Purity Mountain | |
---|---|
Highest point | |
Elevation | 3,149 m (10,331 ft) [1] [2] [3] |
Prominence | 497 m (1,631 ft) [2] |
Parent peak | Mount Wheeler (3,336 m) [4] |
Isolation | 3.89 km (2.42 mi) [3] |
Listing | Mountains of British Columbia |
Coordinates | 51°05′41″N117°28′09″W / 51.09472°N 117.46917°W [5] |
Geography | |
Interactive map of Purity Mountain | |
Country | Canada |
Province | British Columbia |
District | Kootenay Land District |
Protected area | Glacier National Park |
Parent range | Selkirk Mountains Purity Range |
Topo map | NTS 82N3 Mount Wheeler [5] |
Climbing | |
First ascent | 1890 |
Purity Mountain is a 3,149-metre (10,331-foot) summit in British Columbia, Canada.
Purity Mountain is located along the southern boundary of Glacier National Park, and is the westernmost peak of the compact Purity Range, a subrange of the Selkirk Mountains. [6] Purity is an attractive peak surrounded on three sides by névés, with no less than six glaciers radiating from it. [6] On every side there is a wilderness of snow and ice above the rich green forests of the valleys. Precipitation runoff from the mountain drains north into Van Horne Brook, and southeast into Battle Brook which are both tributaries of the Incomappleux River. Purity Mountain is more notable for its steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the summit rises 1,650 m (5,410 ft) above Van Horne Brook in 3 km (1.9 mi).
The mountain was named in August 1890 by Harold Ward Topham of the Alpine Club of England who saw it from Donkin Pass. [7] [6] The mountain's toponym was officially adopted on May 29, 1901, by the Geographical Names Board of Canada. [7]
The first ascent of the summit was made in 1890 by Harold Ward Topham, Emil Huber, and Henry Forster. [6]
Based on the Köppen climate classification, Purity Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. [8] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Van Horne Névé on the south slope, Odin Glacier on the east slope, and Purity Glacier to the north of the peak.
Mount Wheeler, is a 3,336-metre (10,945-foot) mountain summit located in Glacier National Park of British Columbia, Canada. It is the third-highest peak in the park, and sixth-highest in the Selkirk Mountains range. The mountain is a remote 60 km (37 mi) east of Revelstoke, and 40 km (25 mi) southwest of Golden. Its nearest higher peak is Mount Selwyn, 5.1 km (3.2 mi) to the north-northwest. Mount Wheeler is surrounded by ice, including the Deville Glacier, Deville Névé, Black Glacier, and Thor Glacier. Precipitation runoff from the mountain and meltwater from its glaciers drains into tributaries of the Incomappleux and Beaver Rivers.
Mount Topham, is a 2,872-metre (9,423-foot) mountain summit located in Glacier National Park of British Columbia, Canada. It is part of the Selkirk Mountains range. The mountain is a remote 60 km (37 mi) east of Revelstoke, and 32 km (20 mi) southwest of Golden. Its nearest higher peak is Mount Selwyn, 2.66 km (1.65 mi) to the west. Mount Topham is situated along the western edge of the Deville Glacier. Precipitation runoff from the mountain drains into the Beaver River. Mount Topham was named in 1902 by Arthur Oliver Wheeler to honor Harold Ward Topham (1857–1915), an English mountaineer who explored and mapped the Selkirks. The mountain's name was officially adopted September 8, 1932, by the Geographical Names Board of Canada. Based on the Köppen climate classification, Mount Topham is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.
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