Squamish-Lillooet Regional District

Moran Dam, also called High Moran Dam or Moran Canyon Dam, was a 1950s proposal to dam the Fraser River in the Canadian province of British Columbia (BC). The structure was planned in the wake of devastating floods in a time of rapidly growing power demand, and if built, would have powered the largest hydroelectric facility in North America. After a protracted environmental battle, Moran Dam was defeated in 1972, mainly over concerns of its adverse impact on salmon populations in the Fraser River basin. The shelving of the project also influenced cancellation of other hydro developments along the river, and today the Fraser remains one of the most productive salmon fisheries on the continent.

Pavilion Mountain is the highest summit of the southern Marble Range in the South Cariboo region of southwestern British Columbia. "Mount Carson", a subsidiary peak, was misapplied to the whole mountain 1957–1965, before the well-established local name was restored. Pavilion Creek is to the south. Pavilion Lake and Marble Canyon are to the southeast.

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.

Fred Antoine Provincial Park is a provincial park in British Columbia, Canada, 25 kilometres northwest of Lillooet, British Columbia. The park, which is 2,230 hectares in size, was established in 2010.

The Leckie Range is a small mountain range in southwestern British Columbia, Canada, located northwest of Gun Lake between Leckie Creek and Slim Creek. It has an area of 78 km² and is a subrange of the Chilcotin Ranges which in turn form part of the Pacific Ranges of the Coast Mountains.

The Spruce Lake Protected Area, formerly known variously as the Southern Chilcotin Mountains Provincial Park, Southern Chilcotins, and also as South Chilcotin Provincial Park, is a 71,347-hectare Protected Area in the British Columbia provincial parks system, approximately 200 km north of Vancouver. The area had been the subject of an ongoing preservationist controversy since the 1930s. In 2007, its status as a provincial park was downgraded to protected area.

Tyoax Pass is a mountain pass in the Chilcotin Ranges of the Pacific Ranges, the southernmost main subdivision of the Coast Mountains of British Columbia, Canada. Located at the head of Tyaughton Creek, a north tributary of the Bridge River, it connects the basin of the Bridge River with that of Big Creek in the southern Chilcotin District, and is therefore at the boundary between the Spruce Lake Protected Area and Big Creek Provincial Park.

Griswold Pass is a mountain pass in the Pacific Ranges of the Coast Mountains of British Columbia, located at the head of Nichols Creek, a tributary of the upper Bridge River (S), and the head of Griswold Creek, a tributary of the Lord River (N), which feeds the Taseko Lakes and is effectively a tributary of the Taseko River (which enters those lakes separately). The Nichols Creek area is part of the volcanic formation known as the Bridge River Cones, while to the north of the pass the Taseko Lakes basin is part of Tsy'los Provincial Park.

The Lillooet Museum in Lillooet, British Columbia, Canada is located on that town's Main Street, across from the "Mile '0'" cairn marking the beginning point of the Old Cariboo Road to Alexandria in the Cariboo region.

Keatley Creek is a left tributary of the Fraser River in the Glen Valley area of the Fraser Canyon in the Interior of British Columbia, Canada. Its outlet into the Fraser is between those of Pavilion and Fountain Creeks, approximately 16 miles upstream from the town of Lillooet; the next tributary southwards is the larger Sallus Creek.

The Bridge River is a river in southern British Columbia, Canada. It flows south-east from the Coast Mountains. Until 1961, it was a major tributary of the Fraser River, entering that stream about six miles upstream from the town of Lillooet; its flow, however, was near-completely diverted into Seton Lake with the completion of the Bridge River Power Project, with most of the river's water now entering the Fraser just south of Lillooet as a result. The Bridge River hydroelectric complex, operated by BC Hydro, consists of three successive dams, providing water for four hydro power plants with the total rated power of total 492 megawatts.

Lillooet Airport (ICAO: CYLI) is located 1.5 nautical miles (2.8 km; 1.7 mi) east southeast of Lillooet, British Columbia, Canada.

CHLS-FM is a Canadian radio station, broadcasting at 100.5 FM in Lillooet, British Columbia. The station airs a community radio format branded as Radio Lillooet.

Cayoosh Creek is a northeast-flowing tributary of the Seton River in the Canadian province of British Columbia. The name Cayoosh Creek remains on the bridge-sign crossing the stream on BC Highway 99 and continues in use locally to refer to the final reaches of the Seton River, formerly Seton Creek, which prior to the renaming ending at the confluence with Cayoosh Creek. The creek is the namesake of Cayoosh Creek Indian Reserve No. 1, one of the main Indian reserves of the Cayoose Creek Indian Band (aka the Sekwelwas First Nation), which lies adjacent to what was renamed the Seton River without local consultation.

Fort Berens, also spelled Fort Behrens, was a never-completed establishment of the Hudson's Bay Company on the Fraser River, located immediately across the river from today's town of Lillooet, British Columbia, Canada, in that province's central Fraser Canyon region. The post was designated and materials ordered for its construction in 1859, and was intended to serve as a supply outlet for the gold rush population of the area, which was the northern centre of gold-mining activity on the Fraser during the Fraser Canyon Gold Rush (1858–60). Although a plot of land was allocated, and building supplies were brought into the site, the post was never constructed and by 1861 orders from company headquarters decommissioned the post and the supplies were removed due to an absence of economic viability with the collapse of the rush. A "satellite" of Fort Kamloops, the post was named after Henry Hulse Berens, deputy Hudson's Bay Company governor 1856-58 and governor 1858-63. Immediately adjacent to the site that was to be Fort Berens, just to its north, were the boomtowns of Parsonville (or Parsonsville) and Marysville, which likewise disappeared by the end of the rush, though the Parsonville name remained in use as a tobacco press and farm for the locality for some time. A cable ferry connected the town of Lillooet and the three localities on the east bank of the Fraser. The route to the Cariboo known as the Old Cariboo Road (not to be confused with the Cariboo Road from Yale) started from the east bank and ran via Pavilion and Clinton to Alexandria.

Pavilion is an unincorporated community on the eastern side of the Fraser River in the South Cariboo region of southwestern British Columbia. The place is near Mile 21 of the Old Cariboo Road. On BC Highway 99, the locality is by road about 36 kilometres (22 mi) northeast of Lillooet and 135 kilometres (84 mi) west of Kamloops.

The Seton Canal is a diversion of the flow of the Seton River from Seton Dam, just below the flow of Seton Lake, to the Seton Powerhouse on the Fraser River at the town of Lillooet, British Columbia, Canada. The canal bridges Cayoosh Creek 300m below its commencement and is about 3.5 km in length, ending just below a bridge used by the Texas Creek Road (aka the West Side Road), where the canal's waterflow is fed into tunnels which feed the Seton Powerhouse on the farther side of a small rocky hill. Most of the water carried by the canal is the volume of the diverted Bridge River, which is fed into Seton Lake via BC Hydro's Bridge River generating stations at Shalalth, 16 km to the west, which are supplied by diversion tunnels through Mission Ridge from Carpenter Lake, the reservoir created by Terzaghi Dam.

The Seton River is a tributary of the Fraser River in the Canadian province of British Columbia. The name is relatively new, and encompasses what had formerly been the Seton Portage River or Portage Creek (aka Portage River) and Seton Creek (which shows up on some topos as "Section Creek" due to a mis-read of old hand-written maps).

The T'it'q'et also known as the T'it'k'it, the Tl'itl'kit and as the Lillooet Indian Band, is a First Nations government located in the Central Interior-Fraser Canyon region of the Canadian province of British Columbia.

Xaxli'p, (Lillooet: xáxl̓ǝpamx) also known as the Fountain or the Fountain Indian Band, is a First Nations government located in the Central Interior-Fraser Canyon region of the Canadian province of British Columbia. It is a member of the Lillooet Tribal Council, which is the largest grouping of band governments of the St'at'imc people (aka the Lillooet people).

The Lillooet Suspension Bridge, also known as the Lillooet Old Bridge, is a suspension bridge located in Lillooet, British Columbia. The bridge passes over the Fraser River and connects the town of Lillooet with British Columbia Highway 99.

A series of ferries and bridges have crossed the Fraser River in the vicinity of Lillooet in the Squamish-Lillooet region of southwestern British Columbia. From the 1850s, these crossings have connected both north–south and local traffic.

Mount McLean is a 2,427-metre (7,963-foot) mountain summit located in British Columbia, Canada.

The Bridge River Power Project is a hydroelectric power development in the Canadian province of British Columbia, located in the Lillooet Country between Whistler and Lillooet. It harnesses the power of the Bridge River, a tributary of the Fraser, by diverting it through a mountainside to the separate drainage basin of Seton Lake, utilizing a system of three dams, four powerhouses and a canal.

Mission Pass is a historic mountain pass in the Bridge River-Lillooet Country of the Interior of British Columbia, Canada, around 20 km (12 mi) west of Lillooet, towards the west end of Seton Lake. The summit is 1,187 metres (3,894 ft) above sea level.

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.

Mount Bishop is a mountain in the Camelsfoot Range in the Lillooet Country of the Central Interior of British Columbia. Named for an old settler, it is located four km north of the settlement of Moha, which is at the confluence of the Bridge and Yalakom Rivers.

The Seton Lake First Nation, a.k.a. the Seton Lake Indian Band, is a First Nations government located in the Central Interior-Fraser Canyon region of the Canadian province of British Columbia. It is a member of the Lillooet Tribal Council, which is the largest grouping of band governments of the St'at'imc people (a.k.a. the Lillooet people). Other St'at'imc governments include the smaller In-SHUCK-ch Nation on the lower Lillooet River to the southwest, and the independent N'quatqua First Nation at the farther end of Anderson Lake from Seton Portage, which is the location of three of the band's reserve communities.

The Shulaps Range is a subrange of the Chilcotin Ranges subset of the Pacific Ranges of the Coast Mountains in southwest-central British Columbia. The range is 55 km NW–SE and 15 km SW–NE and 2,970 km² (1,150 sq mi) in area.

The Yalakom River is a tributary of the Bridge River, which is one of the principal tributaries of the Fraser River, entering it near the town of Lillooet, British Columbia. In frontier times it was also known as the North Fork of the Bridge River, and joins the Bridge River proper at Moha, a rural community with a history in ranching, farming and mining. The river is approximately 56 kilometres (35 mi) in length. The valley's climate is semi-arid in character and lodgepole pine predominates below treeline.

Gun Creek is a major left (north) tributary of the Bridge River in the Interior of British Columbia, Canada. Located at its mouth into today's Carpenter Lake was Minto City, a gold mining town established in the 1930s and destroyed by a flood in the later 1940s. Carpenter Lake is a reservoir of the Bridge River Hydroelectric Project. Gun Lake is part of the creek's basin but is not on the creek itself, but connected to it by a short stream from its northeastern end.

Whitecap Mountain is a 2,918-metre (9,573-foot) summit in British Columbia, Canada.

The Bendor Range is a small but once-famous subrange of the Pacific Ranges of the Coast Mountains, about It is approximately 7,000 square kilometres (2,700 sq mi) in area and about 40 km long (NW to SE) and about 18 km at its widest. It lies between Anderson Lake on the southeast and the Carpenter Lake Reservoir or the Bridge River Power Project on the north, with the gold-rich valley of Cadwallader Creek on its southwest.

Cadwallader Creek is an important tributary of the Hurley River in the Bridge River Country of the British Columbia Interior, Canada, most notable for its role as the home of the Bralorne and Pioneer Mines and associated gold claims and workings. Less than twenty miles in length, the creek is joined by Noel Creek within the area of the town of Bralorne, and just below Bralorne joins the Hurley River just above Hurley Falls and that river's ten-mile canyon prior to its own confluence with the Bridge River near the town Gold Bridge. Standard Creek, a short tributary of Cadwallader Creek near its upper end, connects via McGillvray Pass to the creek of the same name and, on Anderson Lake far below, the resort townlet of McGillivray Falls. One-time plans to build a cog railway to the mines from the Pacific Great Eastern at McGillivary Falls were never fulfilled.

McGillivray Pass (1867 m or 6215 ft) is a mountain pass in the Pacific Ranges of southwestern British Columbia, Canada, located about 30 miles west of the town of Lillooet and immediately west of the upper end of Anderson Lake, above the former resort community of McGillivray (formerly McGillivray Falls). The pass connects the head of McGillivray Creek with the head of Standard Creek, a tributary of Cadwallader Creek and was used as a route by prospectors, miners and hunters heading for the upper Bridge River Country beyond the pass.

