| Reference Type | Journal (article/letter/editorial) |
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| Title | Coquitlam Drift: a pre-Vashon Fraser glacial formation in the Fraser Lowland, British Columbia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Hicock, Stephen R. | Author |
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| Armstrong, John E. | Author |
| Year | 1981 (September 1) | Volume | 18 |
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| Issue | 9 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e81-135Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 477211 | Long-form Identifier | mindat:1:5:477211:2 |
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| GUID | 0 |
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| Full Reference | Hicock, Stephen R., Armstrong, John E. (1981) Coquitlam Drift: a pre-Vashon Fraser glacial formation in the Fraser Lowland, British Columbia. Canadian Journal of Earth Sciences, 18 (9) 1443-1451 doi:10.1139/e81-135 |
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| Plain Text | Hicock, Stephen R., Armstrong, John E. (1981) Coquitlam Drift: a pre-Vashon Fraser glacial formation in the Fraser Lowland, British Columbia. Canadian Journal of Earth Sciences, 18 (9) 1443-1451 doi:10.1139/e81-135 |
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| In | (1981, September) Canadian Journal of Earth Sciences Vol. 18 (9) Canadian Science Publishing |
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| Abstract/Notes | Coquitlam Drift is formally defined and stratotypes established for it in the Coquitlam β Port Moody area, B.C. It is a Pleistocene formation consisting of till, glaciofluvial, ice-contact, and glaciomarine sediments deposited between 21β700 and 18β700 years BP, during the Fraser Glaciation (late Wisconsin) and prior to the main Vashon glacial maximum at about 14β500 years BP. The drift was deposited in short pulses by valley and piedmont glaciers fluctuating into the Fraser Lowland from the Coast Mountains to the north and Cascade Mountains to the east. |
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