Franklin Glacier | |
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![]() Mt. Waddington and Franklin Glacier | |
Type | Mountain glacier |
Location | British Columbia, Canada |
Coordinates | 51°15′59″N125°23′5″W / 51.26639°N 125.38472°W [1] |
Franklin Glacier is a mountain glacier in the Waddington Range of the Pacific Ranges in southwestern British Columbia, Canada. It lies at the head of the Franklin River adjacent to Mount Waddington, the highest mountain entirely within British Columbia. [1] [2]
The name of the glacier was officially adopted in 1928 after having been submitted by mountaineer Don Munday in August 1927 for its association with the Franklin River. [1] It is the namesake of the Franklin Glacier Complex, a heavily eroded geologic feature consisting of dikes, subvolcanic intrusions and overlying volcanic rocks. [3]
A base camp was established on the Franklin Glacier on June 23, 1934, by climbers Neal Carter, Alan Lambert, Alec Dalgleish and Eric Brooks as part of an attempted first ascent of Mount Waddington. Their ascent abruptly ended three days later when Dalgleish fell to his death from Waddington's southeast ridge. [4] [5]
Mount Waddington, once known as Mystery Mountain, is the highest peak in the Coast Mountains of British Columbia, Canada. Although it is lower than Mount Fairweather and Mount Quincy Adams, which straddle the United States border between Alaska and British Columbia, Mount Waddington is the highest peak that lies entirely within British Columbia. It and the subrange which surround it, known as the Waddington Range, stand at the heart of the Pacific Ranges, a remote and extremely rugged set of mountains and river valleys.
Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway, and is commonly photographed along this route.
Mount Garibaldi is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of 2,678 metres and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a landslide feature that formed in a series of collapses between 12,800 and 11,500 years ago. These collapses resulted in the formation of a large debris flow deposit that fans out into the Squamish Valley.
Mount Tiedemann 3,838 m (12,592 ft), prominence 848 m (2,782 ft), is one of the principal summits of the Pacific Ranges subdivision of the Coast Mountains of British Columbia. It is located 3 km (1.9 mi) northeast of Mount Waddington in the Waddington Range massif between the Homathko and Klinaklini Rivers.
The Franklin Glacier Complex is a deeply eroded volcano in the Waddington Range of southwestern British Columbia, Canada. Located about 65 km (40 mi) northeast of Kingcome, this sketchily known complex resides at Franklin Glacier near Mount Waddington. It is over 2,000 m (6,600 ft) in elevation and because of its considerable overall altitude, a large proportion of the complex is covered by glacial ice.
Asperity Mountain is a mountain located in British Columbia, Canada, rising to 3,716 metres (12,192 ft). It is located between Tellot and Tiedemann Glaciers on the north and south respectively, in the Waddington Range, a subrange of the Pacific Ranges. The gorge of the Homathko River runs north to south on the east side of the mountain, carrying runoff from the mountain and glaciers to the Pacific Ocean.
Mount Bute, also known as Bute Mountain, is a 2,810-metre (9,220-foot) mountain located in the Coast Mountains of British Columbia, Canada. Situated at the southern extreme of the Homathko Icefield, Mount Bute has an impressive 800-metre sheer granite west face, and Bute Glacier dominates the north aspect. This imposing mountain is visible from Waddington Harbour at the head of Bute Inlet, in a remote wilderness area that few visit. Its nearest higher peak is Mount Grenville, 13.0 km (8.1 mi) to the east-northeast. Mount Grenville is the highest summit of the icefield. Mount Bute is 63.0 km (39.1 mi) southeast of Mount Waddington, the highest peak of the entire Coast Mountains range.
Mount Rogers, is a 3,169-metre (10,397-foot) massif located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Mount Rogers is situated at the north end of the Hermit Range, and is the highest point of the range. Its nearest higher peak is Mount Sir Donald, 12.57 km (7.81 mi) to the southeast. The peak is prominently visible from eastbound Highway 1, the Trans-Canada Highway at Rogers Pass. The Rogers massif includes five individually-named summits: Rogers Peak, Grant Peak, Fleming Peak, Swiss Peak, and Truda Peaks. Numerous glaciers radiate from all sides, including the Rogers Glacier, Swiss Glacier, Tupper Glacier, and Hermit Glacier.
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 Wheeler, is a 3,336-metre (10,945-foot) mountain summit located in Glacier National Park of British Columbia, Canada. It is the third-highest peak in the park, and sixth-highest in the Selkirk Mountains range. The mountain is a remote 60 km (37 mi) east of Revelstoke, and 40 km (25 mi) southwest of Golden. Its nearest higher peak is Mount Selwyn, 5.1 km (3.2 mi) to the north-northwest. Mount Wheeler is surrounded by ice, including the Deville Glacier, Deville Névé, Black Glacier, and Thor Glacier. Precipitation runoff from the mountain and meltwater from its glaciers drains into tributaries of the Incomappleux and Beaver Rivers.
Mount Cooper is a prominent 3,094-metre (10,151 ft) glaciated mountain summit located in the Selkirk Mountains of southeast British Columbia, Canada. It is situated 36 km (22 mi) northwest of Kaslo, within Goat Range Provincial Park. Mt. Cooper is the highest peak in the Goat Range and Slocan Ranges, which are subsets of the Selkirks. The nearest higher peak is Truce Mountain, 33 km (21 mi) to the east-northeast. The first ascent of Mount Cooper was made August 10, 1962, by William Boulton, Terry Beck, Richard Hahn, Lorna Ream, Jack Steele, Edward Bouttin and Gary Johnson via the Spokane Glacier. This climbing party was from the Spokane Mountaineers organization. The mountain was named in association with Cooper Creek, which in turn was named after an 1880s Kaslo prospector and trapper. The mountain's name was officially adopted June 9, 1960, when approved by the Geographical Names Board of Canada. Prior to 1960 it was called Cooper Mountain.
Neal Marshall Carter was a Canadian marine biologist, cartographer, photographer, mountaineer and surveyor. He is most famous for his explorations in British Columbia, especially in the Coast Mountains where he made several first ascents.
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