| Reference Type | Journal (article/letter/editorial) |
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| Title | Northern extent of Lake Agassiz in eastern Saskatchewan |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Langford, F. F. | Author |
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| Year | 1977 (June 1) | Volume | 14 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e77-117Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 475413 | Long-form Identifier | mindat:1:5:475413:2 |
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| GUID | 0 |
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| Full Reference | Langford, F. F. (1977) Northern extent of Lake Agassiz in eastern Saskatchewan. Canadian Journal of Earth Sciences, 14 (6) 1286-1291 doi:10.1139/e77-117 |
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| Plain Text | Langford, F. F. (1977) Northern extent of Lake Agassiz in eastern Saskatchewan. Canadian Journal of Earth Sciences, 14 (6) 1286-1291 doi:10.1139/e77-117 |
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| In | (1977, June) Canadian Journal of Earth Sciences Vol. 14 (6) Canadian Science Publishing |
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| Abstract/Notes | Surveys for a proposed hydroelectric dam, disclosed extensive deposits of late Pleistocene lacustrine clay in the valleys of the Churchill and Reindeer Rivers. The presence of montmorillonite in these clays and the topographic configuration suggest continuous connection to the main body of Glacial Lake Agassiz. The presence of till layers above the lacustrine deposits is explained by subaqueous slumping rather than read vance of the glacier, which retreated from this area between 10 000 and 9 000 years ago. |
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