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The Yukon River proper starts at the northern end of Marsh Lake, just south of Whitehorse. Some argue that the source of the Yukon River should really be Teslin Lake and the Teslin River, which has a larger flow when it reaches the Yukon at Hootalinqua. The upper end of the Yukon River was originally known as the Lewes River until it was ...
The Yukon River Basin is located between the Yukon Territory in Canada and Alaska in the United States, with a small portion in British Columbia, Canada. This basin is made up of 13 other individual basins that drain into the Yukon River and other adjoining rivers and tributaries .
The Klondike River (Hän: Tr'ondëk) is a tributary of the Yukon River in Canada that gave its name to the Klondike Gold Rush and the Klondike region of the Yukon Territory. The Klondike River rises in the Ogilvie Mountains and flows into the Yukon River at Dawson City .
Yukon [a] is the smallest and westernmost of Canada's three territories.It is the most densely populated of the three territories, with an estimated population of 46,948 as of 2024, [3] though it has a smaller population than all provinces.
In the north, in basins of Peel River and Porcupine River there lived Kutchin or as they call themselves Gwitchin. [6] About the middle of Yukon River, on the border with Alaska, there lived the Hän people. Northern Tutchone occupied most of the central part of the Yukon, in the basins of the Pelly River and the Stewart River.
Yukon covers 482,443 km 2, of which 474,391 km 2 is land and 8,052 km 2 is water, making it the forty-first largest subnational entity in the world, and, among the fifty largest, the least populous. Yukon is bounded on the south by the 60th parallel of latitude. Its northern coast is on the Beaufort Sea. Its western boundary is 141° west ...
Located along the Yukon River in the sub-arctic region of Northwest Canada, Tr’ondëk-Klondike lies within the homeland of the Tr’ondëk Hwëch’in First Nation. It contains archaeological and historic sources that reflect Indigenous people’s adaptation to unprecedented changes caused by the Klondike Gold Rush at the end of the 19th century.
The sides are usually terraced and in places, the stream for long distances, has cut a secondary rock-walled channel, similar to that noticed on Indian river and Stewart River, through the bottom of its old valley. The country bordering Sixtymile River forms part of the Yukon plateau, a highland worn into rounded hills and long zigzag ridges ...