White Horse Rapids in the context of Miles Canyon basalt

⭐ Core Definition: White Horse Rapids

The Whitehorse rapids were rapids on the Yukon River in Canada's Yukon Territory, named for their supposed resemblance to the mane of a charging white horse. The rapids formed where the Yukon River flows across and cuts down through lava flows of the Miles Canyon basalt. These rapids presented a major navigational obstacle on the Yukon River during the Klondike Gold Rush, and lent their name to the nearby town of Whitehorse.

The Whitehorse dam, constructed in 1957–1958, submerged the rapids beneath the newly created Schwatka Lake.

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White Horse Rapids in the context of Whitehorse

Whitehorse (French pronunciation: [wajtɔʁs]) is the capital of Yukon, and the largest city in Northern Canada. It was incorporated in 1950 and is located at kilometre 1426 (Historic Mile 918) on the Alaska Highway in southern Yukon. Whitehorse's downtown and Riverdale areas occupy both shores of the Yukon River, which rises in British Columbia and meets the Bering Sea in Alaska. The city was named after the White Horse Rapids for their resemblance to the mane of a white horse.

Because of the city's location in the Whitehorse valley and relative proximity to the Pacific Ocean, the climate tends to be milder. At this latitude, winter days are short and summer days have up to about 19 hours of daylight.

View the full Wikipedia page for Whitehorse

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