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Intertidal Holocene footprints and their archaeological significance

Published online by Cambridge University Press:  02 January 2015

Gordon Roberts ,
Silvia Gonzalez  and
David Huddart
Gordon Roberts
Affiliation:
School of Biological and Earth Sciences, Liverpool John Moores University, Liverpool L3 3AF, England
Silvia Gonzalez
Affiliation:
School of Biological and Earth Sciences, Liverpool John Moores University, Liverpool L3 3AF, England
David Huddart
Affiliation:
School of Education and Community Studies, Liverpool John Moores University, Liverpool L3 3AF, England
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Extract

The Holocene mud-flats of Formby Point, at the mouth of the Mersey estuary in northwest England, have long provided information about their palaeoenvironment. Now they yield a more direct evidence — in the form of preserved footprints — of the people and animals that frequented the foreshore.

Type
Notes
Information
Antiquity , Volume 70 , Issue 269 , September 1996 , pp. 647 - 651
Copyright
Copyright © Antiquity Publications Ltd. 1996

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References

Aldhouse-Green, S. H.R., Whittle, R.A.W., Allen, J.R.L., Caseldine, A.E., Culver, S. J., Day, M. H., Lundquist, J. & Upton, D.. 1992. Prehistoric human footprints from the Severn Estuary at Uskmouth and Magor Pill, Gwent, Wales, Archaeo-logia Cambrensis 141: 14–55.Google Scholar
Bell, M. 1995. Field survey and excavation at Goldcliff, 1994, in Bell, M. (ed.), Archaeology in the Severn Estuary, Annual Report of the Severn Estuary Levels Research Committee: 115–44.Google Scholar
Charteris, J., Wall, J. C. & Nottrodt, J. W.. 1981. Functional reconstruction of gait from the Pliocene hominid footprints at Laetoli, northern Tanzania, Nature 290: 496–8.CrossRefGoogle Scholar
Cowell, R. W. 1991 The prehistory of Merseyside, Journal of the Merseyside Archaeological Society 7: 21–60.Google Scholar
Cowell, R. W., Milles, A. & Roberts, G.. 1993. Prehistoric footprints on Formby Point Beach, Merseyside, North West Wetlands Survey, Annual Report: 43–52.Google Scholar
Gonzalez, S., Huddart, D. & Roberts, G.. In press. Holocene development of the Sefton coast: a multidisciplinary approach to understanding the archaeology, in Sinclair, A. (ed.), Proceedings of the Archaeological Sciences Conference, 1995, Liverpool. Oxford: Oxbow. Archaeological Monograph series.Google Scholar
Gresswell, R. K. 1953. Sandy shores in South Lancashire. Liverpool: Liverpool University Press.Google Scholar
Grieve, D. W. & Gear, R. J.. 1966. The relationships between lenghts of stride, step frequency, time of swing and speed of walking for children and adults, Ergonomics 5: 379–99.Google Scholar
Huddart, D. 1992. Coastal environmental changes and morpho-stratigraphy in southwest Lancashire, England, Proceedings of the Geologists’ Association 103: 217–36.Google Scholar
Neal, A. 1993. Sedimentology and morphodynamics of a Holocene coastal dune barrier complex, northwest England. Unpublished Ph.D thesis. University of Reading.Google Scholar
Parker, W. R. 1975. Sediment mobility and erosion on a multi-barred foreshore (Southwest Lancashire, UK), in Hails, J., J., & Carr, A. (ed), Nearshore sediment dynamics and sedimentation: 151–79. London: Wiley.Google Scholar
Politis, G. G. & Bayon, C.. 1995. Early Holocene human footprints and sea mammals in the tidal zone of the Argentinean seashore, Past 20: 5–6.Google Scholar
Price, N. 1995. Houses and horses in the Swedish Bronze Age: recent excavation in the Malar Valley, Past 20: 10–12.Google Scholar
Pye, K. & Neal, A.. 1993. Stratigraphy and age structure of the Sefton dune complex: preliminary results of field drilling investigations, in Atkinson, D. & Houston, J. (ed.), The sand dunes of the Sefton coast: 41–4. Liverpool: National Museums and Galleries on Merseyside.Google Scholar
Pye, K. & Neal, A.. 1994. Coastal dune erosion at Formby Point, North Merseyside, England: causes and mechanisms, Marine Geology 119: 39–56.Google Scholar
Pye, K., Stokes, S. & Neal, A.. 1995. Revised chronostratigraphy of aeolian sand deposits on the Sefton coast, northwest England, using 14C and optical dating methods, Proceedings of the Geologists’ Association 106 (4) 281–92.Google Scholar
Reade, T. M. 1871. The geology and physics of the post-glacial period as shown in the deposits and organic remains in Lancashire and Cheshire, Proceedings of the Liverpool Geological Society 2: 36–88.Google Scholar
Roberts, E. J. 1995. The height distribution of a Neolithic/Bronze Age population compared with that of a present-day population. Unpublished report.Google Scholar
Tooley, M. J. 1970. The peat beds of the south-west Lancashire coast, Nature in Lancashire 1: 19–26.Google Scholar
Tooley, M.J. 1978. Sea level changes in Northwest England during the Flandrian stage, Oxford: Clarendon Press.Google Scholar
Topinard, P. 1877. L'Anthropologie. Paris: Reinwald.Google Scholar
Wilkinson, T.). & Murphy, P.L.. 1995. The archaeology of the Essex Coast 1: The Hullbridge Survey. Chelmsford: East Anglian Archaeology. Report 71.Google Scholar
Wkay, D.A. & Cope, F. W.. 1948. Geology of Southport and Formby, Memoirof the Geological Survey of the United Kingdom. Google Scholar