Latest Pleistocene and Holocene behaviour of Franklin Glacier, Mt. Waddington Area, British Columbia Coast Mountains, Canada
Holocene climate variability in the British Columbia Coast Mountains has resulted in repeated intervals of glacier expansion and retreat. Since reaching their late Holocene maximum positions in the late 20th century, glaciers in the region have experienced significant volumetric loss. The subsequent...
| Main Author: | |
|---|---|
| Other Authors: | |
| Language: | English en |
| Published: |
2015
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/1828/6111 |