Extensive areas of uplifted Holocene marine sediments are covered by permafrost mounds- domes and ridges up to 7 m high, and thermokarst lakes. The domes are related to both open system pingos and palsas but the ridges are of uncertain origin and not hitherto described. They all may be the result of...

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Main Author: Michael Kelly
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1981
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.623.2024
http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.623.2024 2023-05-15T17:54:29+02:00 Michael Kelly The Pennsylvania State University CiteSeerX Archives 1981 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.623.2024 http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.623.2024 http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf text 1981 ftciteseerx 2016-01-08T15:06:07Z Extensive areas of uplifted Holocene marine sediments are covered by permafrost mounds- domes and ridges up to 7 m high, and thermokarst lakes. The domes are related to both open system pingos and palsas but the ridges are of uncertain origin and not hitherto described. They all may be the result of an extension of permafrost in the late Neoglacial following a milder mid Holocene period. Text palsas permafrost Thermokarst Unknown
institution Open Polar
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language English
description Extensive areas of uplifted Holocene marine sediments are covered by permafrost mounds- domes and ridges up to 7 m high, and thermokarst lakes. The domes are related to both open system pingos and palsas but the ridges are of uncertain origin and not hitherto described. They all may be the result of an extension of permafrost in the late Neoglacial following a milder mid Holocene period.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Michael Kelly
spellingShingle Michael Kelly
author_facet Michael Kelly
author_sort Michael Kelly
publishDate 1981
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.623.2024
http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf
genre palsas
permafrost
Thermokarst
genre_facet palsas
permafrost
Thermokarst
op_source http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.623.2024
http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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