Minto City, often called just Minto, sometimes Minto Mines_, Minto Mine, Skumakum, or "land of plenty", was a gold mining town in the Bridge River Valley of British Columbia from 1930 to 1936, located at the confluence of that river with Gun Creek, one of its larger tributaries. The mine prospect was never much successful although a model townsite was built by promoter "Big Bill" Davidson, who imported soil to build a specially-built rodeo ground and baseball diamond on the rocky site. The larger mine of Bralorne was nearby. The mine shut down in 1936 due to productivity issues, but restarted in 1940. The valley has since been significantly altered when most of the vestiges of the town were inundated by the waters of the Carpenter Lake reservoir following completion of the Bridge River Power Project. In 1941, around two dozens of Japanese Canadian families were relocated to Minto Mine, and ordered to live in the empty miners' houses due to the impacts of the war.

Tyaughton Creek, formerly gazetted as the Tyaughton River, also historically known as Tyoax Creek, is a 50 kilometre tributary of British Columbia's Bridge River, flowing generally southeast to enter the main flow of that river about mid-way along the length of Carpenter Lake, a reservoir formed by Terzaghi Dam of the Bridge River Power Project.

Mount Sloan is a 2,720-metre (8,924-foot) mountain summit located in British Columbia, Canada.

Haylmore is a location in the Bridge River Country of the southwestern Interior of British Columbia, Canada, located near the town of Gold Bridge just below the confluence of the Bridge River and its south fork, the Hurley River.

Mount Thiassi is a 2,772-metre (9,094-foot) mountain summit located in the Thiassi Range of the Coast Mountains, in southwestern British Columbia, Canada. It is the third-highest point in the Thiassi Range. Mount Thiassi is situated 56 km (35 mi) northwest of Pemberton, and 6.9 km (4 mi) south-southwest of Mount Vayu, which is its nearest higher peak. Precipitation runoff from the peak and meltwater from unnamed glaciers on its slopes drain into tributaries of the Lillooet, Bridge, and Hurley Rivers. The first ascent of the mountain was made in 1965 by Dick Culbert and Alice Purdey. The mountain's name was submitted by this first ascent party to commemorate Thiassi, the god of storms according to Norse mythology. The name was officially adopted June 22, 1967, by the Geographical Names Board of Canada.

Sessel Mountain is a 2,746-metre (9,009-foot) mountain summit located in the Thiassi Range of the Coast Mountains, in southwestern British Columbia, Canada. It is the fourth-highest point in the Thiassi Range. Sessel is situated 46 km (29 mi) northwest of Pemberton, and 4.3 km (3 mi) northwest of Mount Sampson, which is its nearest higher peak. An unnamed icefield rests on the northern side of the peak, and the Boomerang Glacier lies at the base of the south slopes. Precipitation runoff from the peak drains into tributaries of the Lillooet and Hurley Rivers. The mountain's descriptive name was submitted by mountaineer Karl Ricker of the Alpine Club of Canada for its similar shape to a sessel, the German word for "armchair". The name was officially adopted January 23, 1979, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1974 by John Clarke.

The Hurley River is a major tributary of the Bridge River of west-central British Columbia that was earlier known as the South Fork of that larger river. It was for a while known as "Hamilton's River" after Danny Hamilton, an American who was among the first to settle in the goldfields region of the upper Bridge River. By the 1920s that name was changed to the Hurley River, commemorating one of the main pioneers of the Lillooet Country, Dan Hurley.

The Dickson Range is a subrange of the Chilcotin Ranges subset of the Pacific Ranges of the Coast Mountains in southwest-central British Columbia. It is located just west of the town of Gold Bridge between the valley of Slim Creek to the north (a tributary of Gun Creek) and Downton Lake Reservoir to the south. At its eastern foot is Gun Lake; its western limit is at a pass between Slim Creek and Nichols Creek (which feeds the upper Bridge River just before it enters Downton Lake) near the pass which separates the Bridge River basin from that of the Lord River, which feeds the Taseko Lakes.

Downton Lake, originally Downton Reservoir, and also known as Downton Lake Reservoir, is a reservoir in the Bridge River Country of the Interior of British Columbia, Canada, formed by Lajoie Dam, the uppermost of the series of dams and diversions of the Bridge River Power Project.

Mount Noel is a Miocene volcanic complex in the Chilcotin Group in British Columbia, Canada, located 7 km (4 mi) southwest of Bralorne and north of a tributary of Noel Creek. It is 150 km (93 mi) east of the Garibaldi Volcanic Belt and is made up of flat-lying, columnar-jointed basalt flows along with debris flows and minor pyroclastic rocks. Mount Noel is thought to have formed as a result of back-arc extension behind the Cascadia subduction zone.

Mount Penrose, known locally as Penrose, 2,634 m (8,642 ft), is the easternmost summit of the Dickson Range, a subrange of the Chilcotin Ranges, near Gold Bridge, British Columbia, Canada and immediately above and to the west of Gun Lake. It was named for Senator Boies Penrose, of Philadelphia, Pennsylvania, who was the first to climb it, during a hunting expedition led by famed guide W.G. "Bill" Manson.

The Bridge River Cones, sometimes referred to as the Lillooet Cones and Salal Creek Cones, is the name given to a volcanic field located on the north flank of the upper Bridge River, about 40 km (25 mi) west of the town of Gold Bridge. The cones are in the lee of the Lillooet Icecap and sit astride a group of passes between the Bridge River, which flows W-E to their south, and the Lord River, which flows north to the Taseko Lakes in the Chilcotin District.

The Bridge River Vent is a volcanic crater in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located 51 km (32 mi) west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of 1,524 m (5,000 ft), it lies on the steep northern face of Plinth Peak, a 2,677 m (8,783 ft) high volcanic peak comprising the northern portion of Meager. The vent rises above the western shoulder of the Pemberton Valley and represents the northernmost volcanic feature of the Mount Meager massif.

The Plinth Assemblage, also known as the Plinth Formation, is an accreted terrane of igneous rocks in southwestern British Columbia, Canada, located just north of the Lillooet River and on the northern flank of the Mount Meager massif. It is named after Plinth Peak, a peak made of Plinth Assemblage rocks.

The Salal Glacier volcanic complex is a complex volcano in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located near the upper Bridge River. It is part of a volcanic group called the Bridge River Cones which in turn is part of the Garibaldi Volcanic Belt of the Canadian Cascade Arc.

Sham Hill is a volcanic plug in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located near the upper Bridge River. It is part of a volcanic group called the Bridge River Cones which in turn is part of the Garibaldi Volcanic Belt of the Canadian Cascade Arc.

Tuber Hill is a small 600,000-year-old basaltic stratovolcano that was constructed on the Bridge River highlands when nearby valleys were packed with ice. Tuber Hill is part of the Garibaldi segment of the Canadian Cascade Arc, but is not in the geographic Cascade Range.

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.

Nesikep is an unincorporated settlement in British Columbia, Canada, located at the mouth of Nesikep Creek in the Fraser Canyon, to the south of Lillooet and southeast of Texas Creek. It is primarily defined by Nesikep Indian Reserve No. 6 and Nesikep Indian Reserve No. 6A. Nesikep Indian Reserve No. 6 flanks both sides of the Fraser, though the community is only on the right (west) bank.

Texas Creek is a medium-sized right tributary of the Fraser River in the Fraser Canyon region of that river's course, located approximately 16 miles down the river from the town of Lillooet. Texas Creek is also the name of the rural neighbourhood in the area of the creek, and also that of the Texas Creek Ranch which is one of the larger holdings.

Fountain Valley, officially named Three Lake Valley and also known as the Fountain Lakes Valley, is a valley and rural community located on the east flank of Fountain Ridge, just east of the town of Lillooet, British Columbia, Canada and immediately south of the Indian reserve community of Fountain. The valley is historically significant as part of the River Trail, which ran up the length of the Fraser River from Yale to Big Bar and beyond, diverging at various points to connect to trails farther east and with the Old Cariboo Road at Fountain, then known as the Upper Fountains and an important junction and staging-ground for freight wagons and travellers bound northwards to the Cariboo goldfields. The trail through the valley, which developed into a wagon road whose roadgrade is largely used by today's road through the valley, climbs a steep grade from its southern end, near Fountainview Farms on the Fraser, and descends relatively gently towards Fountain. The three lakes in the valley, which give it its official name, are Cinquefoil Lake, Kwotlenemo Lake (aka Fountain Lake), and Chilhil Lake, the three of them collectively being known as the Fountain Lakes There are many recreational dwellings and small ranches forming a community in the valley, which is something of a rural "suburb" of Lillooet.

Mount Brew is a mountain located 12 km (7 mi) south of Lillooet and 44 km (27 mi) north of Skihist Mountain in south-central British Columbia, Canada. It lies on the western side of the Fraser River and is the third-highest mountain of the Lillooet Ranges, after Skihist Mountain and Petlushkwohap Mountain in the Cantilever Range to the west of Lytton.

Mount Rohr is a 2,423-metre (7,949-foot) mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 29 km (18 mi) east of Pemberton, 8.2 km (5 mi) east of Cayoosh Mountain, and 6.8 km (4 mi) northeast of Joffre Peak, its nearest higher peak. Highway 99 traverses the southern base of the mountain between Cayoosh Pass and the west end of Duffy Lake, while Mount Chief Pascall rises on the opposite (south) side of this highway. Mount Rohr forms the westernmost boundary of Duffey Lake Provincial Park as it also represents the park's highest point . The mountain's name was submitted by Rev. Damasus Payne, a mountaineer, to honor Rev. Victor Sebastian Rohr (1873-1965), who spent 40 years in British Columbia and was a missionary to the First Nations in the region between Skookumchuck and Williams Lake. The name was officially adopted on April 21, 1966, by the Geographical Names Board of Canada. Two established climbing routes are the West Ridge and via Rohr Lake, both of which can be skied in winter. Precipitation runoff from the peak drains north into headwaters of Haylmore Creek, or south into Cayoosh Creek.

The Cayoosh Range is the northernmost section of the Lillooet Ranges, which are a subrange of the Pacific Ranges of the Coast Mountains in British Columbia, Canada. The range covers an area of c. 1,000 km² (390 sq mi) and is approximately 65 km (40 mi) SW to NE and about 20 km (12 mi) SE to NW.

The N'Quatqua First Nation (Lillooet: nk̓ʷʕáthamx), also known as the N'quatqua Nation, the N'Quatqua Nation, the Nequatque First Nation, the Anderson Lake Indian Band, the Anderson Lake First Nation and the Anderson Lake Band , is a First Nations government of the St'at'imc (Stl'atl'imx or Lillooet) people, located in the southern Coast Mountains region of the Canadian province of British Columbia at the community of D'Arcy, where the British Columbia Railway meets the head of Anderson Lake, about midway between the towns of Pemberton and Lillooet.

Mount Aragorn is a 2,435-metre (7,989-foot) mountain summit located in the Cadwallader Range in southwestern British Columbia, Canada. It is situated 36 km (22 mi) north of Pemberton, 56 km (35 mi) west of Lillooet, and immediately north of Mount Gandalf. Precipitation runoff from the peak drains into tributaries of the Fraser River.

Mount Chief Pascall is a 2,206-metre (7,238-foot) mountain summit located in the Joffre Group of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 26 km (16 mi) east of Pemberton, 8 km (5 mi) southwest of Duffy Lake, and within Nlháxten/Cerise Creek Conservancy. Cayoosh Pass lies immediately northwest of the mountain, with Cayoosh Mountain on the opposite side of the pass. Its nearest higher peak is Joffre Peak, 2.1 km (1 mi) to the south, and Mount Rohr rises 5 km (3 mi) to the northeast. Precipitation runoff from the peak drains into tributaries of Cayoosh Creek.

Mount Gandalf is a 2,391-metre (7,844-foot) mountain summit in the Cadwallader Range in southwestern British Columbia, Canada. It is at the northeast corner of Birkenhead Lake Provincial Park, 35 km (22 mi) north of Pemberton, 56 km (35 mi) west of Lillooet, 2.9 km (2 mi) north of Tolkien Peak, and immediately south of Mount Aragorn, which is its nearest higher peak. Precipitation runoff from the peak drains into tributaries of the Fraser River.  

The Gates River is a short river in the Lillooet Country of the Southern Interior of British Columbia, Canada. Approximately 14.5 km in length, it flows generally northeast from the outlet of Birken Lake (aka Gates Lake or Summit Lake) to its mouth at the head of Anderson Lake. Its main tributaries are Haylmore Creek, from the southeast, and Blackwater Creek, from the northwest, which originates near the head of Birkenhead Lake. Augmented by the waters of McGillivray Creek, Lost Valley Creek and others, its flow becomes the Seton River from the foot of Anderson Lake onwards.

