Fairén, A. G. and Davies, Neil S. and Squyres, S. W. (2013) Equatorial Ground Ice and Meandering Rivers on Mars. In: The 44th Lunar and Planetary Science Conference, March 18–22, 2013, The Woodlands, Texas.
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On Earth, vegetation is the most common provider of the fundamental control element determining scroll-bar and meander formation in fluvial channels. Studies of ancient terrestrial alluvium have demonstrat-ed that there is little evidence for heterolithic meander-ing fluvial systems in strata deposited prior to the evo-lution of land plants, indirectly demonstrating that the bank stability, bed roughness, and channel-corralling necessary to promote meandering are, on Earth, most often provided by vegetation. How-ever, lateral accretion and meander belts on Mars (Figs. 1 and 2), and occasionally within Precambrian alluvium, attest to the existence of alternative medi-ators for the prevention of continuous reworking of meanders.
|Item Type:||Conference or Workshop Item (Paper)|
|Subjects:||02 - Geodynamics, Geophysics and Tectonics|
|Divisions:||02 - Geodynamics, Geophysics and Tectonics|
|Journal or Publication Title:||LPI Contributions|
|Page Range:||p. 2948|
|Depositing User:||Sarah Humbert|
|Date Deposited:||24 Nov 2013 18:21|
|Last Modified:||16 Dec 2013 12:52|
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