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In the NW quadrant of a rath (SL032-163001-). According to local information, an opening to a drystone-built passage was blocked some time ago. The surface evidence for the souterrain now consists of a low sod-covered rise (Wth c. 2m) which extends from the bank of the rath at WNW for 10m south-eastwards into the interior. At the ESE end it expands into an irregular sod-covered stony rise. The SSE side of the rise is formed by a concentration of large stones in a roughly horseshoe-shaped setting.
The above description is derived from the published 'Archaeological Inventory of County Sligo' compiled by Ursula Egan, Elizabeth Byrne, Mary Sleeman with Sheila Ronan and Connie Murphy (Dublin Stationery Office, 2005).
Date of upload: 18 January 2008
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