The nature of Late Flandrian alluviation in the Humberhead levels.
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Colleges, School and Institutes
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
|Number of pages||13|
|Journal||East Midland Geographer|
|Publication status||Published - 1 Jan 1985|