a depositional feature whose form is independent of topography and is constructed by the accumulation of drift
An accumulation of earth, STONES, etc , deposited by a glacier, usually in the form of a mound, ridge or other prominence on the terrain
(More-rain) n an accumulation of boulders, stones, or other debris carried and deposited by a glacier
A mound, ridge, or other distint accumulation of unsorted, unstratified glacial drift, deposited chiefly by direct action of glacier ice The geomorphic name for a landform composed mainly of till that has been deposited by either a living or extinct glacier
A single, large mass of glacial till that accumulates, typically at the edge of a glacier
Deposits of rocks, boulders, gravel and sand (called glacial drift) left behind by glaciers as they melted Terminal moraines are at the end of a glacier
a mass of earth or pieces of rock moved along by a glacier and left in a line at the bottom of it. Accumulation of rock debris (till) carried or deposited by a glacier. The material may range in size from blocks or boulders to sand and clay, is unstratified when dropped by the glacier, and shows no sorting or bedding. Several kinds of moraines are recognized, depending on how they are deposited by the glacier; these include lateral moraines along the margins of the glacier and terminal moraines at its leading edge
A ridge of rubbly stones, boulders and fine clay left behind when a glacier or ice sheet melts
The rocks and soil carried and deposited by a glacier An "end moraine," either a ridge or low hill running perpendicular to the direction of ice movement, forms at the end of a glacier when the ice is melting