An examination of subsidence in north-east England due to the dissolution of sub-surface gypsum using the shallow seismic reflection technique
Along a narrow swath from Nottingham through to Hartlepool, broad shallow depressions up to 100m in diameter and, more rarely, scarp-edged subsidence hollows are observed. These topographical features coincide with the sub-crop of the Permian strata beneath the Quaternary deposits and are attributed...
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Durham University
2009
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.492912 |