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The Stikine River is a major river in northern British Columbia (BC), Canada and southeastern Alaska in the United States. It drains a large, remote upland area known as the Stikine Country east of the Coast Mountains. Flowing west and south for 610 kilometres (379 mi), it empties into various straits of the Inside Passage near Wrangell, Alaska. About 90 percent of the river's length and 95 percent of its drainage basin are in Canada. Considered one of the last truly wild large rivers in BC, the Stikine flows through a variety of landscapes including boreal forest, steep canyons and wide glacial valleys.
Stanley Peak is a 3,155-metre (10,351 ft) mountain located in the Ball Range, at the northeastern section of Kootenay National Park, in the Canadian Rocky Mountains. The mountain was named in 1901 by its first climber, the English explorer Edward Whymper, after Frederick Stanley, 16th Earl of Derby, the sixth Governor-General of Canada. There are sources that date the naming in 1912 after Stanley H. Mitchell, Secretary-Treasurer of Alpine Club of Canada.
This is a list of the extreme points of The Americas, the points that are farther north, south, east or west than any other location on the continent. The continent's southernmost point is often said to be Cape Horn, which is the southernmost point of the Chilean islands. The Americas cross 134° of longitude east to west and 124° of latitude north to south.
The Boundary Ranges, also known in the singular and as the Alaska Boundary Range, are the largest and most northerly subrange of the Coast Mountains. They begin at the Nass River, near the southern end of the Alaska Panhandle in the Canadian province of British Columbia and run to the Kelsall River, near the Chilkoot Pass, beyond which are the Alsek Ranges of the Saint Elias Mountains, and northwards into the Yukon Territory flanking the west side of the Yukon River drainage as far as Champagne Pass, north of which being the Yukon Ranges. To their east are the Skeena Mountains and Stikine Plateau of the Interior Mountains complex that lies northwest of the Interior Plateau; the immediately adjoining subregion of the Stikine Plateau is the Tahltan Highland. To their northeast is the Tagish Highland, which is a subregion of the Yukon Plateau. Both highlands are considered in some descriptions as included in the Coast Mountains. The Alexander Archipelago lies offshore and is entirely within Alaska.
Lower Post is an aboriginal community in the Stikine Region of northern British Columbia, Canada, located on Highway 97, the Alaska Highway, approximately 15 miles southeast of Watson Lake, Yukon. Its historical mile designation is Mile 620. It is located near the confluence of the Dease and Liard Rivers.
Tā Chʼilā Provincial Park, formerly Boya Lake Provincial Park, is a provincial park located in the Stikine Region of British Columbia, Canada. The park located 120 km north-by-northwest of the community of Dease Lake near BC Highway 37. Boya Lake is named for Charlie Boya, a First Nations man from the area.
Chutine Peak is one of the highest mountains in the Boundary Ranges, a group of subranges of the northern Coast Mountains of British Columbia and Alaska. Chutine Peak lies just east of the Stikine Icecap, and to the north and west of the Stikine River, and south of the basin of the Whiting River. It is notable for its huge west face: the drop to Chutine Lake is 2,600 m (8,530 ft) in 3.5 km (2 mi). Due to its remoteness, however, it is rarely visited.
Hoodoo Mountain, sometimes referred to as Hoodoo Volcano, is a potentially active stratovolcano in the Northern Interior of British Columbia, Canada. It is located 25 kilometres northeast of the Alaska–British Columbia border on the north side of the Iskut River opposite of the mouth of the Craig River. With a summit elevation of 1,850 metres and a topographic prominence of 900 metres, Hoodoo Mountain is one of many prominent peaks within the Boundary Ranges of the Coast Mountains. Its flat-topped summit is covered by an ice cap more than 100 metres thick and at least 3 kilometres in diameter. Two valley glaciers surrounding the northwestern and northeastern sides of the mountain have retreated significantly over the last hundred years. They both originate from a large icefield to the north and are the sources of two meltwater streams. These streams flow along the western and eastern sides of the volcano before draining into the Iskut River.
Mount Edziza, sometimes called Edziza Mountain or Edziza Peak, is a stratovolcano in Cassiar Land District of northwestern British Columbia, Canada. It is located on the Big Raven Plateau of the Tahltan Highland which extends along the western side of the Stikine Plateau. The mountain has an elevation of 2,786 metres, making it the highest volcano of the Mount Edziza volcanic complex. However, it had an elevation of at least 3,396 metres before its original summit was likely destroyed by a violent, climactic eruption in the geologic past; its current flat summit contains an ice-filled, 2-kilometre (1.2-mile) in diameter crater. Mount Edziza contains several lava domes, cinder cones and lava fields on its flanks, as well as an ice cap that is characterized by several outlet glaciers stretching out to lower altitudes. All sides of the mountain are drained by tributaries of Mess Creek and Kakiddi Creek which are situated within the Stikine River watershed.
