Did ice streams shape the largest channels on

been interpreted as the probable erosional trace of catastrophic flooding. It is argued here that ice-streaming within ancient ice sheets emplaced by atmospheric precipitation at high mean obliquity may instead account for these channels, explaining similarities between the region and terrestrial Pl...

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Main Authors: Edwin S. Kite, Richard C. A. Hindmarsh
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.661.7077
http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.661.7077 2023-05-15T16:40:25+02:00 Did ice streams shape the largest channels on Edwin S. Kite Richard C. A. Hindmarsh The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.661.7077 http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.661.7077 http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf text 2007 ftciteseerx 2016-01-08T16:54:29Z been interpreted as the probable erosional trace of catastrophic flooding. It is argued here that ice-streaming within ancient ice sheets emplaced by atmospheric precipitation at high mean obliquity may instead account for these channels, explaining similarities between the region and terrestrial Pleistocene subglacial landscapes. An ice-sheet model shows extensive basal melting in and only in the NSV region, and ice streams which have significant Text Ice Sheet Unknown
institution Open Polar
collection Unknown
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language English
description been interpreted as the probable erosional trace of catastrophic flooding. It is argued here that ice-streaming within ancient ice sheets emplaced by atmospheric precipitation at high mean obliquity may instead account for these channels, explaining similarities between the region and terrestrial Pleistocene subglacial landscapes. An ice-sheet model shows extensive basal melting in and only in the NSV region, and ice streams which have significant
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Edwin S. Kite
Richard C. A. Hindmarsh
spellingShingle Edwin S. Kite
Richard C. A. Hindmarsh
Did ice streams shape the largest channels on
author_facet Edwin S. Kite
Richard C. A. Hindmarsh
author_sort Edwin S. Kite
title Did ice streams shape the largest channels on
title_short Did ice streams shape the largest channels on
title_full Did ice streams shape the largest channels on
title_fullStr Did ice streams shape the largest channels on
title_full_unstemmed Did ice streams shape the largest channels on
title_sort did ice streams shape the largest channels on
publishDate 2007
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.661.7077
http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf
genre Ice Sheet
genre_facet Ice Sheet
op_source http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.661.7077
http://geosci.uchicago.edu/%7Ekite/doc/Kite_and_Hindmarsh_GRL_2007.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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