The Bugaboos are a mountain range in the Purcell Mountains of eastern British Columbia, Canada. The granite spires of the group are a popular mountaineering destination. The Bugaboos are protected within Bugaboo Provincial Park.
Bugaboo Spire is a peak in Bugaboo mountain range in Canada, located between the Vowell and Crescent glaciers, just under 2 km West of the ACC's Conrad Kain hut. It is known for its alpine climbing. The Spire was first climbed by Conrad Kain in 1916.
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 (9 mi) northwest of Squamish, and 4.6 km (3 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 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 Rexford is a prominent 2,329-metre (7,641-foot) mountain summit located in the Cascade Mountains of southwestern British Columbia, Canada. It is situated 3.5 km (2 mi) north of the Canada–United States border, 7 km (4 mi) west of Chilliwack Lake, and 5.5 km (3 mi) east of Slesse Mountain, which is its nearest higher neighbor. Precipitation runoff from the peak drains into Nesakwatch and Centre Creeks, both tributaries of the Chilliwack River. Originally known as Ensawkwatch, the mountain was named for an early settler in the area, Rexford, who had a cabin near Slesse Creek and had trap lines in the vicinity. The mountain has two subsidiary peaks known as the Nesakwatch Spires. The mountain's name was officially adopted on June 2, 1950, by the Geographical Names Board of Canada. Mount Rexford was first climbed in July 1951 by Herman Genschorek and Walt Sparling via the West Ridge.
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.
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.
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.
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.
Hermit Mountain is a 3,050-metre (10,010-foot) mountain summit located in Glacier National Park, in the Hermit Range of the Selkirk Mountains in British Columbia, Canada. Hermit Mountain is situated 64 km (40 mi) northeast of Revelstoke, and 39 km (24 mi) west of Golden. It is also set 2.7 km (1.7 mi) north-northwest of Mount Tupper, and 6 km (3.7 mi) north of Rogers Pass, from which it can be seen from the Trans-Canada Highway. The nearest higher peak is Swiss Peak on Mount Rogers, 1 km (0.62 mi) to the west. The first ascent of the mountain was made August 4, 1904, by Alex M. Gordon, Samuel Harper Gray, James C. Herdman, Edward Feuz, and Edward Feuz Jr. via the Southeast Couloir. The mountain's name was adopted in 1904, then re-approved September 8, 1932, by the Geographical Names Board of Canada.
Eyebrow Peak is a prominent 3,362-metre (11,030-foot) glaciated mountain summit located in the Purcell Mountains in southeast British Columbia, Canada. It is the ninth-highest peak in the Purcells. It is situated 28 km (17 mi) south of The Bugaboos, 44 km (27 mi) west of Invermere, 6 km (3.7 mi) north of Mount Monica, and 18 km (11 mi) east of Duncan Lake. Its nearest higher peak is Commander Mountain, 11.4 km (7.1 mi) to the southeast. The first ascent of the mountain was made in 1914 by Edward Warren Harnden, D. Brown, L. Nettleton, and E. Parson via the west slopes. The name Eyebrow Peak came about by Arthur Oliver Wheeler in 1910 when viewing two broad rock scars near the summit, and their arrangement in connection with the surrounding snow created the appearance of enormous eyebrows. However, using the same sightings as Wheeler, Professor Peter Robinson showed that Wheeler actually saw Mount Farnham. Poor weather conditions led to Wheeler's error, and the Eyebrow moniker was then moved to its present location. The mountain's name was officially adopted June 9, 1960, by the Geographical Names Board of Canada.
Deluge Mountain is a mountain summit located in British Columbia, Canada.
Phalanx Mountain is a 2,441-metre (8,009-foot) summit located in Garibaldi Provincial Park of southwest British Columbia, Canada.
Spire Peaks is a 2,279-metre (7,477-foot) mountain 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).
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).
