GEOLOGY, BY DR. BOASE.

The church is situated on the borders of the granite, which extends to

the extreme northern part of the parish, and is for the most part of

that common kind which is shipped at Penryn for the London market.

Proceeding southward from the church town this granite is bounded by a

belt of rocks belonging to the porphyritic series, such as the felspar

and hornblend rocks; but in the vicinity of the Helford river these

are succeeded by the calcareous series.

The Parochial History of Cornwall, Volume 1 (of 4) · 第 192 / 315 题