Earth Flows Along Henry Creek, Northern Alaska

ABSTRACT. Many earth flows occurred during the summer of 1979 in the hilly terrain near Umiat, Alaska, particularly along Henry Creek. Most were shallow, involving only the tundra mat and no more than 1.5 m of the underlying mud. The summer of 1979 was the warmest and wettest for the period of recor...

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Main Authors: L. David Carter, John P. Galloway
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.576.1933
http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.576.1933 2023-05-15T14:19:30+02:00 Earth Flows Along Henry Creek, Northern Alaska L. David Carter John P. Galloway The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.576.1933 http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.576.1933 http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf Key words earth flows text ftciteseerx 2016-01-08T12:45:47Z ABSTRACT. Many earth flows occurred during the summer of 1979 in the hilly terrain near Umiat, Alaska, particularly along Henry Creek. Most were shallow, involving only the tundra mat and no more than 1.5 m of the underlying mud. The summer of 1979 was the warmest and wettest for the period of record at Umiat, and precipitation was characterized by brief but intense localized rainstorms. Failure probably was triggered by the heavy rains and facilitated by an absorbent tundra mat over a clayey substrate, and perhaps in some cases by a thicker than normal ctive layer. Flows of this kind have occurred repeatedly in the Umiat area, most likely during summers in which climatic conditions were similar to those of 1979. Text Arctic Tundra Alaska Unknown Henry Creek ENVELOPE(-138.363,-138.363,64.769,64.769)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Key words
earth flows
spellingShingle Key words
earth flows
L. David Carter
John P. Galloway
Earth Flows Along Henry Creek, Northern Alaska
topic_facet Key words
earth flows
description ABSTRACT. Many earth flows occurred during the summer of 1979 in the hilly terrain near Umiat, Alaska, particularly along Henry Creek. Most were shallow, involving only the tundra mat and no more than 1.5 m of the underlying mud. The summer of 1979 was the warmest and wettest for the period of record at Umiat, and precipitation was characterized by brief but intense localized rainstorms. Failure probably was triggered by the heavy rains and facilitated by an absorbent tundra mat over a clayey substrate, and perhaps in some cases by a thicker than normal ctive layer. Flows of this kind have occurred repeatedly in the Umiat area, most likely during summers in which climatic conditions were similar to those of 1979.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author L. David Carter
John P. Galloway
author_facet L. David Carter
John P. Galloway
author_sort L. David Carter
title Earth Flows Along Henry Creek, Northern Alaska
title_short Earth Flows Along Henry Creek, Northern Alaska
title_full Earth Flows Along Henry Creek, Northern Alaska
title_fullStr Earth Flows Along Henry Creek, Northern Alaska
title_full_unstemmed Earth Flows Along Henry Creek, Northern Alaska
title_sort earth flows along henry creek, northern alaska
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.576.1933
http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf
long_lat ENVELOPE(-138.363,-138.363,64.769,64.769)
geographic Henry Creek
geographic_facet Henry Creek
genre Arctic
Tundra
Alaska
genre_facet Arctic
Tundra
Alaska
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.576.1933
http://pubs.aina.ucalgary.ca/arctic/Arctic34-4-325.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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