Cromer Forest Bed
| Cromer Forest-bed Formation | |
|---|---|
Ma | |
.JPG) Cromer Forest-bed Formation exposed at the base of the West Runton Cliffs | |
| Type | Geological formation |
| Unit of | Dunwich Group |
| Sub-units | Sheringham Member, Runton Member, West Runton Member, and Bacton Member |
| Underlies | Middle Pleistocene glacial deposits |
| Overlies | Wroxham Crag Formation or unconformity with Chalk Group |
| Thickness | 6-to-8-metre (20 to 26 ft) |
| Lithology | |
| Primary | sands and silts |
| Other | peat, mud, silty marl |
| Location | |
| Coordinates | 52°56′28″N 1°15′11″E / 52.941°N 1.253°E |
| Region |  Norfolk |
| Country |  England |
| Type section | |
| Named for | Cromer |
| Named by | Clement Reid |
| Location | The coast of North Norfolk from Weybourne to Happisburgh |
| Year defined | 1882 |
| Country | England |
The Cromer Forest-bed Formation, sometimes known as the Cromer Forest Bed, is a geological formation in Norfolk, England. It consists of river gravels, estuary and floodplain sediments predominantly silt, sand, and muds as well as peat along the coast of northern Norfolk.[1] It is the type locality for the Cromerian Stage of the Pleistocene between 0.8 and 0.5 million years ago.[2] The deposit itself range varies in age from about 0.8 to 0.5 million years ago. It is about 6-to-8-metre (20 to 26 ft) thick and is exposed in cliff section near the town of West Runton.
Paleontology and Paleobotany
For over a century this formation, named after the local town of Cromer, has been famous for its assemblage of fossil mammal remains, containing the diverse remains of numerous taxa, including deer,[3] carnivorans[4] and birds.[5] Although most of the forest bed is now obscured by coastal defence, the Cromer Forest-bed Formation continues to be eroded and is rich in fossils including the skeletal remains of the West Runton Mammoth which was discovered in 1990.[6][7][8][9]
Archaeology
The oldest human footprints outside Africa, the Happisburgh footprints as well as handaxes and bison bones with cut marks were also found in layers considered to belong to this deposit near the town of Happisburgh.[10]
See also
References
- ^ "Cromer Forest-bed Formation". The BGS Lexicon of Named Rock Units. British Geological Survey.
- ISBN 978-0-00-815035-8.
- .
- .
- ^ Harrison, C. J. O. (May 1979). "Birds of the Cromer Forest Bed Series of the East Anglian Pleistocene" (PDF). Transactions of the Norfolk & Norwich Naturalists' Society. 24: 277–287.
- ^ "Clues of Britain's First Humans (Published 2010)". The New York Times. Archived from the original on 30 May 2023.
- ^ "First humans arrived in Britain 250,000 years earlier than thought". The Guardian. 7 July 2010. Archived from the original on 22 June 2023.
- ^ Royal Anthropological Institute of Great Britain and Ireland (1931)
- .
- PMID 24516637.
Further reading
- Bowen, D.Q., 1978, Quaternary geology: a stratigraphic framework for multidisciplinary work. Pergamon Press, Oxford, United Kingdom. 221 pp. ISBN 978-0-08-020409-3
- West, R.G., 1980, The pre-glacial Pleistocene of the Norfolk and Suffolk Coasts Cambridge University Press. ISBN 0-521-21962-0
- Ehlers, J., P. L. Gibbard, and J. Rose, eds., 1991, Glacial deposits in Great Britain and Ireland Balkema, Rotterdam. 580 pp ISBN 978-90-6191-875-2
- Mangerud, J., J. Ehlers, and P. Gibbard, 2004, Quaternary Glaciations: Extent and Chronology 1: Part I Europe, Elsevier, Amsterdam. ISBN 0-444-51462-7
- Sibrava, V., Bowen, D.Q, and Richmond, G.M., 1986, Quaternary Glaciations in the Northern Hemisphere, Quaternary Science Reviews, vol. 5, pp. 1–514.
External links
Gibbard, P.L., S. Boreham, K.M. Cohen and A. Moscariello, 2007, Global correlation tables for the Quaternary, Subcommission on Quaternary Stratigraphy, Department of Geography, University of Cambridge, Cambridge, England.
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