The Bridge River Country is a historic geographic region and mining district in the Interior of British Columbia, Canada, lying between the Fraser Canyon and the valley of the Lillooet River, south of the Chilcotin Plateau and north of the Lillooet Ranges. "The Bridge River" can mean the Bridge River Country as opposed to the Bridge River itself, and is considered to be part of the Lillooet Country, but has a distinct history and identity within the larger region. As Lillooet is sometimes considered to be the southwest limit of the Cariboo, some efforts were made to refer to the Bridge River as the "West Cariboo" but this never caught on.

CFNB-FM is a Canadian radio station that broadcasts a community radio format at 97.5 FM in D'arcy, British Columbia. The station is owned and operated by the Anderson Lake Recreational and Cultural Society.

The Cadwallader Range, originally named the Cadwallader Mountains, is a sub-range of the Pacific Ranges of the Coast Mountains in the Bridge River-Lillooet Country of the South-Central Interior of British Columbia, Canada, located between the south end of Anderson Lake (E) and the Hurley River. According to the provincial basemap, the precise alpine boundaries of the range are McGilliray Pass, at its eastern extremity and beyond which is the Bendor Range, and the pass between Noel and Sockeye Creeks on its west, which is immediately north of the lower end of Birkenhead Lake. The officially unnamed range west of that has been called the Noel Range, after its main peak Mount Noel. At the foot of the range along its northeast flank is Cadwallader Creek, scene of the historic and once-rich Bralorne and Pioneer Mines and the ghost town of Bralorne (a.k.a. Bralorne-Pioneer).

Cayoosh Pass (1,275 m / 4,183 ft) is a mountain pass in the Lillooet Ranges of the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada. It lies just west of Duffey Lake on BC Highway 99 between the towns of Lillooet and Pemberton, formed by the headwaters of Cayoosh Creek to the east, flowing to the Fraser River at Lillooet, and Joffre Creek to the west, flowing steeply downhill to Lillooet Lake just southeast of the Mount Currie Indian Reserve.

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.

Gates is an unincorporated rural-recreational community in the Gates Valley of the Lillooet Country in the Southern Interior of British Columbia, Canada. It is located about midway along the length of the Gates River, between the communities of Birken and D'Arcy.

Haylmore Creek is the largest tributary of the Gates River, flowing northwest from its origin in the central Cayoosh Range to join that river at the community of Devine, British Columbia, Canada, in the Lillooet Country of the Southern Interior of British Columbia.

McGillivray Creek is a creek located in the Interior of British Columbia, in the Lillooet Country.

N'Quatqua, variously spelled Nequatque, N'quat'qua, is the proper historic name in the St'at'imcets language for the First Nations village of the Stl'atl'imx people of the community of D'Arcy, which is at the upper end of Anderson Lake about 35 miles southeast of Lillooet and about the same distance from Pemberton. The usage is synonymous with Nequatque Indian Reserve No. 1, which is 177 ha. in size and located adjacent to the mouth of the Gates River (see N'Quatqua First Nation for a list of other reserves administered by the band, some of which are also named Nequatque).

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 (or "thalweg") 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 (also known as Birken Lake), at the summit of the pass (also known historically as Summit Lake or Gates Lake), which flows to the Fraser via Anderson and Seton Lakes and the Seton River.

The Nlháxten/Cerise Creek Conservancy is a 2,272-hectare conservancy north of Pemberton, British Columbia, established in 2008. Located within the mountainous Joffre Group between the Pacific Cayoosh ranges, it encompasses diverse terrain, including mountain tarns in the Anniversary Glacier area, subalpine meadows, Engelmann spruce forest ecosystems, and portions of the Cerise Creek watershed. Mount Chief Pascal (2,204 meters) stands at the center of the conservancy, with other striking peaks like Joffre Peak and Mount Matier forming its boundary. It abuts the popular Joffre Lakes Provincial Park. The area is popular for backcountry skiing and other outdoor recreation, and is the site of a mountain hut that predates the conservancy's establishment.

Mount Marriott is a mountain located in British Columbia, Canada. It is a dry peak near the head of the Cayoosh Creek. Access to the basin below is easily reached by trail, and the summit can be reached by a class 3 scramble route. The best time to climb the mountain is during the months of July–September. There are a few lakes in close proximity to the mountain peak that are swimmable during the months of August and September.

Mount Olds is a 2,542-metre (8,340-foot) mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 17 km (11 mi) northeast of Pemberton, 2 km (1 mi) south-southeast of Mount Gardiner, and 1 km (1 mi) east of Mount Oleg, which is its nearest higher peak. The mountain's name was officially adopted on June 21, 1976, by the Geographical Names Board of Canada. Precipitation runoff from the peak drains into tributaries of the Fraser River.

Mount Shadowfax is a 2,315-metre (7,595-foot) mountain summit in southwest British Columbia, Canada.

Sun God Mountain is a 2,421-metre (7,943-foot) summit located in British Columbia, Canada.

Cirque Peak is a 2,531-metre (8,304-foot) mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 19 km (12 mi) northeast of Pemberton, 4.4 km (3 mi) west-northwest of Cayoosh Mountain, 3.2 km (2 mi) east-southeast of Mount Gardiner, and immediately east of the Place Glacier. The mountain's cirque name, which describes the shape of the peak, was submitted by mountaineer Karl Ricker of the Alpine Club of Canada. The name was officially adopted on January 23, 1979, by the Geographical Names Board of Canada. Precipitation runoff from the peak drains into tributaries of the Fraser River.

Mount Gardiner is a 2,406-metre (7,894-foot) mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 17 km (11 mi) northeast of Pemberton, immediately west of the Place Glacier, and 1.8 km (1 mi) north of Mount Oleg, its nearest higher peak. The mountain was named for William and Henry Gardiner, early settlers who farmed in Pemberton Meadows. The name was officially adopted on June 11, 1979, by the Geographical Names Board of Canada. Precipitation runoff from the peak drains into tributaries of the Fraser River.

Mount Oleg is a prominent 2,587-metre (8,488-foot) mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 16 km (10 mi) northeast of Pemberton, 1.8 km (1 mi) south of Mount Gardiner, and 9.6 km (6 mi) southwest of Mount Marriott, which is its nearest higher peak. Precipitation runoff from the peak drains into tributaries of the Fraser River.

Tolkien Peak is a 2,380-metre (7,810-foot) mountain summit located in the Cadwallader Range in southwestern British Columbia, Canada. It is situated in Birkenhead Lake Provincial Park, 32 km (20 mi) north of Pemberton, and 2.9 km (2 mi) south of Mount Gandalf, which is its nearest higher peak. The peak is named for J. R. R. Tolkien (1892–1973), author of the novels The Hobbit and The Lord of the Rings. The names for nearby Mount Aragorn, Mount Gandalf, and Mount Shadowfax were taken from fictional characters in his books, which were read while waiting out stormy weather during the 1972 first ascents of those mountains. Precipitation runoff from the peak drains into tributaries of the Fraser River.

Face Mountain is a 2,485-metre (8,153-foot) mountain summit located in British Columbia, Canada.

Goat Peak is a 2,473-metre (8,114-foot) summit located in the Pemberton Valley of British Columbia, Canada.

Mount Ronayne is a 2,290-metre (7,513-foot) summit located in the Pemberton Valley of British Columbia, Canada.

Rhododendron Mountain is a 2,523-metre (8,278-foot) glaciated summit in British Columbia, Canada.

The Pemberton Valley is a valley flanking the Lillooet River upstream from Lillooet Lake, including the communities of Mount Currie, Pemberton, British Columbia and the agricultural district surrounding them and flanking the river as far upstream as the Pemberton Meadows area. The term is normally used only to refer to inhabited parts of the valley, not the unsettled areas to the north of Pemberton Meadows although the official definition extends from the head of Lillooet Lake all the way up to the confluence of Meager Creek. Historically the region was part of the Lillooet Country but due to re-orientation of the area's economy and society since the opening and expansion of BC Highway 99 the area is now more considered to be part of the Sea-to-Sky Corridor.

Pemberton Meadows is an unincorporated community on the west shore of the Lillooet River in the Squamish-Lillooet region of southwestern British Columbia. On Pemberton Meadows Road, the locality is by road about 170 kilometres (110 mi) north of Vancouver, 49 kilometres (30 mi) north of Whistler, and 17 kilometres (11 mi) northwest of Pemberton.

Mount Barbour is a 2,290-metre (7,513-foot) summit located in the Pemberton Valley of British Columbia, Canada.

Tenquille Mountain is a 2,391-metre (7,844-foot) summit located in the Pemberton Valley of British Columbia, Canada.

Mount Sampson is a 2,811-metre (9,222-foot) mountain summit located in the Thiassi Range of the Coast Mountains, in the Pemberton Valley of southwestern British Columbia, Canada. It is the highest point in the Thiassi Range. Sampson is situated 41 km (25 mi) northwest of Pemberton, and 21.5 km (13 mi) southeast of Mount Ethelweard, which is its nearest higher peak. Precipitation runoff from the peak drains into tributaries of the Lillooet and Hurley Rivers.

Seven O'clock Mountain is a 2,341-metre (7,680-foot) summit located near the Pemberton Valley of British Columbia, Canada.

Locomotive Mountain is a 2,340-metre (7,680-foot) mountain summit located in the Railroad Group of the Coast Mountains, in the Pemberton Valley of southwestern British Columbia, Canada. It is situated 35 km (22 mi) northwest of Pemberton, 3 km (2 mi) east of Handcar Peak, and 2.1 km (1 mi) south of Face Mountain, which is the nearest higher neighbor. Precipitation runoff from the peak drains into tributaries of the Fraser River. The mountain's name was proposed in 1978 by mountaineer Karl Ricker of the Alpine Club of Canada, in association with Railroad Pass, Railroad Creek, and other railroad-related names of the immediate vicinity. The toponym was officially adopted January 23, 1979, by the Geographical Names Board of Canada.

Handcar Peak is a 2,338-metre (7,671-foot) mountain summit located in the Railroad Group of the Coast Mountains, in the Pemberton Valley of southwestern British Columbia, Canada. It is situated 38 km (24 mi) northwest of Pemberton and 3 km (2 mi) west of Locomotive Mountain. Precipitation runoff from the peak drains into Sampson Creek and Buck Creek which are both tributaries of the Lillooet River. Handcar Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 2,050 meters (6,725 ft) above Lillooet River and Pemberton Valley in approximately 4 km (2.5 mi). The mountain's name was proposed in 1978 by mountaineer Karl Ricker of the Alpine Club of Canada, in association with Railroad Pass, Railroad Creek and other railroad-related names of the immediate vicinity. The toponym was officially adopted January 23, 1979, by the Geographical Names Board of Canada.

The Ryan River is a short but major tributary of the Lillooet River in British Columbia, Canada, running largely eastward approximately 42 kilometres (26 mi) from its source on the eastern flank of the Pemberton Icefield before joining the Lillooet River in the area of Pemberton Meadows.

Chipmunk Mountain is a mountain in southwestern British Columbia, Canada, located 23 km (14 mi) southwest of Bralorne. It has an elevation of 2,390 m (7,840 ft) and a topographic prominence of 540 m (1,770 ft), making it the highest point on an east-trending screed ridge. This horn-like rocky tower is similar to The Black Tusk in Garibaldi Provincial Park.

The Pemberton Volcanic Belt is an eroded Oligocene-Miocene volcanic belt at a low angle near the Mount Meager massif, British Columbia, Canada. The Garibaldi and Pemberton volcanic belts appear to merge into a single belt, although the Pemberton is older than the Garibaldi Volcanic Belt. The Pemberton Volcanic Belt is one of the geological formations comprising the Canadian Cascade Arc. It formed as a result of subduction of the former Farallon Plate.

Boulder Creek, originally Pebble Creek, is a stream in the southern Pacific Ranges of the Coast Mountains in British Columbia, Canada. It flows southwest into the Lillooet River approximately 95 km (59 mi) northwest of the village of Pemberton.

The 1975 Devastation Glacier landslide was a massive rock avalanche that originated from Devastation Glacier on the southern flank of the Mount Meager massif on July 22, 1975. It had a volume of 13,000,000 m³ (460,000,000 cu ft) and buried and killed a group of four geologists at the confluence of Devastation Creek and Meager Creek.

Capricorn Mountain is one of the several volcanic peaks of the Mount Meager massif in southwestern British Columbia, Canada. Its slopes appear to be more gentle than those of the massif's other volcanic peaks. The mountain consists of a boomerang-shaped ridge, with one summit at each end and the main summit in the centre.

Devastator Peak, also known as The Devastator, is the lowest and southernmost of the six subsidiary peaks that form the Mount Meager massif in southwestern British Columbia, Canada. It is located 55 km (34 mi) west of Bralorne.

