The phenomenon in which meltwater accumulates at the base of a glacier, so that the mass of the glacier slides on a layer of water or on a slurry of water and sediment.
The motion of the basal ice of the glacier relative to the material immediately beneath the glacier.
The process by which a glacier undergoes thawing at its base, producing a film of water along which the glacier then flows. Basal sliding primarily affects glaciers in warm climates or mid-latitude mountain ranges.
The sliding of a glacier over the ground on a layer of water.
The sliding of a glacier over the surface it rests on. Caused by the gradient of the slope and the weight of the glacier's mass.
the sliding of a glacier over bedrock.