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The Denali Wilderness is a wilderness area within Denali National Park that protects the higher elevations of the central Alaska Range, including Denali. The wilderness comprises about one-third of the current national park and preserve—2,146,580 acres (3,354 sq mi; 8,687 km 2 ) that correspond with the former park boundaries before 1980.
Mount Johnson is an 8,400+ ft (2,560+ m) mountain summit located in the Alaska Range, in Denali National Park and Preserve, in Alaska, United States.It is situated on the west side of the Ruth Gorge, 15 miles (24 km) southeast of Denali and six miles (9.7 km) south-southwest of The Moose's Tooth.
Mountains in Denali National Park and Preserve are part of the Alaska Range, with several subsidiary ranges included within the overall Alaska Range. Denali (also known as Mount McKinley), is the highest peak in the park and the highest peak in North America at 20,320 feet (6,194 m) [1] [2] The names listed here reflect the official names in the USGS U.S. Board on Geographic Names database.
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Easiest route Trail, scrambling Mount Healy , also known in Denaʼina language as Dlel Neelghu Nodaadlghunee (meaning "mountains that are joined together"), is a 5,716-foot (1,742 meter) elevation mountain summit located in the Alaska Range , in Denali National Park and Preserve , in Alaska, United States .
Denali State Park is located in southern Alaska on the southeastern border of the much larger Denali National Park and Preserve, formerly known as Mt. McKinley National Park. It is situated between Fairbanks and Anchorage along George Parks Highway (Alaska Route 3), which connects the two cities and runs directly through the park. [ 5 ]
Divide Mountain is a 5,195 ft (1,580 m) summit located in Denali National Park and Preserve, in the Alaska Range, in the U.S. state of Alaska. [3] It is a landmark in the Toklat River valley visible to tourists from the park road.
The Polychrome Glaciers are five glaciers in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glaciers originate in parallel glaciated north-trending valleys in the Alaska Range, opposite Polychrome Mountain across Polychrome Pass. [1] [2] [3]
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