Everything about Gates Of The Arctic National Park And Preserve totally explained
Gates of the Arctic National Park and Preserve is one of several large
U.S. National Parks in
Alaska. The park lies just north of, and is entirely within, the
Arctic Circle. The park consists primarily of portions of the
Brooks Range of mountains and covers 13,238 mi² (
39,460 km²), about the same size as
Switzerland. It was first protected as a
U.S. National Monument on
December 1,
1978 before becoming a national park and preserve two years later in
1980 upon passage of the
Alaska National Interest Lands Conservation Act. A large part of the park is preserved as a
wilderness area; some 11,321 mi² (29,322 km²) of wilderness which with the adjoining
Noatak Wilderness Area forms the largest contiguous wilderness in the United States.
The park's name dates to
1929, when wilderness activist
Bob Marshall, exploring the North Fork of the
Koyukuk River, encountered a pair of mountains (Frigid Crags and Boreal Mountain), one on each side of the river. He christened this portal the "Gates of the Arctic."
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Unusual for a U.S. national park, some 1,500 people reside in 10 small communities in the park's "resident subsistence zone" where they rely on park resources for survival.
There are no established roads, trails, visitor facilities, or campgrounds in the park. However, the
Dalton Highway (Alaska State Highway 11) comes within five miles of the park's eastern boundary. The National Park Service maintains a small visitor center in nearby
Coldfoot on the highway.
The geography contains the
arête-peaked Brooks Range and rolling valleys of wild
tundra. Fauna include
moose,
barren-ground grizzlies,
Dall sheep,
black bears,
wolves, and
caribou.
The park contains mountains such as the
Arrigetch Peaks and
Mount Igikpak. The park also features six
Wild and Scenic Rivers:
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