Phyllis's Engine

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Phyllis's Engine
Trips 05 - Garibaldi - 45 - Phyllis Engine (90954468).jpg
North-northwest aspect
Highest point
Elevation 2,517 m (8,258 ft) [1]
Prominence 21 m (69 ft) [2]
Parent peak Castle Towers Mountain [2]
Isolation 0.13 km (0.081 mi) [2]
Listing Mountains of British Columbia
Coordinates 49°56′01″N122°56′23″W / 49.93361°N 122.93972°W / 49.93361; -122.93972 [3]
Geography
Canada British Columbia relief location map.jpg
Red triangle with thick white border.svg
Phyllis's Engine
Location in British Columbia
Canada relief map 2.svg
Red triangle with thick white border.svg
Phyllis's Engine
Phyllis's Engine (Canada)
Phyllis's Engine
Interactive map of Phyllis's Engine
Country Canada
Province British Columbia
District New Westminster Land District
Protected area Garibaldi Provincial Park
Parent range Garibaldi Ranges
Coast Mountains
Topo map NTS 92G15 Mamquam Mountain [3]
Geology
Rock type granite [4]
Climbing
First ascent 1966
Easiest route class 5.8 climbing

Phyllis's Engine is a 2,517-metre (8,258-foot) granite pinnacle located in British Columbia, Canada.

Contents

Description

Phyllis's Engine is set within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. [1] It is situated 71 km (44 mi) north of Vancouver, 1.26 km (1 mi) north-northwest of Mount Carr, and 700 meters (2,300 feet) south of line parent Castle Towers Mountain. [1] Precipitation runoff and glacial meltwater from the west side of the peak drains to Garibaldi Lake, and the eastern slope drains to Cheakamus Lake. Topographic relief is significant as the west aspect rises 1,040 meters (3,410 feet) in 3 kilometers (1.9 miles).

History

The peak is named after Phyllis Dyke (Mrs. Edward Beltz), a pioneering British Columbia Mountaineering Club member who thought the arrangement of pinnacles and spires resembled a 19th-century steam locomotive, so her fellow climbers jokingly referred to the landform as "Phyllis's Engine", circa 1914. [5] The name was formally submitted by Karl Ricker in 1978 as recommended by Neal Carter of the BC Mountaineering Club, and contrary to popular belief, the name does not refer to Phyllis Munday. [6] The toponym was adopted as "Phyllis' Engine" on March 9, 1979, and officially changed to "Phyllis's Engine" on January 6, 1995, by the Geographical Names Board of Canada. [3]

The first ascent of Phyllis's Engine was made in 1966 by F. Gratwhol and T. Kempter. [4]

Climate

Based on the Köppen climate classification, Phyllis's Engine is located in the marine west coast climate zone of western North America. [7] 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. This climate supports the Sphinx Glacier on the west slope and the Cheakamus Glacier on the east slope.

See also

Related Research Articles

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

Castle Towers Mountain is a triple summit mountain on the east side of Garibaldi Lake in southwestern British Columbia, Canada. The first ascent party from the BC Mountaineering Club named the mountain after its appearance in August 1911.

<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.

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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.

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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.

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Mount Davidson is a 2,516-metre (8,255-foot) mountain summit located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. Visible from the Whistler Blackcomb ski area, it is situated 18 km (11 mi) south of Whistler, and its nearest higher peak is Castle Towers Mountain, 3 km (2 mi) to the west. The Cheakamus Glacier lies between these two summits, and precipitation runoff from the peak and meltwater from the glacier drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1929 by Neal M. Carter and Emmy Milledge. The mountain is named after Professor John Davidson, who contributed a large amount of botanical knowledge about Garibaldi Park. The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

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Decker Mountain is a 2,421-metre (7,943-foot) flat-topped 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 9 km (6 mi) southeast of Whistler, and 3.9 km (2 mi) west-northwest of Tremor Mountain, which is the highest point in the Spearhead Range. Precipitation runoff from the south side of the peak drains into Fitzsimmons Creek which is a tributary of the Cheakamus River, and meltwater from the Decker Glacier on the northeastern slope drains to Wedge Creek.

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References

  1. 1 2 3 "Phyllis's Engine, British Columbia". Peakbagger.com. Retrieved 2023-01-21.
  2. 1 2 3 "Phyllis's Engine, Peakvisor.com" . Retrieved 2023-01-21.
  3. 1 2 3 "Phyllis's Engine". Geographical Names Data Base . Natural Resources Canada . Retrieved 2023-01-21.
  4. 1 2 Dick Culbert (1969), A Climber's Guide to the Coastal Ranges of British Columbia, Alpine Club of Canada, p. 364
  5. ↑ G. P. V. Akrigg, Helen B. Akrigg (1997), British Columbia Place Names, UBC Press, ISBN   9780774806374, p. 207
  6. ↑ "Phyllis's Engine". BC Geographical Names . Retrieved 2023-01-21.
  7. ↑ 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.
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