Quaternary geology of large-scale superficial features at Ashford Hill, Hampshire, England
A diapiric mass of chalk rises some 35 m through Palaeogene strata beneath the floodplain of the Baughurst Stream, a tributary of the River Kennet. It is argued that this chalk anomaly was initially formed by the rise of Upper Chalk during a period (s) of permafrost degradation. This ultimately pier...
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University of Reading
1985
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.442412 |