GEOLOGY, BY DOCTOR BOASE.

This parish is composed of the same kind of rocks as the neighbouring

parishes of Cubert, Colan, and St. Columb Minor. It is entirely placed

within the calcareous series. At Trevemper bridge is a bed of compact

limestone, similar to that which is so common in many parts of

Cornwall, and is provincially known by the name of black lime. This

rock has been noticed under the head of St. Germans, and it is very

abundant at Rock Ferry, in St. Minver, opposite Padstow.

* * * * *

It may be proper to add that Newlyn, west of Penzance, grown to be in

reality a town of some importance, is legally no more than a village

in the parish of Paul, without any separation whatever.

The Parochial History of Cornwall, Volume 3 (of 4) · 第 247 / 434 题