Phenomenon: Crevasses Are Glaciers’ Hidden Hazards

These gaping glacier cracks are dramatic—and deadly. Here's how they form, plus three safe places to see crevasses up close.

Photo: Ascent Xmedia/Getty Images

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Read more: The Outdoors’ Most Spectacular Natural Phenomena, Explained

Glacier trekking ranks high on the exhilaration scale–but hiking across one of these dynamic ice masses can be as treacherous as it is thrilling. Glaciers act more like fields of moving lava than static blocks of ice, flowing downhill at the geologically rapid rate of tens to even thousands of feet per year. All that motion over rugged mountain terrain causes the ice to split into yawning cracks, called crevasses, that make glacier travel the wilderness equivalent of walking through a minefield. Here’s how and where crevasses form in glaciers on Lower 48 peaks like Rainier, Hood, Olympus, and Adams.

The Basics of Crevasses


The Salmon Glacier outside of Hyder, Alaska demonstrates how crevasses can eventually lead to a complicated pattern. Travel up this glacier is very slow and dangerous due to the many crevasses on the surface. Photo: DCrane08/Getty Images

Crevasses often appear where a glacier scrapes against uneven valley walls or turns a corner. Ice flows slowly at the edges but moves progressively faster toward the center, a pattern that causes cracks to form in the brittle, uppermost layers of the glacier, pointing upstream. These cracks sometimes rotate as the entire ice mass shifts, leading to a complicated pattern of new fractures crisscrossing with old ones.


Mt. Everest’s deadly Khumbu Icefall. Photo: Jason Maehl/Getty Images

Dramatic jumbles of crevassed ice that resemble frozen waterfalls often form where small, higher-elevation tributary glaciers flow into larger ice masses below (just as small streams feed into larger ones). At those junctures, the steep step between the tributary and the main glacier leads to high stress on the ice, creating a crevassed drop-off like Mt. Everest’s infamous Khumbu Icefall or Yosemite’s once-frozen Bridal Veil Falls.


A close-up look at a crevasse. Photo: Anke Wittkowski/Getty Images

If a glacier is flowing quickly enough (it’s thick and heavy, or moving down a particularly steep slope), crevasses can form where sections of ice stretch apart because the ice lower down is moving faster than the ice above it. Once a crack appears, the motion and weight of the glacier act together to pull these starter fissures into gaping chasms.


Crevasses can often appear fairly harmless from the surface, but may actually go down hundreds or thousands of feet.
Crevasses can often appear fairly harmless from the surface, but may actually go down hundreds or thousands of feet. Photo: Jan-Stefan Knick/Getty Images

Cracks usually start at the surface of the ice and work their way down, widening to anywhere from a few inches to thousands of feet. Theoretically, the weight of the deep ice limits crevasse depth to about 100 feet–farther down, there is enough compressive force on the ice to prevent cracks from opening. But if water (which is denser than ice) gets into a growing crevasse, it acts like a wedge to carve an extra-deep fracture–sometimes thousands of feet through the entire glacier.

Novice Ice Hikes

Not all glacial hikes are treacherous. Here, a woman hikes on the Grinnell Glacier Trail where she will likely see some crevasses.
Not all glacial hikes are treacherous. Here, a woman hikes on the Grinnell Glacier Trail. Photo: Jordan Siemens/Getty Images

Get an up-close look at a crevasse–mountaineering skills not required–on the Eliot Glacier View Trail (Mt. Hood National Forest, Oregon), the Grinnell Glacier Trail (Glacier National Park, Montana), and the Root Glacier Trail (Wrangell-St. Elias National Park, Alaska).

Snow Bridges

Trusting snow bridges and the edges of crevasses is something reserved for experienced mountaineers
Trusting snow bridges and crevasse edges is something reserved for experienced mountaineers. Photo: Alex Ratson/ Getty Images

“Bridges” of ice and snow often cover crevasses, providing safe passage for mountaineers early in the season when the formations are thick. But warming weather makes snow bridges unstable and hazardous–especially in the afternoon when sunlight softens the snow. In early spring’s melting season, snow bridges are most common in the glacier’s accumulation zone, where new snow falls faster than older snow melts.

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