Kennicott Glacier

Overview

About Kennicott Glacier

Kennicott Glacier is the big, “dirty-looking” river of ice you see spilling toward the Kennecott valley—dirty because its surface is mantled with rocks and soil carried by tributary glaciers. Those debris bands merge into striking stripes (medial moraines) you can see from near town. Beneath that rubble, the ice is thick and powerful—and changing fast. Studies show the glacier lowered by roughly 115–330 feet between 1957 and 2007 and is still thinning by about 6–23 feet per year in many places.

It’s also impressively long—about 26 miles—fed high on the flanks of Mount Blackburn before merging with Gates and Root Glaciers and sliding past the historic Kennecott mill townsite. The glacier ends in a broad, rock-armored snout with meltwater streams that become the Kennicott River.

Why stop

Reachable on foot via the Root Glacier Trail from Kennecott (about 1.5 miles to the ice)
Photogenic debris-striped ice with broad medial moraines and blue pools/streams

Heads up

Real glacier travel demands proper gear/skills or a guide; debris-covered ice is slick and ice caves are unstable
Access logistics: park at McCarthy Footbridge and shuttle to Kennecott; services are limited and seasonal

Few big valley glaciers are this easy to approach. The debris mantle creates dramatic patterns you can appreciate from overlooks, trails, and the townsite—while the Root Glacier gives confident hikers a practical, close-up way to experience the ice.

Parkwolf’s verdictWhy It’s Special

Map

Where it is

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Full map

SightKennicott Glacier61.60027, -143.06972

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Local know-how

Tips for visiting Kennicott Glacier

Park at the McCarthy Footbridge, walk across, and ride the shuttle to Kennecott—build in extra time.
Bring traction (crampons or microspikes) for glacier ice or go with a guide.
Avoid ice caves unless properly trained and equipped; they can collapse at any time.
After rain, debris-covered ice becomes extremely slick—adjust plans accordingly.
No fuel or reliable cell service in McCarthy/Kennecott; stock up and confirm seasonal restrooms.

Plan your stop

Before you go

Best time to visit

Summer is prime for on-foot glacier experiences and when most facilities operate. After rain, both clean and debris-covered ice become treacherously slick. Expect high, silty meltwater flows in summer; winter flows typically drop and clear, but on-ice travel then demands winter skills and gear.

Access & Logistics

Most visitors experience Kennicott via its neighbor, Root Glacier. Park near the McCarthy Footbridge at the end of McCarthy Road, cross on foot, and take the local shuttle to Kennecott (no public vehicle access over the footbridge). From Kennecott, it’s about a 1.5-mile walk on the Root Glacier Trail to step onto the ice.

Seasonal basics cluster around Kennecott: vault toilets are typically available at the Kennecott Visitor Center area, the General Store area, and the Root Glacier Trailhead in the main summer season. Expect very limited cell coverage, no public park WiFi, and no fuel in McCarthy/Kennecott—top off well before turning down the Edgerton Highway. Food and store hours are seasonal.

A park ranger sits on a dash-mounted phone, talking, as Parkwolf’s Tour Guide plays “Army Cutworm Moths: A Grizzly Bear Buffet” on Grand Loop Road below Dunraven Pass in Yellowstone — Parkwolf Tour GuideThe highest, rockiest slopes around here are a summer buffet for grizzly bears.

Wrangell-St. Elias Tour Guide

Your drive to Kennicott Glacier, narrated.

Parkwolf is a GPS audio tour guide for Wrangell-St. Elias National Park. As you drive, it chimes in with what’s ahead: hidden gems, upcoming stops, history, geology, and wildlife, right through your car’s speakers.

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98 audio storiesacross Wrangell-St. Elias’s roads, triggered by GPS as you drive
Wildlife heatmapsfor Grizzly Bear, Moose, Humpback Whale, and 13 more
Works offlinemaps, 13 trails, 28 places, and audio download before you lose signal
CarPlay readysimple controls built for the drive

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Guide

More about Kennicott Glacier

What You’ll SeeDebris stripes and towering moraines that tell the story of many tributary ice flows.

Debris stripes and towering moraines that tell the story of many tributary ice flows.
On guided glacier walks, expect sculpted ice, vivid blue pools, and surface streams.
Big-picture perspective: flightseeing shows just how ice-dominated this landscape is (about 35% of the park is glaciated).

Safety EssentialsGlacier travel is serious.

Glacier travel is serious. Crampons/traction, appropriate boots, and know-how are musts; many visitors hire a local guide. Even rubble-covered ice gets extremely slick when wet. Beautiful ice caves can form—and collapse without warning—so don’t enter them without proper training, equipment, and current local knowledge. Typical hazards here include swift glacial rivers, rockfall, mudslides, avalanches, bugs, bears, and volatile weather. Speak with rangers about conditions and your plans. In glaciated regions, sudden outburst floods can occur—stay alert around proglacial lakes and streams and verify conditions before committing to crossings.

Wildlife

Wildlife in Wrangell-St. Elias

All Wrangell-St. Elias wildlife maps

112 sightingsGrizzly BearMost seen around 9 PMSighting map

63 sightingsMooseMost seen around 8 PMSighting map

21 sightingsHumpback WhaleMost seen around 1 PMSighting map

46 sightingsSteller Sea LionMost seen around 11 AMSighting map

37 sightingsBlack BearMost seen around 8 PMSighting map

48 sightingsBald EagleMost seen around 5 PMSighting map

Sighting maps show where each species has been reported across Wrangell-St. Elias. Wildlife moves, so no sighting is guaranteed.