Lingon Mountain is a 4,098-foot (1,249 m) elevation mountain summit located in the Chugach Mountains, in Anchorage Municipality in the U.S. state of Alaska. The peak is situated in Chugach National Forest, between the Glacier Creek and Twentymile River valleys, 36 mi (58 km) southeast of downtown Anchorage, and 5 mi (8 km) east of the Alyeska Resort and Girdwood areas. Precipitation runoff from the peak drains into Turnagain Arm. This mountain's unofficial name refers to the lingonberry. Other berry-theme peaks nearby include Highbush Peak, Lowbush Peak, Nagoon Mountain, Blueberry Hill, and Bearberry Point.[1]

Lingon Mountain
Lingon Mountain, west aspect
Highest point
Elevation4,098 ft (1,249 m)[1]
Prominence941 ft (287 m)[2]
Parent peakHighbush Peak[2]
Isolation0.99 mi (1.59 km)[2]
Coordinates60°57′05″N 148°58′24″W / 60.95139°N 148.97333°W / 60.95139; -148.97333[1]
Geography
Lingon Mountain is located in Alaska
Lingon Mountain
Lingon Mountain
Location in Alaska
Map
Interactive map of Lingon Mountain
LocationChugach National Forest
Anchorage Municipality, Alaska
United States
Parent rangeChugach Mountains
Topo mapUSGS Seward D-6

Climate

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Based on the Köppen climate classification, Lingon Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers.[3] Weather systems coming off the Gulf of Alaska are forced upwards by the Chugach Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports a small unnamed glacier on its south slope. The months May through June offer the most favorable weather for climbing or viewing.

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See also

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References

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  1. ^ a b c "Lingon Mountain, Alaska". Peakbagger.com. Retrieved 2020-04-18.
  2. ^ a b c ""Lingon Mountain" - 4,097' Alaska". listsofjohn.com. Retrieved 2020-04-18.
  3. ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.
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