V-shaped valleys, waterfalls, meanders, oxbow lakes, and deltas.
In high altitudes and latitudes, glaciers act as powerful erosional agents. Singh describes cirques, arêtes, U-shaped valleys, and fjords as classic glacial erosional forms, while moraines, drumlins, and eskers represent deposition. The periglacial realm (cold but non-glaciated) produces unique features like patterned ground, pingos, and solifluction lobes—critical for understanding high-altitude regions like the Himalayas and Tibet.
GROUP STRENGTH