Highway 99, also known as the Fraser Delta Thruway south of Vancouver, and the Sea to Sky Highway, the 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 American border.
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 Squamish-Lillooet Regional District is a quasi-municipal administrative area in British Columbia, Canada. It stretches from Britannia Beach in the south to Pavilion in the north. Lillooet, Pemberton, Whistler and Squamish are the four municipalities in the regional district. Its administrative offices are in the Village of Pemberton, although the district municipalities of Squamish, Whistler, and Lillooet are all larger population centres. The district covers 16,353.68 km² of land area.
The Capilano River flows from north to south through the Coast Mountains on Vancouver's North Shore between West Vancouver and North Vancouver and empties into Burrard Inlet, opposite Stanley Park. The river is one of three primary sources of drinking water for residents of Greater Vancouver, and flows through the Capilano watershed. The Cleveland Dam, built in 1954, impounds a reservoir for this purpose. The entire area of the reservoir and watershed area upstream of the dam is closed to the public to ensure the quality of the drinking water. Prior to construction of the Cleveland Dam, the Capilano River deposited large amounts of sediment into Burrard Inlet. A dredge was needed to remove this sediment build-up in order to keep Burrard Inlet open for ship traffic.
The Fraser Canyon is a major landform of the Fraser River where it descends rapidly through narrow rock gorges in the Coast Mountains en route from the Interior Plateau of British Columbia to the Fraser Valley. Colloquially, the term "Fraser Canyon" is often used to include the Thompson Canyon from Lytton to Ashcroft, since they form the same highway route which most people are familiar with, although it is actually reckoned to begin above Williams Lake, British Columbia at Soda Creek Canyon near the town of the same name.
The Squamish River is a short but very large river in the Canadian province of British Columbia. Its drainage basin is 3,328 square kilometres (1,285 sq mi) in size. The total length of the Squamish River is approximately 80 kilometres (50 mi).
The Elaho River is a c.70 km long river beginning in the Coast Mountains northwest of the towns of Whistler and Pemberton, British Columbia. It is a tributary of the Squamish River and is known for its whitewater rafting and kayaking as well as for the intense alpine scenery lining its route.
The Klinaklini River is one of the major rivers of the Pacific Ranges section of the Coast Mountains in the Canadian province of British Columbia. It originates in the Pantheon Range and empties into the head of Knight Inlet.
Brandywine Falls Provincial Park is a provincial park in British Columbia, Canada, located adjacent to BC Highway 99 between Garibaldi and Whistler, British Columbia. It is managed by Sea to Sky Parks for BC Parks.
The Sea-to-Sky Corridor, often referred to as the Corridor or the Sea to Sky Country, is a region in British Columbia spreading from Horseshoe Bay through Whistler to the Pemberton Valley and sometimes beyond to include Birken and D'Arcy. From Whistler on up, the region overlaps with the older and more historic Lillooet Country, of which Squamish, at the region's centre, was once the southward extension in the days when it was the rail-port terminus from the Interior, via Lillooet, and accessible from the Lower Mainland only by sea. Most of the region is in the Squamish-Lillooet Regional District, although south of Britannia Beach a small part of the region is in the Greater Vancouver Regional District.
The Callaghan Valley is located in the Sea to Sky Country of southwestern, British Columbia, in the Pacific Ranges of the Coast Mountains 90 km north of Vancouver. It was the home of the 2010 Winter Olympics's Whistler Olympic Park, the venue for the Nordic events of the Olympics, and adventure tourism operations including Canadian Wilderness Adventures.
The Cheakamus River derailment occurred on August 5, 2005, when nine cars that were from a Canadian National Railway freight train derailed and crashed into the Cheakamus River in British Columbia. The cars contained approximately 40,000 litres of caustic soda, which entered the river, killing more than 500,000 fish from 10 different species, including chinook salmon, coho salmon, pink salmon, and rainbow trout, both freshwater and ocean-dwelling.
