GEOLOGY, BY DR. BOASE.

The western moiety of this parish runs much further south than the

eastern, stretching in an irregular form into the granite near

Roughton and Brown Walley.

The rocks adjoining this granitic portion are compost and schistose

felspar, as at Alternun, and in a similar position. These are

succeeded in the vicinity of the church by a peculiar calcareous rock,

consisting almost entirely of hornblend and calcareous spar. The

northern part makes part of a downs, extending almost to Launceston,

and abounding in manganese.

The Parochial History of Cornwall, Volume 1 (of 4) · 第 168 / 315 题