| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Late Quaternary geology and geomorphology of the Elk Valley, southeastern British Columbia |
|---|
| Journal | Canadian Journal of Earth Sciences |
|---|
| Authors | George, H. | Author |
|---|
| Gorman, W. A. | Author |
| VanDine, D. F. | Author |
| Year | 1987 (April 1) | Volume | 24 |
|---|
| Issue | 4 |
|---|
| Publisher | Canadian Science Publishing |
|---|
| DOI | doi:10.1139/e87-072Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 479500 | Long-form Identifier | mindat:1:5:479500:5 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | George, H., Gorman, W. A., VanDine, D. F. (1987) Late Quaternary geology and geomorphology of the Elk Valley, southeastern British Columbia. Canadian Journal of Earth Sciences, 24 (4) 741-751 doi:10.1139/e87-072 |
|---|
| Plain Text | George, H., Gorman, W. A., VanDine, D. F. (1987) Late Quaternary geology and geomorphology of the Elk Valley, southeastern British Columbia. Canadian Journal of Earth Sciences, 24 (4) 741-751 doi:10.1139/e87-072 |
|---|
| In | (1987, April) Canadian Journal of Earth Sciences Vol. 24 (4) Canadian Science Publishing |
|---|
| Abstract/Notes | Glacial stratigraphy and geomorphology of the bottom areas of the Elk Valley support the existence of one major ice advance, presumably during the late Wisconsinan. Its retreat probably occurred in two stages by orderly frontal withdrawal. Glacial Lake Elk, formed within the Elk Valley from meltwaters released by this glacier, was dammed initially by an ice plug from the Rocky Mountain Trench glacier at a point near Morrissey and subsequently less than 3 km upvalley from Elko. The lake drained in at least three stages. |
|---|
These are possibly similar items as determined by title/reference text matching only.
