The extreme northern part of this parish is formed of a narrow slip
which runs out considerably beyond the regular boundaries, and
terminates on the sea shore; about half of the protuberance is
composed of felspathic rocks, belonging to the porphyritic series, and
all the rest of the parish is situated on granite.
[3] This is in Ludgvan.
[4] An Inquisitio post mortem.
[5] April the 6th, 1644.