GEOLOGY, BY DOCTOR BOASE.

A small triangular portion, forming the extreme southern part of this

parish, rests on granite, as does also an irregular tract on the

south-eastern boundary; but all the remainder, that is by far the

greater part of the parish, is situated on felspathic rocks, belonging

to the porphyritic series, which are very metalliferous, constituting,

with similar rocks in Camborne and Gwennap (all surrounding the same

central mass of granite) the most important mining district in

Cornwall.

[13] The Cranes (of Crane) are noticed by the Heralds as

residing in Camborn for five descents previously to 1620.

Their arms, Argent, a crane Sable, on a perch raguly Vert.

The Parochial History of Cornwall, Volume 3 (of 4) · 第 357 / 434 题