The Crooked River is a river in the Central Interior of British Columbia, Canada, beginning at Summit Lake [1] and the community of the same name, flowing north into McLeod Lake. [2] It is part of the drainage area of the Pack River, via the McLeod River north from McLeod Lake and which feeds Lake Williston, and therefore also part of the Peace River basin and in the Arctic Ocean drainage. South of its source at Summit Lake is the drainage basin of the Fraser River, and so of the Pacific Ocean. Crooked River Provincial Park is located close its course, on Bear Lake just south of the community of Bear Lake. [3]
The Crooked River is known to contain at least 39 species of caddisflies (Trichoptera), several of which were the first records of their species for British Columbia. [4]
The Continental Divide of the Americas is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and Arctic Ocean, including those that drain into the Gulf of Mexico, the Caribbean Sea, and Hudson Bay.
Dease Lake is a small community in the Cassiar Country of the Northern Interior of British Columbia, Canada. It is 230 km south of the Yukon border on Stewart–Cassiar Highway at the south end of the lake of the same name. Dease Lake is the last major centre before the Alaska Highway while driving northbound, and also the junction to Telegraph Creek and the Grand Canyon of the Stikine. Dease Lake Indian Reserve No. 9 is nearby and is under the governance of the Tahltan First Nation band government.
McLeod Lake is an unincorporated community located on Highway 97 in northern British Columbia, Canada, 140 km (87 mi) north of Prince George. It is notable for being the first continuously inhabited European settlement established west of the Rocky Mountains in present-day Canada.
The Parsnip River is a 240-kilometre (150 mi) long river in central British Columbia, Canada. It flows generally north-westward from the Parsnip Glacier in the Hart Ranges to the Parsnip Reach of Williston Lake, formed by the impounding of the waters of the Peace River by the W.A.C. Bennett Dam in 1968. Prior to that, the Parsnip joined with the Finlay River to form the Peace at Finlay Forks, with both sharing an alignment along the Rocky Mountain Trench.
The Kechika River is a tributary of the Liard River, about 300 kilometres (190 mi) long, in northern British Columbia, Canada. The Kechika flows generally northwest through the northernmost section of the Rocky Mountain Trench before turning east to join the Liard, a major branch of the Mackenzie River system. The river's 22,700 km2 (8,800 sq mi) drainage basin is characterized by high glaciated peaks, boreal forest, and open tundra. With no settlements, roads or dams along its course, the Kechika is considered "one of British Columbia's finest examples of wilderness and undisturbed wildlife habitat."
Liard River Hot Springs Provincial Park is a provincial park in British Columbia, Canada. It is home to the second largest natural hot springs in Canada, after Deer River Hot Springs 15 km to the north east. It is a natural river of hot water rather than a spring fed man made pool. The park is part of the larger Muskwa-Kechika Management Area. The community of Liard River, British Columbia is located nearby.
Arctic Pacific Lakes Provincial Park is a provincial park in British Columbia, Canada, protecting a pair of lakes known as Arctic and Pacific Lakes, which as their name indicate are on the divide between the Pacific and Arctic drainages. Inherently, the Continental Divide runs between the two lakes, which lie in a narrow valley amid the rugged mountains of the northwesternmost McGregor Plateau. The pass formed by the lakes was important during early fur trade operations and was one of the main links between New Caledonia and the fur companies' eastern territories beyond the Rockies.
Babine Mountains Provincial Park is a provincial park in British Columbia, Canada, located to the east of the Bulkley River between the town of Smithers (SW) and Babine Lake (NE). Established by Order-in-Council as the Babine Mountains Recreation Area in 1984, it was upgraded to park status and its name changed in 1999. It contains approximately 31,465 hectares.
Birkenhead Lake Provincial Park is a provincial park in British Columbia, Canada, located in the Lillooet Country region to the northeast of Pemberton and immediately northwest of Birkenhead Peak and Gates Lake at the community of Birken.
Clendinning Provincial Park is a provincial park in British Columbia, Canada. It surrounds the drainage of Clendinning Creek, which is a tributary of the Elaho River. Its name is shared by the Clendinning Range, of which Mount Clendinning is the highest summit.
