Late pleistocene glacial and environmental history of the Skagit valley, Washington and British Columbia
Drainage patterns established in the Tertiary in the North Cascades were reorganized to accommodate southern drainage of Cordilleran Ice Sheet meltwater. Repeated continental glaciation rendered the Skagit an interconnected valley, with meltwater routes opening it to the Fraser and Okanogan watershe...
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| Format: | Thesis |
| Language: | English |
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2007
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| Online Access: | http://summit.sfu.ca/item/8099 |