Observations on a Collapsing Kame Terrace In Glacier Bay National Monument, South-Eastern Alaska
Keyword(s):
Abstract Detailed observations on a collapsing kame terrace indicate that the terrace is being reshaped by: slumping and sliding of debris into depressions, melt-water erosion on the side of the terrace, debris flows in the gullies, and stagnant-ice bursts, a phenomenon analogous to a glacier burst except in the mode of formation of the water. Temperatures in the gravel over the ice, where the gravel is about 4 m thick, indicate that the rate of melting of the upper surface of the ice due to conduction may be as high as 24 cm year−1. Highest temperatures in the gravel were recorded during periods of heavy rainfall.
Keyword(s):
1939 ◽
Vol 66
(7)
◽
pp. 453
◽
1982 ◽
Vol 28
(100)
◽
pp. 483-497
◽
Keyword(s):
2017 ◽
pp. 19-27
Keyword(s):
1974 ◽