The rocks forming Start Point are schists. They are probably metamorphosed Devonian Rocks, but could be remnants of a Lower Paleozoic or pre-Paleozoic landmass that was brought into contact with Lower Devonian rocks by faulting.
Uploaded to Geograph by Edmund Shaw on 13 September 2015
Photo © Edmund Shaw, 13 September 2015.
Licensed for reuse under this Creative Commons licence