| Title | Early growth of the last Cordilleran ice sheet deduced from glacio-isostatic depression in southwest British Columbia, Canada
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| Author | Clague, J J; Froese, D; Hutchinson, I; James, T S ; Simon, K M |
| Source | Quaternary Research (New York) vol. 63, 2005 p. 53-59, https://doi.org/10.1016/j.yqres.2004.09.007 |
| Image |  |
| Year | 2005 |
| Alt Series | Geological Survey of Canada, Contribution Series 2003322 |
| Publisher | Cambridge University Press (CUP) |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| File format | pdf (Adobe Acrobat Reader) |
| Province | British Columbia |
| NTS | 92B; 92C; 92F; 92G; 92J; 92K |
| Lat/Long WENS | -126.0000 -122.0000 51.0000 48.0000 |
| Subjects | general geology; structural geology; sea level changes; paleo-sea levels; isostatic rebound; eustatic submergence; ice sheets; glaciation |
| Illustrations | location maps; photographs; cross-sections, stratigraphic; tables |
| Program | NSERC Natural Sciences and Engineering Research Council of
Canada |
| Program | Simon Fraser University, Funding Program |
| Released | 2017 01 20 |
| Abstract | Relative sea level at Vancouver, British Columbia rose from below the present datum about 30,000 cal yr B.P. to at least 18 m above sea level 28,000 cal yr B.P. In contrast, eustatic sea level in this
interval was at least 85 m lower than at present. The difference in the local and eustatic sea-level positions is attributed to glacio-isostatic depression of the crust in the expanding forefield of the Cordilleran ice sheet during the initial phase
of the Fraser Glaciation. Our findings suggest that about 1 km of ice was present in the northern Strait of Georgia 28,000 cal yr B.P., early during the Fraser Glaciation. |
| GEOSCAN ID | 215393 |
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