Highway 99, also known as the Fraser Delta Thruway south of Vancouver, and the Sea to Sky Highway, Squamish Highway, or Whistler Highway north of Vancouver, is the major north–south artery running through the Greater Vancouver area of British Columbia from the U.S. border, up Howe Sound through the Sea to Sky Country to Lillooet, and connecting to Highway 97 just north of Cache Creek. The highway's number was derived from the former U.S. Route 99, with which the highway originally connected to at the border. The highway currently connects with Interstate 5 at the United States border.
Highway 97 is the longest continuously numbered route in the Canadian province of British Columbia, running 2,081 km (1,293 mi) from the Canada–United States border near Osoyoos in the south to the British Columbia/Yukon boundary in the north at Watson Lake, Yukon. The route takes its number from U.S. Route 97, with which it connects at the international border. The highway was initially designated '97' in 1953.
Dawson Creek is a city in northeastern British Columbia, Canada. The municipality of 24.37 square kilometres (9.41 sq mi) had a population of 12,978 in 2016. Dawson Creek derives its name from the creek of the same name that runs through the community. The creek was named after George Mercer Dawson by a member of his land survey team when they passed through the area in August 1879. Once a small farming community, Dawson Creek became a regional centre after the western terminus of the Northern Alberta Railways was extended there in 1932. The community grew rapidly in 1942 as the US Army used the rail terminus as a transshipment point during construction of the Alaska Highway. In the 1950s, the city was connected to the interior of British Columbia via a highway and a railway through the Rocky Mountains. Since the 1960s, growth has slowed, but the area population has increased.
The Stikine River is a major river in northern British Columbia, Canada and southeastern Alaska in the United States. Draining a large, remote upland area known as the Stikine Country east of the Coast Mountains, it flows west and south for 610 kilometres (379 mi), emptying into various straits of the Inside Passage near Wrangell, Alaska. About 90 percent of the river's length and 95 percent of its drainage basin are in Canada. Considered one of the last truly wild large rivers in British Columbia, the Stikine flows through a variety of landscapes including boreal forest, steep canyons and wide glacial valleys.
The Peace River is a 1,923-kilometre-long (1,195 mi) river in Canada that originates in the Rocky Mountains of northern British Columbia and flows to the northeast through northern Alberta. The Peace River joins the Athabasca River in the Peace-Athabasca Delta to form the Slave River, a tributary of the Mackenzie River. The Finlay River, the main headwater of the Peace River, is regarded as the ultimate source of the Mackenzie River. The combined Finlay–Peace–Slave–Mackenzie river system is the 13th longest river system in the world.
The Skagit River is a river in southwestern British Columbia in Canada and northwestern Washington in the United States, approximately 150 mi (240 km) long. The river and its tributaries drain an area of 1.7 million acres (690,000 hectares) of the Cascade Range along the northern end of Puget Sound and flows into the sound.
The Skeena River is the second-longest river entirely within British Columbia, Canada. Since ancient times, the Skeena has been an important transportation artery, particularly for the Tsimshian and the Gitxsan—whose names mean "inside the Skeena River" ,and "people of the Skeena River," respectively. The river and its basin sustain a wide variety of fish, wildlife, and vegetation, and communities native to the area depend on the health of the river. The Tsimshian migrated to the Lower Skeena River, and the Gitxsan occupy territory of the Upper Skeena.
The Thompson River is the largest tributary of the Fraser River, flowing through the south-central portion of British Columbia, Canada. The Thompson River has two main branches, the South Thompson River and the North Thompson River. The river is home to several varieties of Pacific salmon and trout. The area's geological history was heavily influenced by glaciation, and the several large glacial lakes have filled the river valley over the last 12,000 years. Archaeological evidence shows human habitation in the watershed dating back at least 8,300 years. The Thompson was named by Fraser River explorer, Simon Fraser, in honour of his friend, Columbia Basin explorer David Thompson. Recreational use of the river includes whitewater rafting and angling.
