Long-term nivation rates, Cathedral Massif, northwestern British Columbia
Cryoplanation terraces (CTs) are large (3000–800 000 m2) erosional landforms found in upland periglacial environments. Two hypotheses for the formation of CTs are supported in contemporary literature: (1) CT formation is controlled primarily by geologic structure; and (2) CTs are climatically contro...
| Main Authors: | , |
|---|---|
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
NRC Research Press (a division of Canadian Science Publishing)
2020
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/1807/102078 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2019-0176 |