The 2010 Mount Meager landslide was a large catastrophic debris avalanche that occurred in southwestern British Columbia, Canada, on August 6 at 3:27 a.m. PDT (UTC-7). More than 45,000,000 m³ (1.6×10⁹ cu ft) of debris slid down Mount Meager, temporarily blocking Meager Creek and destroying local bridges, roads and equipment. It was one of the largest landslides in Canadian history and one of over 20 landslides to have occurred from the Mount Meager massif in the last 10,000 years.

Mount Meager (also known as The Cathedral, or Q̓welq̓welústen in the St'at'imcets (Lillooet) language) is a mountain in the Pacific Ranges of the Coast Mountains in British Columbia, Canada. It represents the second highest peak of the Mount Meager massif, a group of coalescent stratovolcanoes in the Garibaldi Volcanic Belt.

Meager Creek is a creek in the southern Pacific Ranges of the Coast Mountains in British Columbia, Canada. It flows northeast into the Lillooet River approximately 95 km (59 mi) northwest of the village of Pemberton and is adjacent to the Upper Lillooet Provincial Park.

Mount Job is one of six named volcanic peaks of the Mount Meager massif in British Columbia, Canada. It is a pile of rubble held together by volcanic ash and sand. The main summit of Mount Job is hard to climb because of difficult access and its horribly loose rock.

The Pemberton Icefield or Pemberton Icecap, is the southernmost of a series of very large icefields studding the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada.

Perkin's Pillar was a vertical pillar of volcanic rock of the Mount Meager massif in southwestern British Columbia, Canada. It existed on the steep north flank of Capricorn Mountain. The upper half of Perkin's Pillar collapsed sometime in June 2005 and only a jagged sliver remains of the previously mighty summit.

Pylon Peak is the southernmost of six named volcanic peaks comprising the Mount Meager massif in British Columbia, Canada. Two pinnacled ridges extend from Pylon and are named respectively the Pylons and the Marionettes. Pylon Peak overlooks the Meager Creek Hot Springs.

The Salal Creek Pluton, also called the Salal Creek stock, is a small circular quartz monzonite intrusion with an area of 35 sq mi (91 km²). It is eight million years old, containing 52 dikes composed of basalt and was probably formed 5 mi (8.0 km) or less below the Earth's surface. It forms part of the Pemberton Volcanic Belt, a geological formation that formed as a result of subduction zone magmatism in the Canadian Cascade Arc.

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.

The Clendinning Range is a subrange of the Pacific Ranges of the Coast Mountains of British Columbia. About 1,500 km² (580 sq mi) in area and lies to the northwest of the better-known Tantalus Range near Squamish. Heavily glaciated and very rugged, with severe weather year-round, it is between the valleys of the Elaho River (east) and the Toba River (west).

Vantage Peak is a 2,235-metre (7,333-foot) mountain summit located in the Coast Mountains of British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 28.5 km (18 mi) east of Pemberton on the boundary of the Nlháxten/Cerise Creek Conservancy. Precipitation runoff from the peak drains southwest into Twin One Creek thence Lillooet Lake; the north slope drains into headwaters of Cerise Creek; and the east slope drains into Caspar Creek thence Cayoosh Creek which is within the Fraser River watershed. Vantage Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,135 meters (3,724 ft) above Twin One Creek in 4 km (2.5 mi). The nearest higher neighbor is Mount Duke, 2.08 km (1 mi) to the southeast.

Arrowhead Mountain is a 2,185-metre (7,169 ft) mountain located east of Lizzie Lake in the Lillooet Ranges of British Columbia, Canada.

Mount Duke is a 2,379-metre (7,805-foot) mountain summit located in the Joffre Group of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated 30 km (19 mi) east of Pemberton, and 10 km (6 mi) southwest of Duffy Lake. The highest peak in the Joffre Group, Mount Matier, rises 4.4 km (3 mi) to the west. The mountain's name was submitted by Reverend Damasus Payne, a Benedictine monk and mountaineer, to honor Archbishop William Mark Duke. It was officially adopted on April 21, 1966, by the Geographical Names Board of Canada. Precipitation runoff from the peak drains into Caspar Creek and Twin One Creek.

The Birkenhead River, formerly known as the Portage River, the Pole River and the Mosquito River, is a major tributary of the Lillooet River, which via Harrison Lake and the Harrison River is one of the major tributaries of the lower Fraser River. It is just over 50 km long from its upper reaches in the unnamed ranges south of Bralorne, British Columbia (these ranges are sometimes called the Noel Ranges or the Birkenhead Ranges); their western area towards the named Bendor Range east of Bralorne is sometimes called the Cadwallader Ranges.

The Green River is a tributary of the Lillooet River in southwestern British Columbia, Canada. Approximately 25 kilometres in length, it begins at the outflow of Green Lake at the north of Whistler, and flows northeast to join the Lillooet River about two kilometres above where the river flows into Lillooet Lake. Its main tributaries are the Soo River and the river-like Rutherford Creek, which is the location of one of only two artificial whitewater kayaking courses in Canada. Just below Rutherford Creek is Nairn Falls.

Pemberton Regional Airport (ICAO: CYPS) is a registered aerodrome located 5 nautical miles (9.3 km; 5.8 mi) south southeast of Pemberton, British Columbia, Canada. Canadians and a few US pilots practiced landing here, to train for Kandahar, Afghanistan.

The Bastion Range is a small mountain range at the northeastern corner of Garibaldi Provincial Park in the Garibaldi Ranges of the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Overlooking Lillooet Lake, it has an area of 50 km².

The Lilʼwat First Nation (Lillooet: líl̓watǝmx), a.k.a. the Lilʼwat Nation or the Mount Currie Indian Band, is a First Nation band government located in the southern Coast Mountains region of the Interior of the Canadian province of British Columbia. It is a member of the Lillooet Tribal Council, which is the largest grouping of band governments of the Stʼatʼimc or Stlʼatlʼimx people (a.k.a. the Lillooet people). Other Stʼatʼimc governments include the smaller In-SHUCK-ch Nation on the lower Lillooet River to the southwest, and the independent N'quatqua First Nation at the near end of Anderson Lake from Mount Currie, which is the main reserve of the Lilʼwat First Nation, and also one of the largest Indian reserves by population in Canada.

The Pemberton Festival was a three-day summer music festival inaugurated in 2008. It was held in Pemberton, British Columbia, a village just north of popular ski resort Whistler. Produced by Live Nation Canada, the festival featured primarily rock and indie rock musicians, with a small proportion of hip hop. Musicians played on one of two stages, picturesquely situated at the foot of Mount Currie and the surrounding mountain range. The site, a 400-acre (1.6 km²) hayfield, was discovered by concert-promoter, Shane Bourbonnais, of Live Nation, just down the street from his home. He emphasized event sustainability and environmentalism as priorities in running the festival.

Mount Currie (Lillooet: Ts̓zil [tsʼzel]) is the northernmost summit of the Garibaldi Ranges in southwestern British Columbia, Canada. Its north face dominates the "skyline" of the Pemberton Valley and is one of the peaks visible from the Whistler-Blackcomb Ski Area just southwest. Mount Currie is the namesake of Mount Currie, British Columbia and the adjoining Mount Currie Indian Reserve, home of the Lil'wat First Nation.

Mount Howard is a 2,551-metre (8,369-foot) mountain summit located in the Coast Mountains of British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. Mount Howard is situated 27 km (17 mi) east of Pemberton and immediately southeast of Mount Matier. Precipitation runoff from the peak drains into Twin One Creek thence Lillooet Lake which is within the Lillooet River watershed. Mount Howard is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,650 meters (5,413 ft) above Twin One Creek in 4 km (2.5 mi).

Duffey Peak is a 2,219-metre (7,280-foot) mountain summit located in southwest British Columbia, Canada.

Slalok Mountain, originally known as Rex's Pillar, is a 2,653-metre (8,704-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the third-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 24 km (15 mi) east of Pemberton, and 8 km (5 mi) northeast of Lillooet Lake. It is 4 km (2 mi) northeast of Duffey Peak and the nearest higher peak is Mount Matier, 1.9 km (1 mi) to the east. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The first ascent of the mountain was made in 1963 by C. Adam, T. Anderson, and G. Richardson. The mountain's name Slalok is the traditional name for the settlement of nearby Mount Currie. The name was officially adopted on June 11, 1979, by the Geographical Names Board of Canada. The mountain and its climate supports the Matier Glacier, Stonecrop Glacier, and Tszil Glacier on the northern slopes.

Mount Taylor is a 2,318-metre (7,605-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 21 km (13 mi) east of Pemberton, and 7 km (4 mi) northeast of Lillooet Lake. Its nearest higher peak is Slalok Mountain, 1.9 km (1 mi) to the east. Precipitation runoff from the peak drains into Joffre Creek, a tributary of the Lillooet River. The mountain's name was submitted by Karl Ricker of the Alpine Club of Canada to honor Ada C. Taylor, a Pemberton pioneer and the first nurse in that community. The toponym was officially adopted January 23, 1979, by the Geographical Names Board of Canada.

Parkhurst Mountain is a 2,494-metre (8,182-foot) mountain summit located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated 11 km (7 mi) east-northeast of Whistler, south of Wedgemount Lake, and on the west side of Wedgemount Glacier. Parkhurst's nearest neighbor is Rethel Mountain, 0.89 km (1 mi) to the northwest, and its nearest higher peak (and also the highest peak in Garibaldi Park) is Wedge Mountain, 1.8 km (1 mi) to the southeast. Mount Weart, the second-highest peak in the park, rises 2.6 km (2 mi) northeast of Parkhurst. Precipitation runoff from the peak drains into Wedge Creek, Wedgemount Creek, and Rethel Creek, which are all tributaries of the Green River, which in turn is a tributary of the Lillooet River. The present day ghost town of Parkhurst was an old logging town in the 1920s and 1930s set on the edge of Green Lake, 9 km (6 mi) west of Parkhurst Mountain. The site was named for Mr. and Mrs. Parkhurst who preempted the land on Green Lake in 1902 and built a small house where they lived with their family. The mountain's name was officially adopted on June 25, 1975, by the Geographical Names Board of Canada.

Twin Goat Mountain is a 2,128-metre (6,982-foot) summit in British Columbia, Canada.

Mount Cook is a 2,676-metre (8,780-foot) mountain located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated above the north shore of Wedgemount Lake, 13 km (8 mi) northeast of Whistler, and its nearest higher peak is Mount Weart, 1.2 km (1 mi) to the southeast. The Armchair Glacier is set between Cook and Weart, and the Weart Glacier rests on the northern slope of Cook. Precipitation runoff from the peak and meltwater from the glaciers drains into Wedgemount Lake and Green River.

Mount Hartzell is a 2,615-metre (8,579-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 25 km (16 mi) east of Pemberton, midway between Mount Matier and Mount Spetch, each a half kilometre either side of Hartzell. The mountain's name was submitted by Karl Ricker of the Alpine Club of Canada to honor Carl A. Hartzell, an early settler and postmaster at Pemberton. The name was officially adopted on January 23, 1979, by the Geographical Names Board of Canada. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The mountain and its climate supports the Hartzell Glacier on the southeast slope, and the Matier Glacier on the northern slope.

Joffre Peak is a 2,721-metre (8,927-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 26 km (16 mi) east of Pemberton and 11 km (7 mi) northeast of Lillooet Lake. Joffre is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,500 meters (4,920 ft) above Cayoosh Creek in 4 km (2.5 mi). The nearest higher peak is Mount Matier, 1.6 km (1 mi) to the south. The mountain's climate supports the Matier Glacier on the southwest slope, and the Anniversary Glacier on the southeast slope. Precipitation runoff from the peak drains into Joffre Creek and Cayoosh Creek which are both within the Fraser River watershed.

Mount Matier is a prominent 2,783-metre (9,131-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the highest point of the Joffre Group, which is a subset range of the Coast Mountains. It is situated 26 km (16 mi) east of Pemberton, and 9 km (6 mi) northeast of Lillooet Lake. Its nearest higher peak is Mount Weart, 30 km (19 mi) to the southwest. The slopes of the mountain are covered by the Matier Glacier on the northwest, Anniversary Glacier on the northeast, Twin One Glacier on the southeast, and Hartzell Glacier to the south. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River.

Mount Moe is a 2,664-metre (8,740-foot) glaciated summit in British Columbia, Canada.

Mount Neal is a 2,552-metre (8,373-foot) glaciated summit in British Columbia, Canada.