Daisy Lake, also referred to as Daisy Lake Reservoir, is a reservoir on the Cheakamus River in the Sea to Sky Corridor of southwestern British Columbia, Canada, just south of the Resort Municipality of Whistler and immediately north of the abandoned townsite of Garibaldi.
Brandywine Creek, also formerly known as the Long John River after a local prospector and trapper, is a tributary of the Cheakamus River in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, entering that stream via Daisy Lake, just below Brandywine Falls. The creek is about 14 km in length and originates on the south slope of Brandywine Mountain in Brandywine Meadows, at the southern end of the Powder Mountain Icefield and is the next basin immediately southwest of that of the Callaghan Valley, the site of the Nordic events facility for the 2010 Olympics. The creek's valley has been partially logged. An unnamed hot spring lies in its upper reaches, near Mount Fee.
Ashlu Creek is a short and swift river-like creek in British Columbia. It is a tributary of the Squamish River and enters it about 24.3 km northwest of Squamish.
Salmon Inlet, formerly Salmon Arm, is a fjord branching east from Sechelt Inlet in the British Columbia, Canada. Its companion, Narrows Inlet, another side-inlet of Sechelt Inlet, lies roughly 10 km (6.2 mi) north. Misery and Sechelt Creeks flow freely into the inlet, while the Clowhom River flows in from the artificial Clowhom Lake, formed by a small hydroelectric power development. The fjord is 23 km (14 mi) long; Clowhom Lake, covering a waterfall on the Clowhom River, stretches a further 12 km (7.5 mi) to the western base of Mount Tantalus, which is best known from the direction of Squamish and the Cheakamus Canyon stretch of British Columbia Highway 99. Heavily affected by logging and milling operations, the inlet is split almost into two portions by an alluvial fan spreading from the mouth of Sechelt Creek.
The Mount Cayley volcanic field (MCVF) is a remote volcanic zone on the South Coast of British Columbia, Canada, stretching 31 km (19 mi) from the Pemberton Icefield to the Squamish River. It forms a segment of the Garibaldi Volcanic Belt, the Canadian portion of the Cascade Volcanic Arc, which extends from Northern California to southwestern British Columbia. Most of the MCVF volcanoes were formed during periods of volcanism under sheets of glacial ice throughout the last glacial period. These subglacial eruptions formed steep, flat-topped volcanoes and subglacial lava domes, most of which have been entirely exposed by deglaciation. However, at least two volcanoes predate the last glacial period and both are highly eroded. The field gets its name from Mount Cayley, a volcanic peak located at the southern end of the Powder Mountain Icefield. This icefield covers much of the central portion of the volcanic field and is one of the several glacial fields in the Pacific Ranges of the Coast Mountains.
Cheekye is an unincorporated locality on the Cheakamus River just upstream from its confluence with its parent stream, the Squamish, and just north of Brackendale, British Columbia, which is part of the District of Squamish, British Columbia, Canada.
Paradise Valley is a rural-residential area north of Brackendale, British Columbia, Canada, located along the right (west) bank of the Cheakamus River. It begins just below that river's canyon, and continues downstream towards Cheekye, where the road from Brackendale crosses the Cheakamus. Located to the southwest of Brohm Lake, which is in the rocky upland on the other side of the Cheakamus and adjacent to BC Highway 99, it is largely flat and a floodplain and is home to the main facility of the Coast Mountain Outdoor School as well as the C-Dar Lodge Biodynamic facility. Many Paradise Valley residents participate at the weekly farmers market in nearby Squamish.
The Mount Cayley massif is a group of mountains in the Pacific Ranges of southwestern British Columbia, Canada. Located 45 km (28 mi) north of Squamish and 24 km (15 mi) west of Whistler, the massif resides on the edge of the Powder Mountain Icefield. It consists of an eroded but potentially active stratovolcano that towers over the Cheakamus and Squamish river valleys. All major summits have elevations greater than 2,000 m (6,600 ft), Mount Cayley being the highest at 2,385 m (7,825 ft). The surrounding area has been inhabited by indigenous peoples for more than 7,000 years while geothermal exploration has taken place there for the last four decades.
