A pre-Paris ice-sheet limit near Guelph, southern Ontario
The Guelph Moraine, a previously undesignated end moraine between Hespeler and Rockwood, is described and shown to be the consequence of a limited readvance that interrupted the general recession from the Guelph area of ice that deposited the Port Stanley Till rather than of a precursive advance of...
| Published in: | Canadian Journal of Earth Sciences |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Canadian Science Publishing
1988
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| Online Access: | http://dx.doi.org/10.1139/e88-176 http://www.nrcresearchpress.com/doi/pdf/10.1139/e88-176 |