Glacier Pikes

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Glacier Pikes
Garibaldi Lake3.jpg
Glacier Pikes (upper left)
Highest point
Elevation 2,145 m (7,037 ft) [1]
Prominence 247 m (810 ft) [1]
Coordinates 49°52′46″N122°58′44″W / 49.87944°N 122.97889°W / 49.87944; -122.97889 [2]
Geography
Country Canada
Province British Columbia
District New Westminster Land District
Protected area Garibaldi Provincial Park
Parent range Garibaldi Ranges
Topo map NTS   92G15 Mamquam Mountain
Geology
Age of rock Pleistocene
Mountain type Lava dome
Last eruption Pleistocene
Climbing
First ascent 1911 BCMC Party [3]
Easiest route Scramble

Glacier Pikes is a lava dome, located in the Garibaldi Lake volcanic field, British Columbia, Canada. The dome has two rocky points at the southern end of the Sentinel Glacier Neve. It is located within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. The mountain's toponym was officially adopted on May 3, 1951, by the Geographical Names Board of Canada. [2]

Contents

Climate

Based on the Köppen climate classification, Glacier Pikes is located in the marine west coast climate zone of western North America. [4] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

See also

View from Panorama Ridge with Guard Mountain (left), Glacier Pikes, Garibaldi Lake, The Table, Mt. Garibaldi, and Mount Price (right) Guard Mountain, The Table, Mt. Garibaldi, Mt. Price.jpg
View from Panorama Ridge with Guard Mountain (left), Glacier Pikes, Garibaldi Lake, The Table, Mt. Garibaldi, and Mount Price (right)
Aerial view looking southeast down at Glacier Pikes summit. Glacier Pikes aerial view.jpg
Aerial view looking southeast down at Glacier Pikes summit.

Related Research Articles

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

Blackcomb Peak is a mountain located east of Whistler, British Columbia that forms the boundary between the Whistler Blackcomb ski resort and Garibaldi Provincial Park. Like Whistler Mountain, it is located on the edge of Garibaldi Provincial Park and the ski lifts are often used to access the park, particularly for the Spearhead Traverse.

<span class="mw-page-title-main">The Spearhead</span>

The Spearhead is a 2,457 m (8,061 ft) peak in the Garibaldi Ranges of British Columbia, Canada, and is one of the main summits of the Blackcomb Mountain portion of the Whistler Blackcomb ski resort, located at the apex of the Blackcomb and Spearhead Glaciers, which is named for it. It also is the namesake of the Spearhead Range, which is the short range flanking the north side of Fitzsimmons Creek and ending on its northwest end at Blackcomb Mountain. The mountain's name was officially adopted on August 27, 1965, by the Geographical Names Board of Canada.

<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">Overlord Mountain</span> Mountain in the country of Canada

Overlord Mountain is a 2,625-metre (8,612-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges, and can be readily seen from the Whistler Blackcomb ski area. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Mount Macbeth, 3 km (2 mi) to the north-northeast. The Benvolio Glacier rests below the south aspect of the summit, the Fitzsimmons Glacier on the east aspect, and the expansive Overlord Glacier spans the northern and western aspects of the mountain. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1923 by Phyllis Munday and Don Munday via the Benvolio Glacier. The mountain's descriptive name was recommended by the Garibaldi Park Board and officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

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

Mount Fitzsimmons is a 2,603-metre (8,540-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the third-highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Mount Benvolio, 0.5 km (0 mi) to the west-southwest. The Diavolo Glacier spreads out below the southeast aspect of the summit, and the Fitzsimmons Glacier descends the northwest slopes. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River. The first ascent of the mountain was made on August 19, 1924, by a party of the British Columbia Mountaineering Club. The peak was named for prospector James Fitzsimmons, who built a trail along Fitzsimmons Creek in an effort to haul supplies to a small copper mine he staked and worked. The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

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

Mount Macbeth is a 2,639-metre (8,658-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is part of the Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 14 km (9 mi) southeast of Whistler, and 2 km (1 mi) south of Tremor Mountain, which is the highest point in the Spearhead Range. The Naden Glacier spreads out below the eastern aspect of the summit, the Macbeth Glacier lies below the south aspect, and the Curtain Glacier descends the northern slope. Precipitation runoff from the peak and meltwater from its glaciers drains into Fitzsimmons Creek which is a tributary of the Cheakamus River. Macbeth is most often climbed as part of the Spearhead Traverse. The first ascent of the mountain was made in 1969 by P. Starr, E. Bass, B. Ellis, and P. Macec via the northeast ridge. The peak was named in 1964 by an Alpine Club of Canada climbing party, to commemorate the 400th anniversary of William Shakespeare's birth. The mountain's name was officially adopted on August 27, 1965, by the Geographical Names Board of Canada.

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

Mount Benvolio is a 2,613-metre (8,573-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the second-highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Overlord Mountain, 0.7 km (0 mi) to the northwest. The Benvolio Glacier is set on the western slope of the peak, the Diavolo Glacier spreads out below the eastern aspect of the summit, and the Fitzsimmons Glacier descends the north slope. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River.

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

Tremor Mountain is a prominent 2,691-metre (8,829-foot) summit located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the highest point of the Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 13 km (8 mi) southeast of Whistler, and 8.7 km (5 mi) south of Wedge Mountain, its nearest higher peak. Precipitation runoff from the south side of the peak as well as meltwater from the Platform Glacier drains into Fitzsimmons Creek which is a tributary of the Cheakamus River. Meltwater from the Tremor Glacier on the northwestern slope drains to Wedge Creek, and meltwater from the Shudder Glacier on the northeast slope drains into Billygoat Creek, a tributary of the Lillooet River. Tremor Mountain is often climbed as part of the Spearhead Traverse. The first ascent of the mountain was made in 1928 by A.J. Campbell Garibaldi survey party. The mountain's name origin refers to unexplained earth tremors when the first ascent party was on the summit. The mountain's name was officially adopted on September 6, 1951, by the Geographical Names Board of Canada.

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

Cheakamus Mountain is a 2,588-metre (8,491-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the fourth-highest peak of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 16 km (10 mi) southeast of Whistler, and its nearest higher peak is Mount Benvolio, 1.65 km (1 mi) to the northwest. The Diavolo Glacier spreads out below the north aspect of the peak, and precipitation runoff from the peak with meltwater from the glacier drains into tributaries of the Cheakamus River. The peak was named in association with the river, which in turn is anglicized from Tseearkamisht, a Squamish word meaning "people who use the cedar rope fishing net". The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1950 by Roy Hooley, Jimmy Kilborn, and Ian Kirk.

<span class="mw-page-title-main">Panorama Ridge</span>

Panorama Ridge is a mountain ridge in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It is located on the north side of Garibaldi Lake in Garibaldi Provincial Park.

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References

  1. 1 2 "Glacier Pikes, British Columbia". Peakbagger.com. Retrieved 2023-02-11.
  2. 1 2 "Glacier Pikes". Geographical Names Data Base . Natural Resources Canada . Retrieved 2023-02-11.
  3. "Glacier Pikes". BC Geographical Names . Retrieved 2023-02-11.
  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. ISSN   1027-5606.