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Cirque Morphometry in the Canadian Cordillera∗

Dados Bibliográficos

ID8375872
AutoresAlan S Trenhaile (University of Windsor, autor correspondente)
Ano1976
Volume66
Fascículo3
Páginas451-462
Data de publicação1976-09-01
Peer ReviewedSim
Open AccessNão
TipoARTICLE
PeriódicoAnnals of the Association of American Geographers (JOURNAL)
Identificadores do periódicoISSN: 0004-5608 • E-ISSN: 1467-8306
EditoraInforma UK Limited (PUBLISHER • GB)
DOI10.1111/j.1467-8306.1976.tb01101.x
OpenAlexW2043774019
IdiomaEN
Citações recebidas1
Referências 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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    Open Access•Rachel P Oien, Bartosz Kurjański•Quaternary International•2026

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Obras citantes distintas1
Citações por ano1
Intervalo de citações2026 - 2026 (1)
Velocidade de citaçãocurrent
Altamente citadoNão
Tipos de citaçãoNeutras: 1
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