데이터셋 상세
캐나다
On the origin of aggradational ice in permafrost
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데이터 정보
연관 데이터
Cryostratigraphic record of permafrost degradation and recovery following historic (1898–1992) surface disturbances in the Klondike region, central Yukon Territory
공공데이터포털
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The Cordilleran Glacier
공공데이터포털
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Studies of an active rock glacier, east side Slims River valley, Yukon Territory
공공데이터포털
not_specified
Snow-pack development and ground freezing, Blackstone Uplands, Yukon Territory
공공데이터포털
not_specified
Glacial history, paleogeography and paleoenvironments in glaciated North America
공공데이터포털
not_specified
Formation and wastage of neoglacial surge moraines of the Klutlan Glacier, Yukon Territory, Canada
공공데이터포털
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Gravity and temperature measurement on the Fox glacier, Yukon
공공데이터포털
not_specified
Isotopic identification of subglacial processes
공공데이터포털
A comprehensive stable isotope study of basal ice and debris layers in two Yukon surging glaciers suggests an isotopically variable basal freezing cycle. Trapridge and Backe glaciers, St. Elias Range, Yukon, have parallel basal debris layers that extend for hundreds of metres along marginal ice faces and in meltwater tunnels. Both glaciers are subpolar surging glaciers that surge on a cycle of 40-50 years. They are approximately 5 km long and 1 km wide with a lower ablation zone that is frozen to the bed and an upper accumulation zone that has basal ice at the pressure melting temperature.
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