Late Holocene glacial activity of Bridge Glacier, British Columbia coast mountains

Bridge Glacier is a prominent eastward-flowing valley glacier located on the east side of the Pacific Ranges within the southern British Columbia Coast Mountains. The terminus of Bridge Glacier has retreated at rates ranging from 0 to 125 m/year over the last 50 years and currently calves into progl...

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Bibliographic Details
Main Author: Allen, Sandra Michele
Other Authors: Smith, Daniel J.
Language:English
en
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/1828/2259