Mount Charlton (Canada)
Mount Charlton is a 3,217-metre (10,554-foot) mountain summit located on the west side of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Unwin, 1.2 km (0.75 mi) to the west.[1]
Mount Charlton | |
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Highest point | |
Elevation | 3,217 m (10,554 ft)[1][2] |
Prominence | 197 m (646 ft)[1] |
Parent peak | Mount Brazeau (3470 m)[1] |
Listing | Mountains of Alberta |
Coordinates | 52°36′41″N 117°30′40″W[3] |
Geography | |
Mount Charlton Location in Alberta Mount Charlton Mount Charlton (Canada) | |
Country | Canada |
Province | Alberta |
Parent range | Queen Elizabeth Ranges Canadian Rockies |
Topo map | NTS 83C12 Athabasca Falls |
Climbing | |
First ascent | 1921 W.R. Hainsworth, M.M. Strumia[1] |
History
The peak was named in 1911 by Mary Schäffer for H. R. Charlton, a railroad official who served with the Grand Trunk Pacific Railway as the General Advertising Agent.[4]
The first ascent was made in 1921 by W.R. Hainsworth and M.M. Strumia.[5][1]
The mountain's name was made official in 1947 by the Geographical Names Board of Canada.[3]
Climate
Based on the Köppen climate classification, Mount Charlton is located in a subarctic climate with cold, snowy winters, and mild summers.[6] Temperatures can drop below −20 degrees Celsius (−4 degrees Fahrenheit) with wind chill factors below −30 °C (−22 °F). Precipitation runoff from Mount Charlton drains into the Maligne River, which is a tributary of the Athabasca River.
References
- "Mount Charlton". Bivouac.com. Retrieved 2018-05-11.
- "Topographic map of Mount Charlton". opentopomap.org. Retrieved 2023-08-18.
- "Mount Charlton". Geographical Names Data Base. Natural Resources Canada. Retrieved 2018-12-16.
- Place-names of Alberta. Ottawa: Geographic Board of Canada. 1928. p. 32.
- "Mount Charlton". cdnrockiesdatabases.ca. Retrieved 2021-03-07.
- 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.