<< Our Photo Pages >> Banc Du Causewayed Enclosure - Causewayed Enclosure in Wales in Pembrokeshire
Submitted by Bladup on Monday, 11 January 2016 Page Views: 5944
Neolithic and Bronze AgeSite Name: Banc Du Causewayed EnclosureCountry: Wales County: Pembrokeshire Type: Causewayed Enclosure
Map Ref: SN06123065
Latitude: 51.940483N Longitude: 4.822018W
Condition:
5 | Perfect |
4 | Almost Perfect |
3 | Reasonable but with some damage |
2 | Ruined but still recognisable as an ancient site |
1 | Pretty much destroyed, possibly visible as crop marks |
0 | No data. |
-1 | Completely destroyed |
5 | Superb |
4 | Good |
3 | Ordinary |
2 | Not Good |
1 | Awful |
0 | No data. |
5 | Can be driven to, probably with disabled access |
4 | Short walk on a footpath |
3 | Requiring a bit more of a walk |
2 | A long walk |
1 | In the middle of nowhere, a nightmare to find |
0 | No data. |
5 | co-ordinates taken by GPS or official recorded co-ordinates |
4 | co-ordinates scaled from a detailed map |
3 | co-ordinates scaled from a bad map |
2 | co-ordinates of the nearest village |
1 | co-ordinates of the nearest town |
0 | no data |
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Causewayed Enclosure and other features in Pembrokeshire. Surveys suggest three main periods of activity across the hill. The earthworks of the earliest visible phase show an inner boundary defining an oval space that is perhaps open against the cragline on the east side.
Outside is an outer boundary that appears to start on the cragline, cross the neck of the promontory on the north side, and then curve around the west side to run close and parallel to the inner boundary to the south.
A single evaluation trench was opened in August 2005. This demonstrated that the bank, about 3.8m wide, was preserved to c. 40 cm, and had been apparently set onto an old, deturfed land surface. Postholes towards the front and rear were suggestive of a timber lacing within the bank. The ditch was 2.8m wide and a maximum of 1m deep with a U-shaped profile. Radiocarbon dates obtained through the AHRC-funded Neolithic Enclosure Dating Project show that the initial silt accumulated at around 3650 BC, whilst the middle fills contained material from the period 3000-2600 BC.
Examination of pollen evidence concludes that the enclosure was built in a heath-dominated landscape with some local scrubby woodland including oak and hazel.
The most recent phase comprises extensive ridge and furrow cultivation probably associated with a now-abandoned, putatively medieval or later, long house settlement or small hamlet downslope to the north-west. Earlier than this are two curved trackways that seem to provide access to a single long-house dwelling or structure. It is currently unclear whether these are contemporary or successive.
Coflein site no. 308024
Text by DeborahWales
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