Level Mountain is a large volcanic complex in the Northern Interior of British Columbia, Canada. It is located 50 kilometres north-northwest of Telegraph Creek and 60 kilometres west of Dease Lake on the Nahlin Plateau. With a maximum elevation of 2,164 metres, it is the second-highest of four large complexes in an extensive north–south trending volcanic region. Much of the mountain is gently-sloping; when measured from its base, Level Mountain is about 1,100 metres tall, slightly taller than its neighbour to the northwest, Heart Peaks. The lower, broader half of Level Mountain consists of a shield-like structure while its upper half has a more steep, jagged profile. Its broad summit is dominated by the Level Mountain Range, a small mountain range with prominent peaks cut by deep valleys. These valleys serve as a radial drainage for several small streams that flow from the mountain. Meszah Peak is the only named peak in the Level Mountain Range.
Nahta Cone is a small cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 1,670 metres and lies near the northern edge of the Arctic Lake Plateau, a glacially scored plateau of the Tahltan Highland which in turn extends along the western side of the Stikine Plateau. The cone is about 70 kilometres south-southeast of the community of Telegraph Creek and lies in the southwestern corner of Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia.
Mount Ratz is a mountain located just west of the Stikine River, about 5 km (3 mi) east of the British Columbia-Alaska border. It is the highest peak in the Stikine Icecap and of the Boundary Ranges which in turn form part of the Coast Mountains. It is an extremely high-prominence summit, with a difference in elevation with its "key col" at Hyland Ranch Pass of 2,430 m (7,972 ft). Thus making it one of Canada's Ultra peaks.
Seton Dam is a dam on the Seton River, 350m below the outlet of Seton Lake 5 km west of the town of Lillooet, British Columbia, Canada, and with the related Seton Canal is part of the lowest and last stage of BC Hydro's Bridge River Power Project. The 18-meter-high (59 ft) concrete dam, completed in 1956, raised the height of Seton Lake only 10 feet in order to maximize the elevation differential between that lake and the Fraser River in order to extract the maximal potential output of power generation at the Seton Powerhouse, which is located on the Fraser just south of the confluence of the Seton River proper.
The Mount Edziza volcanic complex is a group of volcanoes and associated lava flows in northwestern British Columbia, Canada. Located on the Tahltan Highland, it is 40 kilometres southeast of Telegraph Creek and 85 kilometres southwest of Dease Lake. The complex encompasses a broad, steep-sided lava plateau that extends over 1,000 square kilometres. Its highest summit is 2,786 metres in elevation, making the MEVC the highest of four large complexes in an extensive north–south trending volcanic region. It is obscured by an ice cap characterized by several outlet glaciers that stretch out to lower altitudes.
The Tahltan River is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally east and southeast about 95 km (59 mi) to join the Stikine River at Tahltan, British Columbia. The lower Tahltan River marks the boundary between the Tahltan Highland and the Nahlin Plateau, both of which are part of the larger Stikine Plateau region.
The Jennings River is a river in far northern British Columbia, Canada. It is approximately 150 kilometres (93 mi) long. The river was named for William T. Jennings (1846-1906), a civil engineer who, in 1897, assessed various road and railroad routes from the Pacific Ocean to the Yukon.
Simpson Peak 2170 m is the northernmost officially-named summit in the Stikine Ranges of the Cassiar Mountains system in northernmost British Columbia, Canada. It stands on the north side of the lower reaches of the Jennings River, just east of the south end of Teslin Lake, and is to the south of Swan Lake, which is an expansion of the Swift River. The mountain is named for Scott Simpson, an early explorer in the area. The next-highest summit in the unnamed subrange of the Cassiars to the north of the Jennings River is Toozaza Peak.
The Frog Lakes are a group of lakes, drained eastward by an unnamed stream feeding the Frog River, a tributary of the Kechika River in the Stikine Ranges of the northern interior of British Columbia. Though not the hydrological source of the Frog River, the lakes are in an east–west aligned valley which forms the divide between the basins of the Stikine River and that of the Liard, and are therefore on the Continental Divide between the Pacific and Arctic drainages. Draining from their west is the Pitman River, a Stikine tributary, from an unnamed lake just to their west, while the Kechika is a major tributary of the Liard, which is a tributary of the Mackenzie. Frog Lakes Pass, at an elevation of 1015 m (3330 ft), is the prominence col for the 2668 m (8753 ft) Sharktooth Mountain, giving it a prominence of 1653 m.
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.
Mount Monashee is a summit in British Columbia. At an elevation of 3274 meters, it is the highest point in the Monashee Mountains.
References
- 1 2 "Bennett Peak, British Columbia". peakbagger.com. Retrieved 5 July 2019.
- ↑ "Elevation of Bennett Peak, Stikine Region, BC V0W, Canada". Worldwide Elevation Finder. Retrieved 5 July 2019.
- ↑ "Bennett Lake". yukoninfo.com. Retrieved 5 July 2019.
59°57′23″N134°58′15″W / 59.95639°N 134.97083°W
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