| Crowfoot Mountain | |
|---|---|
| Crowfoot Glacier and Mountain, plus Bow Lake | |
| Highest point | |
| Elevation | 3,055 m (10,023 ft) [1] |
| Prominence | 355 m (1,165 ft) [1] |
| Parent peak | Mount Olive |
| Listing | Mountains of Alberta |
| Coordinates | 51°37′30″N116°26′00″W / 51.62500°N 116.43333°W [1] |
| Geography | |
| |
| Interactive map of Crowfoot Mountain | |
| Location | Alberta, Canada |
| Parent range | Canadian Rockies |
| Topo map | NTS 82N9 Hector Lake [2] |
| Climbing | |
| First ascent | 1950 by 1950 E. Cromwell and G. Engelhard [1] |
Crowfoot Mountain is a mountain within Banff National Park in Alberta, Canada. The Crowfoot Glacier sits on the northeastern flank of the mountain.
The mountain was named in 1959 after the glacier. [1]
Like other mountains in Banff Park, Crowfoot Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. [3] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. [4]
Based on the Köppen climate classification, Crowfoot Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. [5] Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Crowfoot Mountain drains into the Bow River which is a tributary of the Saskatchewan River.
Media related to Crowfoot Mountain at Wikimedia Commons