Site Record

Highly inclined boundary stone (source OS495card: SN75NE3), but scheduled as a Bronze Age standing stone (Cadw).
A report has been received (17.04.2014) that this stone (whatever its identity) has 'cracked and fallen' and now lies in two pieces, the lower part still earthfast. The fracture appears to have occurred along a natural fault line in the rock, probably 'by natural processes rather than by any deliberate vandalism'.

RCAHMW, 23 April 2014