Tuya Mountains Provincial Park

Last updated
Tuya Mountains Provincial Park
Canada British Columbia relief location map.jpg
Red pog.svg
Location British Columbia, Canada
Nearest city Cassiar
Coordinates 59°10′19″N130°29′59″W / 59.17194°N 130.49972°W / 59.17194; -130.49972
Area180.01 km2 (69.50 sq mi)
EstablishedApril 11, 2001 (2001-04-11)
Governing body BC Parks

Tuya Mountains Provincial Park is a provincial park in British Columbia, Canada, protecting the Tuya Range, a volcanic region at the head of the Tuya River. [1] The park is located on the north side of Tuya Lake. The park is named for nearby Tuyas, steep-sided, flat-topped types of volcano.

Related Research Articles

Stikine River River in British Columbia and Alaska

The Stikine River is a river, historically also the Stickeen River, approximately 610 kilometres (380 mi) long, in northwestern British Columbia in Canada and in southeast Alaska in the United States.

Liard River Hot Springs Provincial Park

Liard River Hot Springs Provincial Park is a provincial park in British Columbia, Canada. It is home to the largest natural hot springs in Canada. It is a natural river of hot water rather than a spring fed man made pool The park is part of the larger Muskwa-Kechika Management Area. The community of Liard River, British Columbia is located nearby.

Buckinghorse River Wayside Provincial Park Provincial park in British Columbia, Canada

Buckinghorse River Wayside Provincial Park is a provincial park in British Columbia, Canada located on the Alaska Highway, approximately 175 km northwest of the city of Fort St. John. It is located on the north side of the Buckinghorse River, to the northwest of the community of Pink Mountain. The park is 36 ha. in size and is near the community of Buckinghorse River.

Bishop River Provincial Park is a provincial park in the Pacific Ranges of the Coast Mountains on the Mainland of British Columbia, Canada, located southwest of and adjoining Ts'yl-os Provincial Park."Bishop River Park". BC Geographical Names. It lies along the upper course of the Bishop River, the main tributary of the Southgate River, from the Bishop's source at the western side of the Lillooet Icecap to midway along its course above its confluence with the Southgate. The park is 19,947 ha. in size. There are no roads or trails in the park although a forest service road from Waddington Harbour at the head of Bute Inlet leads up the Southgate to within a few miles of the park boundary.

Kinaskan Lake Provincial Park

Kinaskan Lake Provincial Park is a provincial park in British Columbia, Canada, located at the south end of Kinaskan Lake along the Stewart-Cassiar Highway near Mowdade Lake and southeast of Mount Edziza. At the south end of the park, the Iskut River, of which the lake is an expansion, spills over 12.2-metre Cascade Falls. The park is approximately 800 ha. in size.

Kitwanga Mountain Provincial Park

Kitwanga Mountain Provincial Park is a provincial park in British Columbia, Canada located on the north side of the Skeena River just west of the Gitxsan community of Kitwanga (Gitwangak).

Wapiti Lake Provincial Park Provincial park in British Columbia, Canada

Wapiti Lake Provincial Park is a 16,837-hectare (41,610-acre) provincial park in British Columbia, Canada. It is 60 kilometres (37 mi) south of Tumbler Ridge, at the headwaters of Wapiti River, including its watershed from the Wapiti Pass to Wapiti Lake in the Canadian Rockies. The area contains significant amounts of fossils (ichthyosaurs) and fossil beds. There is habitat for grizzly bears, mountain goats, and bull trout. It was established as a Provincial Park on June 26, 2000. It is recognized by the provincial government as being an area traditionally used by First Nations people. Hunting and fishing are permitted in the park.

Sechelt Inlets Marine Provincial Park

Sechelt Inlets Marine Provincial Park is a provincial park in British Columbia, Canada, at various locations on Sechelt Inlet, Salmon Inlet and Narrows Inlet, near Sechelt. Established initially as a recreation area in 1980, it was converted to a park in 1999, containing approximately 140 hectares.

Tuya Flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet

A tuya is a flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet. They are rare worldwide, being confined to regions which were covered by glaciers and had active volcanism during the same period.

