The nature of Late Flandrian alluviation in the Humberhead levels.

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The changing character of floodplain deposits in the Humberhead Levels and adjacent areas is discussed with reference to palaeo-ecological evidence, principally fossil insects, from Sandtoft, Humberside. An anthropogenic origin for a major change in the late Roman period is discussed and a flow diagram presenting the evidence in its wider context is included. -Authors


Original languageEnglish
Pages (from-to)239-251
Number of pages13
JournalEast Midland Geographer
Issue number8
Publication statusPublished - 1 Jan 1985

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