Mount Spetch is a 2,579-metre (8,461-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 25 km (16 mi) east of Pemberton, midway between Mount Matier and Slalok Mountain, both one kilometre either side of Spetch. The mountain's name was submitted by Karl Ricker of the Alpine Club of Canada to honor Samuel W. Spetch, who operated the general store at Birken, and other businesses in Pemberton. The name was officially adopted on January 23, 1979, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1971 by J. Oswald and G. Walter. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The mountain and its climate supports the Matier Glacier on the northern slope.

Mount Weart is a 2,835-metre (9,301-foot) triple-summit mountain located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated 14 km (9 mi) northeast of Whistler, and its nearest higher peak is Wedge Mountain, 3.7 km (2 mi) to the south, which is the only peak within the park higher than Weart. The Armchair Glacier rests below the west aspect of the summit, and the massive Weart Glacier spans the northern and eastern aspects of the mountain. Precipitation runoff from the peak and meltwater from the glaciers drains into Wedgemount Lake and tributaries of the Lillooet River.

Alpine skiing at the 2010 Winter Olympics was held in Canada at Whistler Creekside in Whistler, British Columbia, north of Vancouver. The ten events were scheduled for 13–27 February; weather delayed the first event, the men's downhill, two days until Monday, 15 February.

The biathlon competition at the 2010 Winter Olympics were held at Whistler Olympic Park in Whistler, British Columbia. The events were held between the 13th and 26 February 2010.

The nordic combined competition of the 2010 Winter Olympics was held at Whistler Olympic Park. The events were held between 14 and 25 February 2010. Sprint and individual Gundersen events of 7.5 km and 15 km events were replaced by two 10 km individual events with one jump each from the normal and large hills respectively. Team event went from two jumps down for one jump per team member. This was done during the 2008–09 Nordic Combined World Cup season and was also applied to the FIS Nordic World Ski Championships 2009 in Liberec, Czech Republic.

The women's 7.5 kilometre + 7.5 kilometre double pursuit cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada was held on 19 February at Whistler Olympic Park in Whistler, British Columbia at 13:00 PST.

The men's pursuit competition in biathlon at the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on February 16, 2010. It was won by Swedish athlete Björn Ferry, after both Ferry and second place finisher Christoph Sumann of Austria successfully pursued and overtook the leader at the start of the race, France's Vincent Jay.

The luge competition events of the 2010 Winter Olympics were held between 13 and 17 February 2010 at the Whistler Sliding Centre in Whistler, British Columbia, Canada.

Phalanx Mountain is a 2,441-metre (8,009-foot) summit located in Garibaldi Provincial Park of southwest British Columbia, Canada.

Mount Trorey is a 2,461-metre (8,074-foot) mountain summit located in British Columbia, Canada.

Decker Mountain is a 2,421-metre (7,943-foot) flat-topped peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is part of the Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 9 km (6 mi) southeast of Whistler, and 3.9 km (2 mi) west-northwest of Tremor Mountain, which is the highest point in the Spearhead Range. Precipitation runoff from the south side of the peak drains into Fitzsimmons Creek which is a tributary of the Cheakamus River, and meltwater from the Decker Glacier on the northeastern slope drains to Wedge Creek.

Sisqa Peak is a 2,357-metre (7,733-foot) mountain in British Columbia, Canada.

The women's 10 kilometre freestyle cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada was held on February 15 at Whistler Olympic Park in Whistler, British Columbia at 10:00 PST.

The men's sprint competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on February 14, 2010.

The men's mass start competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on February 21, 2010.

The men's individual large hill/10 km Nordic combined competition for the 2010 Winter Olympics in Vancouver, Canada was held at Whistler Olympic Park in Whistler, British Columbia on 25 February.

The men's team large hill/4 × 5 km Nordic combined competition for the 2010 Winter Olympics in Vancouver, Canada was held at Whistler Olympic Park in Whistler, British Columbia on 23 February. The Austrian team of Michael Gruber, Christoph Bieler, Felix Gottwald, and Mario Stecher were the defending Olympic champions. Gruber retired after the 2007-08 season. Gottwald originally retired after the 2006-07 World Cup season, but came out of retirement in May 2009 to compete for the 2009-10 World Cup season including the 2010 Games. The defending world champions were the Japanese team of Yūsuke Minato, Taihei Kato, Akito Watabe, and Norihito Kobayashi. The last World Cup event prior to the 2010 Games in this format took place on 12 December 2009 in Harrachov, Czech Republic, but that event was cancelled on 4 December 2009 to warm weather and lack of snow. A team normal hill event took place prior to the 2010 Winter Games in Schonach, Germany on 24 January 2010 and was won by the German team of Georg Hettich, Eric Frenzel, Björn Kircheisen, and Tino Edelmann.

The men's super-G competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia, on Friday, February 19.

The men's individual normal hill/10 km Nordic combined competition for the 2010 Winter Olympics in Vancouver, Canada, was held at Whistler Olympic Park in Whistler, British Columbia, on 14 February.

The bobsleigh competition of the Vancouver 2010 Olympics was held at the Whistler Sliding Centre between 20 and 27 February 2010.

The Women's 7.5 kilometre sprint biathlon competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on 13 February 2010. This competition started at 1:00 PM PST.

The men's 15 kilometre freestyle cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada, was held on 15 February at Whistler Olympic Park in Whistler, British Columbia, at 12:30 PST.

The women's slalom competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia on February 26, 2010.

The cross-country skiing competition of the 2010 Winter Olympics in Vancouver were held at Whistler Olympic Park. The events were held between 15 and 28 February 2010.

Whistler Olympic Park Ski Jumps är tre hoppbackar i Callaghan Valley i närheten av staden Whistler i British Columbia i Kanada. Stora backen (K125 HS140) och normalbacken (K95 HS106) användes under olympiska vinterspelen 2010.

The women's team sprint cross-country skiing competition in the freestyle technique at the 2010 Winter Olympics in Vancouver, Canada was held on 22 February at Whistler Olympic Park in Whistler, British Columbia.

The doubles luge event at the 2010 Winter Olympics was held on 17 February at the Whistler Sliding Centre in Whistler, British Columbia. Twenty teams participated. Austrian brothers Andreas and Wolfgang Linger, the defending Olympic and European champions, won the gold medal. The silver medal was also won by a pair of brothers, Andris and Juris Šics of Latvia. Germans Patric Leitner and Alexander Resch clinched the bronze medal after edging out Italians Christian Oberstolz and Patrick Gruber, who were in third place after the first run.

The men's giant slalom competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia. Originally scheduled for February 21, it was rescheduled to February 23, due to delays of preceding alpine events.

The four-man bobsleigh competition at the 2010 Winter Olympics in Vancouver, British Columbia, Canada, was held at the Whistler Sliding Centre in Whistler, British Columbia, on 26–27 February. The German team of André Lange, René Hoppe, Kevin Kuske, and Martin Putze were the defending Olympic champion in this event. America's team of Steve Holcomb, Justin Olsen, Steve Mesler, and Curtis Tomasevicz were the defending world champions in this event. The test event was won by the Latvian team of Jānis Miņins, Daumants Dreiškens, Oskars Melbardis, and Intars Dambis. The last World Cup event prior to the 2010 Games place took place in Igls, Austria (southeast of Innsbruck) on 24 January 2010 and was won by the German team of Lange, Hoppe, Kuske, and Putze. Holcomb of the United States won both the four-man and the combined World Cups.

The men's 4 × 10 kilometre relay cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada, was held on 24 February at Whistler Olympic Park at 11:15 PST.

The Whistler Olympic Park is the location of the Nordic and Biathlon 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 Women's 4 × 6 kilometre relay biathlon competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on 23 February 2010. The race consisted of four laps of cross-country skiing, each lap a total of 6 km. Every 2 km there would be a shooting zone, the first one is prone and the second one is standing. Any misses in the shooting zones count as penalties which must be completed by going around a penalty loop right after the second shooting zone. There were four racers per team, each completing one lap. As all the teams started together, the team that crossed the finish line first would win.

The Men's Downhill competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia. The competition was scheduled for Saturday, February 13, but was postponed due to rain and warm temperatures; it was held on Monday, February 15.

The women's super combined competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia, on February 18, 2010. The competition was originally scheduled to be held on February 14, 2010, but was postponed due to bad weather, which delayed previous events.

The women's downhill competition of the Vancouver 2010 Olympics was held at Whistler Creekside on Wednesday, February 17.

The women's 10 kilometre pursuit biathlon competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on 16 February 2010.

The Men's sprint cross-country skiing competition in the classical technique at the 2010 Winter Olympics in Vancouver, Canada was held on 17 February at Whistler Olympic Park in Whistler, British Columbia.

The men's luge at the 2010 Winter Olympics took place on 13–14 February 2010 at the Whistler Sliding Centre in Whistler, British Columbia. Germany's Felix Loch was the two-time defending world champion and won the gold medal with the fastest time in each of the four runs. The test event that took place at the venue was won by Germany's David Möller, who would win the silver medal in this event. Italy's Armin Zöggeler was the two-time defending Olympic champion and won a bronze medal in this event. The last World Cup event prior to the 2010 games took place in Cesana, Italy on 30 January 2010 and was won by Zöggeler, who also won the overall World Cup title.

The Women's sprint cross-country skiing competition in the classical technique at the 2010 Winter Olympics in Vancouver, Canada was held on 17 February at Whistler Olympic Park in Whistler, British Columbia.

The women's super-G competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia, on Saturday, February 20.

The men's 15 kilometre + 15 kilometre double Pursuit cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada, was held on 20 February at Whistler Olympic Park in Whistler, British Columbia, at 13:30 PST.

Blackcomb Peak (Ucwalmícwts: Tsíqten) is a mountain located east of Whistler, British Columbia that forms the boundary between the Whistler Blackcomb ski resort and Garibaldi Provincial Park. Like Whistler Mountain, it is located on the edge of Garibaldi Provincial Park and the ski lifts are often used to access the park, particularly for the Spearhead Traverse.

The women's 4 × 5 kilometre relay cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada was held on 25 February at Whistler Olympic Park at 11:15 PST.

The women's luge at the 2010 Winter Olympics in Vancouver, Canada took place on 15–16 February at the Whistler Sliding Centre in Whistler, British Columbia. Germany's Sylke Otto was the two-time defending Olympic champion. Otto retired midway through the 2006-07 season in January 2007 to pregnancy and after suffering a crash at the track in Königssee, Germany. Erin Hamlin of the United States was the defending world champion. The test event that took place at the venue was won by Germany's Natalie Geisenberger. The last World Cup event prior to the 2010 games took place in Cesana, Italy on 31 January 2010 and was won by Geisenberger. Geisenberger's teammate Tatjana Hüfner, the defending Olympic bronze medalist, won the overall World Cup for 2009-10 season in women's singles.

The women's giant slalom competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia, on February 24. Following the first run, the event was postponed due to heavy fog in the afternoon; the second run was held the next morning, February 25.

The men's individual competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on February 18, 2010. Two silver medals were awarded for a second-place tie. No bronze medal was awarded.

The men's slalom competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia, on February 27, 2010.

The Women's 12.5 kilometre mass start biathlon competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on 21 February 2010.

The men's super combined competition of the Vancouver 2010 Olympics was held at Whistler Creekside in Whistler, British Columbia. The competition was scheduled for February 16, but was postponed due to weather delays in preceding races; it was held five days later on February 21. American athlete Bode Miller won his only Olympic gold medal, Ivica Kostelić of Croatia won silver, and Silvan Zurbriggen of Switzerland took the bronze.

The men's 50 kilometre classical cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada was held on 28 February at Whistler Olympic Park in Whistler, British Columbia at 09:30 PST. on the final day of the Games.

The men's team sprint cross-country skiing competition in the freestyle technique at the 2010 Winter Olympics in Vancouver, Canada was held on 22 February at Whistler Olympic Park in Whistler, British Columbia.

The women's 30 kilometre classical cross-country skiing competition at the 2010 Winter Olympics in Vancouver, Canada was held on 27 February at Whistler Olympic Park in Whistler, British Columbia at 11:45 PST.

The Women's 15 kilometre individual biathlon competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on 18 February 2010.

The men's relay competition of the Vancouver 2010 Olympics was held at Whistler Olympic Park in Whistler, British Columbia on February 26, 2010. The race consisted of four laps of cross-country skiing, each lap a total of 7.5 km. Every 2.5 km there would be a shooting zone, the first one is prone and the second one is standing. Any misses in the shooting zones count as penalties which must be completed by going around a penalty loop right after the second shooting zone. There were four racers per team, each completing one lap. As all the teams started together, the team that crossed the finish line first would win.

