GEOLOGY, BY DR. BOASE.

One corner of this parish, immediately north of Penryn, extends on the

slate in the form of a very narrow and short stripe; but all the

remainder rests entirely on granite, which is for the most part

coarse-grained and crystalline, abounding in porphyritic crystals and

felspar. It, however, also contains numerous beds of a finer quality,

which being well adapted for building is extensively quarried.

The Parochial History of Cornwall, Volume 3 (of 4) · 第 88 / 434 题