Muldrow Glacier

Denali’s surging giant and historic northern climbing route
Muldrow Glacier, Denali National Park
InsideDenali National Park

Overview

Muldrow Glacier pours off the northeastern flank of Denali, a massive, land‑terminating river of ice that ultimately feeds the McKinley River. At about 39 miles long, it’s the park’s heavyweight glacier—remote, rough, and more the realm of climbers and scientists than casual sightseers.

Why it’s different

Muldrow is a surging glacier. Instead of creeping along at a steady pace, it occasionally lurches forward dramatically. A historic surge in 2021 sent the glacier racing—orders of magnitude faster than normal—and left a maze of new crevasses and broken ice. The National Park Service closely documented the event and continues to monitor it as a living laboratory of glacier dynamics.

What you’ll actually see

Don’t expect tidewater calving or roadside ice caves; Denali’s glaciers are inland and end on land. From the park road, you’ll only glimpse the tip. The full sweep—medial and lateral moraines, the Great Icefall above, and the fractured “Hill of Cracks”—is best appreciated on a flightseeing tour or by skilled backcountry travel.

Access and how people experience it

There are no developed trails or facilities here. Reaching the glacier typically involves a serious, permitted backcountry approach from the park’s north side, including river crossings and complex route‑finding beyond places like McGonagall Pass. Mountaineers know Muldrow as part of the historic northern route to Denali’s summit, but post‑surge crevassing has made travel even more committing.

Landscape and features

Expect long ridges of rock (moraines) riding the ice, debris‑covered lower reaches, deep crevasses, and occasional meltwater pools. The glacier is fed from higher icefalls and tributaries, then bends and flows down‑valley toward the McKinley River, constantly reshaping the landscape as it grinds along.

Wildlife context

The ice itself is harsh, but the surrounding tundra and foothills can host caribou, Dall sheep, and birds of prey. Sightings are most likely on the approaches rather than on the glacier proper.

Science and history notes

Surges were recorded in the early 1900s, the 1950s, and again in 2021. During the most recent event, the park used modern mapping techniques to track the glacier’s surface changes and motion. The glacier also holds a notable place in Denali mountaineering history as the classic northern approach.

Planning realities

There are no amenities—no parking, no restrooms, no signage. If your goal is to actually see Muldrow in full, book a flightseeing tour. If you plan to approach on foot, secure the appropriate backcountry permits, be fully self‑sufficient, and prepare for rapidly changing conditions on both tundra and ice.

Pros

  • Longest glacier in the park at roughly 39 miles
  • Rare, dramatic surge behavior documented most recently in 2021
  • Historic northern route for Denali summit attempts

Cons

  • No road access or facilities; true backcountry only
  • Heavily crevassed and hazardous terrain, especially post‑surge
  • Only a small tip is visible from the park road

Tips

  • Book a flightseeing tour if you want meaningful views of the glacier.
  • From the park road, expect to see only the glacier’s distant tip.
  • Backcountry travel here requires permits and advanced route‑finding skills.
  • Crossing the McKinley River can be hazardous; plan conservatively.
  • Post‑2021 surge, crevasse patterns shift—expect routes to change year to year.
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