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Kootenay National Park is a national park of Canada in southeastern British Columbia. The park consists of 1,406 km2 (543 sq mi) of the Canadian Rockies, including parts of the Kootenay and Park mountain ranges, the Kootenay River and the entirety of the Vermilion River. While the Vermilion River is completely contained within the park, the Kootenay River has its headwaters just outside the park boundary, flowing through the park into the Rocky Mountain Trench and eventually joining the Columbia River. The park ranges in elevation from 918 m (3,012 ft) at the southwestern park entrance to 3,424 m (11,234 ft) at Deltaform Mountain.
Glacier National Park is part of a system of 43 parks and park reserves across Canada, and one of seven national parks in British Columbia. Established in 1886, the park encompasses 1,349 km2 (521 sq mi), and includes a portion of the Selkirk Mountains which are part of the larger grouping of mountains, the Columbia Mountains. It also contains the Rogers Pass National Historic Site.
The Illecillewaet River is a tributary of the Columbia River located in British Columbia, Canada. Fed by the Illecillewaet Glacier in Glacier National Park, the river flows approximately 62 kilometres (39 mi) to the southwest, where it flows into the north end of Upper Arrow Lake at Revelstoke. The river's drainage basin is 1,202 square kilometres (464 sq mi).
Kicking Horse Pass is a high mountain pass across the Continental Divide of the Americas of the Canadian Rockies on the Alberta–British Columbia border, and lying within Yoho and Banff national parks. Divide Creek forks onto both sides of the Continental Divide.
The Chehalis River is located in the southwest corner of British Columbia, Canada near the city of Chilliwack. It flows south-eastward out of the Douglas Ranges of the Coast Mountains, draining into the Harrison River.
The Klinaklini River is one of the major rivers of the Pacific Ranges section of the Coast Mountains in the Canadian province of British Columbia. It originates in the Pantheon Range and empties into the head of Knight Inlet.
E.C. Manning Provincial Park is a provincial park in British Columbia, Canada. It is usually referred to as Manning Park, although that nomenclature is also used to refer to the resort and ski area at the park's core. The park covers 83,671 hectares and was the second most visited provincial park in 2017-18 after Cypress Provincial Park. The park lies along British Columbia Highway 3, and occupies a large amount of land between Hope and Princeton along the Canada-United States border.
Hamber Provincial Park is a provincial park in British Columbia, Canada, located 130 kilometres (80.7 mi) north of Golden. Straddling the Great Divide on the provincial boundary with Alberta, the park is surrounded on three sides by Jasper National Park and protects the headwaters of the Wood River at Fortress Lake.
Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine.
The Clearwater River is the largest tributary of the North Thompson River, joining it at the community of Clearwater, British Columbia. The Clearwater rises from glaciers in the Cariboo Mountains and flows in a mostly southerly direction for 201 km (125 mi) to the North Thompson. Its entire course, except the last 5 km (3 mi), is within Wells Gray Provincial Park. Its confluence with the North Thompson is protected by North Thompson River Provincial Park.
The North Thompson River is the northern branch of the Thompson River, the largest tributary of the Fraser River, in the Canadian province of British Columbia. It originates at the toe of the Thompson Glacier in the Premier Range of the Cariboo Mountains, west of the community of Valemount. The river flows generally south through the Shuswap Highland towards Kamloops where it joins the South Thompson River to form the main stem Thompson River.
The Beaver River is a tributary of the Liard River, entering that stream in the area of its Grand Canyon just south of the British Columbia-Yukon border after running generally south-east from its origin in the extreme southeast corner of the Yukon Territory.
The Kitimat River is a river in the Canadian province of British Columbia. It originates in the Kitimat Ranges, near the sources of the Dala River, Kemano River, Atna River, and Clore River. It flows in a curve north, then west, then south, emptying into Kitimat Arm at the head of Douglas Channel, at the town of Kitimat.
