crevasses are formed by glaciers creating pressure on the land.
A crevasse.
A crevasse forms as a result of erosion. It is a deep crack or fissure in a glacier caused by movement and stress, rather than a location of deposition of sediment.
A crevasse in a glacier is a deep crack or fissure that forms in the ice due to stress and movement. It is typically caused by the glacier's flow over uneven terrain or changes in speed. Crevasse formation can also be influenced by factors such as temperature changes and the glacier's internal structure.
The answer is Crevasse.
A deep wedge shaped opening in a moving mass of ice is called a crevasse. This feature forms as a result of stress and movement within the glacier, and can be dangerous to traverse as they can be hidden beneath a thin snow layer.
Into the Crevasse was created on 2009-10-22.
Sauvé's Crevasse happened in 1849.
the earthquake resulted a huge crevasse in the small town
Bonnet Carré Crevasse happened in 1871.
What best to describes a crevasse is a crack in the topmost section of a glacier.
The zone that seals the base of a crevasse is known as the "crevasse floor" or "crevasse base." This area is typically composed of dense, compacted ice that has formed as a result of pressure and accumulation. The crevasse floor can be smooth or rough, depending on the ice's characteristics and the dynamics of the surrounding glacier. It plays a crucial role in the stability and evolution of the crevasse as the glacier continues to move.
Bergschrund: A crevasse that forms at the top of a glacier where it separates from the rock or ice below. Transverse crevasse: Formed perpendicular to the flow of the glacier, typically due to the glacier bending or encountering obstructions. Marginal crevasse: Found at the edges or margins of a glacier and are often caused by variations in stress and strain as the glacier moves.