Late Pleistocene evolution of glacial Lake Purcell: a potential floodwater source to the Channeled Scabland
The Quaternary history of the Channeled Scabland (CS) and its primary floodwater sources during marine isotope stage (MIS) 2 are well documented and understood. However, putative floodwaters from glacial lakes in British Columbia are poorly understood; these lakes may have supplied floodwaters to th...
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| Format: | Thesis |
| Language: | unknown |
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2012
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| Online Access: | http://summit.sfu.ca/item/12488 |