Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska
Reports investigations of perennially frozen mounds beneath individual trees growing in silty clay on a terrace of the McKinley River. Climate, vegetation and parent material of the spruce stand are described. The mounds, 2-4 m in diam, contain a frozen lens-shaped core. The permafrost results from...
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Language: | English |
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The Arctic Institute of North America
1965
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ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/66527 2023-05-15T14:19:20+02:00 Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska Viereck, Leslie A. 1965-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66527 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66527/50440 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66527 ARCTIC; Vol. 18 No. 4 (1965): December: 205–288; 262-267 1923-1245 0004-0843 Sarqaq culture info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1965 ftunivcalgaryojs 2022-03-22T21:23:21Z Reports investigations of perennially frozen mounds beneath individual trees growing in silty clay on a terrace of the McKinley River. Climate, vegetation and parent material of the spruce stand are described. The mounds, 2-4 m in diam, contain a frozen lens-shaped core. The permafrost results from lower temperatures under the trees due to less snow cover and a thicker moss layer. A proposed cycle of development and collapse of the tree mounds is outlined. Article in Journal/Newspaper Arctic permafrost Sarqaq Alaska University of Calgary Journal Hosting McKinley River ENVELOPE(-102.385,-102.385,65.601,65.601) ARCTIC 18 4 262 |
institution |
Open Polar |
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University of Calgary Journal Hosting |
op_collection_id |
ftunivcalgaryojs |
language |
English |
topic |
Sarqaq culture |
spellingShingle |
Sarqaq culture Viereck, Leslie A. Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska |
topic_facet |
Sarqaq culture |
description |
Reports investigations of perennially frozen mounds beneath individual trees growing in silty clay on a terrace of the McKinley River. Climate, vegetation and parent material of the spruce stand are described. The mounds, 2-4 m in diam, contain a frozen lens-shaped core. The permafrost results from lower temperatures under the trees due to less snow cover and a thicker moss layer. A proposed cycle of development and collapse of the tree mounds is outlined. |
format |
Article in Journal/Newspaper |
author |
Viereck, Leslie A. |
author_facet |
Viereck, Leslie A. |
author_sort |
Viereck, Leslie A. |
title |
Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska |
title_short |
Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska |
title_full |
Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska |
title_fullStr |
Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska |
title_full_unstemmed |
Relationship of White Spruce to Lenses of Perennially Frozen Ground, Mount McKinley National Park, Alaska |
title_sort |
relationship of white spruce to lenses of perennially frozen ground, mount mckinley national park, alaska |
publisher |
The Arctic Institute of North America |
publishDate |
1965 |
url |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66527 |
long_lat |
ENVELOPE(-102.385,-102.385,65.601,65.601) |
geographic |
McKinley River |
geographic_facet |
McKinley River |
genre |
Arctic permafrost Sarqaq Alaska |
genre_facet |
Arctic permafrost Sarqaq Alaska |
op_source |
ARCTIC; Vol. 18 No. 4 (1965): December: 205–288; 262-267 1923-1245 0004-0843 |
op_relation |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66527/50440 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66527 |
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