A Forest Ecosystem on a Glacier in Alaska

The ecosystem on the snout of Kushtaka Glacier, a branch of the Martin River Glacier about 60 mi ESE of Cordova has reached the developmental stage when spruce forest has almost eliminated the alder from the site. Mosses carpet the forest floor. A 55 ft spruce was found to be 65 yr old when felled....

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Published in:ARCTIC
Main Author: Stephens, F.R.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1969
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/66287 2023-05-15T14:19:20+02:00 A Forest Ecosystem on a Glacier in Alaska Stephens, F.R. 1969-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287/50200 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287 ARCTIC; Vol. 22 No. 4 (1969): December: 365–456; 441-444 1923-1245 0004-0843 Glaciation Plant succession Plant ecology Glaciers Glacial epoch Deglaciation info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1969 ftunivcalgaryojs 2022-03-22T21:23:12Z The ecosystem on the snout of Kushtaka Glacier, a branch of the Martin River Glacier about 60 mi ESE of Cordova has reached the developmental stage when spruce forest has almost eliminated the alder from the site. Mosses carpet the forest floor. A 55 ft spruce was found to be 65 yr old when felled. A profile through the 36-in soil layer on the ice is described. Similar brush and forest growth occurs on many glaciers in coastal Alaska. Superglacial vegetation on stagnant ice of the Wisconsin glaciation may have been the seed sources for much newly deglaciated land. Article in Journal/Newspaper Arctic glacier glaciers Alaska University of Calgary Journal Hosting ARCTIC 22 4
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Glaciation
Plant succession
Plant ecology
Glaciers
Glacial epoch
Deglaciation
spellingShingle Glaciation
Plant succession
Plant ecology
Glaciers
Glacial epoch
Deglaciation
Stephens, F.R.
A Forest Ecosystem on a Glacier in Alaska
topic_facet Glaciation
Plant succession
Plant ecology
Glaciers
Glacial epoch
Deglaciation
description The ecosystem on the snout of Kushtaka Glacier, a branch of the Martin River Glacier about 60 mi ESE of Cordova has reached the developmental stage when spruce forest has almost eliminated the alder from the site. Mosses carpet the forest floor. A 55 ft spruce was found to be 65 yr old when felled. A profile through the 36-in soil layer on the ice is described. Similar brush and forest growth occurs on many glaciers in coastal Alaska. Superglacial vegetation on stagnant ice of the Wisconsin glaciation may have been the seed sources for much newly deglaciated land.
format Article in Journal/Newspaper
author Stephens, F.R.
author_facet Stephens, F.R.
author_sort Stephens, F.R.
title A Forest Ecosystem on a Glacier in Alaska
title_short A Forest Ecosystem on a Glacier in Alaska
title_full A Forest Ecosystem on a Glacier in Alaska
title_fullStr A Forest Ecosystem on a Glacier in Alaska
title_full_unstemmed A Forest Ecosystem on a Glacier in Alaska
title_sort forest ecosystem on a glacier in alaska
publisher The Arctic Institute of North America
publishDate 1969
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287
genre Arctic
glacier
glaciers
Alaska
genre_facet Arctic
glacier
glaciers
Alaska
op_source ARCTIC; Vol. 22 No. 4 (1969): December: 365–456; 441-444
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287/50200
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66287
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