mars.".
- Arsinoes_Chaos wikiPageID "45519169".
- Arsinoes_Chaos wikiPageLength "4683".
- Arsinoes_Chaos wikiPageOutDegree "19".
- Arsinoes_Chaos wikiPageRevisionID "682318207".
- Arsinoes_Chaos wikiPageWikiLink Butte.
- Arsinoes_Chaos wikiPageWikiLink Category:Mars.
- Arsinoes_Chaos wikiPageWikiLink Chaos_terrain.
- Arsinoes_Chaos wikiPageWikiLink Climate_of_Mars.
- Arsinoes_Chaos wikiPageWikiLink Geology_of_Mars.
- Arsinoes_Chaos wikiPageWikiLink Groundwater_on_Mars.
- Arsinoes_Chaos wikiPageWikiLink HiRISE.
- Arsinoes_Chaos wikiPageWikiLink HiWish.
- Arsinoes_Chaos wikiPageWikiLink HiWish_program.
- Arsinoes_Chaos wikiPageWikiLink List_of_areas_of_chaos_terrain_on_Mars.
- Arsinoes_Chaos wikiPageWikiLink Margaritifer_Sinus_quadrangle.
- Arsinoes_Chaos wikiPageWikiLink Mars_Reconnaissance_Orbiter.
- Arsinoes_Chaos wikiPageWikiLink Martian_chaos_terrain.
- Arsinoes_Chaos wikiPageWikiLink Mesa.
- Arsinoes_Chaos wikiPageWikiLink Mineral.
- Arsinoes_Chaos wikiPageWikiLink Outflow_channels.
- Arsinoes_Chaos wikiPageWikiLink Ptolemy.
- Arsinoes_Chaos wikiPageWikiLink Salt_(chemistry).
- Arsinoes_Chaos wikiPageWikiLink Salts.
- Arsinoes_Chaos wikiPageWikiLink Transverse_aeolian_ridges.
- Arsinoes_Chaos wikiPageWikiLink Yardang.
- Arsinoes_Chaos wikiPageWikiLinkText "Arsinoes Chaos".
- Arsinoes_Chaos hasPhotoCollection Arsinoes_Chaos.
- Arsinoes_Chaos wikiPageUsesTemplate Template:Main.
- Arsinoes_Chaos wikiPageUsesTemplate Template:Reflist.
- Arsinoes_Chaos subject Category:Mars.
- Arsinoes_Chaos comment "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. 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.".
- Arsinoes_Chaos label "Arsinoes Chaos".
- Arsinoes_Chaos sameAs m.012z2f3y.
- Arsinoes_Chaos wasDerivedFrom Arsinoes_Chaos?oldid=682318207.
- Arsinoes_Chaos isPrimaryTopicOf Arsinoes_Chaos.