Abstract
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 language | English |
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Pages (from-to) | 239-251 |
Number of pages | 13 |
Journal | East Midland Geographer |
Volume | 8 |
Issue number | 8 |
Publication status | Published - 1 Jan 1985 |
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)