Theoretical researches into planetary atmospheres and their influence upon surface features
The interface between certain geological and atmospheric phenomena on Mars was studied by examining those geological features which are associated with the presence of water in the liquid or solid phases. Several classes of Martian surface features thought to have had their origins in flow processes...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19740027141 2023-05-15T16:41:58+02:00 Theoretical researches into planetary atmospheres and their influence upon surface features Goody, R. Unclassified, Unlimited, Publicly available Oct 1, 1974 application/pdf http://hdl.handle.net/2060/19740027141 unknown Document ID: 19740027141 Accession ID: 74N35254 http://hdl.handle.net/2060/19740027141 No Copyright CASI SPACE SCIENCES NASA-CR-140188 1974 ftnasantrs 2019-07-21T05:29:58Z The interface between certain geological and atmospheric phenomena on Mars was studied by examining those geological features which are associated with the presence of water in the liquid or solid phases. Several classes of Martian surface features thought to have had their origins in flow processes were studied in order to determine the role ice may have played in their creations. Preliminary studies concerning the behavior of Martian ice shelves were conducted, with the conclusion that flow rates of Martian and earth ice sheets are similar. Withdrawal of subsurface ice was found to be among the explanations for the origins of the chaotic terrains and drifted blocks. Other/Unknown Material Ice Shelves NASA Technical Reports Server (NTRS) |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
language |
unknown |
topic |
SPACE SCIENCES |
spellingShingle |
SPACE SCIENCES Goody, R. Theoretical researches into planetary atmospheres and their influence upon surface features |
topic_facet |
SPACE SCIENCES |
description |
The interface between certain geological and atmospheric phenomena on Mars was studied by examining those geological features which are associated with the presence of water in the liquid or solid phases. Several classes of Martian surface features thought to have had their origins in flow processes were studied in order to determine the role ice may have played in their creations. Preliminary studies concerning the behavior of Martian ice shelves were conducted, with the conclusion that flow rates of Martian and earth ice sheets are similar. Withdrawal of subsurface ice was found to be among the explanations for the origins of the chaotic terrains and drifted blocks. |
format |
Other/Unknown Material |
author |
Goody, R. |
author_facet |
Goody, R. |
author_sort |
Goody, R. |
title |
Theoretical researches into planetary atmospheres and their influence upon surface features |
title_short |
Theoretical researches into planetary atmospheres and their influence upon surface features |
title_full |
Theoretical researches into planetary atmospheres and their influence upon surface features |
title_fullStr |
Theoretical researches into planetary atmospheres and their influence upon surface features |
title_full_unstemmed |
Theoretical researches into planetary atmospheres and their influence upon surface features |
title_sort |
theoretical researches into planetary atmospheres and their influence upon surface features |
publishDate |
1974 |
url |
http://hdl.handle.net/2060/19740027141 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Ice Shelves |
genre_facet |
Ice Shelves |
op_source |
CASI |
op_relation |
Document ID: 19740027141 Accession ID: 74N35254 http://hdl.handle.net/2060/19740027141 |
op_rights |
No Copyright |
_version_ |
1766032439282499584 |