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Studies of Martian polar regionsThe flow law determined experimentally for solid CO2 establishes that an hypothesis of glacial flow of CO2 at the Martian poles is not physically unrealistic. Compression experiments carried out under 1 atmosphere pressure and constant strain rate conditions demonstrate that the strength of CO2 near its sublimation point is considerably less than the strength of water ice near its melting point. A plausible glacial model for the Martian polar caps was constructed. The CO2 deposited near the pole would have flowed outward laterally to relieve high internal shear stresses. The topography of the polar caps, and the uniform layering and general extent of the layered deposits were explained using this model.
Document ID
19750003808
Acquisition Source
Legacy CDMS
Document Type
Contractor Report (CR)
Authors
Smith, C. I.
(Michigan Univ. Ann Arbor, MI, United States)
Clark, B. R.
(Michigan Univ. Ann Arbor, MI, United States)
Eschman, D. F.
(Michigan Univ. Ann Arbor, MI, United States)
Date Acquired
September 3, 2013
Publication Date
January 1, 1974
Subject Category
Lunar And Planetary Exploration
Report/Patent Number
NASA-CR-140819
Accession Number
75N11880
Funding Number(s)
CONTRACT_GRANT: NGR-23-005-563
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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