Bennett Range

Last updated
Bennett Range
Geography
Country Canada
Provinces British Columbia and Yukon
Range coordinates 59°55′N134°59′W / 59.917°N 134.983°W / 59.917; -134.983 Coordinates: 59°55′N134°59′W / 59.917°N 134.983°W / 59.917; -134.983
Parent range Tagish Highland

The Bennett Range is a subrange of the Tagish Highland, located on the west side of Bennett Lake in Yukon and British Columbia, Canada.

Name origin

The lake from which the range name comes was named in 1883 by Frederick Schwatka, US Army officer and explorer, after James Gordon Bennett Jr (1841–1918), editor of the New York Herald , who was sponsor of Schwatchka's search for the remains of the Franklin Expedition, 1878–81. [1]

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Yukon Territory of Canada

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Yukon River River in the Yukon Territory of Canada

The Yukon River is a major watercourse of northwestern North America. The river's source is in British Columbia, Canada, from which it flows through the Canadian Yukon Territory. The lower half of the river lies in the U.S. state of Alaska. The river is 3,190 kilometres (1,980 mi) long and empties into the Bering Sea at the Yukon–Kuskokwim Delta. The average flow is 6,430 m3/s (227,000 ft3/s). The total drainage area is 832,700 km2 (321,500 mi2), of which 323,800 km2 (126,300 mi2) is in Canada. The total area is more than 25% larger than Texas or Alberta.

Bennett may refer to:

Bennett Lake

Bennett Lake is a lake in the Province of British Columbia and Yukon Territory in northwestern Canada. It is just north of the border with the United States state of Alaska, near the Alaskan port of Skagway.

Bennett, British Columbia Ghost town in Canada

Bennett, British Columbia, Canada, is an abandoned town next to Bennett Lake and along Lindeman Creek. The townsite is now part of the Chilkoot Trail National Historic Site of Canada and is managed by Parks Canada. Bennett is also a stop on the White Pass and Yukon Route Railroad during the summer months.

White Pass

White Pass, also known as the Dead Horse Trail, is a mountain pass through the Boundary Ranges of the Coast Mountains on the border of the U.S. state of Alaska and the province of British Columbia, Canada. It leads from Skagway, Alaska, to the chain of lakes at the headwaters of the Yukon River, Crater Lake, Lake Lindeman, and Bennett Lake.

Carcross Place in Yukon, Canada

Carcross, originally known as Caribou Crossing, is an unincorporated community in Yukon, Canada, on Bennett Lake and Nares Lake. It is home to the Carcross/Tagish First Nation. At the 2016 census it had a population of 301.

Tagish Lake Lake in British Columbia and Yukon in Canada

Tagish Lake is a lake in Yukon and northern British Columbia, Canada. The lake is more than 100 km (62 mi) long and about 2 km (1 mi) wide.

Geography of Yukon

Yukon is in the northwestern corner of Canada and is bordered by Alaska and the Northwest Territories. The sparsely populated territory abounds with natural scenic beauty, with snowmelt lakes and perennial white-capped mountains, including many of Canada's highest mountains. The territory's climate is Arctic in the north, subarctic in the central region, between north of Whitehorse and Old Crow, and has a humid continental climate in the far south, south of Whitehorse and in areas close to the British Columbia border. The long sunshine hours in the short summer allow a profusion of flowers and fruit to blossom. Most of the territory is boreal forest, tundra being the main vegetation zone only in the extreme north and at high elevations.

Marsh Lake

Marsh Lake is a widening of the Yukon River southeast of Whitehorse, Yukon, Canada. It is over 30 kilometres long and ranges from three to four kilometres wide. The co-ordinates of the lake are 60°26′10″N134°15′02″W, and is 2,147 feet above sea level. The lake forms part of a chain of finger lakes, sometimes referred to as "The Southern Lakes", they form the headwaters of the Yukon River.

Tagish Highland Landform of the western coast of North America

The Tagish Highland is an upland area on the inland side of the northernmost Boundary Ranges of the Coast Mountains, spanning far northwestern British Columbia from Atlin Lake to the area of the pass at Champagne, Yukon between the Alsek and Yukon Rivers. In some classification systems, and in local terminology, the Tagish Highland is considered to be part of the Boundary Ranges, as is the neighbouring Tahltan Highland to its south. As classified by the Canadian Mountain Encyclopedia per S. Holland, the Tagish Highland is part of the system unofficially described as the Interior Mountains.

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.

The Skukum Group is a 55-million-year-old volcanic group in northern British Columbia and southern Yukon, Canada. It consists of discrete calderas in a linear range from the south end of Atlin Lake to Bennett Lake, then to Aishihik Lake. The cluster of rocks crowds the Mount Skukum gold deposit southwest of Whitehorse. One of the calderas within the group is the Bennett Lake Volcanic Complex.

Carcross Desert

Carcross Desert, located outside Carcross, Yukon, Canada, is often considered the smallest desert in the world. The Carcross Desert measures approximately 2.6 km2 (1.0 sq mi), or 259 ha.

The Atlin District, also known as the Atlin Country, is a historical region located in the far northwestern corner of the Canadian province of British Columbia, centred on Atlin Lake and the gold-rush capital of the region, the town of Atlin. The term "Atlin District" was also used synonymously with the official administrative area named the Atlin Mining District, established during the gold-mining heyday contemporaneous with the Klondike Gold Rush. The region also includes adjoining Teslin and Tagish Lakes and the Bennett Lake area in the narrow strip of BC separating the Alaska Panhandle from the Yukon. The Atlin District is currently part of the Stikine Region in the regional district system. The communities of the Atlin lakes district, as the area is casually called, are referred to in national weather reports as "the Southern Lakes", as in "Whitehorse and the Southern Lakes", although this also includes towns on the Yukon end of the lakes.

Teslin Lake

Teslin Lake is a large lake spanning the border between British Columbia and Yukon, Canada. It is one of a group of large lakes in the region of far northwestern BC, east of the upper Alaska Panhandle, which are the southern extremity of the basin of the Yukon River, and which are known in Yukon as "the Southern Lakes". The lake is fed and drained primarily by the Teslin River, south and north, but is also fed from the east by the Jennings River and the Swift River, and from the west by the Hayes River.

Kusawa Lake

Kusawa Lake is a lake in the southern Yukon, Canada. Kusawa means "long narrow lake" in the Tlingit language. The Kusawa Lake is a lake in Canada's Yukon Territory. It is located at an altitude of 671 m (2,201 ft) and is 60 km (37 mi) southwest of Whitehorse near the British Columbia border. It meanders over a length of 75 km (47 mi) with a maximum width of about 2.5 km (1.6 mi) through the mountains in the north of the Boundary Ranges. It is fed by the Primrose River and Kusawa River. The Takhini outflows to the Yukon River from the northern tip of Kusawa Lake. Kusawa Lake has an area of 142 km2 (55 sq mi). The lake has a maximum depth of 140 m (460 ft) and is of glacial origin. It is a common tourist destination and is also popular for fishing.

<i>A. J. Goddard</i>

A. J. Goddard was a Klondike Gold Rush era sternwheeler owned by Seattle businessman Albert J. Goddard and built for transport of men and supplies on the Upper Yukon River in Canada. She was assembled from pieces which were manufactured in San Francisco, shipped up to Skagway, Alaska, hauled over the Coast Mountains, and finally assembled at Lake Bennett. She made one trip to Dawson during the gold rush, was sold and sank in a storm on Lake Laberge in 1901. Her wreck was discovered in 2008 by Doug Davidge and was designated as a Yukon Historic Site.

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