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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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 |
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Open Polar |
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Unknown |
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ftciteseerx |
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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. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Michael Kelly |
spellingShingle |
Michael Kelly |
author_facet |
Michael Kelly |
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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 |
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palsas permafrost Thermokarst |
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palsas permafrost Thermokarst |
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http://2dgf.dk/xpdf/bull30-01-02-45-50.pdf |
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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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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766162242382856192 |