The two-woman bobsleigh competition at the 2010 Winter Olympics in Vancouver, British Columbia, Canada, was held at the Whistler Sliding Centre in Whistler, British Columbia, on 20–21 February.

The two-man bobsleigh competition at the 2010 Winter Olympics in Vancouver, British Columbia, Canada, was held at the Whistler Sliding Centre in Whistler, British Columbia on 20–21 February. The German team of André Lange and Kevin Kuske were the defending Olympic champions in this event. Switzerland's team of Ivo Rüegg and Cedric Grand were the defending world champions in this event. The test event held at the Olympic venue was won by the German duo of Thomas Florschütz and Marc Kühne. The last World Cup event prior to the 2010 Games took place in Igls, Austria (southeast of Innsbruck) on 23 January 2010 and was won by the Swiss duo of Beat Hefti and Thomas Lamparter while Rüegg won the overall World Cup in the two-man event.

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 Peak 2 Peak Gondola is a tricable gondola lift at Whistler Blackcomb Resort in Whistler, British Columbia, linking Whistler Mountain's Roundhouse Lodge with Blackcomb Mountain's Rendezvous Lodge. It is the first lift to join the two side-by-side mountains. It held the world record for the longest free span between ropeway towers at 3.03 kilometres (1.88 mi) until 2017 when the Eibsee Cable Car exceeded it by 189 metres (620 ft). It is still the highest point above the ground in a gondola at 436 metres (1,430 feet), although a temporary aerial tramway in Switzerland used between 1979 and 1986 had larger span. The gondola was built by the Doppelmayr Garaventa Group in 2007 and 2008 at a cost of CDN$51 million. The Gondola is the first Doppelmayr "3S" tri-cable lift in North America; there are four similar but smaller lifts in Europe which were built in 1991, 1994, 2002, 2004 and 2010 in Switzerland, Austria, France and Germany. Whistler Blackcomb promotes the gondola as an attraction and uses it to transport skiers in the winter months, as well as sightseers year-round.

CKEE-FM is a Canadian radio station broadcasting at 101.5 FM in Whistler, British Columbia, British Columbia with a Top 40/CHR format branded on-air as 101.5 Whistler FM.

CFPV-FM was a Canadian radio station. Owned by McBride Communications, the station broadcasts at 98.9 FM in Pemberton, British Columbia.

Fitzsimmons Creek is a large creek in Whistler, British Columbia, Canada, having its origins at the Fitzsimmons Glacier in the Garibaldi Ranges of the Coast Mountains. For half its length of approximately 10 kilometres, the creek courses a U-shaped glacial valley which separates two ski mountains of the Whistler Blackcomb resort, Blackcomb to the north and Whistler to the south.

Rethel Mountain is a 2,408-metre (7,900-foot) mountain summit located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated 11 km (7 mi) northeast of Whistler, on the south side of Wedgemount Lake and west side of Wedgemount Glacier. Its nearest higher peak is Parkhurst Mountain, 1.3 km (1 mi) to the southeast. Rethel is set 3.2 km (2 mi) northwest of Wedge Mountain, the highest peak in Garibaldi Park, and 2.9 km (2 mi) southwest of Mount Weart, the second-highest in the park.  Precipitation runoff from the peak drains into Wedgemount Creek and Rethel Creek, both tributaries of the Green River, which in turn is a tributary of the Lillooet River. It was named in association from Rethel station (since closed) on the Pacific Great Eastern Railway route. The mountain's name was officially adopted on February 27, 1978, by the Geographical Names Board of Canada.

Ipsoot Mountain is a 2,576-metre (8,451-foot) glaciated summit located in southwest British Columbia, Canada.

Rainbow Mountain is a broad glaciated mountain forming the northeastern wall of the Callaghan Valley in the Pacific Ranges of British Columbia, Canada. Located in the middle of the Sea to Sky Country, the mountain is just 9 km (5.6 mi) northwest of the resort town of Whistler, and is a popular destination for hiking, snowshoeing and ski touring.

Rutherford Creek is a tributary of the Green River, British Columbia, Canada, entering that river a few miles above Nairn Falls Provincial Park, near the village of Pemberton. The creek's headwaters are on the eastern side of the Pemberton Icefield, from where it flows southeast for the first half of its course, then generally east for the remainder. It is approximately 24 km (15 mi) in length. The mouth is at 50° 16' 3" N, 122° 57' 41" W.

The Soo River is a tributary of the Green River in the Pacific Ranges of the Coast Mountains in British Columbia, Canada, joining that river just north of the Resort Municipality of Whistler. Approximately 35 kilometres (22 mi) long, it begins on the south flank of the Pemberton Icefield. Its course is generally eastward from there to the Green River valley, although upon reaching that valley it runs north for about 3.5 kilometres (2.2 mi) roughly parallel to the Green before joining it. For much of its course, known as the Soo Valley, it forms a serpentine marshland until reaching a short canyon before entering the valley of the Green River.

The Spearhead Range is a short subrange of the Garibaldi Ranges of southwestern British Columbia, Canada, adjacent to the resort town of Whistler, British Columbia and ending at its northwestern apex in Blackcomb Mountain, one of two mountains forming the Whistler Blackcomb ski resort. Other notable summits are Tremor Mountain (highest point of the range), The Spearhead, Mount Macbeth, Decker Mountain, Mount Trorey, Phalanx Mountain and Shatter, Shudder, Quiver and other similarly named peaks and glaciers. The range was named by Don and Phyllis Munday as the range's peaks resembled spearheads rising from the alpine fog. To the north of the range is Lone Goat Pass, formed by Wedge Creek and Lone Goat Creek, which is fed by the Spearhead Glacier, the largest glacier in the range. The valley of Fitzsimmons Creek is on the range's south side, and is the location of the Whistler Sliding Centre, which was built for the 2010 Winter Olympics.

The Spearhead is a 2,457 m (8,061 ft) peak in the Garibaldi Ranges of British Columbia, Canada, and is one of the main summits of the Blackcomb Mountain portion of the Whistler Blackcomb ski resort, located at the apex of the Blackcomb and Spearhead Glaciers, which is named for it. It also is the namesake of the Spearhead Range, which is the short range flanking the north side of Fitzsimmons Creek and ending on its northwest end at Blackcomb Mountain. The mountain's name was officially adopted on August 27, 1965, by the Geographical Names Board of Canada.

Whistler Transit Ltd., a division of Pacific Western Transportation, operates the public transit service in Whistler and the Pemberton Valley area of British Columbia, Canada. Buses operate every day between 5:30 a.m. and 3 a.m. and are equipped with racks for skis or bikes, depending on the season.

Ashlu Mountain is a 2,561-metre (8,402-foot) pyramidic mountain summit located in the Pacific Ranges in the Coast Mountains of southwestern British Columbia, Canada known for its glaciation and climbing routes. It is situated 50 km (31 mi) northwest of Squamish, in the Elaho-Jervis Divide, where it is the tallest peak in that subrange. Its nearest higher peaks are Mount Tantalus in the Tantalus Range, 33 km (20 mi) to the southeast, and its line parent, Mount Tinniswood, 33.5 km (21 mi) to the northwest at the head of Princess Louisa Inlet.

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 Mount Cayley volcanic field (MCVF) is a remote volcanic zone on the South Coast of British Columbia, Canada, stretching 31 kilometres (19 miles) 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.

Brandywine Mountain, 2,213 m or 7,260 ft, is a summit in the Powder Mountain Icefield of the Pacific Ranges of the Coast Mountains of southwestern British Columbia, Canada, about 25 km (16 mi) west of the resort town of Whistler.

Clendinning Creek is a river in British Columbia. It is the largest tributary of the Elaho River. It is located entirely within Clendinning Provincial Park.

The Powder Mountain Icefield, also called the Powder Mountain Icecap and the Cayley Icefield, is a glacial field in the Pacific Ranges of southwestern British Columbia, Canada, about 20 kilometres (12 mi) west of Whistler and about 90 kilometres (56 mi) north of Vancouver. On the west side of the icefield is the valley of the Squamish River, while on its east is the Callaghan Valley, which is the setting for the Nordic facilities for the 2010 Winter Olympics.

Pyroclastic Peak is the second highest of the five named volcanic peaks immediately south of Mount Cayley in British Columbia, Canada. It is steep and rotten and is located 12 km (7 mi) southwest of Callaghan Lake and 24 km (15 mi) west of Whistler. It is part of the Pacific Ring of Fire that includes over 160 active volcanoes.

The Vulcan's Thumb is a rock pinnacle in the Pacific Ranges of southwestern British Columbia, Canada. It is the largest of a number of slender pinnacles protruding from the sharp summit ridge of Pyroclastic Peak, which forms part of the Mount Cayley massif.

Mount Callaghan is a mountain east of the headwaters of the Squamish River, just northeast of the Powder Mountain Icefield and just south of the Pemberton Icefield in the Sea to Sky Country of southwestern British Columbia, Canada, about 20 km directly west of the Resort Municipality of Whistler. A crack was observed across Callaghan's summit in the spring of 1999. In 2000, a section of the summit collapsed. Callaghan Lake lies below the south face of the mountain.

Pali Dome is a subglacial volcano in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is part of the Mount Cayley volcanic field and its elevation is 2,250 m (7,380 ft). For the past 2 million years, the Mount Cayley volcanic field has had interactions between ice and lava which have created some unique landforms and an in-ice drainage system."Pali" comes from the Hawaiian word that means cliff or steep hill, while dome refers to the lava dome, which is when doughy lava flows from a volcanic vent which is usually rounded and flat on top.

Mount Fee is a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located 13 km (8.1 mi) south of Callaghan Lake and 21 km (13 mi) west of the resort town of Whistler. With a summit elevation of 2,162 m (7,093 ft) and a topographic prominence of 312 m (1,024 ft), it rises above the surrounding rugged landscape on an alpine mountain ridge. This mountain ridge represents the base of a north-south trending volcanic field which Mount Fee occupies.

Ring Mountain, also known as Crucible Dome, is a tuya in the Mount Cayley volcanic field, British Columbia, Canada. It features a horseshoe shaped crater on the east side of the upper Squamish River. Outcrops on Ring Mountain's western side contain highly variable, fine-scale jointing and are locally broken down into many small spires and knobs. The age of Ring Mountain is unknown, but it likely formed during the Fraser Glaciation, as did most tuyas in Canada.

Shovelnose Creek is a creek in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It flows southwest into the Squamish River and south of the Elaho River.

The Squamish volcanic field is a small north–south trending volcanic field on the South Coast of British Columbia, Canada. It extends for only about 3 km (1.9 mi) from the eastern side of Howe Sound northeast of Britannia Beach to the heavily forested slope on the western side of the Squamish River mouth. It forms the southernmost end of the Garibaldi Volcanic Belt, which comprises part of the Canadian Cascade Arc. Its volcanoes are relatively minor to the more voluminous stratovolcanoes found throughout the Garibaldi Belt and are composed of dacite and lesser basaltic andesite. The field gets its name from the nearby community of Squamish at the north end of Howe Sound on the Sea to Sky Highway.

Slag Hill is a subglacial volcano associated with the Mount Cayley volcanic field in British Columbia, Canada. It consists of glassy, augite-phyric basaltic andesite in steep-sided, glassy, finely jointed domes and one small, flat-topped bluff. The finely jointed domes are similar to those of Ember Ridge. There are quench features at Slag Hill, which is suggesting that the volcanic activity was subglacial. Slag Hill was formed throughout the Pleistocene period, but its most recent volcanic activity produced a lava flow on its western lobe that shows no evidence of ice-contact volcanism. This indicates the lava flow was erupted less than 10,000 years ago after the last glacial period.

Turbid Creek is a stream in southwestern British Columbia, Canada, flowing southwest into the Squamish River.

Powder Mountain, 2,347 m (7,700 ft), is a volcanic summit in the Powder Mountain Icefield in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada.

Mount Tinniswood is a 2,606-metre (8,550-foot) mountain summit located in British Columbia, Canada.

Forger Peak is a 2,423-metre (7,949-foot) mountain summit in British Columbia, Canada.