Sutherland River Provincial Park and Protected Area is a provincial park in British Columbia, Canada.
Pemberton Pass, 505 m (1,657 ft), also formerly known as Mosquito Pass, is the lowest point on the divide between the Lillooet and Fraser River drainages, located at Birken, British Columbia, Canada, in the principal valley connecting and between Pemberton and Lillooet. The pass is a steep-sided but flat-bottomed valley adjacent to Mount Birkenhead and forming a divide between Poole Creek, a tributary of the Birkenhead River, which joins the Lillooet at Lillooet Lake, and the Gates River which flows northeast from Gates Lake, at the summit of the pass, which flows to the Fraser via Anderson and Seton Lakes and the Seton River.
Churn Creek is a tributary of the Fraser River in the Canadian province of British Columbia.
The Gates Valley is a valley and group of communities in the Lillooet Country of the Southern Interior of British Columbia, Canada, located between the summit of Pemberton Pass and the head of Anderson Lake at the community of D'Arcy. Though the term strictly refers to the valley of the Gates River, it is usually used more in a sense of the communities located in the valley and is not a term used for the river's drainage basin, which is much larger.
Mission Ridge, also known as Mission Mountain, is a ridge in the Bridge River-Lillooet Country of the South-Central Interior of British Columbia, Canada, extending westward from the town of Lillooet along the north side of Seton Lake to Mission Pass, which is immediately above and to the north of the lakeside community of Shalalth. The road over the pass is also known as Mission Mountain, which is short for "Mission Mountain Road". Mission Creek lies on the north side of the pass, and is a tributary of the Bridge River, the lower reaches of which lie on the north side of the ridge, and which was the only road access into the upper Bridge River Country before the construction of a road through the Bridge River Canyon in the mid-1950s opened that region up to road access from the lower Bridge River valley and the town of Lillooet via the community of Moha. Most, or virtually all, of the ridge, is Indian Reserves, notably Slosh 1, under the administration of the Seton Lake Indian Band, and Bridge River 1, which is under the administration of the Bridge River Indian Band. Parts of the ridge's eastern end are in reserves controlled by the Lillooet Indian Band, including its final spires above Lillooet, which were dubbed St. Mary's Mount by the Reverend Lundin Brown in the 1860s, though that name never stuck and is ungazetted.
Summit Lake, elevation 710 m (2329 ft), is a lake in the Central Interior of British Columbia, Canada, located to the north of the city of Prince George. It is the namesake of the community of the same name, which lies alongside the John Hart Highway to the south of the community of McLeod Lake. It is at the head of the Crooked River, which flows north to McLeod Lake.
Upper Summit Lake is a lake in Cariboo Land District, in the Central Interior of British Columbia, Canada, about 40 kilometres (25 mi) north of the city of Prince George and 20 kilometres (12 mi) south of the community of Bear Lake. It lies just west of Highway 97.
The Lillooet Land District is one of the 59 cadastral subdivisions of British Columbia, which were created by the Lands Act of the Colony of British Columbia in 1859, defined as "a territorial division with legally defined boundaries for administrative purposes". The land district's boundaries came to be used as the boundary of the initial Lillooet riding for the provincial Legislature from 1871, when the colony became a province. In addition to use in descriptions of land titles and lot surveys, the Land District was also the basis of the Lillooet Mining District.
Otter Mountain is a prominent 2,693-metre (8,835-foot) glaciated summit located in the Coast Mountains of British Columbia, Canada. It is situated 16 kilometers northeast of Stewart, British Columbia, and the nearest higher peak is Mount Pattullo, 25.4 km (15.8 mi) to the north. Otter ranks as the 23rd most topographically prominent summit of Canada. Topographic relief is significant as the summit rises 2,380 meters above Bitter Creek Valley in 5 kilometers. This mountain's toponym was adopted as "Mount Otter" on 24 July 1945, and officially renamed Otter Mountain on 5 November 1953 by the Geographical Names Board of Canada. Precipitation runoff from the mountain drains west into Bitter Creek which is a tributary of the Bear River, or east to Nelson Creek which is part of the Nass River drainage basin, and all ultimately finds its way to the Inside Passage.
54°50′19″N122°53′15″W / 54.83861°N 122.88750°W