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Prehistoric Roads and Tracks in Somerset, England: 2. Neolithic1

Published online by Cambridge University Press:  06 September 2016

John M. Coles
Affiliation:
Faculty of Archaeology & Anthropology, Cambridge
F. Alan Hibbert
Affiliation:
Sub-Department of Quaternary Research, Cambridge
Colin F. Clements
Affiliation:
9 Clifford Avenue, Taunton, Somerset

Extract

The Somerset Levels are the largest area of low-lying ground in south-west England, covering an extensive region between the highlands of Exmoor, the Brendon Hills and the Quantock Hills to the west, and the Cotswold and Mendip Hills to the east (Pl. XXIII, inset). The Quantock Hills and the Mendip Hills directly border the Levels themselves, and reach heights of over 250 metres above sea level. The valley between extends to 27 metres below sea level, but is filled to approximately the height of the present sea by a blue-grey clay. The Levels are bisected by the limestone hills of the Poldens, and both parts have other smaller areas of limestone and sand projecting above the peat deposits that cap the blue-grey clay filling. In this paper we are concerned with the northern part of the Levels, an area at present drained by the River Brue.

The flat, peat-covered floor of the Brue Valley is some six kilometres wide and is flanked on the north by the Wedmore Ridge, and on the south by the Polden Hills (Pl. XXIII). In the centre of the valley, surrounded by the peat, is a group of islands of higher ground, Meare, Westhay, and Burtle. These islands, which would always have provided relatively dry ground in the Levels, are linked together by Neolithic trackways of the third millennium B.C. Several of these trackways formed the basis of a paper in these Proceedings in 1968 (Coles and Hibbert, 1968), which continued the work of Godwin and others (Godwin, 1960; Dewar and Godwin, 1963).

Type
Research Article
Copyright
Copyright © The Prehistoric Society 1970

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References

REFERENCES

Bulleid, A., 1933. ‘Ancient Trackway in Meare Heath, Somerset’, Proc. Som. Arch. and Nat. Hist. Soc., 79, 20.Google Scholar
Clark, J. G. D., 1933. ‘Mesolithic Sites on the Burtle Beds, near Bridgwater, Somerset’, Man, 33, no. 65.CrossRefGoogle Scholar
Clark, J. G. D., 1963. ‘Neolithic Bows from Somerset, England, and the Prehistory of Archery in north-west Europe’, PPS, 29, 50.Google Scholar
Coles, J. M., 1968. ‘A Neolithic God-Dolly from Somerset, England’, Antiquity, 42, 275.CrossRefGoogle Scholar
Coles, J. M. and Hibbert, F. A., 1968. ‘Prehistoric Roads and Tracks in Somerset, England: 1. Neolithic’, PPS, 34, 238.Google Scholar
Dewar, H. S. L. and Godwin, H., 1963. ‘Archaeological Discoveries in the Raised Bogs of the Somerset Levels, England’, PPS, 29, 17.Google Scholar
Dymond, C., 1880. ‘The Abbot's Way’, Proc. Som. Arch. and Nat. Hist. Soc., 26, 107.Google Scholar
Godwin, H., 1960. ‘Prehistoric Wooden Trackways of the Somerset Levels: their construction, age and relation to climatic change’, PPS, 26, 1.Google Scholar
Iversen, J., 1949. ‘The Influence of prehistoric man on vegetation’, Danm. Geol. Unders. R. IV: 6.Google Scholar
Tauber, H., 1965. ‘Differential pollen dispersion and the interpretation of pollen diagrams’, Danm. Geol. Unders. R. II: 89.Google Scholar
Turner, J., 1964. ‘Surface sample analyses from Ayrshire, Scotland’, Pollen et Spores 6, 583.Google Scholar
Wainwright, G. J., 1960. ‘Three microlithic industries from south-west England and their affinities’, PPS, 26, 193.Google Scholar