Mount Tuzo, previously "Peak Seven" or "Shagowa", was named in 1907 after its first ascendant Henrietta L. Tuzo. It is located within the Valley of the Ten Peaks in the Canadian Rockies, along the Continental Divide, which forms the boundary between British Columbia and Alberta in this region.[1][2]
Mount Tuzo | |
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Highest point | |
Elevation | 3,248 m (10,656 ft)[1] |
Prominence | 210 m (690 ft)[2] |
Listing | Mountains of Alberta Mountains of British Columbia |
Coordinates | 51°18′06″N 116°13′42″W[3] |
Geography | |
Mount Tuzo Location in Alberta | |
Location | Alberta/British Columbia, Canada |
Parent range | Valley of the Ten Peaks |
Topo map | NTS 82N8 Lake Louise[3] |
Climbing | |
First ascent | 15 September 1906 Henrietta Tuzo, Christian Kaufmann |
Easiest route | Peak 7 |
Like other mountains in Banff Park, Mount Tuzo is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.[4] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[5]
Based on the Köppen climate classification, Mount Tuzo is located in a subarctic climate zone with cold, snowy winters, and mild summers.[6] Temperatures can drop below -20 C with wind chill factors below -30 C.
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