The Cambria Icefield is an icefield in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada, located southeast of Stewart.
The Mamquam Icefield is an icefield in southwestern British Columbia, Canada, located at the headwaters of Skookum Creek. It lies at the southern end of Garibaldi Provincial Park and is one of the southernmost icefields in the Pacific Ranges of the Coast Mountains. The highest summit of the icefield is Mamquam Mountain, located at its southern end with an elevation of 2,588 m (8,491 ft).
Mamquam Mountain is a mountain in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located 6 km (3.7 mi) southeast of Eanastick Meadows and 22 km (14 mi) east of Brackendale. It represents the highest summit of the Mamquam Icefield and lies at the southern end of Garibaldi Provincial Park. Mamquam Mountain was named on September 2, 1930, in association with the Mamquam River.
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.
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.
Lydia Mountain is a 2,100-metre (6,890-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 14.5 km (9 mi) northwest of Squamish, and 5.46 km (3 mi) south-southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. The nearest higher neighbor is The Red Tusk, 0.5 km (0 mi) to the west, and Mount Niobe lies 2.17 km (1 mi) to the east-southeast. Lake Lovely Water lies below the eastern slope of the peak and precipitation runoff from the peak drains east to the Squamish River, and west to the Clowhom River via Red Tusk Creek. Topographic relief is significant as Lydia Mountain rises 1,400 meters (4,600 feet) above Red Tusk Creek in approximately three kilometers (two miles). The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada. The mountain was named for mythic Lydia, of which Tantalus was a primordial ruler in Greek mythology. Several peaks in the Tantalus Range are named in association with Tantalus. The first ascent of Lydia Mountain was made in 1914 by Basil Darling and Allan Morkill.
Otter Mountain is a prominent 2,693-metre (8,835-foot) glaciated summit located in the Coast Mountains of British Columbia, Canada. It is situated 16 kilometers northeast of Stewart, British Columbia, and the nearest higher peak is Mount Pattullo, 25.4 km (15.8 mi) to the north. Otter ranks as the 23rd most topographically prominent summit of Canada. Topographic relief is significant as the summit rises 2,380 meters above Bitter Creek Valley in 5 kilometers. This mountain's toponym was adopted as "Mount Otter" on 24 July 1945, and officially renamed Otter Mountain on 5 November 1953 by the Geographical Names Board of Canada. Precipitation runoff from the mountain drains west into Bitter Creek which is a tributary of the Bear River, or east to Nelson Creek which is part of the Nass River drainage basin, and all ultimately finds its way to the Inside Passage.
Cathedral Mountain is a mountain summit located in British Columbia, Canada.
Mount Tinniswood is a 2,606-metre (8,550-foot) mountain summit located in British Columbia, Canada.
Mount Trorey is a 2,461-metre (8,074-foot) mountain summit located in British Columbia, Canada.
Mount Farrow is a mountain summit in British Columbia, Canada.
Mount Carr is a 2,590-metre (8,497-foot) mountain summit located in 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.
Guard Mountain is a 2,177-metre (7,142-foot) summit in British Columbia, Canada.
Hour Peak is a 2,329-metre (7,641-foot) mountain summit located in British Columbia, Canada.
Gentian Peak is a 2,197-metre (7,208-foot) summit in British Columbia, Canada.
Deception Peak is a 2,233-metre (7,326-foot) summit in British Columbia, Canada.
Mount Leland is a 7,810-foot-elevation (2,380-meter) glaciated mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. It is situated 27 miles (43 km) southeast of Skagway along the western edge of the Juneau Icefield, on land managed by Tongass National Forest. Topographic relief is significant as the summit rises 4,400 feet (1,340 m) above the Meade Glacier in 1.25 mi (2.01 km). Precipitation runoff and glacial meltwater from the mountain drains to Lynn Canal via the Katzehin River. Mount Leland's toponym was officially adopted in 1972 by the U.S. Board on Geographic Names to commemorate surveyor Ora Miner Leland (1876–1962), who led the International Boundary Commission Party of 1907. The peak rises a little over four miles (6.4 km) from the US–Canada boundary.
