Geomorphological characterisation and interpretation of a mid-latitude glacier-like form Icarus, 211 2025

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Glaciers are large masses of ice on land that form in places where more snow accumulates in a year than melts. As they slowly move across the land, they erode large amounts of rock and leave distinct depositional features behind.
A glacier is a large, perennial accumulation of crystalline ice, snow, rock, sediment, and often liquid water that originates on land and moves down slope under the influence of its own weight and gravity.
Glacial geomorphology is the scientific study of the processes, landscapes, and landforms produced by ice sheets, valley glaciers, and other ice masses on the surface of the Earth. These processes include understanding how ice masses move, and how glacial ice erodes, transports, and deposits sediment.
Three conditions are necessary to form a glacier: (1) Cold local climate (polar latitudes or high elevation). (2) snow must be abundant; more snow must fall than melts, and (3) snow must not be removed by avalanches or wind.
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