Banded Peak is a 2,934-metre (9,626-foot) summit located in the Elbow River valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. Banded Peak has a distinctive limestone cliff band which gave it its descriptive name. Its name has been used since around 1896.[1] The peak is visible from Highway 66, weather permitting. The mountain's name became official in 1951 by the Geographical Names Board of Canada.[2]
| Banded Peak | |
|---|---|
.jpg) Banded Peak | |
| Highest point | |
| Elevation | 2,934 m (9,626 ft)[1] |
| Prominence | 282 m (925 ft)[1] |
| Parent peak | Outlaw Peak (2957 m)[1] |
| Coordinates | 50°43′06″N 114°55′05″W / 50.71833°N 114.91806°W[2] |
| Geography | |
  Banded Peak Location of Banded Peak in Alberta  Banded Peak Banded Peak (Canada) | |
| Location | Alberta, Canada |
| Parent range | Kananaskis Range Canadian Rockies |
| Topo map | NTS 82J10 Mount Rae[2] |
| Geology | |
| Rock age | Cambrian |
| Rock type | limestone, shale |
| Climbing | |
| Easiest route | Scrambling |
Geology
editBanded Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[3]
Climate
editBased on the Köppen climate classification, Banded Peak is located in a subarctic climate with cold, snowy winters, and mild summers.[4] Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from the mountain drains into the Elbow River which is a tributary of the Bow River.
Gallery
edit-
Banded Peak in upper right corner
.jpg)
See also
editReferences
edit- ^ a b c d "Banded Peak". Bivouac.com. Retrieved 2018-11-15.
- ^ a b c "Banded Peak". Geographical Names Data Base. Natural Resources Canada. Retrieved 2018-11-15.
- ^ Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
- ^ Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.