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.
Garibaldi Provincial Park, also called Garibaldi Park, is a wilderness park located on the coastal mainland of British Columbia, Canada, 70 kilometres (43.5 mi) north of Vancouver. It was established in 1920 and named a Class A Provincial Park of British Columbia in 1927. The park is a popular destination for outdoor recreation, with over 30,000 overnight campers and over 106,000 day users in the 2017/2018 season.
Kitimat is a district municipality in the North Coast region of British Columbia, Canada. It is a member municipality of the Regional District of Kitimat–Stikine regional government. The Kitimat Valley is part of the most populous urban district in northwest British Columbia, which includes Terrace to the north along the Skeena River Valley. The city was planned and built by the Aluminum Company of Canada (Alcan) during the 1950s. Its post office was approved on 6 June 1952.
The Kitimat Ranges are one of the three main subdivisions of the Coast Mountains in British Columbia, Canada, the others being the Pacific Ranges to the south and the Boundary Ranges to the north.
Gitnadoiks River Provincial Park is a 58,000 hectare provincial park in British Columbia, Canada. It is centred on the Gitnadoix River, a tributary of the Skeena River in Northwestern British Columbia, 50 km west of Terrace.
The Mount Meager massif is a group of volcanic peaks in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located 150 km (93 mi) north of Vancouver at the northern end of the Pemberton Valley and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.
The Skeena Mountains, also known as the Skeenas, are a subrange of the Interior Mountains of northern British Columbia, Canada, essentially flanking the upper basin of the Skeena River. They lie just inland from the southern end of the Boundary Ranges of the Coast Mountains, and also of the northern end of the Kitimat Ranges. Their southern limit is described by the Bulkley River and the upper northwestern reaches of Babine and Takla Lakes, and on their northeast by the upper reaches of the Omineca River.
The Hazelton Mountains are a grouping of mountain ranges on the inland lee of the Kitimat Ranges of the Coast Mountains in northwestern British Columbia, Canada, spanning the area of Hazelton south to the Nechako Reservoir. Defined by the British Columbia geographic names office, they span from the Nass River to the Nechako Plateau, and between the Coast Mountains and the Bulkley River, they are considered by geographers to be part of the Interior Mountains complex, though in local perspective they are considered to be part of the Coast Mountains. They are neighboured on the west by the Kitimat Ranges and on the east by the southernmost section of the Skeena Mountains; beyond the Nass River, which is their northern boundary, are the Boundary Ranges of the Coast Mountains. To their southeast is the Nechako Plateau, including the Quanchus Range on the near-island between Ootsa and Eutsuk Lakes of the Nechako Reservoir.
The Kitimat River is a river in the Canadian province of British Columbia. It originates in the Kitimat Ranges, near the sources of the Dala River, Kemano River, Atna River, and Clore River. It flows in a curve north, then west, then south, emptying into Kitimat Arm at the head of Douglas Channel, at the town of Kitimat.
The Kitlope River is a river in the Kitimat Ranges in the North Coast of British Columbia, Canada, flowing north for 100 km (62 mi), into the head of the Gardner Canal to the south of the smelter town of Kitimat. It is named for the Gitlope group of Haisla, now part of the Haisla Nation government and community at Kitamaat Village near Kitimat. The name is a Tsimshian language reference to the people, who call themselves Henaksiala, and means "people of the rocks" or "people of the opening in the mountains". The Haisla language name for the river is Xesduwaxwsdu.
The Kitlope Range is a small subrange of the Kitimat Ranges, located southeast of Kitlope Lake in British Columbia, Canada. It is surrounded by the Tezwa and Kitlope Rivers.
The Tenaiko Range is a small subrange of the Kitimat Ranges in British Columbia, Canada. It is surrounded by the Gamsby River and Tenaiko Creek. It reaches a height of 1,042 meters above sea level.
Chatsquot Mountain, 2365 m, is a high-prominence summit in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada, located northwest of Kimsquit Lake, east of the lower Kitlope River, and at the upper end of the basin of the Kimsquit River. It is part of the Kitimat Ranges which in turn form part of the Coast Mountains. With a topographic prominence of 1,981 m (6,499 ft), it is one of Canada's Ultra peaks and is the 98th most prominent summits of North America. It is also one of the most isolated mountain peaks of Canada.
Anchor Cone is a mountain in western British Columbia, Canada, located on the south side of Lowe Inlet, Grenville Channel, and southwest of Kitimat. It lies in the Countess of Dufferin Range, a subrange of the Kitimat Ranges which in turn form part of the Coast Mountains.
Mount Blane is a mountain in western British Columbia, Canada, located east of Kitlope Lake and southeast of the head of Whidbey Reach. It lies in the Kitlope Range, a subrange of the Kitimat Ranges which in turn form part of the Coast Mountains.
Mount Priestley is a mountain in the Kitimat Ranges of the Coast Mountains of British Columbia, Canada. Mount Priestly has an elevation 2,366 metres (7,762 ft) and prominence measure of 1,945 metres (6,381 ft) making it one of Canada's many ultra prominent peaks. It was first climbed by Drew Copeland, John Gill and Jordan Craven June 20, 2017.
Kimsquit Peak, 2268 m, is a mountain in the Kitimat Ranges of the Coast Mountains of British Columbia, Canada, located immediately north of the former Nuxalk village of Kimsquit, which is at the mouth of the Dean River. Immediately to its west across the head of Dean Channel is Comet Mountain.
Mount Meager is a mountain in the Pacific Ranges of the Coast Mountains in British Columbia, Canada. It represents the second highest peak of the Mount Meager massif, a group of coalescent stratovolcanoes in the Garibaldi Volcanic Belt.
The Ecstall River is a tributary of the Skeena River in the province of British Columbia, Canada. It originates in the Kitimat Ranges, and flows about 110 km (68 mi) to the lower tidal reach of the Skeena River at Port Essington, about 30 km (19 mi) southeast of Prince Rupert, 95 km (59 mi) southwest of Terrace, and 85 km (53 mi) northwest of Kitimat. Its drainage basin covers about 1,485 km2 (573 sq mi) and contains the largest blocks of unlogged land on the north coast of British Columbia, although large-scale industrial logging operations, both active and proposed, have been occurring in the watershed since the 1980s.
The Zymagotitz River is a tributary of the Skeena River located in the North Coast Regional District of the province of British Columbia, Canada. It originates in the Kitimat Ranges of the Coast Mountains, and flows south and west about 45 km (28 mi) to the Skeena River, about 10 km (6.2 mi) downriver from Terrace and about 100 km (62 mi) east of Prince Rupert.
