The Lecture Cutters | |
---|---|
Highest point | |
Elevation | 2,524 m (8,281 ft) [1] |
Prominence | 124 m (407 ft) [1] |
Parent peak | Mount Sir Richard [1] |
Isolation | 2.35 km (1.46 mi) [1] |
Listing | Mountains of British Columbia |
Coordinates | 49°58′52″N122°43′02″W / 49.98111°N 122.71722°W [2] |
Geography | |
Interactive map of The Lecture Cutters | |
Location | British Columbia, Canada |
District | New Westminster Land District |
Protected area | Garibaldi Provincial Park |
Parent range | Coast Mountains McBride Range [3] |
Topo map | NTS 92G15 Mamquam Mountain |
Climbing | |
First ascent | 1971 John Clarke [4] |
The Lecture Cutters are 2,524-metre (8,281-foot) mountain peaks in British Columbia, Canada.
The Lecture Cutters is located in the McBride Range of the Coast Mountains, and 23 kilometres (14 mi) southeast of Whistler in Garibaldi Provincial Park. It is the third-highest point of the McBride Range. [1] Precipitation runoff and glacial meltwater from this mountain's slopes drains into the Cheakamus River. The Lecture Cutters is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 1,200 metres (3,937 ft) above the river in three kilometres (1.9 mi).
The mountain's toponym was officially adopted August 27, 1965, by the Geographical Names Board of Canada as proposed by Dr. Roy Hooley (1924–1996), Alpine Club of Canada and professor of civil engineering at the University of British Columbia. [5] He was accustomed to students skipping his classes, especially members of UBC's Varsity Outdoors Club who regularly climbed in the Garibaldi Park area. [6]
Based on the Köppen climate classification, The Lecture Cutters 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 McBride Glacier on the east slope. The months of July and August offer the most favorable weather for climbing The Lecture Cutters.
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.
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.
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 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.
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 Green 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 toponym was officially adopted on September 6, 1951, 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.
Mount Ronayne is a 2,290-metre (7,513-foot) summit located in the Pemberton Valley of British Columbia, Canada.
Phyllis's Engine is a 2,517-metre (8,258-foot) granite pinnacle located in British Columbia, Canada.
Whirlwind Peak is a 2,427-metre (7,963-foot) mountain summit in southwestern British Columbia, Canada.
Deception Peak is a 2,233-metre (7,326-foot) summit in British Columbia, Canada.
Cloudraker Mountain is a 2,385-metre (7,825-foot) glaciated summit in British Columbia, Canada.
Mount Sir Richard is a 2,681-metre (8,796-foot) glaciated summit in British Columbia, Canada.
In-SHUCK-ch Mountain is a 2,386-metre (7,828-foot) summit in British Columbia, Canada.
Outlier Peak is a 2,422-metre (7,946-foot) mountain summit in British Columbia, Canada.
Nivalis Mountain is a 2,659-metre (8,724-foot) mountain summit in British Columbia, Canada.
Mount Neal is a 2,552-metre (8,373-foot) glaciated summit in British Columbia, Canada.
Carcajou Peak is a 2,239-metre (7,346-foot) mountain summit in British Columbia, Canada.
Mount Moe is a 2,664-metre (8,740-foot) glaciated summit in British Columbia, Canada.
Shudder Mountain is a 2,671-metre (8,763-foot) summit in British Columbia, Canada.
Mount Pitt is a 2,487-metre (8,159-foot) summit in British Columbia, Canada.