Mount Denali (Usa) – Location, History, Facts

Mount Denali is the highest mountain in North America, with a summit elevation of 20,310 feet (6,190 meters).

Mount Denali, Usa.

Country: Usa
Coordinates: 63.0692° N, 151.0064° W

Mount Denali overview

Mount Denali is the highest mountain in North America, with a summit elevation of 20,310 feet (6,190 meters). It is a major glaciated peak located in the north-central interior of the U.S. state of Alaska and serves as a principal reference point for high-latitude alpine research. The mountain’s elevation is established by modern geodetic surveying and is regularly cited in continental-scale geological and cartographic literature.

Mount Denali coordinates

Mount Denali is commonly mapped at approximately 63.0692° N, 151.0064° W, or 63.0692, -151.0064 in decimal degrees.

Degrees: 63.0692° N, 151.0064° W

Decimal: 63.0692, -151.0064

Where Mount Denali is located

Mount Denali is located at approximately 63.0695° N latitude and 151.0074° W longitude in interior Alaska. The peak occupies a central position within the Alaska Range and rises amid a complex of ridges and glacial valleys. Administratively the mountain lies inside the U.S. state of Alaska and on federally managed lands in that region. Significant surrounding physical features include the Kahiltna Glacier on the southwest side, the Muldrow Glacier on the northeast slopes, and the deep Ruth Gorge carved into the massif.

Why Mount Denali is important

Mount Denali matters because it concentrates geological, ecological, and cultural significance into a single prominent massif on the continent. The peak’s high-latitude elevation supports extensive glacier systems that provide important field data for glaciology and permafrost research. Mount Denali also functions as a cultural landmark for Alaska Native communities and as a subject in national conservation and geological studies. Its combination of exceptional relief, concentrated glacial activity, and accessible scientific records distinguishes it from other North American summits.

History of Mount Denali

Geologically, Mount Denali emerged through regional uplift related to plate interactions along the northern margin of the North American Plate, involving pluton emplacement and metamorphism that produced a resistant massif. Successive glacial cycles sculpted steep faces, cirques, and deep valleys, leaving extensive moraines and ice-carved features. Human engagement spans millennia, with Alaska Native groups incorporating the mountain into regional oral traditions and subsistence landscapes. Euro-American mapping, surveying, and scientific interest increased in the late nineteenth and early twentieth centuries, prompting detailed geological investigation and documentation of the massif’s form and context.

Natural features of Mount Denali

Mount Denali’s core consists of hard intrusive and metamorphic rock that forms rugged ridgelines and prominent granite exposures. Large glaciers descend from multiple aspects, feeding extensive moraine fields and displaying icefalls and serac zones on steep slopes. The massif shows sharp arêtes, steep faces, and broad snowfields near the summit, with distinctive contrasts between exposed rock and perennial ice. Mount Denali’s morphology includes extensive glacial troughs and a pronounced northwest face, illustrating the interplay of uplift, rock type, and high-latitude alpine glaciation.

Environment, protection, and monitoring of Mount Denali

The peak lies within Denali National Park and Preserve, which is managed by the U.S. National Park Service and focuses on long-term conservation and scientific monitoring. Surrounding ecosystems range from boreal forest at lower elevations to sparse alpine tundra and specialized high-elevation communities. Conservation priorities include protecting native wildlife populations, preserving glacial and permafrost systems, and maintaining intact ecological processes. Long-term stewardship involves coordinated scientific research, monitoring programs, park management planning, and cooperation with Alaska Native organizations and federal agencies.

Mount Denali facts

The first recorded successful ascent of the summit was completed in 1913 by a party led by Hudson Stuck, with Walter Harper reaching the top first.
Mount Denali's topographic prominence measures approximately 20,156 feet, making it the most prominent peak in North America.
The indigenous Koyukon Athabaskan name Denali translates as "the high one" and reflects the mountain's cultural prominence.
On its northwest side the mountain rises roughly eighteen thousand feet from adjacent lowland glaciers, producing one of Earth's greatest base-to-summit reliefs.
The U.S. federal government officially restored the name Mount Denali to the peak in 2015, replacing its earlier federal designation.

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