- Sven Lukas
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Ice-cored moraines are ice-marginal landforms that comprise a discrete body of glacier ice buried underneath sediment. These landforms are transitional because any incorporated ice needs to melt out before the final resulting landform, e.g. a stable moraine, is formed.
The term “ice-cored moraine” was introduced into the scientific literature by Østrem (1959, 1965) to describe the frequently observed occurrence of bodies of ice within sediment accumulations at or near ice fronts. Such landforms are widespread in modern glacier forelands and have been investigated in numerous settings over the past five decades.
Usually, ice-cored moraines evolve through a chain of processes involving: (a) the isolation of a body of glacier ice through the establishment of a sediment/debris cover near the margin which, if sufficiently thick ...
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- Lukas, S., 2007. Englacial thrusting and (hummocky) moraine formation: a reply to comments by Graham et al. (2007).Boreas,36, 108–113.
- Lukas, S., Nicholson, L. I., Ross, F. H., and Humlum, O., 2005. Formation, meltout processes and landscape alteration of high-arctic ice-cored moraines - examples from Nordenskiöld Land, central Spitsbergen.Polar Geography,29, 157–187.
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- Schomacker, A., and Kjær, K. H., 2008. Quantification of dead-ice melting in ice-cored moraines at the high-Arctic glacier Holmströmbreen, Svalbard.Boreas,37, 211–225.
- Ice-Cored Moraines
- Reference Work Title
- Encyclopedia of Snow, Ice and Glaciers
- pp 616-619
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- Encyclopedia of Earth Sciences Series
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- Springer Netherlands
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- Springer Science+Business Media B.V.
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