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Situated towards the head of a N-S valley at the headwaters of a stream that runs S and then W to the N-S Mahon River. A spring was just E of the site. It was first identified as a burnt spread by C. Moloney (2006) in testing (06E0163) on the line of a water pipe, and subsequently sample excavated (06E0283) by T. Janes.
This was an extensive area of burnt stone and charcoal-rich soil (dims. c. 18m x c. 17m) which produced a C14 date of 1013-841 Cal BC (Janes 2008, 3, App. 8). No other features or artefacts were recovered. Burnt mound (WA024-119----) is further up the valley c. 120m to the NNE. (Janes 2009)
Compiled by: Michael Moore.
Date of upload/revision: 12th May, 2011.
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