| Mount Murchison | |
| Elevation M: | 3348 |
| Elevation Ref: | [1] |
| Prominence M: | 988 |
| Prominence Ref: | [2] |
| Range: | Murchison Group Canadian Rockies |
| Parent Peak: | Mount Hector (3394 m)[3] |
| Listing: | Mountains of Alberta |
| Etymology: | Roderick Murchison |
| Location: | Alberta, Canada |
| Map: | Canada Alberta#Canada |
| Coordinates: | 51.9331°N -116.675°W |
| Coordinates Ref: | [4] |
| Rock: | Sedimentary |
| Age: | Cambrian |
| First Ascent: | August 25, 1996 by Reg Bonney, Rick Collier, John Holmes, Jerre Skvaril |
| Easiest Route: | technical climb |
Mount Murchison is a 33480NaN0 mountain summit located at the convergence of the North Saskatchewan River valley and Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The main summit has two high points: the Southeast Peak is 3,348 m, whereas the Northwest Peak is 3,333 m and separated by 700 m distance. Its nearest higher peak is Mount Cline, 15.71km (09.76miles) to the north.[5] Mount Murchison is situated immediately southeast of the confluence of the North Saskatchewan River, Mistaya River, and Howse River near Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway.
Named by James Hector as he traversed the Mistaya Valley in September of 1858, Mount Murchison honors Sir Roderick Impey Murchison (1792-1871), a prominent English geologist and director of the Geological Survey of Great Britain.[6] The mountain's name became official in 1924.[4] The first ascent of the Northwest Peak was in 1902 by Norman Collie, H.E.M. Stutfield, G.M. Weed, and Hans Kaufmann.[7] The first ascent of the Southeast Peak was made August 25, 1996, by Reg Bonney, Rick Collier, John Holmes, and Jerre Skvaril.[1]
Like other mountains in Banff Park, the Murchison massif 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.[8] The massif, which covers an area measuring five km by seven km (7400 acres), is characterized by seven rocky towers and glacial ice of the Murchison Icefield.
| Name | Elevation | Prominence | First Ascent | |
|---|---|---|---|---|
| Hall Tower | 3216 m | 183 m | 1940 | |
| Bison Tower | 3185 m | 183 m | ||
| Cromwell Tower | 3213 m | 28 m | ||
| Feuz Tower | 3124 m | 183 m | 1941 | |
| Gest Tower | 3170 m | 690 m | 1937 | |
| South East Tower | 3094 m | 153 m | 1939 | |
| Englehard Tower | 3216 m | 366 m |
Based on the Köppen climate classification, Mount Murchison is located in a subarctic climate with cold, snowy winters, and mild summers.[9] Temperatures can drop below -20 °C with wind chill factors below -30 °C. Weather conditions during winter make Mount Murchison a destination in the Rockies for ice climbing. Precipitation runoff from Mount Murchison drains into tributaries of the Saskatchewan River.
Ice Climbing Routes with grades on Mount Murchison[10] [11]