Tuya Butte is a tuya in the Tuya Range of north-central British Columbia, Canada. It is a bit less isolated from other ranges than neighbouring Mount Josephine. Some of the other volcanoes in the area include South Tuya, Ash Mountain, and Mathews Tuya.

Ash Mountain (British Columbia) Mountain in British Columbia, Canada

Ash Mountain is the highest summit in the Tuya Range of the Stikine Ranges in northcentral British Columbia, Canada, located immediately north of High Tuya Lake at the north end of Tuya Mountains Provincial Park. It is one of the six tuyas clustered close to Tuya Lake. The base of the volcano comprises pillow lava and hyaloclastite indicating that the volcano formed beneath ice or under a large lake. The volcano comprises loose debris as well as dikes of basaltic rock that intruded into the volcanic pile. Other tuyas in the area include Tuya Butte, South Tuya and Mathews Tuya, although most of the group of tuyas are unnamed.

Tuya Range

The Tuya Range is a mountain range in the Stikine Ranges of the Cassiar Mountains in the far north of the Canadian province of British Columbia, near its border with the Yukon Territory and to the southwest of Watson Lake, Yukon, which is the nearest major settlement.

Interior Mountains

The Interior Mountains or Northern Interior Mountains are the semi-official names for an expansive collection of mountain ranges that comprises much of the northern half of the Canadian province of British Columbia and a large area of southern Yukon.

Bill Mathews

William Henry Mathews (1919–2003) was a Canadian geologist, volcanologist, engineer, and professor. He is considered a pioneer in the study of subglacial eruptions and volcano-ice interactions in North America. Many of his publications continue to be regarded as classics in their field.

Powder Mountain Icefield

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.

Sezill Volcano is a lava dome in Mount Edziza Provincial Park of northern British Columbia, Canada. It is thought to have formed and last erupted during the Miocene period. The volcano gets its name from being adjacent to Sezill Creek.

The Cottonwood River is a tributary of the Dease River in the Cassiar Country of the Northern Interior of British Columbia, Canada. Rising in the northern Stikine Ranges just east of Toozaza Peak, and just south of the origins of the Jennings and Little Rancheria River near the border with Yukon, it flows south along the east flank of the Tuya Range to meet the Dease just north of that river's source at Dease Lake, between the north end of that lake and McDame Creek and the former mining centre and community of McDame Post.

Terminal Range

The Terminal Range is the northernmost mountain range of the Canadian Rockies, so-named for its position at the northern terminus of the Rockies. Lying west of Muncho Lake and the Trout River, its northern perimeter is the Liard River. The Sentinel Range lies to its east.

Horneline Creek Provincial Park

Horneline Creek Provincial Park is a provincial park in far northern British Columbia, Canada. It is located west of the Kechika River about 130 km south of Lower Post and 30 km north of Denetiah Provincial Park and southwest of the community of Liard River.

Tuya River

The Tuya River is a major tributary of the Stikine River in northwest part of the province of British Columbia, Canada. From its source at High Tuya Lake in Tuya Mountains Provincial Park just south of Ash Mountain, the highest peak of the Tuya Range, the Tuya River flows south about 200 km (120 mi) to meet the Stikine River in the Grand Canyon of the Stikine. The Tuya River's main tributary is the Little Tuya River. The Tuya River divides the Tanzilla Plateau on the east from the Kawdy Plateau, to the northwest, and the Nahlin Plateau, to the southwest. All three are considered sub-plateaus of the Stikine Plateau. The Tuya River's watershed covers 3,575 km2 (1,380 sq mi), and its mean annual discharge is estimated at 36.9 m3/s (1,300 cu ft/s). The mouth of the Tuya River is located about 24 km (15 mi) northeast of Telegraph Creek, British Columbia, about 67 km (42 mi) southwest of Dease Lake, British Columbia, and about 210 km (130 mi) east of Juneau, Alaska. The Tuya River's watershed's land cover is classified as 35.7% shrubland, 31.4% conifer forest, 14.0% mixed forest, 7.2% herbaceous, and small amounts of other cover.

References

  1. "Tuya Mountains Park". BC Geographical Names. Retrieved 28 September 2021.

Coordinates: 59°10′20″N130°30′00″W / 59.1722°N 130.5000°W / 59.1722; -130.5000