Mount Fitzsimmons is a 2,603-metre (8,540-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the third-highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Mount Benvolio, 0.5 km (0 mi) to the west-southwest. The Diavolo Glacier spreads out below the southeast aspect of the summit, and the Fitzsimmons Glacier descends the northwest slopes. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River. The first ascent of the mountain was made on August 19, 1924, by a party of the British Columbia Mountaineering Club. The peak was named for prospector James Fitzsimmons, who built a trail along Fitzsimmons Creek in an effort to haul supplies to a small copper mine he staked and worked. The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

Mount Macbeth is a 2,639-metre (8,658-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is part of the Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 14 km (9 mi) southeast of Whistler, and 2 km (1 mi) south of Tremor Mountain, which is the highest point in the Spearhead Range. The Naden Glacier spreads out below the eastern aspect of the summit, the Macbeth Glacier lies below the south aspect, and the Curtain Glacier descends the northern slope. Precipitation runoff from the peak and meltwater from its glaciers drains into Fitzsimmons Creek which is a tributary of the Cheakamus River. Macbeth is most often climbed as part of the Spearhead Traverse. The first ascent of the mountain was made in 1969 by P. Starr, E. Bass, B. Ellis, and P. Macec via the northeast ridge. The peak was named in 1964 by an Alpine Club of Canada climbing party, to commemorate the 400th anniversary of William Shakespeare's birth. The mountain's name was officially adopted on August 27, 1965, by the Geographical Names Board of Canada.

Carcajou Peak is a 2,239-metre (7,346-foot) mountain summit in British Columbia, Canada.

Outlier Peak is a 2,422-metre (7,946-foot) mountain summit in British Columbia, Canada.

Cheakamus Mountain is a 2,588-metre (8,491-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the fourth-highest peak of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 16 km (10 mi) southeast of Whistler, and its nearest higher peak is Mount Benvolio, 1.65 km (1 mi) to the northwest. The Diavolo Glacier spreads out below the north aspect of the peak, and precipitation runoff from the peak with meltwater from the glacier drains into tributaries of the Cheakamus River. The peak was named in association with the river, which in turn is anglicized from Tseearkamisht, a Squamish word meaning "people who use the cedar rope fishing net". The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1950 by Roy Hooley, Jimmy Kilborn, and Ian Kirk.

The Lecture Cutters are 2,524-metre (8,281-foot) mountain peaks in British Columbia, Canada.

Tremor Mountain is a prominent 2,691-metre (8,829-foot) summit located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the highest point of the Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 13 km (8 mi) southeast of Whistler, and 8.7 km (5 mi) south of Wedge Mountain, its nearest higher peak. Precipitation runoff from the south side of the peak as well as meltwater from the Platform Glacier drains into Fitzsimmons Creek which is a tributary of the Green River. Meltwater from the Tremor Glacier on the northwestern slope drains to Wedge Creek, and meltwater from the Shudder Glacier on the northeast slope drains into Billygoat Creek, a tributary of the Lillooet River. Tremor Mountain is often climbed as part of the Spearhead Traverse. The first ascent of the mountain was made in 1928 by A.J. Campbell Garibaldi survey party. The mountain's name origin refers to unexplained earth tremors when the first ascent party was on the summit. The mountain's toponym was officially adopted on September 6, 1951, by the Geographical Names Board of Canada.

Mount Sir Richard is a 2,681-metre (8,796-foot) glaciated summit in British Columbia, Canada.

The Table, sometimes called Table Mountain, is a 2,021-metre (6,631 ft) high flow-dominated andesite tuya located 4 kilometres (2 mi) south of Garibaldi Lake, 15 kilometres (9 mi) northeast of Cheekye and 5 kilometres (3 mi) north of Mount Garibaldi, British Columbia, Canada. It rises over 530 metres (1,740 ft) above the surface of Garibaldi Lake, which lies less than 1 kilometre (1 mi) to the north.

The Cheakamus River (pron. CHEEK-a-mus) is a tributary of the Squamish River, beginning at the terminus of McBride Glacier on Mount Sir Richard in Garibaldi Provincial Park upstream from Cheakamus Lake on the southeastern outskirts of the resort area of Whistler. The river flows into Cheakamus Lake before exiting it and flowing northwest until it turns south and enters Daisy Lake. Between the outlet of Daisy Lake and its mouth, much of its length is spent going through Cheakamus Canyon, where the river flows through swift rapids and even one good sized waterfall. The river flows south from the lake and through the canyon before joining the Squamish River at Cheekye, a few miles north of the town of Squamish. The river's name is an anglicization of the name of Chiyakmesh ("people of the fish weir"), a village of the Squamish people and a reserve of the Squamish Nation.

The Cheekye River is a river in southwestern British Columbia, Canada. It flows west into the Cheakamus River and north of Squamish.

Squamish Airport (IATA: YSE, ICAO: CYSE) is located 5.4 nautical miles (10.0 km; 6.2 mi) north of Squamish, British Columbia, Canada.

Atwell Peak is a dramatic pyramid-shaped volcanic peak located at the southern edge of Mount Garibaldi, British Columbia, Canada. Atwell Peak was the source of many pyroclastic flows during Garibaldi's development. Frequent landslides on its west face drops steeply into the Cheekye River. Atwell Peak is often mistakenly called Mount Garibaldi when viewed from Squamish, since the main peak is hidden. The peak is usually climbed during winter or early spring when the rock is frozen because it is very loose and rotten. Atwell Peak contains three ridges, the north, east, and south. The two most visible routes are the north and south ridges.

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.

Castle Towers Mountain is a triple summit mountain on the east side of Garibaldi Lake in southwestern British Columbia, Canada. The first ascent party from the BC Mountaineering Club named the mountain after its appearance in August 1911.

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.

Clinker Peak är en bergstopp i Kanada. Den ligger i provinsen British Columbia, i den sydvästra delen av landet, 3 500 km väster om huvudstaden Ottawa. Toppen på Clinker Peak är 1 992 meter över havet. Clinker Peak ligger vid sjön Garibaldi Lake.

Clinker Ridge is a mountain ridge in southwestern British Columbia, Canada, located between Garibaldi Lake and the Cheakamus River. Named for Clinker Peak on the western flank of Mount Price, this ridge is one of the two large lava flows from Clinker Peak that ponded against an ice sheet about 9,000 years ago.

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 (which until 1932 had been also named Daisy Lake).

Fissile Peak, formerly known as Red Mountain, is a mountain peak located on the eastern side of Cheakamus Lake southeast of Whistler in Garibaldi Provincial Park of British Columbia, Canada. The mountain is composed of red slate which is easily divided into thin sheets of uniform thickness; in geological terms this feature is known as fissility.

The Fitzsimmons Range is a small mountain range on the northwestern edge of the Garibaldi Ranges in southwestern British Columbia, Canada, located between the valleys of Cheakamus Lake (SW) and Fitzsimmons Creek (NE). Its most famous summit is Whistler Mountain, which overlooks the resort town of Whistler and is one of the two mountains forming the Whistler Blackcomb ski resort. Most of the range is within Garibaldi Provincial Park, while its northeastern extremity is part of the resort municipality, and of the lands associated with the ski resort operation. Other summits in the range include Oboe Summit, Piccolo Summit and Flute Summit, which are hillocks along the ridge running southeast from Whistler Mountain and were named in association with the renaming of Whistler. Beyond them is Singing Pass and Mount Fitzsimmons 2603 m (8540 ft) which is at the opposite end of the range from Whistler Mountain and the location of Fitzsimmons Glacier, which is the source of Fitzsimmons Creek.

The Garibaldi Lake volcanic field is a volcanic field, located in British Columbia, Canada. It was formed by a group of nine small andesitic stratovolcanoes and basaltic andesite vents in the scenic Garibaldi Lake area immediately north of Mount Garibaldi during the late Pleistocene and early Holocene. The oldest stratovolcano, The Black Tusk, formed between about 1.3 and 1.1 million years ago (Ma). Following glacial dissection, renewed volcanism produced the lava dome and flow forming its summit. Other Pleistocene vents are located along and to the west of the Cheakamus River. Cinder Cone, to the east of The Black Tusk, produced a 9-km-long lava flow during the late Pleistocene or early Holocene.

Corrie Peak is a 2,263-metre (7,425-foot) summit in British Columbia, Canada.

Alice Ridge is a mountain ridge in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It is located just outside of Garibaldi Provincial Park on the east side of the Cheekye River southwest of Mount Garibaldi in New Westminster Land District. It was originally gazetted as Cheekye Ridge on September 12, 1972, but was changed to Alice Ridge on January 30, 1981, due to it being the established local name.

Mount Benvolio is a 2,613-metre (8,573-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the second-highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Overlord Mountain, 0.7 km (0 mi) to the northwest. The Benvolio Glacier is set on the western slope of the peak, the Diavolo Glacier spreads out below the eastern aspect of the summit, and the Fitzsimmons Glacier descends the north slope. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River.

Mount Carr is a 2,590-metre (8,497-foot) mountain summit located in British Columbia, Canada.

Mamquam Mountain is a mountain in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located 6 km (3.7 mi) southeast of Eanastick Meadows and 22 km (14 mi) east of Brackendale. It represents the highest summit of the Mamquam Icefield and lies at the southern end of Garibaldi Provincial Park. Mamquam Mountain was named on September 2, 1930, in association with the Mamquam River.

Mount Brew is a rounded mountain in southwestern British Columbia, Canada, located 18 km (11 mi) southwest of Whistler in the Pacific Ranges of the Coast Mountains. A public cabin run by the Varsity Outdoor Club, Brew Hut, is located near the summit. The alpine area is a popular destination for hiking in the summer and backcountry ski touring in the winter and spring.

The Barrier is a lava dam retaining the Garibaldi Lake system in southwestern British Columbia, Canada. It is over 300 m (980 ft) thick and about 2.4 km (1.5 mi) long where it impounds the lake.

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.

Piccolo Summit is a summit in the Fitzsimmons Range of the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It is located on the north side of Cheakamus Lake just southeast of the town of Whistler in Garibaldi Provincial Park. The mountain is the highest point of a group of hills called the Musical Bumps.

Rubble Creek is a creek in southwestern British Columbia, Canada. It flows northwest from Garibaldi Lake into the Cheakamus River near the abandoned settlement of Garibaldi.

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 to the north, 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 British Columbia 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 Metro Vancouver Regional District.

Cinder Cone is a cinder cone with a small crater on the west side of the Helm Glacier in Garibaldi Provincial Park in British Columbia, Canada. Cinder Cone is surrounded by cinder flats and its crater is filled with meltwater during the summer. Cinder Cone is eroded easily by meltwater during the spring, washing the pyroclastics into the Valley of Desolation. Cinder Cone produced a 9 km (6 mi) long lava flow during the early Holocene.

Flute Summit is a flat-topped summit in the Fitzsimmons Range of the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It is located on the north side of Cheakamus Lake just southeast of the town of Whistler in Garibaldi Provincial Park. The mountain is part of a group of hills called the Musical Bumps.

Diamond Head is a subsidiary peak of Mount Garibaldi in southwestern British Columbia, Canada. It is located west of Mamquam Lake on the south side of Mount Garibaldi in Garibaldi Provincial Park. It was possibly named by Canadian volcanologist William Henry Mathews for its resemblance to Diamond Head in Hawaii. The peak consists of tuff breccia ranging in size from dust to enormous blocks.

Pyramid Mountain is a 2,158-metre (7,080-foot) summit located in British Columbia, Canada.

Gentian Peak is a 2,197-metre (7,208-foot) summit in British Columbia, Canada.

Overlord Mountain is a 2,625-metre (8,612-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges, and can be readily seen from the Whistler Blackcomb ski area. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Mount Macbeth, 3 km (2 mi) to the north-northeast. The Benvolio Glacier rests below the south aspect of the summit, the Fitzsimmons Glacier on the east aspect, and the expansive Overlord Glacier spans the northern and western aspects of the mountain. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1923 by Phyllis Munday and Don Munday via the Benvolio Glacier. The mountain's descriptive name was recommended by the  Garibaldi Park Board and officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

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.

Mount Davidson is a 2,516-metre (8,255-foot) mountain summit located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. Visible from the Whistler Blackcomb ski area, it is situated 18 km (11 mi) south of Whistler, and its nearest higher peak is Castle Towers Mountain, 3 km (2 mi) to the west. The Cheakamus Glacier lies between these two summits, and precipitation runoff from the peak and meltwater from the glacier drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1929 by Neal M. Carter and Emmy Milledge. The mountain is named after Professor John Davidson (1878 – 1970), who contributed a large amount of botanical knowledge about Garibaldi Park. The mountain's toponym was officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

The Gargoyles are two mountain peaks in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. The highest peak has an elevation of 1,823 m (5,981 ft) whereas the lowest peak has an elevation of 1,816 m (5,958 ft). A deeply eroded obsidian dome remnant at The Gargoyles contains 77% silica content and is the only Quaternary high-silica rhyolite identified in the Cascade Volcanic Arc north of the Three Sisters. The age of this rhyolite is poorly known.

Phyllis's Engine is a 2,517-metre (8,258-foot) granite pinnacle located in British Columbia, Canada.

