A glaciated valley or fjord (q.v.), often characterised by steep sides and a flat bottom, with multiple basins, resulting primarily from erosion by strongly channelled ice.
Valley that was influenced by the presence of glaciers. The cross-section of such valleys tends to be U-shaped because of glacial erosion. Similar to glacial trough.
1.Alteration of any part of the earth's surface by passage of a glacier, chiefly by glacial erosion or deposition; distinguish from glacierization. 2.As used in many texts, particularly with respect t
o the ice ages, same as glacierization, for example, "Pleistocene glaciation." 3.The transformation of cloud particles from supercooled water drops to ice crystals. Thus, a cumulonimbus cloud is said to have a glaciated upper portion.
In any small glacierized region, the average of the elevations of the highest unglacierized peak and the lowest glacierized peak. The glaciation level has been used as a regional-scale proxy for the s
teady-state ELA, although a correction is required for this purpose because the glaciation level is known to be systematically higher by about 200 m. See mid-range altitude.