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Kingcome Inlet is one of the lesser principal fjords of the British Columbia Coast, north and east of Broughton Island. It is sixth in sequence of the major saltwater fjords north from the 49th parallel near Vancouver and similar in width, on average 2.5 km (1.6 mi), to longer inlets such as Knight Inlet and Bute Inlet, but it is only 35 km (22 mi) in length from the mouth of the Kingcome River to Sutlej Channel, which ultimately connects around Broughton Island to the main regional waterway of the Queen Charlotte Strait. Kingcome Inlet has a short side inlet, Wakeman Sound, fed by the Wakeman River.
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.
North Bentinck Arm is a short inlet about 17 km (11 mi) in length in the Central Coast region of British Columbia, Canada. It is an arm of Burke Channel and is linked via that waterway and Labouchere Channel to Dean Channel, which is one of the largest inlets of the BC Coast.
The Lower Similkameen Indian Band or Lower Smelqmix, is a First Nations band government in the Canadian province of British Columbia. Their office was in the village of Keremeos in the Similkameen region, until 2015 when they moved into their own $7million multi-purpose facility south of Cawston. They are a member of the Okanagan Nation Alliance.
The Williams Lake First Nation is a First Nations government of the Secwepemc (Shuswap) Nation, located in the Cariboo region of the Central Interior region of the Canadian province of British Columbia, at the city of Williams Lake. It was created when the government of the then-Colony of British Columbia established an Indian reserve system in the 1860s. It is a member government of the Northern Shuswap Tribal Council. Its main Indian Reserve is Williams Lake Indian Reserve No. 1, a.k.a. "Sugarcane" or "The Cane" or "SCB".
The Esk'etemc First Nation, also known as the Alkali Lake Indian Band, is a First Nations government of the Secwepemc (Shuswap) people, located at Alkali Lake in the Cariboo region of the Central Interior of the Canadian province of British Columbia. It was created when the government of the then-Colony of British Columbia established an Indian reserve system in the 1860s. It is one of three Secwepemc bands that is not a member of either the Shuswap Nation Tribal Council or the Northern Shuswap Tribal Council.
The Red Bluff First Nation is a Dakelh First Nations government located in the northern Fraser Canyon region of the Canadian province of British Columbia. It is a member of the Carrier-Chilcotin Tribal Council, which includes both Tsilhqot'in and Carrier (Dakelh) communities.
The Tlʼetinqox-tʼin Government Office is a First Nations government located in the Chilcotin District in the western Central Interior region of the Canadian province of British Columbia. Governing a reserve communities near Alexis Creek known as Anaham Reserve First Nations or Anaham, it is a member of the Tsilhqotʼin Tribal Council aka known as the Tsilhqotʼin National Government. The main reserve is officially known as Anahim's Flat No. 1, and is more commonly as Anaham. Other reserves are Anahim's Meadow No. 2 and 2A, and Anahim Indian Reserves Nos. 3 through 18. Anaham, or Anahim and Alexis were chiefs of the Tsilhqotʼin during the Chilcotin War of 1864, although they and their people did not take part in the hostilities.
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Noohalk Mountain 2099 m is a mountain in the northernmost Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is located on the south side of the Bella Coola Valley between Hagensborg and Bella Coola.
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 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.
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 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.
The Sakumtha River is a river in British Columbia, Canada, flowing south out of the Kitimat Ranges from an origin west of the Tsaydaychuz Peak massif into the Dean River north of Bella Coola.
The Necleetsconnay River is a river in the Central Coast region of British Columbia, flowing southwest from the southernmost Kitimat Ranges to the head of North Bentinck Arm, adjacent to the mouth of the Bella Coola River and the town of Bella Coola.
Salmon House Falls is a waterfall at the confluence of the Takia and Dean Rivers at the western edge of the Interior Plateau, northwest of Tsitsutl Peak.
The Takia River is a tributary of the Dean River in British Columbia, Canada, flowing northwest to meet the Dean to the south of Sigutlat Lake. Salmon House Falls is located at the confluence of the two rivers, which is to the northwest of Tsitsutl Peak.
References
- ↑ "Nuxalk Smayusta: Chako Kunamokst at Kimsquit". nuxalk.net. Retrieved 2020-10-24.
- ↑ "BC Geographical Names". apps.gov.bc.ca. Retrieved 2020-10-24.
- ↑ "BC Geographical Names". apps.gov.bc.ca. Retrieved 2020-10-24.
- ↑ "Nuxalk Smayusta: Chako Kunamokst at Kimsquit". nuxalk.net. Retrieved 2020-10-24.
