Ygdrasil Mountain

Last updated
Ygdrasil Mountain
Ygdrasil Mountain.jpg
Northeast aspect, aerial view
Highest point
Elevation 2,960 m (9,710 ft) [1]
Listing Mountains of British Columbia
Coordinates 51°44′14″N117°49′25″W / 51.73722°N 117.82361°W / 51.73722; -117.82361 [2]
Naming
Etymology Yggdrasil
Geography
Canada British Columbia relief location map.jpg
Red triangle with thick white border.svg
Ygdrasil Mountain
Location in British Columbia
Canada relief map 2.svg
Red triangle with thick white border.svg
Ygdrasil Mountain
Location in Canada
Ygdrasil Mountain
Interactive map of Ygdrasil Mountain
Country Canada
Province British Columbia
District Kootenay Land District [3]
Parent range Adamant Range [1]
Selkirk Mountains
Topo map NTS 82N12 Mount Sir Sandford [2]

Ygdrasil Mountain is a 2,960-metre (9,710-foot) mountain in British Columbia, Canada.[ citation needed ]

Contents

Description

Ygdrasil Mountain is part of the Adamant Range which is a subrange of the Selkirk Mountains. [3] It is located 77 km (48 mi) northwest of Golden and 30 km (19 mi) north of Glacier National Park. Ygdrasil is highly glaciated with glaciers radiating in all directions, most notably the Gothics Glacier to the north. Precipitation runoff and glacial meltwater from the mountain drains to Kinbasket Lake via Smith Creek. Topographic relief is significant as the summit rises 2,200 metres (7,218 ft) above the lake in 9 km (5.6 mi).[ citation needed ]

Etymology

The mountain's toponym was officially adopted on March 4, 1965, by the Geographical Names Board of Canada. [2] The mountain was named in 1954 by William Lowell Putnam III for Yggdrasil, the great ash tree symbolizing the universe according to Norse mythology. [3] It is pronounced "ig DRAYsel" and was so named to follow the naming theme of nearby Mount Wotan and Mount Fria which were also derived from Norse mythology.[ citation needed ]

Climate

Based on the Köppen climate classification, Ygdrasil Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. [4] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports glaciers surrounding the peak.[ citation needed ]

See also

Related Research Articles

<span class="mw-page-title-main">Wedgwood Peak</span> Mountain in the country of Canada

Wedgwood Peak is a 3,024-metre (9,921-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Assiniboine, 2.0 km (1.2 mi) to the south. The mountain is situated northwest of Lake Magog and 1.0 km (0.62 mi) south of Sunburst Peaks.

<span class="mw-page-title-main">Avalanche Mountain</span> Mountain in British Columbia, Canada

Avalanche Mountain is a 2,861-metre (9,386-foot) summit in Glacier National Park in the Selkirk Mountains in British Columbia, Canada. Its nearest higher peak is Mount Macdonald, 2.2 km (1.4 mi) to the north. Mount Sir Donald is 3.83 km (2.38 mi) to the southeast, and Eagle Peak is 1.46 km (0.91 mi) to the south-southeast. The Avalanche Glacier is situated on the east side of the peak, and the Connaught Tunnel lies partially beneath Avalanche Mountain. The peak is visible from eastbound Highway 1, the Trans-Canada Highway approaching Rogers Pass. During winter and spring of each year the western slope, named Avalanche Crest, generates avalanches which can threaten the highway.

<span class="mw-page-title-main">Mount Weart</span> Triple summit mountain in the country of Canada

Mount Weart is a 2,835-metre (9,301-foot) triple-summit mountain located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated 14 km (9 mi) northeast of Whistler, and its nearest higher peak is Wedge Mountain, 3.7 km (2 mi) to the south, which is the only peak within the park higher than Weart. The Armchair Glacier rests below the west aspect of the summit, and the massive Weart Glacier spans the northern and eastern aspects of the mountain. Precipitation runoff from the peak and meltwater from the glaciers drains into Wedgemount Lake and tributaries of the Lillooet River.

<span class="mw-page-title-main">Mount Thiassi</span> Mountain in the country of Canada

Mount Thiassi is a 2,772-metre (9,094-foot) mountain summit located in the Thiassi Range of the Coast Mountains, in southwestern British Columbia, Canada. It is the third-highest point in the Thiassi Range. Mount Thiassi is situated 56 km (35 mi) northwest of Pemberton, and 6.9 km (4 mi) south-southwest of Mount Vayu, which is its nearest higher peak. Precipitation runoff from the peak and meltwater from unnamed glaciers on its slopes drain into tributaries of the Lillooet, Bridge, and Hurley Rivers. The first ascent of the mountain was made in 1965 by Dick Culbert and Alice Purdey. The mountain's name was submitted by this first ascent party to commemorate Thiassi, the god of storms according to Norse mythology. The name was officially adopted June 22, 1967, by the Geographical Names Board of Canada.

