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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Language: | English en |
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2010
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Online Access: | http://hdl.handle.net/1828/2259 |