Brandywine Falls Provincial Park

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.

The Whistler Olympic and Paralympic Village was a 2010 Winter Olympics facility in the resort town of Whistler, British Columbia. The Olympic Village is considered one of Whistler's legacy projects, in that it is being used after the Olympics to help house and train Canadian athletes. Whistler is one of the two host communities for the Games. The site of this athletes' village is in the Cheakamus Valley approximately 20 minutes south of the Whistler Mountain competition venues, and 6 km from the highway cutoff for the Whistler Olympic Park sliding events venue in the Callaghan Valley. The village held 2,400 athletes and officials. The athletes and officials housed in this village participated in the events held at the Whistler Olympic Park, Whistler Creekside and the Whistler Sliding Centre. The cost of the village was estimated at 32 million dollars. It consists of a 100-room lodge and a 20-unit townhouse complex.

Barrier Lake, formerly called Stony Lake, is a small lake in New Westminster Land District of southwestern British Columbia, Canada. It is located west of Garibaldi Lake in Garibaldi Provincial Park. The name of the lake was adopted on September 2, 1930, for its association with The Barrier, a volcanic dam retaining the Garibaldi Lake system. Barrier Lake has a mean annual discharge of 10.44 m3/s (369 cu ft/s). Barrier Lake is an expansion of Rubble Creek, which flows northwest into the Cheakamus River. This stream follows a subterranean channel under The Barrier at Lesser Garibaldi Lake just to the southeast, but at times of exceptionally high water, a part of it flows over the surface of the volcanic dam to Barrier Lake. Rubble Creek then flows through an outlet at the southwestern end of Barrier Lake where it flows over the headwall of The Barrier into the lower valley. Barrier Lake lies within a depression that straddles on a contact between andesitic lava of The Barrier and sedimentary rocks forming the northern side of upper Rubble Creek valley. The sedimentary rocks are of Cretaceous age, whereas the andesitic lava is of Late Pleistocene age. About 13,000 years ago, the andesitic lava was erupted from Clinker Peak and flowed into Rubble Creek valley where it ponded and cooled against residual glacial ice to form The Barrier. The lava lobe damming the southern end of Barrier Lake apparently formed when molten lava broke through the northern levee of The Barrier lava flow. Because the lake is in close proximity to the unstable headwall of The Barrier, it has been suggested that Barrier Lake, along with Lesser Garibaldi Lake, could be released in the event of a catastrophic collapse. If these lakes were to be released, they could initiate a debris flow capable of blocking the Cheakamus River or running out into Daisy Lake. However, the probability of this happening is considered to be very low.

The Black Tusk, known as Q̓elqámtensa ti Skenknápa in the St'at'imcets (Lillooet) language and as T'ákt'akmúten tl'a Ín7inyáx̱a7en in the Sḵwx̱wú7mesh (Squamish) language, is a stratovolcano and a pinnacle of volcanic rock in Garibaldi Provincial Park of British Columbia, Canada. At 2,319 m (7,608 ft) above sea level, the upper spire is visible from a great distance in all directions. It is particularly noticeable from the Sea-to-Sky Highway just south of Whistler, British Columbia. Distinctive and immediately identifiable, The Black Tusk is among the best known mountains in the Garibaldi Ranges of the Coast Mountains. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Canadian Cascade Arc, but it is not within the geographic boundary of the Cascade Range.