<span class="mw-page-title-main">Mount Cartier</span> Mountain in British Columbia, Canada

Mount Cartier is a 2,610-metre (8,563-foot) mountain summit located in British Columbia, Canada.

<span class="mw-page-title-main">Mount Carr</span> Mountain in the country of Canada

Mount Carr is a 2,590-metre (8,497-foot) mountain summit located in British Columbia, Canada.

<span class="mw-page-title-main">Anniversary Peak</span> Mountain in British Columbia, Canada

Anniversary Peak is a 2,947-metre (9,669-foot) summit in The Bugaboos of British Columbia, Canada. It is located southeast of the Bugaboo Glacier, on the southern boundary of Bugaboo Provincial Park. Precipitation runoff from Anniversary Peak drains into Bugaboo Creek which is a tributary of the Columbia River. Anniversary Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,350 meters (4,429 ft) above Bugaboo Creek in 4 km (2.5 mi).

<span class="mw-page-title-main">Howser Peak</span> Mountain in British Columbia, Canada

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. 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).

<span class="mw-page-title-main">Moby Dick Mountain</span> Mountain in the country of Canada

Moby Dick Mountain is a 3,154-metre (10,348-foot) summit in British Columbia, Canada.

<span class="mw-page-title-main">Wallace Peak</span> Mountain in British Columbia, Canada

Wallace Peak is a 2,940-metre (9,650-foot) summit in British Columbia, Canada.

<span class="mw-page-title-main">Mount Nemo (British Columbia)</span> Mountain in the country of Canada

Mount Nemo is a 2,901-metre (9,518-foot) summit in British Columbia, Canada.

<span class="mw-page-title-main">Catamount Peak</span> Mountain peak in British Columbia

Catamount Peak is a 2,733-metre (8,967-foot) mountain located in Glacier National Park in British Columbia, Canada. Catamount Peak is part of the Hermit Range of the Selkirk Mountains and is 7 km (4.3 mi) west of Rogers Pass. It is approximately midway between Revelstoke and Golden. Neighbors include Cheops Mountain, 5.05 km (3.14 mi) to the east, and Ursus Major Mountain, 1.83 km (1.14 mi) to the northeast. Precipitation runoff from the mountain's south slope drains to Illecillewaet River via Cougar Brook, and the north slope drains to the Beaver River via Ursus Creek. Topographic relief is significant as the summit rises 1,230 metres (4,035 ft) above Ursus Creek in 2 km (1.2 mi) and 930 m (3,051 ft) above Cougar Brook in 1 km (0.62 mi). This peak is visible from the Trans-Canada Highway.

<span class="mw-page-title-main">Mount Loki</span> Mountain in British Columbia, Canada

Mount Loki is a 2,779-metre (9,117-foot) mountain summit located in British Columbia, Canada.

<span class="mw-page-title-main">Hall Peak (British Columbia)</span> Mountain in British Columbia, Canada

Hall Peak is a 3,048-metre (10,000-foot) mountain summit located in British Columbia, Canada.

<span class="mw-page-title-main">Houdini Needles</span> Mountain in British Columbia, Canada

Houdini Needles is a 2,663-metre (8,737-foot) mountain in British Columbia, Canada.

<span class="mw-page-title-main">Sentinel Peak (Adamant Range)</span> Mountain in Columbia-Shuswap Regional District, British Columbia, Canada

Sentinel Peak is a 2,992-metre (9,816-foot) mountain in British Columbia, Canada.

<span class="mw-page-title-main">Pioneer Peak (British Columbia)</span> Mountain in British Columbia, Canada

Pioneer Peak is a 3,245-metre (10,646-foot) mountain in British Columbia, Canada.

<span class="mw-page-title-main">Serendipity Spire</span> Mountain in British Columbia, Canada

Serendipity Spire is a 2,857-metre (9,373-foot) mountain in British Columbia, Canada.

<span class="mw-page-title-main">Mount Swiderski</span> Mountain in British Columbia, Canada

Mount Swiderski is a 3,133-metre (10,279-foot) mountain summit in British Columbia, Canada.

<span class="mw-page-title-main">Mount Battisti</span> Mountain in British Columbia, Canada

Mount Battisti is a 3,155-metre (10,351-foot) mountain summit in British Columbia, Canada.

References

  1. 1 2 Glen W. Boles, William Lowell Putnam, Roger W. Laurilla (2006), "Canadian Mountain Place Names", Rocky Mountain Books, ISBN   9781894765794, p. 275.
  2. 1 2 3 "Ygdrasil Mountain". Geographical Names Data Base . Natural Resources Canada . Retrieved 2023-09-04.
  3. 1 2 3 "Ygdrasil Mountain". BC Geographical Names . Retrieved 2023-09-04.
  4. 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.