| ID |
611 |
| Citation |
Eyles, N. and Clague, J.J., 1991. Glaciolacustrine sedimentation during advance and retreat of the Cordilleran Ice Sheet in Central BC. Géographie physique et Quaternaire, 45: 317-331. 128 |
| Organization |
Géographie physique et Quaternaire, 45: 317-331. 128 |
| URL |
http://www.erudit.org/revue/gpq/1991/v45/n3/032878ar.html?vue=resume |
| Abstract/Description or Keywords |
The maximum thickness of Pleistocene sediment in Okanagan Lake basin approaches 800 m. Forty-six seismic reflection traverses and an axial profile show a relatively simple stratigraphy composed of three seismic sequences argued to be no older than the last glacial cycle (< 30 ka). |
| Information Type |
article |
| Regional Watershed |
Province |
| Sub-watershed if known |
|
| Aquifer # |
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| Comments |
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| Project status |
complete |
| Contact Name |
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| Contact Email |
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