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- Crevasse - Wikipedia
A crevasse is a deep crack that forms in a glacier or ice sheet Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement
- CREVASSE Definition Meaning - Merriam-Webster
Crevasse refers to a deep hole or fissure in a glacier or in the earth In most instances, the word appears with enough context that the depth of the opening is easy enough to figure out, as in "a climber who fell 30 feet into a crevasse "
- Crevasse | Glacial, Ice Shelf, Fracture | Britannica
crevasse, fissure or crack in a glacier resulting from stress produced by movement Crevasses range up to 20 m (65 feet) wide, 45 m (148 feet) deep, and several hundred metres long Most are named according to their positions with respect to the long axis of the glacier
- Crevasse - National Geographic Society
A crevasse is a deep, wedge-shaped opening in a moving mass of ice called a glacier Crevasses usually form in the top 50 meters (160 feet) of a glacier, where the ice is brittle
- Glacier Power: What are Crevasses? - NASA Earthdata
A crevasse is a crack in the surface of a glacier caused by extensive stress within the ice For example, extensive stress can be caused by stretching if the glacier is speeding up as it flows down the valley
- CREVASSE | definition in the Cambridge English Dictionary
When a hole breaks in a levee, it's called a crevasse Or: what happens when you're trying to twist through a crevasse? Note the ski trail at upper left leading up to the crevasse The arduous path up the mountain is marked with gaping crevasses and uprooted trees, tossed down the slope
- What Is a Crevasse and How Do They Form? - Biology Insights
A crevasse is a deep, open crack or fissure that forms within a moving body of ice, such as a glacier, ice cap, or ice sheet These fractures manifest the intense stress and strain the ice mass undergoes as it flows across the landscape
- Crevasses - U. S. National Park Service
A second type of crevasse forms when the ice piles up on itself, crunching and cracking These crevasses form like faults in the Earth's crust, with blocks of ice moving past one another along a crack
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