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Cirque Morphometry in the Canadian Cordillera∗

Datos Bibliográficos

ID8375872
AutoresAlan S Trenhaile (University of Windsor, autor de correspondencia)
Año1976
Volumen66
Número3
Páginas451-462
Fecha de publicación1976-09-01
Peer ReviewedSí
Open AccessNo
TipoARTICLE
RevistaAnnals of the Association of American Geographers (JOURNAL)
Identificadores de la revistaISSN: 0004-5608 • E-ISSN: 1467-8306
EditorialInforma UK Limited (PUBLISHER • GB)
DOI10.1111/j.1467-8306.1976.tb01101.x
OpenAlexW2043774019
IdiomaEN
Citas recibidas1
Referencias citadas1

Cirques in the southern Canadian Cordillera are most numerous at lowest elevations and best developed on the north and northeastern flanks of mountains. Cirques at the heads of major valleys are generally at higher elevation, and are larger in area than cirques along the sides of valleys. The elevation frequency distribution is different for various types of cirque. Cirques which are well below mean cirque elevation are large and are almost always oriented to the north and northeast. Cirques well above mean cirque elevation are small and independent of orientation. A model is proposed in which cirque morphometry varies in a vertical plane in relation to the position of the snowline, and in a horizontal plane in relation to orientation

Cirque · Cirque glacier · Climatology · Elevation (ballistics) · Geography · Geometry · Geomorphology · Glacier · Physical geography · Cryospheric studies and observations · Geology · Geology and Paleoclimatology Research · Landslides and related hazards · Mathematics

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Obras citantes distintas1
Citas por año1
Intervalo de citas2026 - 2026 (1)
Velocidad de citacióncurrent
Altamente citadoNo
Tipos de citaNeutras: 1
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