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Excavation of a Barrow near the Hardy Monument, Black Down, Portesham, Dorset

Published online by Cambridge University Press:  27 May 2014

M. W. Thompson
Affiliation:
Inspectorate of Ancient Monuments, Ministry of Works
P. Ashbee
Affiliation:
Inspectorate of Ancient Monuments, Ministry of Works
G. W. Dimbleby
Affiliation:
Dept. of Forestry, Oxford University

Extract

The barrow whose excavation is described below was situated about 770 feet above Ordnance Datum a hundred yards south of the Hardy Monument on Black Down Hill, Portesham, on the edge of a large gravel pit. In the winning of gravel during the war the face of the pit had been worked round the barrow on both sides destroying the southern half of the ditch and part of the south side of the mound. As the mound was slowly falling into the gravel pit, it was decided by the Ministry of Works to excavate the barrow before further deterioration took place. The first-mentioned author undertook the supervision of this work for the Ministry in April and May, 1955, with a further fortnight in October of the same year, with the kind permission of the owner, Mrs H. Tuke.

Type
Research Article
Copyright
Copyright © The Prehistoric Society 1958

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References

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page 125 note 1 PPSEA, VII, pt. I, 204–5Google Scholar.

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page 128 note 10 Abercromby, vol. I, no. 361.

page 128 note 11 Ibid, no. 362; Warne, 28–30.

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page 130 note 1 PPS, IV, 174Google Scholar, fig. 4, 53.

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page 130 note 4 References. For those not familiar with the terms or techniques used here, the following papers may prove helpful:

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2. Dimbleby, G. W. (1955). ‘The Ecological Study of Buried Soils’, Advancement of Science, XII, no. 45, 1116Google Scholar.

3. Dimbleby, G. W. (1957). ‘Pollen Analysis of Terrestrial Soils’, New Phytol., LVI, 1228CrossRefGoogle Scholar.

page 131 note 1 Owing to pressure of space the complete pollen analyses are not given here; they are, however, available for reference at the Dept. of Forestry, Oxford University.

page 132 note 1 I am much indebted to Dr H. Godwin for his help and advice on this point. He says that ‘it seems extremely probable that the grains are those of Hedera despite their high frequency’.