More information : (SU 5845550) Castle Mound Bailey (GT) (1)
Fort. Well. (GT) (2)
Castle Mound and bailey. (3)
The earthwork at Woodgarston is situated on fairly level ground near the edge of the chalk plateau which slopes rapidly down to the Kennet valley about 500 yards to the north. It is circular, 43 yards in diameter from crest to crest of the vallum. The rampart stands 8 feet above the area and 19 above the bottom of the ditch, and there is no bank on the counterscarp.
In the grass field to the west of the road, are traces of the curved bank and ditch of the bailey - C.D. vertical only 3 1/2 feet. The bank begins at the back of the cart sheds and is lost at the corner of the field in the fence which runs northwards on a 5 feet bank. On the east of the road, continuing the line of the buildings beyond the pond, is the faintest fold in the ground curving round to the north-east towards the line of a garden fence.
The rampart of the keep is covered with large flints, both lying loose and embedded. They are especially well seen under the roots of an elm on the west.
The soil is clay - two or three feet thick on chalk and the ground would be naturally forest. There is a well within the keep, still in use. Early mention is made of a chapel at Woodgarston. All the modern farm buildings are within the line of the bailey. (4)
In a grant of land by Eadmund ("B.803" A charter of A.D.945 Cartularium Saxonicum, Vol. II (1887), p. 560, (birch) Wealagaerstune - 'the Grass Enclosure of the Walls' is mentioned. This is now represented by Woodgarston Farm by which are the remains of an old fort; hence the 'Walls' in the old name. (5)
Scheduled as a `ring-motte'. (6)
The main earthwork - a ring motte - is in good preservation, under grass and trees with a few portable sheds and small farm-lumber within it. The bank and ditch, as described by Williams-Freeman, survive on all but the south side. Here, opposite the farmhouse, the bank has been levelled and there is no trace of the ditch. On the west, the ditch has a causeway opposite a lowering of the bank.
The interior of the motte is raised above the general level and its north-east corner is slightly raised possibly indicating the site of a building. On the bank are numbers of large flints and, as stated by Williams-Freeman, under the exposed roots of one tree is the debris of a well. The well is now disused and covered by iron and timber posts.
The bank and ditch described as a bailey by Williams-Freeman accompanies an old hedge-bank, on the south-west. It appears to be a continuation of the hedge bank to the north, and I am of the opinion that it is so slight as to be of doubtful antiquity. No trace of its extension to the east was seen.
Dr. Crawford, in conversation, August 1956, dismissed the
identification of the motte with the Saxon derivation of Woodgarston. (7)
No change. Motte revised at 1/2500. (8)
Listed by Cathcart King. (9) |