A ridge of till deposited at the margin of a glacier during a period of temporary stability in its general recession.
A ridge of glacial sediment that forms when the terminus of a retreating glacier remains at or near a single location for a period of time sufficient for a cross-valley accumulation to form.
A moraine that formed where the ice margin stabilizes during a general retreat of the glacier See: moraine
A moraine, composed of concentric arc-shaped ridges, left behind as a glacier recedes
An end moraine, built during a temporary but significant halt in the final retreat of a glacier.
The end moraine that forms when a glacier stalls for a while as it recedes.
a terminal moraine formed when a receding glacier halts temporarily. [AHDOS