Quaternary stratigraphy and geomorphology of the Lower Thompson Valley , British Columbia
The Thompson Valley between Spences Bridge and Lytton, where it joins the Fraser, merits attention because of the abundance of clear sections of late glacial and postglacial deposits in road and rail cuts, and its position as an important transition zone between the glacial lake deposition of the so...
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Format: | Thesis |
Language: | English |
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University of British Columbia
1970
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Online Access: | http://hdl.handle.net/2429/34677 |