Morphology and palaeoenvironmental inter
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Jasper Knight
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Article
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1999
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Elsevier Science
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English
β 699 KB
Glacial outwash, deposited during deglaciation of the late Devensian ice sheet, is present as a flat-topped valley fill in the Tempo Valley on the southern flanks of the Fintona Hills, Northern Ireland. Sedimentologically, the outwash comprises well-sorted and interbedded rippled to massive sands wh