Guard Mountain | |
---|---|
Highest point | |
Elevation | 2,177 m (7,142 ft) [1] [2] |
Prominence | 203 m (666 ft) [1] |
Parent peak | Castle Towers Mountain [2] |
Isolation | 1.23 km (0.76 mi) [1] |
Listing | Mountains of British Columbia |
Coordinates | 49°54′31″N122°59′08″W / 49.90861°N 122.98556°W [3] |
Geography | |
Interactive map of Guard Mountain | |
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] |
Guard Mountain is a 2,177-metre (7,142-foot) summit in British Columbia, Canada.
Guard Mountain is located within Garibaldi Provincial Park on the southeast side of Garibaldi Lake, [4] and is part of the Garibaldi Ranges of the Coast Mountains. [1] It is situated 70 km (43 mi) north of Vancouver, 4.28 km (3 mi) west-southwest of Mount Carr, and 4.63 km (3 mi) southwest of Castle Towers Mountain. [1] Precipitation runoff from the peak drains into Garibaldi Lake and topographic relief is significant as the summit rises 700 meters (2,300 feet) above the lake in one kilometer (0.6 mile). The mountain's toponym was officially adopted on October 4, 1932, by the Geographical Names Board of Canada. [3]
Based on the Köppen climate classification, Guard Mountain is located in the marine west coast climate zone of western North America. [5] 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 east side of the mountain.
Alpha Mountain is a 2,302-metre (7,552-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 14 km (8.7 mi) northwest of Squamish, and 4.6 km (2.9 mi) southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Serratus Mountain, 1.9 km (1.2 mi) to the west. The Serratus Glacier lies to the west of Alpha, unnamed glaciers lie on the northern and eastern slopes, and Lake Lovely Water lies below the south slope. Precipitation runoff from the peak drains into tributaries of the Squamish River.
Mount Dione is a 2,589-metre (8,494-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 17 km (11 mi) northwest of Squamish, and 0.24 km (0 mi) north of Mount Tantalus, which is its nearest higher peak and the highest peak in the Tantalus Range. The Dione Glacier lies on the southern slope, and the Rumbling Glacier lies to the northeast. Precipitation runoff from the peak drains east into tributaries of the Squamish River, or west into tributaries of the Clowhom River. The first ascent of the mountain was made in 1916 by Tom Fyles and his brother, John Fyles, via the southeast ridge. The mountain names in the Tantalus Range have a Greek mythology theme, and Mount Dione was named for Dione, the wife of Tantalus. The mountain's name was submitted by Neal Carter of the British Columbia Mountaineering Club, and was officially adopted on June 6, 1957, by the Geographical Names Board of Canada.
Mount Matier is a prominent 2,783-metre (9,131-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the highest point of the Joffre Group, which is a subset range of the Coast Mountains. It is situated 26 km (16 mi) east of Pemberton, and 9 km (6 mi) northeast of Lillooet Lake. Its nearest higher peak is Mount Weart, 30 km (19 mi) to the southwest. The slopes of the mountain are covered by the Matier Glacier on the northwest, Anniversary Glacier on the northeast, Twin One Glacier on the southeast, and Hartzell Glacier to the south. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River.
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.
Slalok Mountain, originally known as Rex's Pillar, is a 2,653-metre (8,704-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the third-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 24 km (15 mi) east of Pemberton, and 8 km (5 mi) northeast of Lillooet Lake. It is 4 km (2 mi) northeast of Duffey Peak and the nearest higher peak is Mount Matier, 1.9 km (1 mi) to the east. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The first ascent of the mountain was made in 1963 by C. Adam, T. Anderson, and G. Richardson. The mountain's name Slalok is the traditional name for the settlement of nearby Mount Currie. The name was officially adopted on June 11, 1979, by the Geographical Names Board of Canada. The mountain and its climate supports the Matier Glacier, Stonecrop Glacier, and Tszil Glacier on the northern slopes.
Cayoosh Mountain is a 2,561-metre (8,402-foot) mountain summit located in the Cayoosh Range in southwestern British Columbia, Canada. It is situated 22 km (14 mi) east-northeast of Pemberton, 12 km (7 mi) north-northeast of Lillooet Lake, and immediately north of Cayoosh Pass. Its nearest higher peak is Mount Marriott, 5.43 km (3 mi) to the north-northeast. Precipitation runoff from the peak drains into Cayoosh Creek and other tributaries of the Fraser River. The mountain's name was submitted by Karl Ricker, a mountaineer, and was officially adopted on January 23, 1979, by the Geographical Names Board 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.
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.
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.
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.
Mount Taylor is a 2,318-metre (7,605-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 21 km (13 mi) east of Pemberton, and 7 km (4 mi) northeast of Lillooet Lake. Its nearest higher peak is Slalok Mountain, 1.9 km (1 mi) to the east. Precipitation runoff from the peak drains into Joffre Creek, a tributary of the Lillooet River. The mountain's name was submitted by Karl Ricker of the Alpine Club of Canada to honor Ada C. Taylor, a Pemberton pioneer and the first nurse in that community. The toponym was officially adopted January 23, 1979, by the Geographical Names Board of Canada.
Mount Cook is a 2,676-metre (8,780-foot) mountain located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated above the north shore of Wedgemount Lake, 13 km (8 mi) northeast of Whistler, and its nearest higher peak is Mount Weart, 1.2 km (1 mi) to the southeast. The Armchair Glacier is set between Cook and Weart, and the Weart Glacier rests on the northern slope of Cook. Precipitation runoff from the peak and meltwater from the glaciers drains into Wedgemount Lake and Green River.
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.
Mount Trorey is a 2,461-metre (8,074-foot) mountain summit located in British Columbia, Canada.
Mount Carr is a 2,590-metre (8,497-foot) mountain summit located in British Columbia, Canada.
Pyramid Mountain is a 2,158-metre (7,080-foot) summit located in British Columbia, Canada.
Phyllis's Engine is a 2,517-metre (8,258-foot) granite pinnacle located in British Columbia, Canada.
Mount Howard is a 2,551-metre (8,369-foot) mountain summit located in the Coast Mountains of British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. Mount Howard is situated 27 km (17 mi) east of Pemberton and immediately southeast of Mount Matier. Precipitation runoff from the peak drains into Twin One Creek thence Lillooet Lake which is within the Lillooet River watershed. Mount Howard is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,650 meters (5,413 ft) above Twin One Creek in 4 km (2.5 mi).
Darling Peak is a 2,310-metre (7,580-foot) mountain summit located in British Columbia, Canada.
Deception Peak is a 2,233-metre (7,326-foot) summit in British Columbia, Canada.