Mount Loki | |
---|---|
Highest point | |
Elevation | 2,779 m (9,117 ft) [1] |
Prominence | 609 m (1,998 ft) [2] |
Parent peak | Mount Findlay (3,162 m) [2] |
Isolation | 5.47 km (3.40 mi) [2] |
Listing | Mountains of British Columbia |
Coordinates | 49°50′30″N116°45′10″W / 49.84167°N 116.75278°W [3] |
Naming | |
Etymology | Loki |
Geography | |
Interactive map of Mount Loki | |
Country | Canada |
Province | British Columbia |
District | Kootenay Land District |
Parent range | Purcell Mountains |
Topo map | NTS 82F15 Kaslo [3] |
Climbing | |
Easiest route | Climbing trail |
Mount Loki is a 2,779-metre (9,117-foot) mountain summit located in British Columbia, Canada.
This prominent peak is situated 13 km (8 mi) southeast of Kaslo on the eastern side of Kootenay Lake. [4] It is part of the Purcell Mountains and the nearest higher neighbor is Mount Baldr, 5.5 km (3 mi) to the northeast. [2] Precipitation runoff from the peak's slopes drains west to Kootenay Lake via Loki and Bernard creeks. Topographic relief is significant as the summit rises 1,480 metres (4,855 ft) above Loki Creek in approximately 2.5 km (1.6 mi) and 2,250 metres (7,382 ft) above Kootenay Lake in 7 km (4.3 mi). The peak can be seen from Highway 31.
The mountain is named for Loki, a mischievous character in Norse mythology able to change his shape and engage in sight-deceiving magic. [4] The toponym was officially adopted on December 7, 1937, by the Geographical Names Board of Canada as originally labelled on George Mercer Dawson's Geological Survey of Canada map published in 1890. [4] Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. [5]
Based on the Köppen climate classification, Mount Loki is located in a subarctic climate zone of western North America. [6] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Mount Loki.
Foster Peak is a 3,204-metre (10,512-foot) mountain summit located on the western border of Kootenay National Park. It is the highest point in the Vermilion Range, a sub-range of the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Ball, 14.96 km (9.30 mi) to the northeast. The mountain is part of what is known as The Rockwall. Floe Lake, southeast of the peak, is one of the beauty spots of Kootenay National Park. The area is accessible via the Floe Lake Trail and Rockwall Trail. The Rockwall Trail is a scenic 55 kilometre traverse of alpine passes, subalpine meadows, hanging glaciers, and limestone cliffs, in some places in excess of 900 metres above the trail.
Joffre Peak is a 2,721-metre (8,927-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 26 km (16 mi) east of Pemberton and 11 km (7 mi) northeast of Lillooet Lake. Joffre is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,500 meters (4,920 ft) above Cayoosh Creek in 4 km (2.5 mi). The nearest higher peak is Mount Matier, 1.6 km (1 mi) to the south. The mountain's climate supports the Matier Glacier on the southwest slope, and the Anniversary Glacier on the southeast slope. Precipitation runoff from the peak drains into Joffre Creek and Cayoosh Creek which are both within the Fraser River watershed.
Gladsheim Peak is a prominent 2,830-metre (9,280-foot) mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Gladsheim is the highest point in the Valhalla Ranges. It is situated in the southern part of Valhalla Provincial Park, 2.7 km (1.7 mi) northeast of Gimli Peak, and 12 km (7.5 mi) west of Slocan and Slocan Lake. The name "Valhalla Mountains" first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. Gladsheim is the magnificent meeting hall containing thirteen council seats where, according to Norse mythology, Odin presided over all the realms. In keeping with the Valhalla theme, this peak's name was submitted in 1900 by R. W. Brock to the Geological Survey of Canada for consideration, and it was officially adopted March 31, 1924, by the Geographical Names Board of Canada.
Asgard Peak is a 2,825-metre (9,268-foot) mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Asgard Peak is the second-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, 2.1 km (1.3 mi) to the east. It is situated in the southern part of Valhalla Provincial Park, 6 km (3.7 mi) south of Devils Couch, and 13 km (8.1 mi) west of Slocan and Slocan Lake. The name "Valhalla Mountains" first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. In keeping with the Valhalla theme, this peak's name was submitted February 1970 by Robert Dean of the Kootenay Mountaineering Club for consideration, and it was officially adopted March 3, 1971, by the Geographical Names Board of Canada. Asgard, according to Norse mythology, is the section of Valhalla where the twelve gods dwell. Based on the Köppen climate classification, Asgard Peak has a subarctic climate with cold, snowy winters, and mild summers. This climate supports a small glacier on the peak's north slope. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Slocan River.
Midgard Peak is a 2,807-metre (9,209-foot) mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, 2.9 km (1.8 mi) to the east-northeast. The nearest higher neighbor is Asgard Peak, 0.9 km (0.56 mi) to the northeast. It is situated on the southern border of Valhalla Provincial Park, 1.1 km (0.68 mi) northwest of Gimli Peak, and 14 km (8.7 mi) west of Slocan and Slocan Lake.
Gimli Peak is a 2,806-metre (9,206 ft) mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Gimli Peak is the fourth-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, 2.7 km (1.7 mi) to the north. Its nearest higher peak is Midgard Peak, 1.8 km (1.1 mi) to the northwest. It is situated in southern Valhalla Provincial Park, immediately southwest of Mulvey Lakes, and 12 km (7.5 mi) west of Slocan and Slocan Lake. The name "Valhalla Mountains" first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. In keeping with the Valhalla theme, this peak was originally labelled "Mount Gimli" on a 1900 Geological Survey of Canada publication, and it was officially adopted April 29, 1998, by the Geographical Names Board of Canada as Gimli Peak. According to Norse mythology, Gimli is the place where the righteous survivors of Ragnarök are foretold to live. Based on the Köppen climate classification, Gimli Peak has a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Slocan River.
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