Howser Peak | |
---|---|
Highest point | |
Elevation | 3,094 m (10,151 ft) [1] |
Prominence | 262 m (860 ft) [2] |
Parent peak | Howser Spire (3,412 m) [3] |
Isolation | 2.96 km (1.84 mi) [4] |
Listing | Mountains of British Columbia |
Coordinates | 50°42′17″N116°47′01″W / 50.70472°N 116.78361°W [5] |
Geography | |
Country | Canada |
Province | British Columbia |
District | Kootenay Land District |
Protected area | Bugaboo Provincial Park |
Parent range | Purcell Mountains The Bugaboos [2] |
Topo map | NTS 82K10 Howser Creek |
Geology | |
Age of rock | 135 Million years ago [6] |
Type of rock | Granodiorite [6] |
Climbing | |
First ascent | 1916 by Conrad Kain |
Howser Peak is a 3,094-metre (10,151-foot) summit in The Bugaboos of British Columbia, Canada. It is located south of the Bugaboo Glacier and is the southernmost point of Bugaboo Provincial Park. [7] Precipitation runoff from Howser Peak drains north into Bugaboo Creek which is a tributary of the Columbia River; as well as south to Duncan River via Howser Creek. Howser Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the south aspect rising 1,380 meters (4,527 ft) in 2.5 km (1.6 mi).
The mountain's toponym was published in "A Climber's Guide to the Interior Ranges of British Columbia" by J.M. Thorington in 1947, [7] and it was officially adopted on October 29, 1962, by the Geographical Names Board of Canada. [5] The peak is named in association with Howser Creek which in turn is named after prospector Fred Hauser who found placer gold there in the late 1800s. [1] [8]
The first ascent of the peak was made on August 28, 1916, by Conrad Kain and Captain Albert H. MacCarthy. [9]
Based on the Köppen climate classification, Howser Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. [10] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Bugaboo Glacier on the peak's north slope and smaller unnamed glaciers on the east and west slopes.
The Bugaboos are a mountain range in the Purcell Mountains of eastern British Columbia, Canada. The granite spires of the group are a popular mountaineering destination. The Bugaboos are protected within Bugaboo Provincial Park.
Snowpatch Spire is a mountain peak in British Columbia, Canada. With its first ascent in 1940, it was the last of the Bugaboo Spires to be climbed. It is located southwest of the Conrad Kain hut, between Bugaboo, Vowell and Crescent Glaciers, at the south end of Bugaboo Provincial Park. The mountain's toponym was officially adopted October 29, 1962, by the Geographical Names Board of Canada.
Howser Spire, or Howser Spire Massif, is a group of three distinct granite peaks, and the highest mountain of the Canadian Bugaboo Spires. The mountain is located at the southwest corner of the Vowell Glacier, within the Bugaboo mountain range in the Purcell Mountains, a subrange of British Columbia's Columbia Mountains, The highest of the three spires is the North Tower at 3,412 m (11,194 ft), the Central Tower the lowest, and the South Tower is slightly lower than the North at 3,292 m (10,801 ft).
Cinnamon Peak is a 2,727-metre (8,947-foot) mountain summit located in the northwestern part of Mount Robson Provincial Park, in the Canadian Rockies of British Columbia, Canada. It is situated immediately north of the confluence of the Robson River and the Fraser River, and is visible from the Yellowhead Highway near the park's visitor centre. The peak was labelled "Little Grizzly" on Arthur Oliver Wheeler's 1911 topographic map of Mount Robson. He thought it appeared similar to Mount Grizzly in the Selkirk Mountains, but the name was later changed to Cinnamon, which is the coloration of the peak and the Cinnamon bear, which can be easily mistaken for a grizzly bear. "Little Grizzly" is a colloquial term for the black bear, Ursus americanus. Eastern populations are typically black in color, however western populations can be cinnamon colored. The mountain's toponym was officially adopted in 1951 by the Geographical Names Board of Canada. The nearest higher peak is Whitehorn Mountain, 6.0 km (3.7 mi) to the north.
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