An irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depresson on a retreating glacier, and is then deposited with further melting.[Wikipedia]
A sand and gravel deposit formed by running water on stagnant or moving-glacier ice. Crevasse fills or crevasse ridges form within crevasses. Kames form on flat or inclined ice, in holes, or in cracks
. A kame terrace forms between the glacier and the adjacent land surface. Shapes include hills, mounds, knobs, hummocks, or ridges.
A steep conical hill composed of glaciofluvial sediments. This feature develops when glacial crevasses and depressions in stagnant glacial ice are filled with sand and gravel deposits from sediment lo
aded meltwater.
Valley-side terrace or bench formed by the deposition of fluvial or lake sediment along the margin of a glacier. The terrace is left stranded on the hillside after the glacier has receded.
A long flat ridge composed of glaciofluvial sediment. This feature forms along the margin of a valley glacier where the glacial ice meets the valley's slope. Sediment is deposited by laterally flowing
meltwater streams.