Are lunar rilles inverted eskers.
A proposed mechanism for the formation of lunar rilles argues that escaping volatiles (CO2 and H2O) could produce a sinuous channel between an impermeable basement surface and a developing surficial permafrost layer. Concurrent with the development of the subsurface channel would be the production o...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19730051057 2023-05-15T16:37:17+02:00 Are lunar rilles inverted eskers. Helsley, C. E. Unclassified, Unlimited, Publicly available JAN 1, 1972 http://ntrs.nasa.gov/search.jsp?R=19730051057 unknown http://ntrs.nasa.gov/search.jsp?R=19730051057 Accession ID: 73A35859 Copyright Other Sources 30 Geological Society of America; Memoir 1972 ftnasantrs 2012-02-15T11:28:39Z A proposed mechanism for the formation of lunar rilles argues that escaping volatiles (CO2 and H2O) could produce a sinuous channel between an impermeable basement surface and a developing surficial permafrost layer. Concurrent with the development of the subsurface channel would be the production of a large amount of fragmented ice mixed with rock debris at the surface above and along the sides of the sinuous subsurface channel. Eventual sublimation of the ice in the surficial material down to and perhaps including the subsurface would develop a feature at the surface that would be morphologically very similar to a valley produced by running water. Other/Unknown Material Ice permafrost NASA Technical Reports Server (NTRS) |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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unknown |
topic |
30 |
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30 Helsley, C. E. Are lunar rilles inverted eskers. |
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30 |
description |
A proposed mechanism for the formation of lunar rilles argues that escaping volatiles (CO2 and H2O) could produce a sinuous channel between an impermeable basement surface and a developing surficial permafrost layer. Concurrent with the development of the subsurface channel would be the production of a large amount of fragmented ice mixed with rock debris at the surface above and along the sides of the sinuous subsurface channel. Eventual sublimation of the ice in the surficial material down to and perhaps including the subsurface would develop a feature at the surface that would be morphologically very similar to a valley produced by running water. |
format |
Other/Unknown Material |
author |
Helsley, C. E. |
author_facet |
Helsley, C. E. |
author_sort |
Helsley, C. E. |
title |
Are lunar rilles inverted eskers. |
title_short |
Are lunar rilles inverted eskers. |
title_full |
Are lunar rilles inverted eskers. |
title_fullStr |
Are lunar rilles inverted eskers. |
title_full_unstemmed |
Are lunar rilles inverted eskers. |
title_sort |
are lunar rilles inverted eskers. |
publishDate |
1972 |
url |
http://ntrs.nasa.gov/search.jsp?R=19730051057 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19730051057 Accession ID: 73A35859 |
op_rights |
Copyright |
_version_ |
1766027583851331584 |