Mount Pelops

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.

Omega Mountain is a 1,918-metre (6,293-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 8.2 km (5 mi) southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Mount Pelops, 1.7 km (1 mi) to the west. Lake Lovely Water lies below the northwestern slope of the peak with Alpha Mountain on the opposite side of the lake. Precipitation runoff from the peak drains into tributaries of the Squamish River. The first ascent of the mountain was made in 1916 by Tom Fyles and his brother, John Fyles. The mountain's name comes from Omega, in keeping with nearby peaks being named for Greek alphabet letters, namely Alpha and Iota mountains. Its name was officially adopted on June 6, 1957, by the Geographical Names Board of 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.

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.

Brackendale Eagles Provincial Park is a provincial park in British Columbia, Canada, located on the Squamish River adjacent to Brackendale, a suburban neighbourhood of Squamish. It is notable for its bald eagle population during the winter months and is inaccessible to visitors.

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. Its prominent and enigmatic edifice is composed of basaltic andesite to dacite of unknown age and may represent a group of dikes and lava domes that formed subglacially. At least four dikes protrude its summit. These form the ribs of 60 m (200 ft) to 180 m (590 ft) high lava spines, the tallest being The Castle, which contains horizontal and radiating columnar joints. The spines are covered by welded breccia close to their bases and columnar jointing extends into the welded sequence. The most elevated lava flows and spines are composed of dacite.

The Cheakamus River (pron. CHEEK-a-mus) is a tributary of the Squamish River, beginning on the west slopes of Outlier Peak 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 c. 70 km (c.44 mi) length of the Cheakamus is followed by British Columbia Highway 99 (the Sea-to-Sky Highway) and the British Columbia Railway. The Cheakamus is a whitewater rafting and kayaking route, and is known for its steelhead and salmon fishing. Much of the flow of the upper Cheakamus is diverted from Daisy Lake beneath the mountains to the west to the Cheakamus Powerhouse on the Squamish River. Notable just north of Daisy Lake is Brandywine Falls. The Nordic events complex of the 2010 Winter Olympics was located on Callaghan Creek, a tributary of the Cheakamus just upstream from Brandywine Creek.

Evans Lake is a small, roughly triangular lake having a perimeter of about 1.3 kilometers, on the rise between the Cheakamus and Squamish Rivers in British Columbia, Canada. The 604-acre (2.44 km2) site has been home to youth camps since 1959. For decades Evans Lake was used primarily by the Junior Forest Wardens of BC. Later, the BC Forestry Association ran summer camps for children. The summer program is a combination of ecology-based educational time and structured and unstructured leisure time. During the school year, the Evans Lake Forest Education Center offers schools, community groups, businesses and private parties independent and program-based activities at Evans Lake forest and camp.

Woodfibre, originally Britannia West, was a pulp mill and at one time a small company town, on the west side of upper Howe Sound near Squamish, British Columbia. The mill closed in March 2006.

Squamish Airport (IATA: YSE, ICAO: CYSE) is located 5.4 nautical miles (10.0 km; 6.2 mi) north of Squamish, British Columbia, Canada. Squamish Airport is a general aviation airport with a 2,400 ft (732 m) runway located about 8 km (5.0 mi) from downtown Squamish. It is used for charter services, private aircraft, flying clubs, and other commercial activities. Given its close proximity to Greater Vancouver, there is no regularly scheduled air service at the Squamish Airport. The airport was also used by the Canadian Forces as part of their preparation for the 2010 Vancouver Winter Olympics.

The Castle is a lava spine located west of Squamish in southwestern British Columbia, Canada. Volcanism at The Castle is controlled by north–south structures and there are no hot springs known in the area. It forms part of the Monmouth Creek complex and is part of the Garibaldi Volcanic Belt which is a segment of the Cascade Volcanic Arc.

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 was 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.