Location | near Gussage St Michael, Dorset |
---|---|
Coordinates | 50°54′36″N2°2′31″W / 50.91000°N 2.04194°W |
OS grid reference | ST 971 123 |
History | |
Periods | Neolithic |
Site notes | |
Excavation dates | 1933 |
Archaeologists | Stuart Piggott, C. D. Drew |
Designated | 24 March 1958 |
Reference no. | 1002708 |
The Thickthorn Down Long Barrows are two Neolithic long barrows, near the village of Gussage St Michael in Dorset, England. They are near the south-western end of the Dorset Cursus, a Neolithic feature. The long barrows are a scheduled monument. [1]
The long barrows are situated on a ridge on Thickthorn Down. The barrow to the north-west, which is unexcavated, is rectangular, 44 by 18 metres (144 by 59 ft), and 2.4 metres (7 ft 10 in) high; there is an incomplete ditch around the barrow. It is aligned north-west to south-east, and is immediately south-east of the south-western terminus of the Dorset Cursus. It is thought that the bank at the end of the cursus, which is at an oblique angle to its sides but is aligned with the barrow, was designed to link to the existing monument. [1] [2]
The second barrow, a short distance along the ridge to the south-east, is also aligned north-west to south-east. It is rectangular, 30 by 18 metres (98 by 59 ft), and 2.4 metres (7 ft 10 in) high. There is a ditch around all except the south-east end, where there is a causeway. [1] [3]
The south-eastern barrow was excavated in 1933 by C. D. Drew and Stuart Piggott, and carefully restored. There were three post-holes on the causeway, one being on the central axis of the mound. There were no primary burials, but in the centre there was a structure consisting of two turf walls with a filling between of chalk rubble. The excavators suggested that the mound had been preceded by this structure, but it has more recently been suggested that the monument was constructed as a series of bays divided by hurdles. [1] [3] [4]
There were three secondary burials in the south-west side, two of them accompanied by beakers. In the ditch, mostly at the ends near the causeway, there were stratified finds including pottery of the Early Neolithic period and later Peterborough ware. [1] [4]
There are three related types of Neolithic earthwork that are all sometimes loosely called henges. The essential characteristic of all three is that they feature a ring-shaped bank and ditch, with the ditch inside the bank. Because the internal ditches would have served defensive purposes poorly, henges are not considered to have been defensive constructions. The three henge types are as follows, with the figure in brackets being the approximate diameter of the central flat area:
A causewayed enclosure is a type of large prehistoric earthwork common to the early Neolithic in Europe. It is an enclosure marked out by ditches and banks, with a number of causeways crossing the ditches. More than 100 examples are recorded in France and 70 in Southern England and Wales, while further sites are known in Scandinavia, Belgium, Germany, Italy, Ireland and Slovakia.
Long barrows are a style of monument constructed across Western Europe in the fifth and fourth millennia BCE, during the Early Neolithic period. Typically constructed from earth and either timber or stone, those using the latter material represent the oldest widespread tradition of stone construction in the world. Around 40,000 long barrows survive today.
The Dorset Cursus is a Neolithic cursus monument that spans across 10 km of the chalk downland of Cranborne Chase in east Dorset, United Kingdom. Its extreme length makes it a notable example of this class of linear earthwork; it is better interpreted as a pair of same-length cursus constructed end to end, with the more southerly cursus pre-dating the northerly one.
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