The Iskut River, located in the northwest part of the province of British Columbia is the largest tributary of the Stikine River, entering it about 11 km (6.8 mi) above its entry into Alaska.
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.
Wells Gray Provincial Park is a large wilderness park located in east-central British Columbia, Canada. The park protects most of the southern, and highest, regions of the Cariboo Mountains and covers 5,415 square kilometres. It is British Columbia's fifth largest provincial park, after Tweedsmuir, Tatshenshini, Spatsizi and Northern Rocky Mountains.
Mount Rogers, is a 3,169-metre (10,397-foot) massif located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Mount Rogers is situated at the north end of the Hermit Range, and is the highest point of the range. Its nearest higher peak is Mount Sir Donald, 12.57 km (7.81 mi) to the southeast. The peak is prominently visible from eastbound Highway 1, the Trans-Canada Highway at Rogers Pass. The Rogers massif includes five individually-named summits: Rogers Peak, Grant Peak, Fleming Peak, Swiss Peak, and Truda Peaks. Numerous glaciers radiate from all sides, including the Rogers Glacier, Swiss Glacier, Tupper Glacier, and Hermit Glacier.
Avalanche Mountain, is a 2,861-metre (9,386-foot) mountain summit located in Glacier National Park in the Selkirk Mountains in British Columbia, Canada. Its nearest higher peak is Mount Macdonald, 2.2 km (1.4 mi) to the north. Mount Sir Donald is 3.83 km (2.38 mi) to the southeast, and Eagle Peak is 1.46 km (0.91 mi) to the south-southeast. The Avalanche Glacier is situated on the east side of the peak, and the Connaught Tunnel lies partially beneath Avalanche Mountain. The peak is visible from eastbound Highway 1, the Trans-Canada Highway approaching Rogers Pass. During winter and spring of each year the western slope, named Avalanche Crest, generates avalanches which can threaten the highway.
Grizzly Mountain is a 2,754-metre (9,035-foot) mountain summit located in Glacier National Park, in the Hermit Range of the Selkirk Mountains in British Columbia, Canada. Grizzly Mountain is situated 57 km (35 mi) northeast of Revelstoke, and 42 km (26 mi) west of Golden. It is also set 4 km (2.5 mi) north of Cheops Mountain, and 3 km (1.9 mi) west of Rogers Pass from which it can be seen from the Trans-Canada Highway. The closest peak to Grizzly is Ursus Minor Mountain, 1.27 km (0.79 mi) to the west-southwest, and its nearest higher peak is Mount Sifton, 2.35 km (1.46 mi) to the north. The first ascent of the mountain was made August 31, 1901, by John E. Bushnell, August S. Eggers, Karl Schuluneggar, and Friedrich Michel via the southeast couloir. The first ascent of the north ridge was made in 1921 by Neal Carter, Tom Fyles, and Don Munday. The class 5.2 west ridge was first climbed by Georgia Engelhard and Ernest Feuz in 1933. The mountain's name was adopted in 1906, then re-approved September 8, 1932, by the Geographical Names Board of Canada. It was so-named because of its proximity above Bear Creek, and in keeping with the bear theme of other nearby features such as Ursus Major Mountain, Ursus Minor Mountain, Bruins Pass, and Balu Pass.
The Little Iskut River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about 45 km (28 mi), generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls. The Little Iskut River is part of the Stikine River drainage basin, as the Iskut River is a major tributary of the Stikine.
References
- ↑ "Beaver Glacier". BC Geographical Names .
- ↑ "Beaver River". BC Geographical Names .
- 1 2 3 "Archived Hydrometric Data Search". Water Survey of Canada. Archived from the original on February 21, 2009. Retrieved October 19, 2008. Search for Station 08NB019 Beaver River near the mouth
- ↑ "Beaver Canyon". BC Geographical Names .
- ↑ Parks Canada Agency, Government of Canada (11 August 2021). "Hiking - Glacier National Park". www.pc.gc.ca. Retrieved 17 September 2021.