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Distribution of active glaciers and rock glaciers compared to the distribution of permafrost landforms, based on freezing and thawing indices.

dc.contributor.authorHarris, S. A.en
dc.date.accessioned2025-03-25T01:25:13Z
dc.date.available2025-03-25T01:25:13Z
dc.date.issued1981en
dc.description.abstractClimatic stations near glacial termini and equilibrium lines show a distribution of freezing and thawing indices that does not conform to the boundaries derived from data for stations in areas of continuous and discontinuous permafrost. Active tongue-shaped rock glaciers have similar limits of freezing and thawing indices to the equilibrium lines of glaciers, while active labate rock glaciers have limits paralleling the limit for stations in the zone of continuous permafrost. This difference between the distributions of lobate and tongue-shaped rock glaciers explains why the active tongue-shaped rock glaciers can be used for indicating the limits of the permafrost areas in the Alps (a maritime regime), but cannot be used in that way in continental climates, e.g., Alberta, interior Yukon, and the Northwest Territories. -Authoren
dc.description.statustrueen
dc.format.extent6en
dc.identifier.otherScopus:0019391885en
dc.identifier.urihttps://dspace-test.anu.edu.au/handle/1885/733735835
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=0019391885&partnerID=8YFLogxKen
dc.language.isoEnglishen
dc.sourceCanadian Journal of Earth Sciencesen
dc.titleDistribution of active glaciers and rock glaciers compared to the distribution of permafrost landforms, based on freezing and thawing indices.en
dc.typeArticleen
local.bibliographicCitation.lastpage381en
local.bibliographicCitation.startpage376en
local.contributor.affiliationHarris, S. A.; University of Calgaryen
local.identifier.citationvolume18en
local.identifier.doi10.1139/e81-029en
local.identifier.pure164f5822-a9e4-484d-a172-94867dd85c43en
local.type.statusPublisheden

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