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History and Bathymetry of a Surge-dammed Lake

Bibliographic Data

ID16864158
AuthorsSam G Collins (University of British Columbia), Garry K C Clarke (0000-0002-5658-0580, University of British Columbia)
Year1977
Volume30
Issue4
Publication date1977-01-01
Open AccessYes
TypeARTICLE
VenueARCTIC (JOURNAL)
Journal identifiersISSN: 0004-0843 • E-ISSN: 1923-1245
PublisherThe Arctic Institute of North America (PUBLISHER)
DOI10.14430/arctic2702
OpenAlexW2037209086
LanguageEN
Citations received1
References cited1

A survey was made in 1974 of the small lake which had formed as a result of the surge advance of Steele Glacier, Yukon Territory, in 1965-68. Maximum lake level is controlled by a drainage channel which passes over rock near the hydrologic left margin of Steele Glacier. Since the surge advance of 1965-68 the lake has twice drained subglacially, producing minor outburst floods on Steele Creek and increasing the discharge of the Donjek River which crosses the probable route of the Alaska Highway pipeline

Bathymetry · Channel (broadcasting) · Geography · Geomorphology · Geotechnical engineering · Glacier · Hydrology (agriculture) · Physical geography · Surge · Climate change and permafrost · Cryospheric studies and observations · Geology · Landslides and related hazards · Oceanography

  • A Short and Somewhat Personal History of Yukon Glacier Studies in the Twentieth Century

    Open Access•Garry K C Clarke•ARCTIC•2014

  • The Wood Yukon Expedition of 1935

    Open Access•Walter A Wood•Geographical Review•1936

Citations per year0.08
Citation span2014 - 2014 (1)
Highly citedNo

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