Alligator Lake (Yukon)

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Alligator Lake
Alligator Lake.jpg
Alligator Lake by satellite
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Alligator Lake
Location Yukon
Coordinates 60°22′55″N135°21′10″W / 60.38194°N 135.35278°W / 60.38194; -135.35278
Basin  countriesCanada

The Alligator Lake is an alpine lake near Whitehorse [ citation needed ] in southern [1] Yukon, Canada.Canada. [2] The Alligator Lake volcanic complex, being in the vicinity, is named after it.[ citation needed ]

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Yukon is the smallest and westernmost of Canada's three territories. It is the second-least populated province or territory in Canada, with a population of 45,148 as of 2023. However, Whitehorse, the territorial capital, is the largest settlement in any of the three territories.

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The Alaska Highway was constructed during World War II to connect the contiguous United States to Alaska across Canada. It begins at the junction with several Canadian highways in Dawson Creek, British Columbia, and runs to Delta Junction, Alaska, via Whitehorse, Yukon. When it was completed in 1942, it was about 2,700 kilometres (1,700 mi) long, but in 2012, it was only 2,232 km (1,387 mi). This is due to the realignments of the highway over the years, which has rerouted and straightened many sections. The highway opened to the public in 1948. Once legendary for being a rough, challenging drive, the highway is now paved over its entire length. Its component highways are British Columbia Highway 97, Yukon Highway 1, and Alaska Route 2.

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<span class="mw-page-title-main">Alligator Lake volcanic complex</span>

The Alligator Lake volcanic complex is a group of basaltic cinder cones and lava flows in south central Yukon. The upper part of the Alligator Lake volcanic complex consists of two well-preserved cinder cones capping a small shield volcano. They probably post-date the local Holocene glaciation. Lava flows from both cinder cones traveled to the north and were erupted simultaneously. Their compositions range from alkali olivine basalt to basanitic. Lava flows from the northeast cone are the largest extending 6 km (4 mi) from the cone and expanding to a width of 10 km (6 mi) at the terminus.

Ibex Mountain is a young cinder cone in the Yukon Territory, Canada, located 33 km southwest of Whitehorse and 12 km southeast of Mount Arkell. It is in a group of basaltic cones and lava flows called Alligator Lake and is in the Northern Cordilleran Volcanic Province. It is believed Ibex Mountain last erupted during the Pleistocene. Ibex Mountain is at the head of the Ibex River, which is southeast of Whitehorse. There is a road that runs close to Ibex Lake on the southeast side of the summit. From there is the hike to the summit of the cone.

<span class="mw-page-title-main">Miles Canyon Basalts</span> Rocks in Yukon, Canada

The Miles Canyon Basalts represent a package of rocks that include various exposures of basaltic lava flows and cones that erupted and flowed across an ancient pre-glacial landscape in south-central Yukon.

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References

  1. Geographic Board of Canada (1899). Annual Report of the Geographic Board of Canada Volumes 1-10. Canada: S.E. Dawson. pp. 14, 16. Retrieved 5 February 2024.
  2. Government of Yukon. "Surficial Geology of Alligator Lake (NTS 105D/6), Yukon (1:50 000 scale) - Open Government Portal". open.canada.ca. Retrieved 2024-02-05.