Darling Peak is a 2,310-metre (7,580-foot) mountain summit located in British Columbia, Canada.

Spire Peaks is a 2,279-metre (7,477-foot) mountain located in British Columbia, Canada.

Whirlwind Peak is a 2,427-metre (7,963-foot) mountain summit in southwestern British Columbia, Canada.

Deception Peak is a 2,233-metre (7,326-foot) summit in British Columbia, Canada.

Diavolo Peak is a 2,569-metre (8,428-foot) mountain located in British Columbia, Canada.

Guard Mountain is a 2,177-metre (7,142-foot) summit in British Columbia, Canada.

Hour Peak is a 2,329-metre (7,641-foot) mountain summit located in British Columbia, Canada.

Lydia Mountain is a 2,100-metre (6,890-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 14.5 km (9 mi) northwest of Squamish, and 5.46 km (3 mi) south-southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. The nearest higher neighbor is The Red Tusk, 0.5 km (0 mi) to the west, and Mount Niobe lies 2.17 km (1 mi) to the east-southeast. Lake Lovely Water lies below the eastern slope of the peak and precipitation runoff from the peak drains east to the Squamish River, and west to the Clowhom River via Red Tusk Creek. Topographic relief is significant as Lydia Mountain rises 1,400 meters (4,600 feet) above Red Tusk Creek in approximately three kilometers (two miles). The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada. The mountain was named for mythic Lydia, of which Tantalus was a primordial ruler in Greek mythology. Several peaks in the Tantalus Range are named in association with Tantalus. The first ascent of Lydia Mountain was made in 1914 by Basil Darling and Allan Morkill.

Amicus Mountain is a 2,510-metre (8,235-foot) glaciated summit in British Columbia, Canada.

Alpha Mountain is a 2,302-metre (7,552-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 14 km (8.7 mi) northwest of Squamish, and 4.6 km (2.9 mi) southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Serratus Mountain, 1.9 km (1.2 mi) to the west. The Serratus Glacier lies to the west of Alpha, unnamed glaciers lie on the northern and eastern slopes, and Lake Lovely Water lies below the south slope. Precipitation runoff from the peak drains into tributaries of the Squamish River.

Icecap Peak is a 2,435-metre (7,989-foot) glaciated summit in British Columbia, Canada.

Tzoonie Mountain is a 2,123-metre (6,965-foot) summit in British Columbia, Canada.

Mount Jimmy Jimmy is a 2,208-metre (7,244 ft) glaciated mountain located in the Coast Mountains in southwestern British Columbia, Canada. It is situated 32 kilometres (20 mi) northwest of Squamish, and 10 km (6 mi) northwest of Ossa Mountain, which is its nearest higher peak. Mt. Jimmy Jimmy is the highest point of the Tzoonie-Clowhom Divide. Precipitation runoff from the peak and meltwater from its immense glaciers drains into tributaries of the Squamish River and Clowhom River. The mountain was named for Chief Jimmy Jimmy (native name Swahsh), a leader of the Squamish Nation, who had traplines in the vicinity of the mountain and was a skilled paddler. The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada.  

Ossa Mountain is a 2,261-metre (7,418-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 21 km (13 mi) northwest of Squamish, and 3.54 km (2 mi) north-northwest of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Pelion Mountain, 0.77 km (0 mi) to the east. Unnamed glaciers lie on the northern and eastern slopes. Precipitation runoff from the peak drains into tributaries of the Squamish River and Clowhom River. The first ascent of the mountain was made on July 25, 1960, by Dick Chambers, Jack Bryan, and Howie Rode via the east ridge. The mountain names in the Tantalus Range have a Greek mythology theme, and Ossa Mountain was named for legendary Mount Ossa in Thessaly, upon which the Aloadaes are said to have attempted to pile Mount Pelion on top of Mount Ossa in their attempt to scale Olympus, home of the Greek gods. The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada.

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.

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).

High Falls Creek is a creek in southwestern British Columbia, Canada, located in the New Westminster Land District. It flows southwest into the larger Squamish River.

The Jim Haberl Hut is an alpine hut located in the Tantalus Range near Squamish, British Columbia. The hut is maintained by the Alpine Club of Canada - Vancouver Section.

The Tantalus Range is a subrange of the Pacific Ranges of the Coast Mountains in southern British Columbia, Canada. The range is easily viewed from the "Sea to Sky Highway" that travels from Vancouver to Squamish and Whistler. To Squamish people, the local indigenous people of the area, the name of the Tantalus Range is Tsewílx’ (/tʃə.wilχ/).

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 Mamquam River is a c.35 km (c. 21 mi) tributary of the Squamish River.

The Britannia Range is a small mountain range of the Coast Mountains that runs along the eastern shore of Howe Sound just north of Vancouver, British Columbia, Canada. It is a subrange of the Pacific Ranges and often considered part of the North Shore Mountains. The range is bounded by the Howe Sound to the west, the Stawamus River to the north, Loch Lomond on the upper Seymour River to the east, and Deeks Lake to the south. However, some official maps extend the range further south of these boundaries and many local sources such as hiking guidebooks will often include all of the peaks along the Howe Sound between Deeks Lake and Cypress Mountain as part of the range.

CISQ-FM (107.1 MHz) is a radio station owned by Rogers Radio, a division of Rogers Sports & Media, and operating in southwestern British Columbia. It broadcasts at 107.1 MHz in Squamish and 102.1 MHz in Whistler. It broadcasts an adult contemporary format branded as Mountain FM.

The Monmouth Creek complex is a volcanic complex in southwestern British Columbia, Canada, located 4 km (2.5 mi) southwest of the community of Squamish on the west side of the Squamish River mouth. It lies in the southern Pacific Ranges of the Coast Mountains and is part of the Squamish volcanic field in the southern Garibaldi Volcanic Belt, which represents the northernmost extension of the Cascade Volcanic Arc.

Ring Creek is a creek in southwestern British Columbia, Canada. It flows west and southwest into the Mamquam River, and east of the Squamish River. The community of Ring Creek is located 6 km East of Quest University on the Garibaldi park Road, at an elevation of approximately 2000 feet above sea level. This community is close to Squamish but is outside municipal boundaries, and falls within the SLRD (Squamish Lillooet Regional District). There are permanent residents as well as seasonal dwellers. Population ranges from 40 to 60 persons depending on time of year. This community is fully off grid and has no centrally supplied water, sewer, electricity, garbage collection, or cable services. The origin of the community began with logging in the area. Once road access was established, recreational users began accessing Garibaldi Park, and some unauthorized cabins were constructed in the area. In the late sixties the government surveyed the current lots and offered crown leases to squatters if certain conditions were met, and annual lease fees were paid. As governments changed, leases were offered up for sale as freehold properties. As of this time most lots have been converted to freehold, although over the past 35 years some lots have reverted to the crown, and a few remain crown leases. The community is well known to the mountain biking community as it sits among and near some of the best known, and most widely used mountain bike trails in the sea to Sky Corridor.

The Sea to Sky Gondola is a privately owned recreational aerial tramway about 2 km (1.2 mi) south of Squamish, British Columbia. On BC-99, it offers views over Howe Sound along with cafes, a lodge, hiking trails, and a suspension bridge, the Sky Pilot Suspension Bridge. The majority of the area is located inside of Stawamus Chief Provincial Park. The upper platform, on the slopes of Mount Habrich, is 885 m (2,904 ft) above sea level.

Cobra Crack is a 45-metre (148-foot) long traditional climbing route on a thin crack up an overhanging granite rock face on Stawamus Chief, in Squamish, British Columbia. The route was first ascended by Peter Croft and Tami Knight in 1981 as an aid climb. After it rebuffed many leading climbers, most notably Swiss climber Didier Berthod in 2005, the Canadian climber Sonnie Trotter made the first free ascent in 2006. With subsequent ascents, the consensus grade has settled at 5.14b (8c), which ranked the route as one of the hardest crack climbs in the world, and almost two decades later, it is still considered one of the world's hardest traditional climbing routes.

The Skwelwil'em Squamish Estuary Wildlife Management Area is a wildlife management area on the south coast of British Columbia. It was established in 2007 for the management of fish species as well as terrestrial wildlife. The wildlife management area is on the traditional territory of Squamish Nation, which is involved in management of the area. The freshwater of the Squamish River mixes with the saltwater of Howe Sound, resulting in a varied ecosystem containing different habitats that support an abundance of wildlife. It also provides natural flood control for the Squamish town sites.

Britannia Beach (Sḵwx̱wú7mesh: Shisháyu7áy, [ʃɪʃæjʊʔaj]) is a small unincorporated community in the Squamish-Lillooet Regional District located approximately 55 kilometres north of Vancouver, British Columbia on the Sea-to-Sky Highway on Howe Sound. It has a population of about 300. It includes the nearby Britannia Creek, a small to mid-sized stream that flows into Howe Sound that was historically one of North America's most polluted waterways.

Meslilloet Mountain is a 1,990-metre (6,529-foot) summit located in British Columbia, Canada.

Round Mountain is an eroded volcanic outcrop in the Garibaldi Volcanic Belt in British Columbia, Canada, located 8 km southwest of Eanastick Meadows, 9 km (6 mi) east of Brackendale and 10 km (6 mi) south of Mount Garibaldi. It is the highpoint of Paul Ridge and is located in the southwest corner of Garibaldi Provincial Park. Round Mountain formed as a result of subduction of the Juan de Fuca Plate beneath the North American Plate, known as the Cascadia subduction zone. Round Mountain last erupted during the Pleistocene.

The Squamish Nation, Sḵwx̱wú7mesh Úxwumixw, is a First Nations government of the Squamish people. The Squamish Nation government includes an elected council and an administrative body based primarily in West Vancouver, North Vancouver, and Squamish, BC.

The Stawamus Chief, officially Stawamus Chief Mountain (often referred to as simply The Chief, or less commonly Squamish Chief), is a granitic dome located adjacent to the town of Squamish, British Columbia, Canada. It towers over 700 m (2,297 ft) above the waters of nearby Howe Sound. It is one of the largest granite monoliths in the world.

The Stawamus River is a small, creek-like river in British Columbia. It enters the Howe Sound east of the mouth of the Squamish River.

The Watts Point volcanic centre is a small outcrop of Pleistocene age volcanic rock at Watts Point in British Columbia, Canada, about 10 kilometres (6 mi) south of Squamish and 40 kilometres (25 mi) north of Vancouver, and just north of Britannia Beach. It is the southernmost volcanic zone in the Squamish volcanic field and of the Garibaldi segment of the Cascade Volcanic Arc. The latest research indicates that it is most likely a subglacial mound. It comprises a continuous mass of sparsely porphyritic highly jointed dacitic lava overlying the mid-Cretaceous Coast Plutonic Complex and overlain locally by clay and of glacial till.

Carbon Engineering Ltd. is a Canadian-based clean energy company focusing on the commercialization of direct air capture (DAC) technology that captures carbon dioxide (CO₂) directly from the atmosphere.

Mount Thyestes is a 1,697-metre (5,568-foot) mountain summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 4 km (2 mi) immediately west of Brackendale, 7 km (4 mi) northwest of Squamish, and 10.7 km (7 mi) southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Omega Mountain, 2.4 km (1 mi) to the northwest, and Mount Pelops lies 3.6 km (2 mi) to the west-northwest. Precipitation runoff from the peak drains into tributaries of the Squamish River. The first ascent of the mountain was made in 1942 by R. McLellan, H. Parliament, and F. Roots. The mountain was named for Thyestes, son of Pelops and grandson of Tantalus according to Greek mythology.  The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada.

Howe Sound (French: Baie (de /d')Howe, Squamish: Átl'ka7tsem, Nexwnéwu7ts, Txwnéwu7ts) is a roughly triangular sound, that joins a network of fjords situated immediately northwest of Vancouver, British Columbia, Canada. It was designated as a UNESCO Biosphere Reserve in 2021.

Mount Niobe is a 2,021-metre (6,631-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 10 km (6 mi) northwest of Squamish, and 7.2 km (4 mi) southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Lydia Mountain, 2.03 km (1 mi) to the west-northwest, and Omega Mountain lies 1.1 km (1 mi) to the east. Lake Lovely Water lies below the northern slope of the peak and precipitation runoff from the peak drains into tributaries of the Squamish River. The first ascent of the mountain was made in 1910 by E. Kingsford-Smith and G. Warren via the south side. The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada. The mountain was named for Niobe, daughter of Tantalus in Greek mythology, with several peaks in the Tantalus Range being named for family members of Tantalus.

Watts Point is a point in southwestern British Columbia, Canada, located on the eastern side of Howe Sound northwest of Britannia Beach.