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. [1]
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as stream, creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague.
The British Columbia Coast or BC Coast is Canada's western continental coastline on the North Pacific Ocean. The usage is synonymous with the term West Coast of Canada.
Canada is a country in the northern part of North America. Its ten provinces and three territories extend from the Atlantic to the Pacific and northward into the Arctic Ocean, covering 9.98 million square kilometres, making it the world's second-largest country by total area. Canada's southern border with the United States, stretching some 8,891 kilometres (5,525 mi), is the world's longest bi-national land border. Its capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. As a whole, Canada is sparsely populated, the majority of its land area being dominated by forest and tundra. Consequently, its population is highly urbanized, with over 80 percent of its inhabitants concentrated in large and medium-sized cities, with 70% of citizens residing within 100 kilometres (62 mi) of the southern border. Canada's climate varies widely across its vast area, ranging from arctic weather in the north, to hot summers in the southern regions, with four distinct seasons.
The locality of South Bentinck is located at the river's mouth. [2] There was a Nuxalk village, Nuiku, on a raised mound south of the mouth of the Noieck River. Another village, Kadis, was on the east side of South Bentinck Arm about ¼-mile north of the mouth of the Noieck. [3]
South Bentinck is a locality on South Bentinck Arm in the Central Coast region of British Columbia, Canada, located on the north side of the mouth of the Noeick River on the east shore of that inlet.
The river originates at the Noeick Glacier, which is to the northwest of Mount Jacobsen. [4]
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.
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 north near Vancouver and similar in width to longer inlets such as Knight Inlet and Bute Inlet, but it is only 35 km 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.
Kwikwasut'inuxw Haxwa'mis, formerly the Kwicksutaineuk-ah-kwa-mish First Nation is a First Nations band government based on northern Vancouver Island in British Columbia, Canada, in the Queen Charlotte Strait region. It is a member of the Musgamagw Tsawataineuk Tribal Council, along with the ‘Namgis First Nation and the Tsawataineuk First Nation. The Kwikwasut'inuxw and Haxwa'mis are two of the many subgroups of the peoples known as Kwakwaka'wakw, which means "speakers of Kwak'wala", their language, and were combined into one band by the Department of Indian and Northern Affairs.
Gilford Island is an island in British Columbia, Canada, located between Tribune Channel and Knight Inlet. The island has an area of 382 square kilometres (147 sq mi). Turnour Island is to the south across Tribune Channel, the entrance to Thompson Sound to the east.
Kimsquit is a former village of the Nuxalk at the mouth of the Dean River on the northeast side of Dean Channel in the Central Coast region of British Columbia, Canada. Kemsquit Indian Reserve No. 1 is nearby at 52°49′00″N126°58′00″W, which is on Kimsquit Bay; Kimsquit Mountain is nearby.
Thompson Sound is a sound on the Central Coast of British Columbia, Canada, located on the east side of Tribune Channel and to the east of Gilford Island, part of the Broughton Archipelago. The headland on the north side of the sound's entrance is London Point at 50°46′09″N126°07′07″W. The south side of the entrance is demarcated by Cleave Point at 50°44′35″N126°07′28″W.
Lancelot Inlet is an inlet in the Sunshine Coast region of the South Coast of British Columbia, Canada. It is a sidewater of Malaspina Inlet, and immediately east of the Gifford Peninsula. Via Thors Cove on its east side, its own sidewater is Theodosia Inlet, at the head of which is the mouth of the Theodosia River. The locality of Theodosia Arm is located here.
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.
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.
Taleomy Indian Reserve No. 3, officially Taleomy 3, is an Indian reserve under the governance of the Nuxalk Nation, located at the mouth of the Taleomey River on the east shore of South Bentinck Arm in the Central Coast region of British Columbia, Canada.
The Asseek River is a river in the Central Coast region of British Columbia, Canada, flowing north out of the Pacific Ranges to enter saltwater at the head of South Bentinck Arm. The name has been used since 1930, but an earlier map from 1913 shows it as the Talolail River. Also entering South Bentinck Arm a few miles north on the east side of the inlet is the Taleomey River, whose estuary forms Taleomey Narrows, a constriction of the inlet, and also where is the location of Taleomy Indian Reserve No. 3 of the Nuxalk Nation. Another constriction south of the Taleomey estuary, and immediately north of the Asseek's mouth is Bentinck Narrows, which is formed by the alluvial fan of Ickna Creek.
The Smitley River is a river in the northernmost Pacific Ranges of the Coast Mountains in British Columbia, Canada, flowing southeast to join the Noeick River a few miles above its outlet into South Bentinck Arm. The Smitley begins on the east flank of Mount Saugstad.
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
Tallheo Hot Springs is a hot spring located on the west shore of South Bentinck Arm, an inlet on the Central Coast of British Columbia, Canada, located southwest of the community of Bella Coola. The hot springs, which are known as Ix7piixm in the Nuxalk language, are located opposite Bensins Island, the only island in South Bentinck Arm.
Tribune Channel is a channel or strait on the Central Coast of British Columbia, Canada, separating Gilford Island on the west and north from the mainland. The channel bends around Gilford Island, with the mouth of Thompson Sound at the elbow of the bend, opening eastwards to the mouth of the Kakweiken River.
The Ahta River is a river in the Central Coast of British Columbia, flowing into Bond Sound to the south via the short Ahta Valley, which connects to the head of Kingcome Inlet to the north.
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.
Bensins Island is the only island in South Bentinck Arm, an inlet (fjord) in the Central Coast region of British Columbia, Canada. It is located across the inlet from Tallheo Hot Springs. Slightly north of the island on the shore of the inlet was Qnklst, a Nuxalk village. Qnklst is a Nuxalk name for "island" meaning "stone bottom" or "a bottom of stone".
Coordinates: 52°02′28″N126°40′26″W / 52.04111°N 126.67389°W
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
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