The Liard River of the North American boreal forest flows through Yukon, British Columbia and the Northwest Territories, Canada. Rising in the Saint Cyr Range of the Pelly Mountains in southeastern Yukon, it flows 1,115 km (693 mi) southeast through British Columbia, marking the northern end of the Rocky Mountains and then curving northeast back into Yukon and Northwest Territories, draining into the Mackenzie River at Fort Simpson, Northwest Territories. The river drains approximately 277,100 km2 (107,000 sq mi) of boreal forest and muskeg.
The Peace River Regional District is a regional district in northeastern British Columbia, Canada. The regional district comprises seven municipalities and four electoral areas. Its member municipalities are the cities of Fort St. John and Dawson Creek, the district municipalities of Tumbler Ridge, Chetwynd, Taylor, and Hudson's Hope, and the village of Pouce Coupe. The district's administrative offices are in Dawson Creek.
The Pitt River in British Columbia, Canada is a large tributary of the Fraser River, entering it a few miles upstream from New Westminster and about 25 km ESE of Downtown Vancouver. The river, which begins in the Garibaldi Ranges of the Coast Mountains, is in two sections above and below Pitt Lake and flows on a generally southernly course. Pitt Lake and the lower Pitt River are tidal in nature as the Fraser's mouth is only a few miles downstream from their confluence.
Bearhole Lake Provincial Park is a provincial park in British Columbia, Canada, located 5 km east of the mining community of Tumbler Ridge, on the Alberta Plateau. Established in January 2001, the park includes 12,705 ha of land in the Boreal White and Black Spruce biogeoclimatic zones within the Kiskatinaw Plateau. It is transition zone with mixed wood forests including spruce, pine, and larch. Bearhole Lake, the headwaters of the Kiskatinaw River provides habitat for trumpeter swans, yellow perch, burbot, rainbow trout, and northern pike.
Kiskatinaw Provincial Park is a provincial park located in Peace River Regional District in British Columbia, Canada. It was established on May 1, 1962 to protect a prominent horseshoe-shaped incised meander in the Kiskatinaw River where a historic curved bridge crosses the river along the original alignment of the Alaska Highway.
One Island Lake Provincial Park is a provincial park in British Columbia, Canada.
The Pouce Coupe River is a major tributary of the Peace River in Alberta and British Columbia, Canada. Its name is officially spelled Pouce Coupé River, but it is commonly written without the acute accent.
Bridge Lake is a lake in the Interlakes District of the South Cariboo region of the Interior of British Columbia, Canada. It is the source of Bridge Creek which runs in a curving course west and then northeast to Canim Lake via the town of 100 Mile House. The lake is approximately 16 km2 in area (including the area of several islands and rocks in the lake, the largest of which is named Long Island and is 1136 m in elevation. It is located 560 km north of Vancouver and around 140 km northwest of Kamloops in the Interlakes District close to the Little Fort Highway. It and its neighbours Sheridan Lake and Lac des Roches are the largest lakes along the Interlakes Highway.
The Kiskatinaw Formation is a stratigraphical unit of Mississippian age in the Western Canadian Sedimentary Basin.
Charlie Lake is a lake in north-eastern British Columbia, Canada, situated 8 km (5.0 mi) west from Fort St. John, along the Alaska Highway. The lake provides the water supply for the city of Fort St. John. The Charlie Lake Formation, a stratigraphical unit of the Western Canadian Sedimentary Basin is named for the lake.
The Prophet River is a river in northern British Columbia, Canada. It is a tributary of the Muskwa River.
The Nanaimo River is a river on Vancouver Island, British Columbia, Canada, located near the city of Nanaimo on the island's east coast. Its headwaters are in the Vancouver Island Ranges of central Vancouver Island and its mouth, the Nanaimo River estuary, is at the south end of Nanaimo Harbour in the Strait of Georgia. The estuary is part of the Pacific Estuary Conservation Program.
