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.
Arêtes form when mountains are eroded by ice and glaciation. When two or more corries form back-to-back, the area in between forms a sharp ridge and is called an Arête. Cwm Crib Goch Snowdonia.
(Also called cirque) Armchair-shaped hollow in the mountainside formed by glacial erosion, rotational slip and freeze-thaw weathering. This is where the valley glacier begins. When the ice melts, it can leave a small circular lake called a tarn. Cwm Idwal Snowdonia
A large, relatively flat plain composed of unsorted glacial deposits behind a terminal or end moraine. Low-rolling relief and unclear drainage patterns are characteristic. East Anglia.
area in front of a glacier in which melt water from the glacier has carried & deposited an abundance of sorted material. In front of Athabasca Glacier.
A landform produced by glacial abrasion and plucking that has a shallow slope on one side and a steep slope on the other side. Nant Ffrancon Valley Snowdonia.