Earthwork 370yds (340m) E of Low Stead (Lowick)
(NU 0331 3956 Camp. (1)
Ring-shaped enclosure with single rampart. Area approximately 1/4 acre. (2)
The situation is on the tip of a promontory formed by the junction of two small valleys a little over the 200 foot contour.
The main earthwork has been formed by cutting off the promontory by a deep ditch. Spoil from this ditch has been used to form a strong inner rampart on the south east side of the enclosed area which has been scarped to form an almost perfect circle. On the west side the scarping has encountered a slight shoulder in the natural slope, resulting in the formation of a slight outer ditch at this point.
The main ditch has an average width of 13m. The inner bank has a maximum height of 2.5m internally and 5m above the bottom of the ditch. The only entrance to the enclosed area is to the north west where there is a slight lowering of the lip and a causeway to ease the steep scarped slope. There is a slight rampart on the edge of the scarped slope on each side of the entrance.
The bracken covered interior shows no traces of habitation.
The profile of the slopes is sharp and very little silting up of the ditch has occurred. It is concluded that this earthwork is a ring castle of early medieval date.
Centred NU 03323950. To the immediate south of the above are the remains of an enclosure that apparently consisted of two concentric ramparts. To the north the ramparts have been destroyed by the later ditch of the ring castle, while to the east all traces have been obliterated by cultivation.
The two ramparts consist of banks of earth and stone. The inner bank has an average width of 6m and a maximum height of 1m while the outer bank has corresponding dimensions of 5m and 0.8m. There is a gap, possibly an entrance, on the south side. The bracken-covered interior shows no traces of occupation.
The situation is on level ground with the natural slopes of a small valley immediately to the west.
The remains are too fragmentary for any certain conclusions, but the nature of construction and dimensions of the banks are similar to earthworks discovered in the Cheviot Hills, which have yet to be classified as to period, but whose purpose was possible pastoral.
There are streams forming adjacent sources of water for both earthworks. (3)
The ring castle and adjacent earthwork are as described. No entrance is apparent in the south side of the earlier earthwork. Only the scarp of the inner bank of this work is evident, a later field bank a dike having been built on top; the footings of the later bank continue for some distance south of the earthwork. (4)
Ring Motte. (5)
Condition of motte unchanged, but all trace of the earlier enclosure has been destroyed by recent ploughing. Published survey (25 inch) revised. (6)
Scheduled. (7)
NU 033 395. Earthwork 370yds (340m) E of Low Stead. Scheduled No ND/214. (8a)
Ring-shaped enclosure with single rampart. Area approximately 1/4 acre. (2)
The situation is on the tip of a promontory formed by the junction of two small valleys a little over the 200 foot contour.
The main earthwork has been formed by cutting off the promontory by a deep ditch. Spoil from this ditch has been used to form a strong inner rampart on the south east side of the enclosed area which has been scarped to form an almost perfect circle. On the west side the scarping has encountered a slight shoulder in the natural slope, resulting in the formation of a slight outer ditch at this point.
The main ditch has an average width of 13m. The inner bank has a maximum height of 2.5m internally and 5m above the bottom of the ditch. The only entrance to the enclosed area is to the north west where there is a slight lowering of the lip and a causeway to ease the steep scarped slope. There is a slight rampart on the edge of the scarped slope on each side of the entrance.
The bracken covered interior shows no traces of habitation.
The profile of the slopes is sharp and very little silting up of the ditch has occurred. It is concluded that this earthwork is a ring castle of early medieval date.
Centred NU 03323950. To the immediate south of the above are the remains of an enclosure that apparently consisted of two concentric ramparts. To the north the ramparts have been destroyed by the later ditch of the ring castle, while to the east all traces have been obliterated by cultivation.
The two ramparts consist of banks of earth and stone. The inner bank has an average width of 6m and a maximum height of 1m while the outer bank has corresponding dimensions of 5m and 0.8m. There is a gap, possibly an entrance, on the south side. The bracken-covered interior shows no traces of occupation.
The situation is on level ground with the natural slopes of a small valley immediately to the west.
The remains are too fragmentary for any certain conclusions, but the nature of construction and dimensions of the banks are similar to earthworks discovered in the Cheviot Hills, which have yet to be classified as to period, but whose purpose was possible pastoral.
There are streams forming adjacent sources of water for both earthworks. (3)
The ring castle and adjacent earthwork are as described. No entrance is apparent in the south side of the earlier earthwork. Only the scarp of the inner bank of this work is evident, a later field bank a dike having been built on top; the footings of the later bank continue for some distance south of the earthwork. (4)
Ring Motte. (5)
Condition of motte unchanged, but all trace of the earlier enclosure has been destroyed by recent ploughing. Published survey (25 inch) revised. (6)
Scheduled. (7)
NU 033 395. Earthwork 370yds (340m) E of Low Stead. Scheduled No ND/214. (8a)
N3678
FIELD OBSERVATION, Ordnance Survey Archaeology Division Field Investigation 1955; E Geary
FIELD OBSERVATION, Ordnance Survey Archaeology Division Field Investigation 1964; N K Blood
FIELD OBSERVATION, Ordnance Survey Archaeology Division Field Investigation 1968; D Smith
FIELD OBSERVATION, Ordnance Survey Archaeology Division Field Investigation 1964; N K Blood
FIELD OBSERVATION, Ordnance Survey Archaeology Division Field Investigation 1968; D Smith
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