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Glaciers move by extrusion flow. This involves two main processes; internal deformation and basal sliding.

Internal Deformation

Under the immense weight of overlying ice, individual ice crystals align into layers and slide over each other. (Much like the property of metal ions which leads to the characteristic of maleability).

Basal sliding

Meltwater (from pressure melting) lubricates the base of the glacier, which slides over the bedrock under the influence of gravity.

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