Slamgeesh Range | |
---|---|
Geography | |
Country | Canada |
Province | British Columbia |
Range coordinates | 56°25′N127°45′W / 56.417°N 127.750°W |
Parent range | Skeena Mountains |
The Slamgeesh Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between the Skeena River and Slamgeesh River in northern British Columbia, Canada. The Mosque River, a tributary of the Skeena, flows through the Slamgeesh Range.
The Skeena River is the second-longest river entirely within British Columbia, Canada. Since ancient times, the Skeena has been an important transportation artery, particularly for the Tsimshian and the Gitxsan—whose names mean "inside the River of Mist", and "people of the River of Mist," respectively. The river and its basin sustain a wide variety of fish, wildlife, and vegetation, and communities native to the area depend on the health of the river. The Tsimshian migrated to the Lower Skeena River, and the Gitxsan occupy territory of the Upper Skeena.
The Dean River is one of the major rivers of the Kitimat Ranges subrange of the southern Coast Mountains in British Columbia. It begins at Aktaklin Lake on the Chilcotin Plateau and winds north around the Rainbow Range to enter Dean Channel at the now-uninhabited, remote community of Kimsquit. It is one of the few rivers to fully penetrate the wall of the Coast Mountains between the Fraser's mouth and the mouth of the Skeena River.
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 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 Interior Mountains or Northern Interior Mountains are the semi-official names for an expansive collection of mountain ranges that comprises much of the northern half of the Canadian province of British Columbia and a large area of southern Yukon.
The Nass Ranges are a mountain range north of the Skeena River, west of Hazelton, and northeast of Terrace, British Columbia, Canada. It is a subrange of the Hazelton Mountains, which in turn form part of the Interior Mountains.
The Tatlatui Range is a large and very alpine mountain range on the east flank of the upper Skeena River in northern British Columbia, Canada. It has an area of 2307 km2 and is a subrange of the Omineca Mountains which in turn form part of the Interior Mountains. The range features several lakes, the largest of which, Thutade Lake, is at the head of the Finlay River, and is considered the ultimate source of the Mackenzie River. Tatlatui Lake, the next largest lake in the range, to the northwest of Thutade Lake, is at the head of the Firesteel River, a tributary of the Finlay. Various summits of the range, which as described separates the Pacific and Arctic drainages, form part of the Continental Divide. Most of the range and its lakes are in Tatlatui Provincial Park.
The Bulkley Ranges are a mountain range in northern British Columbia, Canada, located between the Skeena and Bulkley Rivers south of Hazelton, north of the Morice River and Zymoetz River. It has an area of 7851 km2 and is a subrange of the Hazelton Mountains which in turn form part of the Interior Mountains.
The Stikine Plateau is a plateau in northern British Columbia, Canada. It lies between the Boundary Ranges of the Coast Mountains on the west and southwest and the Cassiar Mountains along its northeast, and between the Skeena Mountains on its south and southeast and the Jennings and Nakina Rivers on the north.
The Atna Range is a small subrange of the Skeena Mountains of the Interior Mountains, located in northern British Columbia, Canada.
The Babine Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between Babine Lake, Babine River, Bulkey River and Skeena River in northern British Columbia, Canada.
The Driftwood Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between the headwaters of Driftwood River and Nilkitkwa River in northern British Columbia, Canada.
The Klappan Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between Klappan River and Iskut River in northern British Columbia, Canada.
The Oweegee Range is a small subrange of the Skeena Mountains of the Interior Mountains, located on the east side of Bell-Irving River in northern British Columbia, Canada.
The Sicintine Range is a small subrange of the Skeena Mountains of the Interior Mountains, located south of the Skeena River and between the Sicintine River and Squingula River in northern British Columbia, Canada.
The Strata Range is a subrange of the Skeena Mountains located between the Bell-Irving River and the Taylor River in northern British Columbia, Canada.
Mount Thomlinson is a mountain in the Babine Range of the Skeena Mountains in northern British Columbia, Canada, located at the head of Thomlinson Creek, southeast of the junction of Babine River and Skeena River and north of Hazelton. It has a prominence of 1,661 m (5,449 ft), created by the Babine-Stuart Pass, thus making it one of Canada's many Ultra peaks. Thomlinson is one of the most isolated mountains of Canada.
The Kispiox River is a river in the Skeena Country of British Columbia, Canada. It is a tributary of the Skeena River, flowing southeast to meet that river above its confluence with the Bulkley near Hazelton. It forms the eastern boundary of the Kispiox Range subdivision of the Hazelton Mountains.
The Mosque River is a tributary of the Skeena River in the Stikine Region of the province of British Columbia, Canada. It originates in the Tatlatui Range of the Skeena Mountains, and flows southwest about 50 km (31 mi) to the Skeena River, about 140 km (87 mi) north of Hazelton and about 160 km (99 mi) east of Stewart. Its watershed covers about 148 km2 (57 sq mi), and its mean annual discharge is 15.4 m3/s (540 cu ft/s).