The Annual Emptying of Lake George, Alaska

Description and partial interpretation of the natural emptying of this ice-dammed lake in south-central Alaska. Regional and site characteristics, the 1951 observations and other emptyings since 1935 are described; and the age of the lake as evidenced by terracettes, willows, alders, and exposed del...

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Published in:ARCTIC
Main Author: Stone, Kirk H.
Format: Article in Journal/Newspaper
Language:unknown
Published: The Arctic Institute of North America 1963
Subjects:
Online Access:http://dx.doi.org/10.14430/arctic3519
http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/3519/3494
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spelling crarcticinstna:10.14430/arctic3519 2024-06-09T07:42:04+00:00 The Annual Emptying of Lake George, Alaska Stone, Kirk H. 1963 http://dx.doi.org/10.14430/arctic3519 http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/3519/3494 unknown The Arctic Institute of North America ARCTIC volume 16, issue 1, page 26 ISSN 1923-1245 0004-0843 journal-article 1963 crarcticinstna https://doi.org/10.14430/arctic3519 2024-05-14T12:53:42Z Description and partial interpretation of the natural emptying of this ice-dammed lake in south-central Alaska. Regional and site characteristics, the 1951 observations and other emptyings since 1935 are described; and the age of the lake as evidenced by terracettes, willows, alders, and exposed deltas, is considered. When studied July 20, 1951, it was about 2-4 mi wide, 11-12 mi long, 114 ft deep, and dammed by Knik Glacier. In 12 days, the lake water had undercut the glacier ice and escaped, leaving three small, shallow lakes with 42 % less water surface. The drop in level (up to 12 in/hr) was accompanied by the rise of Knik River from 7 to nearly 20 ft depth, and flooding. A trend is noted toward earlier emptying and greater flooding. Article in Journal/Newspaper Arctic glacier Alaska Arctic Institute of North America Dammed Lake ENVELOPE(-68.258,-68.258,68.496,68.496) Lake George ENVELOPE(-118.569,-118.569,56.226,56.226) ARCTIC 16 1 26
institution Open Polar
collection Arctic Institute of North America
op_collection_id crarcticinstna
language unknown
description Description and partial interpretation of the natural emptying of this ice-dammed lake in south-central Alaska. Regional and site characteristics, the 1951 observations and other emptyings since 1935 are described; and the age of the lake as evidenced by terracettes, willows, alders, and exposed deltas, is considered. When studied July 20, 1951, it was about 2-4 mi wide, 11-12 mi long, 114 ft deep, and dammed by Knik Glacier. In 12 days, the lake water had undercut the glacier ice and escaped, leaving three small, shallow lakes with 42 % less water surface. The drop in level (up to 12 in/hr) was accompanied by the rise of Knik River from 7 to nearly 20 ft depth, and flooding. A trend is noted toward earlier emptying and greater flooding.
format Article in Journal/Newspaper
author Stone, Kirk H.
spellingShingle Stone, Kirk H.
The Annual Emptying of Lake George, Alaska
author_facet Stone, Kirk H.
author_sort Stone, Kirk H.
title The Annual Emptying of Lake George, Alaska
title_short The Annual Emptying of Lake George, Alaska
title_full The Annual Emptying of Lake George, Alaska
title_fullStr The Annual Emptying of Lake George, Alaska
title_full_unstemmed The Annual Emptying of Lake George, Alaska
title_sort annual emptying of lake george, alaska
publisher The Arctic Institute of North America
publishDate 1963
url http://dx.doi.org/10.14430/arctic3519
http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/3519/3494
long_lat ENVELOPE(-68.258,-68.258,68.496,68.496)
ENVELOPE(-118.569,-118.569,56.226,56.226)
geographic Dammed Lake
Lake George
geographic_facet Dammed Lake
Lake George
genre Arctic
glacier
Alaska
genre_facet Arctic
glacier
Alaska
op_source ARCTIC
volume 16, issue 1, page 26
ISSN 1923-1245 0004-0843
op_doi https://doi.org/10.14430/arctic3519
container_title ARCTIC
container_volume 16
container_issue 1
container_start_page 26
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