The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie

The birth and growth of Porsild Pingo (ice-cored hill) can be taken as fairly representative of the birth and growth of the more than 2000 closed-system pingos of the western arctic coast of Canada and adjacent Alaska. Porsild Pingo, named after a distinguished arctic botanist, has grown in the bott...

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Published in:ARCTIC
Main Author: Mackay, J. Ross
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1988
Subjects:
Ice
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64785 2023-05-15T14:19:13+02:00 The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie Mackay, J. Ross 1988-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785/48699 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785 ARCTIC; Vol. 41 No. 4 (1988): December: 261–336; 267-274 1923-1245 0004-0843 Drainage Etymology Interstitial water Lakes Permafrost Pingos Frozen ground Active layer Tuktoyaktuk Peninsula N.W.T info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1988 ftunivcalgaryojs 2022-03-22T21:21:59Z The birth and growth of Porsild Pingo (ice-cored hill) can be taken as fairly representative of the birth and growth of the more than 2000 closed-system pingos of the western arctic coast of Canada and adjacent Alaska. Porsild Pingo, named after a distinguished arctic botanist, has grown in the bottom of a large lake that drained catastrophically about 1900. Porsild Pingo has grown up at the site of a former shallow residual pond. The "birth" probably took place between 1920 and 1930. The high pore water pressure that caused updoming of the bottom of the residual pond to give birth to Porsild Pingo came from pore water expulsion by downward and upward permafrost growth in saturated sands in a closed system. In the freeze-back period of October-November 1934, permafrost ruptured and the intrusion of water into the unfrozen part of the active layer grew a 3.7 m high frost mound photographed by Porsild in May 1935. Porsild Pingo has grown up at, or very close to, the site of the former frost mound. The growth of Porsild Pingo appears to have been fairly steady from 1935 to 1976, after which there has been a decline to 1987. The growth rate has been nearly linear with height, from zero at the periphery to a maximum at the top. The present addition of water to the pingo is about 630 cu m/y. Providing there is no major climatic change. Porsild Pingo may continue to grow for a few centuries.Key words: frost mound, intrusive ice, permafrost, pingo, Porsild Mots clés: monticule de gel, glace d’intrusion, pergélisol, pingo, Porsild Article in Journal/Newspaper Arctic Arctic Ice permafrost pingo Alaska pergélisol University of Calgary Journal Hosting Arctic Canada Porsild Pingo ENVELOPE(-134.106,-134.106,69.150,69.150) Tuktoyaktuk ENVELOPE(-133.006,-133.006,69.425,69.425) Tuktoyaktuk Peninsula ENVELOPE(-131.339,-131.339,69.750,69.750) ARCTIC 41 4
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Drainage
Etymology
Interstitial water
Lakes
Permafrost
Pingos
Frozen ground
Active layer
Tuktoyaktuk Peninsula
N.W.T
spellingShingle Drainage
Etymology
Interstitial water
Lakes
Permafrost
Pingos
Frozen ground
Active layer
Tuktoyaktuk Peninsula
N.W.T
Mackay, J. Ross
The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie
topic_facet Drainage
Etymology
Interstitial water
Lakes
Permafrost
Pingos
Frozen ground
Active layer
Tuktoyaktuk Peninsula
N.W.T
description The birth and growth of Porsild Pingo (ice-cored hill) can be taken as fairly representative of the birth and growth of the more than 2000 closed-system pingos of the western arctic coast of Canada and adjacent Alaska. Porsild Pingo, named after a distinguished arctic botanist, has grown in the bottom of a large lake that drained catastrophically about 1900. Porsild Pingo has grown up at the site of a former shallow residual pond. The "birth" probably took place between 1920 and 1930. The high pore water pressure that caused updoming of the bottom of the residual pond to give birth to Porsild Pingo came from pore water expulsion by downward and upward permafrost growth in saturated sands in a closed system. In the freeze-back period of October-November 1934, permafrost ruptured and the intrusion of water into the unfrozen part of the active layer grew a 3.7 m high frost mound photographed by Porsild in May 1935. Porsild Pingo has grown up at, or very close to, the site of the former frost mound. The growth of Porsild Pingo appears to have been fairly steady from 1935 to 1976, after which there has been a decline to 1987. The growth rate has been nearly linear with height, from zero at the periphery to a maximum at the top. The present addition of water to the pingo is about 630 cu m/y. Providing there is no major climatic change. Porsild Pingo may continue to grow for a few centuries.Key words: frost mound, intrusive ice, permafrost, pingo, Porsild Mots clés: monticule de gel, glace d’intrusion, pergélisol, pingo, Porsild
format Article in Journal/Newspaper
author Mackay, J. Ross
author_facet Mackay, J. Ross
author_sort Mackay, J. Ross
title The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie
title_short The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie
title_full The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie
title_fullStr The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie
title_full_unstemmed The Birth and Growth of Porsild Pingo, Tuktoyaktuk Peninsula, District of Mackenzie
title_sort birth and growth of porsild pingo, tuktoyaktuk peninsula, district of mackenzie
publisher The Arctic Institute of North America
publishDate 1988
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785
long_lat ENVELOPE(-134.106,-134.106,69.150,69.150)
ENVELOPE(-133.006,-133.006,69.425,69.425)
ENVELOPE(-131.339,-131.339,69.750,69.750)
geographic Arctic
Canada
Porsild Pingo
Tuktoyaktuk
Tuktoyaktuk Peninsula
geographic_facet Arctic
Canada
Porsild Pingo
Tuktoyaktuk
Tuktoyaktuk Peninsula
genre Arctic
Arctic
Ice
permafrost
pingo
Alaska
pergélisol
genre_facet Arctic
Arctic
Ice
permafrost
pingo
Alaska
pergélisol
op_source ARCTIC; Vol. 41 No. 4 (1988): December: 261–336; 267-274
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785/48699
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64785
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