A thin, almost knife-like, ridge of rock which is typically formed when two glaciers erode parallel U-shaped valleys.
An amphitheatre-like valley head, formed at the head of a valley glacier by erosion.
A long winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions.
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]
Any glacially formed accumulation of unconsolidated glacial debris (soil and rock) which can occur in currently glaciated and formerly glaciated regions.
A fan-shaped body of sediments deposited by braided streams from a melting glacier. Sediment locked within the ice of the glacier gets transported by the streams of meltwater and deposits on the outwash plain at the terminus of the glacier.
Rock glaciers are distinctive geomorphological landforms of blocky detritus which may extend outward and downslope from talus cones or from glaciers or the terminal moraines of glaciers. [Wikipedia]
A glacial outwash plain formed of sediments deposited by meltwater at the terminus of a glacier.
An extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place depositing the sediments it carried.
A land surface characterised by very irregular surfaces of marshy hollows and small hummocks formed as ice-rich permafrost thaws.