
Terminal Moraine: The end moraine marking the farthest advance of a glacier.

Lateral Moraine: A ridge of till along the sides of a valley glacier composed primarily of debris that fell to the glacier from the valley walls.

Medial Moraine: A ridge of till formed when lateral moraines from two coalescing alpine glaciers join.

Drumlin: A streamlined symmetrical hill composed of glacial till. The steep side of the hill faces the direction from which the ice advanced.

Kettle: Depressions created when blocks of ice become lodged in glacial deposits and subsequently melt.

Esker: Sinuous ridge composed largely of sand and gravel deposited by a stream flowing in a tunnel beneath a glacier near its terminus.

Proglacial lake: A lake formed from glacier runoff, filling a depression caused by the glacier.