FORMATION OF A MODERN ICE-PUSH RIDGE BY THERMAL EXPANSION OF LAKE ICE IN SOUTHEASTERN CONNECTICUT.
A modern ice-push ridge on the northwest shore of Gardner Lake in southeastern Connecticut is 0.6-1.2 m high and 1.2-3.1 m wide. In February and March 1967, the positions of survey stakes placed on the lake ice were measured periodically. During the same period, air and ice temperature and solar rad...
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Format: | Text |
Language: | English |
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1969
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Online Access: | http://www.dtic.mil/docs/citations/AD0694373 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0694373 |