Ice segregation results in rock fracture and frost heave.
2.
The basin will become deeper as it continues to be eroded by ice segregation and abrasion.
3.
The process of nivation follows, whereby a hollow in a slope may be enlarged by ice segregation weathering and glacial erosion.
4.
However the majority of frost heaving and of bedrock fracture results instead from ice segregation in ice lenses in the near-surface frozen regions.
5.
Should ice segregation, plucking and abrasion continue, the dimensions of the cirque will increase, but the proportion of the landform would remain roughly the same.
6.
The temperature within the bergschrund changes very little, however, studies have shown that ice segregation ( frost shattering ) may happen with only small changes in temperature.
7.
However the bulk of recent literature demonstrates that that ice segregation is capable of providing quantitative models for common phenomena while the traditional, simplistic volumetric expansion does not.
8.
Ice segregation erodes the rock vertical rock face and causes it to disintegrate, which may result in an avalanche bringing down more snow and rock to add to the growing glacier.
9.
As a result, when conditions exist for ice segregation ( ice lens formation ) water flows toward the segregated ice and freezes on the surface, thickening the segregated ice layer.
10.
A key phenomenon for understanding ice segregation in soil or porous rock ( also referred to as an ice lens due to its shape ) is premelting, which is the development of a liquid film on surfaces and interfaces at temperatures significantly below their bulk melting temperature.
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