Published September 12, 2021 | Version v1
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Hypsoclinometric evidence of the degree of modification of mountains by glacial erosion.

  • 1. Durham University


Power Point for presentation on-line at Geomorphometry 2021 (Perugia, Italy).

For two mountain ranges in the British Columbia Coast Mountains, the clearest signal of glacial erosion is the high % of steep slopes at cirque headwall altitudes.  This is stronger in the Bendor Range than in the Shulaps.  Steeper slopes also show a clear northward tendency, comparable to that of cirque aspects.


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Conference paper: 10.30437/GEOMORPHOMETRY2020_21. (DOI)