Petroglyph Provincial Park is a Canadian provincial park located at the south end of the city of Nanaimo, British Columbia. The park was established on August 24, 1948, to protect a collection of petroglyphs found near the estuary of the Nanaimo River.
Tŝilhqox Biny, known as Chilko Lake, is a 180 km2 lake in west-central British Columbia, at the head of the Chilko River on the Chilcotin Plateau. The lake is about 65 km long, with a southwest arm 10 km long. It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation. It and Harrison Lake are the largest lakes in the southern Coast Mountains.
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 Chilcotin Ranges are a subdivision of the Pacific Ranges of the Coast Mountains. They lie on the inland lea of the Pacific Ranges, abutting the Interior Plateau of British Columbia. Their northwestern end is near the head of the Klinaklini River and their southeast end is the Fraser River just north of Lillooet; their northern flank is the edge of the Plateau while their southern is the north bank of the Bridge River. In some reckonings they do not go all the way to the Fraser but end at the Yalakom River, which is the North Fork of the Bridge.
The Waddington Range is a subrange of the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is only about 4,000 km2 (1,500 sq mi) in area, relatively small in area within the expanse of the range, but it is the highest area of the Pacific Ranges and of the Coast Mountains, being crowned by its namesake Mount Waddington 4,019 m (13,186 ft). The Waddington Range is also extremely rugged and more a complex of peaks than a single icefield, in contrast to the other huge icefield-massifs of the southern Coast Mountains, which are not so peak-studded and tend to have more contiguous icemasses.
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.
Tŝ’ilʔoŝ, also known as Mount Tatlow, is one of the principal summits of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains of southern British Columbia. Standing on an isolated ridge between the lower end of Chilko Lake and the Taseko Lakes, it is 3,063 m (10,049 ft) in elevation.
The Homathko River is one of the major rivers of the southern Coast Mountains of the Canadian province of British Columbia. It is one of the few rivers that penetrates the range from the interior Chilcotin Country to the coastal inlets of the Pacific Ocean. The Homathko River reaches the sea at the head of Bute Inlet, just west of the mouth of the Southgate River.
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.
Dala-Kildala Rivers Estuaries Provincial Park is a provincial park of 452 ha. in British Columbia, Canada. It protects the mouth of the Dala River in Kildala Arm.
Khutzeeymateen Provincial Park, also known as Khutzeymateen/K'tzim-A-Deen Grizzly Sanctuary, is a Class A provincial park located in the North Coast region of British Columbia, Canada. The park, within the purview of BC Parks, was established on August 15, 1994, to protect critical habitat for the region's grizzly bear population and the largest contiguous stand of old-growth Sitka spruce in the world. It was officially opened by Prince Philip, Duke of Edinburgh, on August 17, 1994.
Miracle Beach Provincial Park is a provincial park on the eastern shore of Vancouver Island in British Columbia, Canada. Located between Comox and Campbell River, the park includes a foreshore area in the Strait of Georgia, much of the Black Creek estuary, and a forested area. According to its Master Plan, it fulfills primarily a recreational role with a focus on beach play, picnicking, nature appreciation, and camping, and a secondary conservation role with a focus on the natural shoreline and estuary. In support of its recreational focus the park is developed with a day-use parking area with accessible trails leading to the shoreline and a camping area with 200 drive-in sites. The park is also hosts a nature centre building and a sheltered group picnic shelter. Vegetation in the park is typical for the region's second-growth forests with Douglas-fir most prominent. Common associates include Western hemlock, Sitka spruce, red alder and bigleaf maple. Salal and sword fern are the most abundant shrub. Black Creek, which flows through the park, is a spawning area for coho salmon.
The Lillooet Icecap, also called the Lillooet Icefield or the Lillooet Crown, is a large icefield in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is about 90 km (56 mi) northwest of the towns of Pemberton and Whistler, and about 175 km (109 mi) north of Vancouver, British Columbia. The Lillooet Icecap is one of the largest of several large icefields in the Pacific Ranges which are the largest temperate-latitude glacial fields in the world. At its maximum extent including its glacial tongues it measures 30 km (19 mi) east to west and 20 km (12 mi) north to south; its central icefield area is approximately 15 km (9 mi) in diameter.
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.
The Taseko Lakes are a pair of lakes, Upper Taseko Lake and Lower Taseko Lake, which are expansions of the upper Taseko River in the southern Chilcotin District of the Central Interior of British Columbia, Canada. Their name is based on the original in the Chilcotin language, Dasiqox Biny, where "Desiqox" means "Mosquito River" and is cognate to the name of the river as in English; the Chilcotin name refers to both lakes as one lake, which was also originally the case with the English usage until official designation of the separate lakes in 1954. The lakes are separated by the short Taseko Narrows, the name of which in Chilcotin is nanats'akash, and is an important crossing place for deer. The Tchaikazan River flows the area between the upper & lower lake from the southwest, while the Taseko River feeds it from the southeast, while the equally large Lord River joins it from the south, at the head of the lake.
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.
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 Teaquahan River, formerly Teaquahan Creek, 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.
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.
