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. [1] The Asseek River also enters the head of South Bentinck Arm, flowing into its head from the south. [2]
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 Pacific Ranges are the southernmost subdivision of the Coast Mountains portion of the Pacific Cordillera. Located entirely within British Columbia, Canada, they run northwest from the lower stretches of the Fraser River to Bella Coola and Burke Channel, north of which are the Kitimat Ranges. The Coast Mountains lie between the Interior Plateau and the Coast of British Columbia.
The Coast Mountains are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the Coast of British Columbia south to the Fraser River. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. The Coast Mountains are part of a larger mountain system called the Pacific Coast Ranges or the Pacific Mountain System, which includes the Cascade Range, the Insular Mountains, the Olympic Mountains, the Oregon Coast Range, the California Coast Ranges, the Saint Elias Mountains and the Chugach Mountains. The Coast Mountains are also part of the American Cordillera—a Spanish term for an extensive chain of mountain ranges—that consists of an almost continuous sequence of mountain ranges that form the western backbone of North America, Central America, South America and Antarctica.
Immediately north of the Taleomey estuary, the Noeick River also enters South Bentinck Arm. [3] On the north side of that river's mouth is the locality of South Bentinck. [4]
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.
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.
Taleomy Indian Reserve No. 3, which is governed by the Nuxalk Nation, is located at the mouth of the Taleomey River. [5] South Bentinck Arm is narrowed offshore from the estuary of the river by Taleomey Narrows. [6]
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 Nuxalk Nation is the band government of the Nuxalk people of Bella Coola, British Columbia. It is a member of the Oweekeno-Kitasoo-Nuxalk Tribal Council, and until March 2008 was a member of the Unrepresented Nations and Peoples Organization. The population is 1,479.
