GEOLOGY, BY DOCTOR BOASE.

This parish, like the last, rests only on granite; at low water,

however, some felspathic rocks may be seen.

The granite exhibits the common varieties of this part of Cornwall,

and is traversed by porphyritic beds; one of which at Mean is a

compound of granular felspar and shorl in various proportions. This

kind is of rare occurrence; it is traversed by veins of quartz, which

are occasionally much intermixed with shorl; this mineral also abounds

in the adjoining granite, but more particularly in the veins by which

it is traversed.

Whitsand Bay is covered with a testaceous sand like that of St. Ives,

of Padstow, and of other places on the north coast; a large tract of

this sand is exposed at low water to the action of the wind, by which

it has been drifted in considerable quantities inland so far as Sennen

Green.

The Parochial History of Cornwall, Volume 3 (of 4) · 第 390 / 434 题