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Wrangell Mountains

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Wrangell Mountains
NameWrangell Mountains
Photo captionView of the Wrangell Mountains from the Glenn Highway.
CountryUnited States
StateAlaska
ParentWrangell Volcanic Field
BorderSaint Elias Mountains, Alaska Range
HighestMount Blackburn
Elevation ft16390
Coordinates61, 44, N, 143...
GeologyAndesite, Dacite, Basalt
PeriodNeogene to Quaternary

Wrangell Mountains. The Wrangell Mountains are a prominent and rugged mountain range located in southeastern Alaska, forming a significant part of the larger Pacific Coast Ranges. This range is renowned for its extensive volcanic activity, containing some of the largest andesitic stratovolcanoes in North America, and is largely encompassed within the expansive Wrangell-St. Elias National Park and Preserve. Its dramatic landscapes, shaped by immense glaciers and volcanic forces, represent a critical component of the Saint Elias Mountains tectonic complex and a vital habitat for subarctic wildlife.

Geography and Geology

The range is situated east of the Copper River and borders the Saint Elias Mountains to the south and the Alaska Range to the north, forming a distinct volcanic province. Geologically, the mountains are part of the Wrangell Volcanic Field, a massive volcanic arc that has been active since Neogene times, driven by the subduction of the Pacific Plate beneath the North American Plate. The predominant rock types are andesite and dacite, with some basalt, resulting in the classic conical shapes of its major peaks. This region is also characterized by significant seismic activity linked to the complex interactions along the Fairweather Fault and the broader Denali Fault system, contributing to ongoing uplift and erosion.

Major Peaks and Glaciers

The skyline is dominated by massive, ice-clad volcanoes, with the highest summit being Mount Blackburn, the fifth-highest peak in the United States. Other major volcanic peaks include the towering Mount Sanford, the active Mount Wrangell, and the distinctive Mount Drum. These volcanoes are heavily mantled by some of the continent's largest glaciers, such as the Nabesna Glacier and the Kennicott Glacier, which flow from the central icefields. The Hubbard Glacier, originating in the Saint Elias Mountains, also drains parts of the range, while the immense Bagley Icefield connects the Wrangells to the neighboring coastal ranges, creating a vast interconnected system of ice.

Climate and Ecology

The climate is predominantly continental in the interior valleys but transitions to a maritime influence on the southern slopes, resulting in heavy precipitation that feeds the extensive glaciers. This creates a sharp ecological gradient, with interior areas featuring taiga forests of white spruce and black spruce, while the wetter southern flanks support dense temperate rainforests of Sitka spruce and western hemlock. The region provides crucial habitat for large mammals like Dall sheep, caribou of the Nelchina Herd, grizzly bear, and gray wolf, alongside significant populations of bald eagle and gyrfalcon. The Copper River delta, influenced by the range's runoff, is a globally important site for migratory birds, including the Arctic tern.

Human History and Exploration

The area has been inhabited for millennia by Ahtna and Upper Tanana Athabaskan peoples, who utilized the Copper River corridor for trade and subsistence. Russian exploration began in the 18th century, with figures like Mikhail Tebenkov mapping the coastline, but significant inland exploration occurred during the late 19th-century Klondike Gold Rush and the subsequent construction of the Copper River and Northwestern Railway. Prospectors and geologists, including Alfred Hulse Brooks of the United States Geological Survey, conducted early surveys. The discovery of copper at the Kennecott Mines led to a major mining boom in the early 20th century, overseen by the Guggenheim family's Alaska Syndicate, which left a lasting historical imprint.

Recreation and Conservation

Today, the range forms the heart of the Wrangell-St. Elias National Park and Preserve, a UNESCO World Heritage Site and the largest national park in the United States. It offers unparalleled opportunities for mountaineering on peaks like Mount Blackburn, backpacking, rafting on the Kennecott River, and flightseeing. Historic sites such as the Kennecott Mines National Historic Landmark draw visitors, while the remote McCarthy Road provides access to the park's interior. Conservation efforts are managed by the National Park Service, focusing on preserving the vast wilderness, glacial systems, and wildlife corridors from potential impacts of climate change and external development pressures, maintaining its status as a premier destination for wilderness adventure.

Category:Mountain ranges of Alaska Category:Volcanic fields of the United States Category:Wrangell-St. Elias National Park and Preserve