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Klondike, Yukon

Region of Yukon, Canada

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Through Canada and Gold

The Klondike is famed due to the Klondike Gold Rush, which started in 1896 and lasted until 1899. Since then, gold has been mined continuously in that area, except for a pause in the late 1960s and early 1970s.

In 2023, the cultural landscape of the Tr'ondëk-Klondike was inscribed as a UNESCO World Heritage Site, because of its testimony to the adaptation of the Tr'ondëk Hwëch'in people to the European colonization that began in the late 19th century.

Climate and ecology

Klondike has a subarctic climate (Köppen Dfc), bordering on a tundra climate (Köppen ET). The climate is warm in the short summer, and very cold during the long winter. By late October, ice forms over the rivers. For the majority of the year, the ground is frozen to a depth of 1 to 3 metres (3 to 10 ft). The landscape is dominated by spruce, aspen, and birch trees interspersed with riparian vegetation.

Salmon have likely been migrating from the Pacific Ocean to the Klondike River to spawn for at least 65,000 years, and archeological evidence suggests that they have been fished as early as 11,500 years ago. Caribou also migrate through the Klondike region during their seasonal migrations. Other species found in the region include moose, black bear, grizzly bear, lynx, marten, wolf, wolverine, Dall's sheep, and beaver.

There is a weather station for Klondike located along the Dempster Highway, near the southern entrance of Tombstone Territorial Park, at an elevation of 973 m (3192 ft).

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