Mount Bryce is a mountain at the southwestern corner of the Columbia Icefield, in British Columbia, Canada, near the border with Alberta. It can be seen from the Icefields Parkway.
Mount Whisler is a mountain of the British Empire Range on Canada's Ellesmere Island. It is the second highest peak of the British Empire Range, of Ellesmere Island, and of the Arctic Cordillera. It is located about 12 km (7.5 mi) northeast of Barbeau Peak, the highest peak in the Cordillera. The Henrietta Nesmith Glacier completely surrounds Mount Whisler.
Mathews Tuya is a tuya in northcentral British Columbia. It is one of the six tuyas close to Tuya Lake. It has been partly glaciated and Ar-Ar geochronology shows that is it about 730,000 years old. It mainly comprises palagonitized tephra but also has a few dykes and jointed lava flows on its flanks. The top still has flat-lying lava flows erupted after the tephra pile grew above the surface of the enclosing lake. The other volcanoes in the area include Tuya Butte, South Tuya and Ash Mountain. The volcanoes in the region form part of the Northern Cordilleran Volcanic Province.
The Milbanke Sound Group, also called the Milbanke Sound Cones, is an enigmatic group of five small basaltic volcanoes in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. Named for Milbanke Sound, this volcanic group straddles on at least four small islands, including Swindle, Price, Lady Douglas and Lake Island. Not much is known about this group of volcanoes and they remain undated. However, they all likely formed in the past 10,000 years after the last glacial period as evidenced by a small amount of erosion. The age of the most recent volcanic activity is also unknown. Most of the Milbanke Sound Cones are covered by mature forest. Kitasu Hill and Helmet Peak are the only two cones that are officially named.
Mount Josephine is a subglacial mound in the Tuya Range in British Columbia, Canada. It is located near the northwestern shore of Tuya Lake.
Armadillo Peak is a 7.5-million-year-old caldera, located about 3 km north of Bourgeaux Creek and northeast of Raspberry Pass, British Columbia, Canada. It is south of Mount Edziza and is overlapped by the Ice Peak central volcano, which was formed during the early Pleistocene. Its caldera is largely destroyed by glaciers. It is part of the Mount Edziza volcanic complex, which is made of basaltic lava flows.
Mount MacKenzie is a volcanic peak, located 40 km (25 mi) northeast of Hagensborg, British Columbia, Canada. It is one of the volcanic peaks of the Rainbow Range, which is one of the three major shield volcanoes that form the Anahim Volcanic Belt. Mount MacKenzie was formed when the North American Plate moved over a hotspot, similar to the one feeding the Hawaiian Islands, known as the Anahim hotspot.
The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over 350 kilometres (220 mi) northwest of the city of Vancouver and about 50 kilometres (31 mi) west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in western Canada, measuring about 30 kilometres (19 mi) long (north-south) and 20 kilometres (12 mi) wide (east-west). Mount Silverthrone, an eroded lava dome on the caldera's northern flank that is 2,864 metres (9,396 ft) high, may be the highest volcano in Canada.
Mount Somolenko is a volcanic peak in southwestern British Columbia, Canada, located 83 km (52 mi) east of Rivers Inlet and 7 km (4 mi) south of Mount Silverthrone. It is the highest peak south of Mount Silverthrone in the Ha-Iltzuk Icefield.
Mount Fitzgerald is a volcanic peak in southwestern British Columbia, Canada, located 84 km (52 mi) east of Rivers Inlet and 4 km (2 mi) east of Mount Silverthrone.
Meszah Peak is a volcanic cone located 66 km (41 mi) north of Telegraph Creek and 136 km (85 mi) southwest of Zus Mountain in British Columbia, Canada. It is the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of the massive Level Mountain shield volcano, which forms the most voluminous and most persistent eruptive centre in the Northern Cordilleran Volcanic Province.
Lake Island is an island on the coast of the Canadian province of British Columbia. It is located between Mathieson Channel and Lady Trutch Passage, and is flanked by Dowager Island, Lady Douglas Island, and a long finger shaped peninsula of the Canadian mainland to the east. Lake Island is not a lake island, as it is in an inlet of the Pacific Ocean, and lies only some 6 kilometres from the open sea.
Lady Douglas Island is an island in the North Coast region of the Canadian province of British Columbia. It is located off the south coast of Dowager Island.
Range 3 Coast Land District is one of the 59 land districts of British Columbia, Canada, which are part of the cadastral divisions of British Columbia.
Mount Farnham is British Columbia's 17th highest peak, and 21st most prominent. It was named after Paulding Farnham from New York. It is the highest peak in the Purcells.
Mount Morkill is located on the border of Alberta and British Columbia, near McBride which is a town in British Columbia, Canada. There is a subpeak to the southwest of the main peak, at an elevation of 2,185 m (7,169 ft) named The Gazetted Peak. It was named in 1965 after D.B. Morkill, a British Columbia land surveyor.
Mount Talbot is located on the northern side of Shale Pass on the Alberta-British Columbia border. It was officially named on 4 November 1925 after Senator Peter Talbot (1854-1919), an early pioneer of the Lacombe region of central Alberta. A teacher and farmer, he turned to politics and became an elected representative of the Northwest Territories and later the province of Alberta. In 1906, Sir Wilfrid Laurier appointed him to the Senate of Canada.
Mount Pauline is located on the south side of Beaverdam Pass on the Alberta-British Columbia border. It is the 26th most prominent in Alberta. It was named in 1925 after F.A. Pauline. The three slopes are covered in mostly metamorphic shale or slate, due to this it is unknown how difficult it would be to climb to the peak.
Whitetop Mountain is a forested hill in the West-Central Interior of British Columbia, Canada. It is on the northwest side of junction of the Chilcotin River and Downton Creek. Whitetop is a volcanic cone of the Chilcotin Plateau and Anahim Volcanic Belt.
The Helmet is a subsidiary peak on the Mount Robson massif located within Mount Robson Provincial Park in British Columbia, Canada. It is part of the Rainbow Range which is a sub-range of the Canadian Rockies.
