(from the article `glacial landform`) ...ice melts away, this ice-contact stratified drift slumps and partially collapses to form stagnant ice deposits. Isolated mounds of bedded sands ... ...debris let down onto the ground surface by the melting glacier. A group of closely associated kames is called a kame field, or kame complex, and ....
Found on
http://www.britannica.com/eb/a-z/k/6
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.
Found on
http://www.physicalgeography.net/physgeoglos/k.html
A deposit, often sloping down-valley more steeply than the valley floor, formed where a glacial stream ran along the glacier margin. The ice-contact margin of the kame terrace is often slumped and mixed with till.
Found on
https://www.encyclo.co.uk/local/20131
Stratified drift deposited between wasting glacier and adjacent valley wall. Stands as a terrace when glacier melts.
Found on
https://www.encyclo.co.uk/local/22327
No exact match found.
