|  |  |  Sketch plan
        of earthwork feature and trenches
 
 
  View from site towards the west
 
 
  North-west facing section through ditch
 |  |  |  | Wat's Dyke is less well known than Offa's Dyke which runs
        parallel to it further west, but is nevertheless an
        important boundary and a major feature of the
        archaeological landscape of the Welsh Marches. It is not
        known exactly when the Dyke was constructed, but recent
        radiocarbon dating evidence has suggested that it was
        probably built between A.D. 268 and A.D. 630. This has
        overturned the previously held belief that it was
        constructed in the 8th century.
 
 Despite many investigations into the course of Wat's Dyke
        over the last thirty years, the route of the section east
        of Chirk remained unclear. In the 18th century Thomas
        Pennant suggested that the route follwed a straight line
        crossing the river Ceiriog and the river Dee. In the
        middle of the 20th century Sir Cyril Fox suggested that
        in forested and marshy areas the dyke was not built. More
        recently David Hill and Margaret Worthington have tested
        this and shown the dyke seems to have been continuous. An
        alternative route for this section of Wat's Dyke was
        along the top edge of the valley through which the
        Ceiriog and the Dee flow.
 
 Prior to laying a new gas pipeline between Overton and
        Chirk a desk based assessment for Transco identified an
        earthwork at the top of a steep hill which may have been
        the course of Wat's Dyke.
 
 A small scale evaluation excavation across the earthwork
        confirmed that there was a 2.1m wide ditch starting 4
        metres below the top of the slope. To the east of the
        ditch were the remains of a bank, increasing the severity
        of the slope. Micromorphology was carried out on a soil
        sample which confirmed that there was a buried soil below
        the bank. The evaluation trench was extended behind the
        bank but no contemporary features were found.
 
 There is no clear reason for a ditch and bank existing in
        isolation and as its form is consistent with other
        excavated parts of the dyke, there seems little doubt
        that this very small investigation has defined the long
        debated course of the Dyke in this area.
 
 Transco have now laid the new pipeline, with no further
        disturbance to this important monument.
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