• Winter in the Wrangells

    Wrangell - St Elias

    National Park & Preserve Alaska

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  • Wrangell-St. Elias Visitor Center to close for the winter on Nov. 1st.

    Wrangell-St. Elias's main visitor center, located near Copper Center, AK, will be closed for the winter starting November 1. The visitor center will re-open on April 1, 2015.

Park Facts

Wrangell-St. Elias National Park and Preserve contains one of the largest concentrations of Dall sheep in North America. Other species of large mammals living here include mountain goats, caribou, moose, brown/grizzly bear, black bear and bison. Some of the smaller mammals are lynx, wolverine, river otter, marten, fox, wolves, marmots, beaver, porcupine, snowshoe hare, and other small furbearers, rodents, and even a species of bat!

The Copper River Basin and Yakutat Bay areas are along major migratory routes for numerous bird species. Wetland areas provide seasonal homes for nesting geese, trumpeter swans, ducks and other waterfowl. Golden and bald eagles, peregrine falcons and gyrfalcons, pine grosbeaks, black-capped chickadees and several woodpeckers nest within the park. Year-round residents include willow ptarmigan, spruce grouse, ravens, goshawks and great horned owls.

Park waters are spawning areas for three types of salmon (red, silver and king) along with rainbow trout, lake trout, grayling, steelhead, Dolly Varden and burbot.

The diversity the of park's landscape and the complex geologic and ecological history are reflected in the composition of the vegetation and flora of the park. Spanning Wrangell-St. Elias National Park and Preserve are four mountain systems, eight physiographic provinces, three climate zones and seven ecoregions.

There are numerous unusual plant communities in the park associated with unique landforms and lithologies such as sand dunes, mud volcanoes, volcanic ash, limestone and south facing bluffs. A recent inventory of the park's flora indicates that there are 936 vascular plant species. The sedge family has the highest number of species (111) in the park, followed by the grass family (79), the sunflower family (86) and the mustard family (74). There are 13 tree species, 27 willow species and 43 introduced species in the park. The park also has 327 documented non-vascular plants including 31 species of liverwort, 131 species of lichen and 165 species of moss.

Forest types range from coastal Sitka spruce on the Malaspina Forelands to the black and white spruce taiga in the interior. Wetlands are common along the coast and in the interior. River corridors and upland areas support more productive forests of white spruce with paper birch and quaking aspen. Sub-alpine zones have a higher coverage of tundra shrubs such as blueberry, dwarf birch and shrub cinquefoil. Vegetation varies in alpine areas depending on whether the site is in a snowbed area, a poorly drained area or a dry site. The vegetation above tree line is composed mostly of dwarf heath shrubs, forbs, sedges, and grasses.

Selected statistics:

  • Largest national park in the United States.
  • Designated, with Glacier Bay National Park and the Canadian neighbors Kluane National Park Reserve, Tatshenshini-Alsek National Park, a World Heritage Site; making the world's largest international protected wilderness.
  • Four major mountain ranges: Wrangell, St. Elias, Chugach, and the eastern part of the Alaskan Range.
  • Mt. St. Elias, at 18,008 feet, is the second highest peak in the United States.
  • Nine of the 16 highest peaks in the United States.
  • Mt. Wrangell, at 14,163 feet, is one of the largest active volcanoes in North America.
  • Nabesna Glacier, at approximately 80 miles, is the longest non-polar valley glacier.
  • Malaspina Glacier, larger than the state of Rhode Island, is the largest non-polar piedmont glacier in North America.
  • The Hubbard Glacier is one of the largest and most active tidewater glaciers in North America.

Did You Know?

Iceworms exist in Alaskan glaciers

No hoax, iceworms do exist. These small, threadlike, segmented black worms, usually less than one inch long, thrive in temperatures just above freezing. Observers as far back as the 1880’s reported the tiny worms on the surface of glaciers. When sunlight strikes, ice worms burrow into the ice.