The Stikine River is a major river in northern British Columbia (BC), Canada and southeastern Alaska in the United States. It drains a large, remote upland area known as the Stikine Country east of the Coast Mountains. Flowing west and south for 610 kilometres (379 mi), it empties into various straits of the Inside Passage near Wrangell, Alaska. About 90 percent of the river's length and 95 percent of its drainage basin are in Canada. Considered one of the last truly wild large rivers in BC, the Stikine flows through a variety of landscapes including boreal forest, steep canyons and wide glacial valleys.
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.
Officially Good Hope Mountain but commonly known as Mount Good Hope is one of the principal summits of the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada. It stands immediately west of Chilko Lake, with the highest peak on the massif rising between the lake's southern arms.
Monarch Mountain is one of the principal summits of the Pacific Ranges subdivision of the Coast Mountains in southern British Columbia. It stands just east of a pass between the Klinaklini River and the south branch of the Atnarko River, which is a tributary of the Bella Coola River. Surrounding Monarch Mountain is the Monarch Icefield, the northernmost of the major icefields of the Pacific Ranges, and just south of it is the Ha-Iltzuk Icefield, which is the largest. Monarch is in the southern end of Tweedsmuir South Provincial Park.
Sechelt Inlet formerly Seechelt Inlet is one of the principal inlets of the British Columbia Coast. The inlet is significant in that it almost makes an island of what is instead the Sechelt Peninsula, whose isthmus is at the town of Sechelt at the head of the inlet. The isthmus is less than 1.2 km (0.75 mi) in length. Sechelt Inlet's mouth is at Jervis Inlet, inland from the Malaspina Strait.
Dean Channel is the upper end of one of the longest inlets of the British Columbia Coast, 105 km (65.2 mi) from its head at the mouth of the Kimsquit River. The Dean River, one of the main rivers of the Coast Mountains, enters Dean Channel about 9.5 km (5.9 mi) below the head of the inlet, at the community of Kimsquit.
Loughborough Inlet is one of the lesser principal inlets of the British Columbia Coast. It penetrates the Coast Mountains on the north side of the Discovery Islands archipelago, running about 35 km (22 mi) from its head at the mouth of the Stafford River to Chancellor Channel and Cordero Channel, which are on the north side of West Thurlow Island. A further 14 km (8.7 mi) west along Chancellor Channel is Johnstone Strait.
The Bella Coola River is a major river on the Pacific slope of the Coast Mountains in southern British Columbia. The town of Bella Coola is at its mouth on North Bentinck Arm. Bella Coola Indian Reserve No. 1 is the location of the main community today of the surviving population of the Nuxalk who gathered there after depredations by smallpox and colonialization.
The Klinaklini River is one of the major rivers of the Pacific Ranges section of the Coast Mountains in the Canadian province of British Columbia. It originates in the Pantheon Range and empties into the head of Knight Inlet.
The North American Cordillera, sometimes also called the Western Cordillera of North America, the Western Cordillera, or the Pacific Cordillera, is the North American portion of the American Cordillera, the mountain chain system along the Pacific coast of the Americas. The North American Cordillera covers an extensive area of mountain ranges, intermontane basins, and plateaus in Western and Northwestern Canada, Western United States, and Mexico, including much of the territory west of the Great Plains.
Homathko Estuary Provincial Park is a provincial park in British Columbia, Canada, located at the head of Bute Inlet surrounding the mouth of the Homathko River in the Pacific Ranges of the Coast Mountains.
Chutine Peak is one of the highest mountains in the Boundary Ranges, a group of subranges of the northern Coast Mountains of British Columbia and Alaska. Chutine Peak lies just east of the Stikine Icecap, and to the north and west of the Stikine River, and south of the basin of the Whiting River. It is notable for its huge west face: the drop to Chutine Lake is 2,600 m (8,530 ft) in 3.5 km (2 mi). Due to its remoteness, however, it is rarely visited.
The Premier Range is a group of mountains within the Cariboo Mountains of east-central British Columbia, Canada. The range is bounded by the Raush River and Kiwa Creek to the north, the North Thompson River on the south and west and the Fraser River and its tributaries to the east.
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 Homathko Icefield is an icefield in British Columbia, Canada. Officially named the Homathko Snowfield from 1950 until the current name was adopted in 1976, it is one of the largest icefields in the southern half of the Coast Mountains, with an area of over 2,000 km2 (770 sq mi). It is located between Chilko Lake and the Homathko River, and lies across the Great Canyon of that river to the east of the Waddington Range. Although adjacent to Mount Queen Bess, the Homathko Icefield is largely an expanse of ice, about 30 km (19 mi) across, ringed by relatively minor peaks and distinguished, relative to the other Coast Mountains icefields, by lack of any major ones. The Lillooet Icecap and the Compton Névé, both similar in size to the Homathko Icefield but much more peak-studded, lie to the Homathko Icefield's southeast across the Southgate River which bends around the icefield-massif's southern flank to reach the head of Bute Inlet adjacent to the mouth of the Homathko River. The icefield is essentially one large ice-girt montane plateau between these two rivers.
The Skwawka River is a medium-sized river in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, flowing southeast 20 kilometers (12 mi) into the head of Queens Reach, which is the uppermost end of Jervis Inlet. The pass at the head of the river, which connects to the head of the Little Toba River, is the prominence col for Mount Alfred, which lies just west of the river's mouth and is the highest summit between Jervis and Toba Inlets. Above the river's lower reaches, on the east flank of Mount Alfred, is 700 meters (2,300 ft) Alfred Creek Falls, one of North America's highest.
The McLennan River is a tributary of the Fraser River in the Robson Valley region of British Columbia. The river was named after an engineer on one of the Canadian Pacific Railway surveys in the 1870s.
The Kimsquit River is a river in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada, flowing into the head of Dean Channel, one of the major inlets of the Central Coast region.
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.
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.
