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Glen Vowell is an Indian reserve community of the Gitxsan people in the Hazelton area of the Skeena Country of northwestern British Columbia, Canada. It is located on the west side of the Skeena River between Hazelton and Kispiox. Its traditional name is Sik i dak, which has also been spelled Sikadoak and is reflected in the name of the reserve, Sik-e-dakh IR 2. Also nearby is another Indian reserve, Anlaw Indian Reserve No. 4. The band government of the reserve is the Glen Vowell Indian Band, which also goes by the name Sik-e-Dakh.
The Chuckwalla River is a river in the Central Coast region of British Columbia, Canada, flowing into Kilbella Bay, which is a side water of Rivers Inlet. The river's headwaters are at 51°52′N127°54′W.
Kilbella Bay is a bay on the Central Coast of British Columbia, Canada, off the north side of Rivers Inlet to the northeast of McAllister Point. A steamer landing formerly operated by the Northland Navigation Company was located on the east side of the bay.
Katit Indian Reserve No. 1 is the main Indian reserve of the Wuikinuxv people, and is one of the three reserves governed by the Wuikinuxv Nation band government. It is located in British Columbia, Canada, on the entrance to Owikeno Lake on the north side of the Wannock River near to, but separate from, the non-native community and sport fishing resort of Rivers Inlet. Similarly named Katit Island is in the Wannock River at 51°40′41″N127°11′48″W, while Kahtit Creek is downstream, near the mouth of the Wannock River at 51°40′47″N127°15′00″W near the Wuikinuxv village known as Oweekeno.
Salloomt Peak is a 1,873 metres (6,145 ft) high mountain in the Kitimat Ranges of the Coast Mountains in the Bella Coola Valley region of British Columbia, Canada. It is located on the north side of the Bella Coola River between the communities of Firvale and Hagensborg.
The Tezwa River is a river in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. It is part of the Kitlope River drainage, feeding that river via the head of Kitlope Lake.
Chatscah Indian Reserve No. 2, officially Chatscah 2 is an Indian reserve of the Nuxalk Nation band government, located at the mouth of the Kimsquit River at the head of Dean Channel. Like nearby Kimsquit, at the mouth of the Dean River to the southeast, this Indian reserve was one of two reserves set aside of the once-populous Kimsquit subgroup of the Nuxalk, whose surviving post-smallpox population gathered at Bella Coola.
Comet Mountain, 1742 m, is a mountain in the Kitimat Ranges of British Columbia, Canada, located immediately west of the head of Dean Channel in the Central Coast region of that province, to the northwest of the town of Bella Coola. The former Nuxalk village and still-Indian reserve Kimsquit is located immediately east across Dean Channel, Chatscah Indian Reserve No. 2 is immediately north at the mouth of the Kimsquit River.
Kimsquit Ridge, 1827 m, is a mountain ridge on the west side of the Kimsquit River in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. It is north of the head of Dean Channel in between Foresight and Robson Creeks. There is a secondary peak, slightly lower than the northern peak, named Whitecone Peak, which is 1823 m elevation. The Bivouac Mountain Encyclopedia has dubbed the northern, slightly higher summit, Bluecone Peak.
The Kapella River is a river in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. It rises west of Cornice Peak and flows northwest to join the Kitlope River.
Cornice Mountain, 1503 m, is a mountain in the Stikine Icecap area of the Boundary Ranges in northwestern British Columbia, Canada. It is located southwest of the confluence of the Flood and Stikine Rivers.
The Taleomey River is a river in the northernmost Pacific Ranges of the Coast Mountains in the Central Coast region of British Columbia, Canada, flowing west to South Bentinck Arm where its waters enter the sea a few miles north of the head of that inlet. The Asseek River also enters the head of South Bentinck Arm, flowing into its head from the south.
The Noeick River is a river in the Central Coast region of British Columbia, Canada, flowing west out of the northernmost Pacific Ranges to enter saltwater on the east side of South Bentinck Arm, immediately to the north of the mouth of the Taleomey River at Taleomey Narrows.
Mount Saugstad is a mountain in the northernmost Pacific Ranges of the Coast Mountains in the Central Coast region of British Columbia, Canada. It is located just south of the community of Hagensborg in the Bella Coola Valley and is immediately southeast of Snootli Peak and also southeast of Big Snow Mountain. The Smitley River has its origins on the west side of the summit at the Saugstad Glacier, which is at 52°15′48″N126°31′36″W
Mount Jacobsen, 3031 m, is a mountain in the northernmost Pacific Ranges of the Coast Mountains in the Central Coast region of British Columbia, Canada, located to the south of the Bella Coola Valley and immediately south of Ape Lake, to the west of the valley of the Talchako River.
The Nekite River is a river in the Central Coast region of British Columbia, Canada, flowing south to the head of Smith Inlet. Nekite Indian Reserve No. 2 is located at the mouth of the river and is one of the many reserves of the Gwa'sala-'Nakwaxda'xw Nations band government located in the area of Smith Sound, of which Smith Inlet is the uppermost part.
Drury inlet is an inlet in the Queen Charlotte Strait region of the Central Coast of British Columbia, Canada, extending west from Wells Passage to the northwest of North Broughton Island, northwest of the town of Port Hardy. Branching off to the northeast from the north side of the head of the inlet is Actaeon Sound.
Waddington Harbour is a harbour at the head of Bute Inlet in the Central Coast region of British Columbia, Canada. Also issuing into the head of Bute Inlet and Waddington Harbour, just east of the mouth of the Homathko, is the Teaquahan River. Issuing directly into the inlet a few miles south on the harbour's southeast is the Southgate River, one of the major rivers of the central Pacific Ranges, which begins on the west side of the Lillooet Icecap. Its lower valley adjacent to the inlet's shores is called Pigeon Valley.
The Bishop River is a river in the Pacific Ranges of the Coast Mountains, flowing west from the western edge of the Lillooet Icecap to join the Southgate River east of the Homathko Icefield. Bishop River Provincial Park surrounds the upper course of the river, from the source at the Lillooet Icecap to midway along its course above its confluence with the Southgate.
The Dall River is a river in northern British Columbia, Canada, flowing northwest into the Turnagain River, a tributary of the Kechika, to the west of Mount Skook Davidson. Originally named the Cold Fish River, it was renamed in 1944 to avoid confusion with another river of that name that is a tributary of the Spatsizi, and because of the presence of Dall's sheep in the area. Dall Lake is along its course, south of Dall River Old Growth Provincial Park, which lies between the lake and the confluence with the Turnagain. Denetiah Provincial Park, on the river's upper course, includes Dall Lake.
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52°58′04″N127°12′44″W / 52.96778°N 127.21222°W
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