The Teaquahan River, formerly Teaquahan Creek, [1] is a river in the Pacific Ranges of the Coast Mountains, flowing into the head of Bute Inlet at Waddington Harbour, immediately east of the mouth of the Homathko River. [2]
The Niut Range is 3600 km² in area. It is a subrange of the Pacific Ranges of the Coast Mountains of British Columbia, although in some classifications it is considered part of the Chilcotin Ranges. The Niut is located in the angle of the Homathko River and its main west fork, Mosley Creek. It is isolated, island-like, by those rivers from its neighbour ranges, as both streams have their source on the Chilcotin Plateau in behind the range. Razorback Mountain is its highest peak.
Mount Tiedemann 3838m, prominence 848m, is one of the principal summits of the Pacific Ranges subdivision of the Coast Mountains of British Columbia. It is located 3 km (1.9 mi) northeast of Mount Waddington in the Waddington Range massif between the Homathko and Klinaklini Rivers.
Bute Inlet is one of the principal inlets of the British Columbia Coast. It is 80 km (50 mi) long from the estuaries of the Homathko and Southgate Rivers at the head of the inlet, to the mouth, where it is nearly blocked by Stuart Island, and it averages about 4 km (2.5 mi) in width. Bute Inlet is in a spectacular wilderness setting and is one of the most scenic waterways in the world. In the upper reaches of the inlet mountains rise 2,700 m (9,000 ft) feet above sea level. Bute Inlet is a spectacular wilderness that is visited by very few people. In more recent years tourists are travelling from around the world to view grizzly bears in a natural setting and explore the wilderness of Bute Inlet.
Bishop River Provincial Park is a provincial park in the Pacific Ranges of the Coast Mountains on the Mainland of British Columbia, Canada, located southwest of and adjoining Ts'yl-os Provincial Park."Bishop River Park". BC Geographical Names. It lies along the upper course of the Bishop River, the main tributary of the Southgate River, from the Bishop's source at the western side of the Lillooet Icecap to midway along its course above its confluence with the Southgate. The park is 19,947 ha. in size. There are no roads or trails in the park although a forest service road from Waddington Harbour at the head of Bute Inlet leads up the Southgate to within a few miles of the park boundary.
Homathko Estuary Provincial Park is a provincial park in British Columbia, Canada, located at the head of Bute Inlet surrounding the mouth of the Homathko River in the Pacific Ranges of the Coast Mountains.
The Lytton First Nation, a First Nations band government, has its headquarters at Lytton in the Fraser Canyon region of the Canadian province of British Columbia. While it is the largest of all Nlaka'pamux bands, unlike all other governments of the Nlaka'pamux (Thompson) people, it is not a member of any of the three Nlaka'pamux tribal councils, which are the Nicola Tribal Association, the Fraser Canyon Indian Administration and the Nlaka'pamux Nation Tribal Council.
The Homathko Icefield is an icefield in British Columbia, Canada. Officially named the Homathko Snowfield from 1950 until the current name was adopted in 1976, it is one of the largest icefields in the southern half of the Coast Mountains, with an area of over 2,000 km2 (770 sq mi). It is located between Chilko Lake and the Homathko River, and lies across the Great Canyon of that river to the east of the Waddington Range. Although adjacent to Mount Queen Bess, the Homathko Icefield is largely an expanse of ice, about 30 km (19 mi) across, ringed by relatively minor peaks and distinguished, relative to the other Coast Mountains icefields, by lack of any major ones. The Lillooet Icecap and the Compton Névé, both similar in size to the Homathko Icefield but much more peak-studded, lie to the Homathko Icefield's southeast across the Southgate River which bends around the icefield-massif's southern flank to reach the head of Bute Inlet adjacent to the mouth of the Homathko River. The icefield is essentially one large ice-girt montane plateau between these two rivers.
Waddington Canyon is a canyon on the Homathko River in the heart of the Pacific Ranges of the Coast Mountains in British Columbia, Canada, located below the confluence of Mosley Creek.
Great Canyon is the official name of a stretch of the Homathko River as it pierces the heart of the Pacific Ranges of the Coast Mountains between the Chilcotin District of the British Columbia Interior and the Central Coast region at Bute Inlet. Also known unofficially as the Grand Canyon of the Homathko, it is located above the confluence of Mosley Creek. The canyon is the largest on the Homathko and lies on the west side of the Waddington Range massif containing Mount Waddington, the range's highest, and like other parts of the Homathko has been proposed as the site of dams in a region-wide hydroelectric development involving the Homathko, Southgate, Chilko and Taseko Rivers.
The Compton Névé is an icefield in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located southeast of the Homathko Icefield and Mount Gilbert and to the south of the Bishop River. It lies west of the Lillooet Icecap and is connected to it by the Ring Glacier, which sits astride Ring Pass, the divide between the Lillooet and Bishop Rivers, and has an area of 714 km2 (276 sq mi).
The Southgate River is a river in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, entering the head of Bute Inlet, on that province's South Coast, just east of the mouth of the Homathko River at Waddington Harbour. The lower reaches of the river's course are flat-bottomed and are named Pigeon Valley. The river is approximately 65 km in length, beginning on the western flank of Good Hope Mountain, to the east of the Homathko Icefield, and then flows generally SSW for about 40 km before turning WNW towards the head of Bute Inlet. The Bishop River enters it from the east after the first 20 km of its course and has its origin at Ring Pass, which lies between the Compton Neve (W) and the Lillooet Icecap (E) and forms the divide with the uppermost Lillooet River.
Yale First Nation is a First Nations government located at Yale, British Columbia. Yale has 16 distinct reserves stretching from near Sawmill Creek to American Creek, with the most southern reserve situated at Ruby Creek in the District of Kent.
Mount Gilbert, 3124 m prominence: 484 m, is a mountain in the Pacific Ranges of the Coast Mountains of British Columbia, Canada. It is located south of the confluence of the Bishop and Southgate Rivers and to the west of the Compton Névé, a large icefield, and to the south of the Homathko Icefield, another large icefield.
The Tahumming River is a river in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, flowing southeast into Toba Inlet near that inlet's head.
Theodosia Inlet is an inlet in the Desolation Sound region of the South Coast region of British Columbia, Canada, located east of Lancelot Inlet, a sub-inlet of Malaspina Inlet. The inlet is fed by the Theodosia River. The locality of Theodosia Arm is located near its outlet at the head of Thors Cove.
Malaspina Inlet is an inlet on the east side of Desolation Sound in the South Coast region of British Columbia, Canada, located between Malaspina and Gifford Peninsulas. Sidewaters include Thors Cove and, via it, Theodosia Inlet, where the locality of Theodosia Arm is located. The upper, southeastern, end of Malaspina Inlet near the City of Powell River is called Okeover Inlet. on the east side of which the steamer landing Larsons Landing is located. Grace Harbour is located on north side of Malaspina Inlet on the southwest side of Gifford Peninsula.
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.
Mosely Creek is a large creek in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, flowing southwest to join the Homathko River in its canyon downstream from Tatlayoko Lake, and a short distance above Murderers Bar at 51°16′00″N124°54′00″W, which is the site of the opening events of the Chilcotin War of 1864.
The Claud Elliott Creek Ecological Reserve is located southwest of the junction of Claud Elliott Creek and the Tsitsika River on northern Vancouver Island, southwest of the community of Sayward. The reserve, which was created to protect representative old-growth montane forests, was established in 1989, comprising approximately 231 hectares. It was expanded slightly in 2004 to a current total area of approximately 233 hectares.
Coordinates: 50°55′52″N124°49′51″W / 50.93111°N 124.83083°W
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