The Whistler Olympic Park is the location of the Nordic events facilities for the 2010 Winter Olympics and is located in the Madeley Creek basin in the Callaghan Valley, west of Whistler, British Columbia, Canada. The facility hosted the biathlon, cross-country skiing, Nordic combined, and ski jumping. After the Olympics the park remains a public facility, complementing the extensive wilderness trails and alpine routes already in use. Three temporary stadiums were built with a capacity for 12,000 spectators each (6,000 for the Paralympics). The location is approximately 8 km from the junction of its access road with Highway 99 and 14 km from the Whistler Olympic Village. The two year construction project saw, 14 km (8.7 mi) of cross country and biathlon trails, two ski jumps (HS 106 and HS 140 metre), and another 20 to 25 km of recreational trails built. There is also a permanent Biathlon range which can be used daily. Overall, $119.7 million was spent on the facilities in the Callaghan Valley. Permanent features were completed in the fall of 2007. It is now a public cross-country and back country ski facility. Located between the ski jumps and cross country area there is an 11,000-square-foot (1,000 m2) Day Lodge. Which has a gift shop, cafeteria, washrooms, lounge and rental center. In addition to the Lodge, there are two 6,000-square-foot (560 m2) Technical Buildings, one for Cross Country and one for Biathlon located at each of the sports main venue area of the park. There are also other necessary infrastructure facilities on site. The park was officially opened to the public on November 22, 2008 at noon PST despite having no snow the previous evening. Inauguration took place at the day lodge to mark the start of the public skiing season. 500 people daily would use the lodge during weekends and 100 during a regular weekday.During the Olympics the park was managed by VANOC, it is now owned and operated by Whistler 2010 Sport Legacies. They also operate the Sliding Center and Training Center. World Cup competitions at the park took place the weekend of January 15–18, 2009 for cross-country skiing and Nordic combined. Eleven Nordic combined teams totalling 50 skiers and 47 support staff along with 17 cross country teams with about 230 skiers participated in the event. Ski jumping World Cup at the venue took place on the weekend of January 22–25, 2009. The Park is the first venue in 2009 to have its operational readiness tested for the upcoming Games in 2010.Winners of the test events for cross country skiing were Slovakia's Alena Prochazkova in women's sprint, Emil Jönsson of Sweden in the men's sprint, Justyna Kowalczyk of Poland in the women's double pursuit, Italy's Pietro Piller Cottrer in the men's double pursuit, and in the team sprint, the winners were Italy for the women (Magda Genuin and Arianna Follis) and Sweden for the men (Jönsson and Robin Bryntesson). The Nordic combined winners were Bill Demong of the United States on the 16th and Norway's Magnus Moan on the 17th. Austria's Gregor Schlierenzauer won both ski jumping test events.

Alexander Falls is a waterfall on Madeley Creek, a tributary of Callaghan Creek in the Callaghan Valley area of the Sea to Sky Country of southwestern British Columbia, Canada. The falls are located just below a bridge on the access road to Callaghan Lake Provincial Park, at the head of the valley, which lies to the west of the resort town of Whistler.The falls consist of three drops that total up to 141 feet (43 m) in total. The falls are about 40 feet (12 m) wide.

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.

CKEE-FM is a Canadian radio station broadcasting at 101.5 FM in Whistler, British Columbia, British Columbia with a modern adult contemporary/classic rock format branded on-air as 101.5 Whistler FM.

Tricouni Peak is a mountain located south of Cypress Peak on the Squamish-Cheakamus divide within the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It was named in 1931 by Tom Fyles et al., the first ascent party. According to Tom Fyles himself, "Tricouni Mountain was the name suggested for the peak, as from a distance it had the appearance of three cones". A misinterpreted "resemblance to a 3-pointed tricouni boot nail" was mentioned only much later, and not by Fyles. The name "Tricouni Peak" was adopted on 22 June 1967.

Panorama Ridge is a mountain ridge in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It is located on the north side of Garibaldi Lake in Garibaldi Provincial Park. Panorama Ridge was named around 1912 by William J. Gray, a Canadian geologist from Vancouver who took most of his panoramic photos on the ridge.

Cypress Peak is a mountain peak south of Brandywine Mountain on the Squamish-Cheakamus divide, west of Whistler in the New Westminster Land District of British Columbia, Canada. The mountain was named after nearby Cypress Creek (which has since been renamed Roe Creek).

Whistler station is a railway station located in Whistler, British Columbia, Canada, along the BC Rail line. The operations of the line are now run by Canadian National via a long-term lease between CN & BC Rail. Rocky Mountaineer runs a single train that calls at the station once a week in high-season, the Rainforest to Gold Rush which provides service from North Vancouver railway station to Quesnel railway station and Jasper railway station. Rocky Mountaineer discontinued the Whistler Sea to Sky Climb, its once-daily service to Whistler, in 2016. The PGE line was established in 1912, and rail service to the Whistler area has been provided since the early days of operation until BC Rail ended all passenger service in 2002. The line is now mostly freight only, with the high-end Rocky Mountaineer utilising the corridor once a week. The current station building was built for Whistler Rail Tours (former operators of the Whistler Sea to Sky Climb) in 2007.During the 2010 Winter Olympics, a special Rocky Mountaineer train sponsored by the government of the neighbouring province of Alberta served as public transit between Vancouver and Whistler.