GEOLOGY, BY DR. BOASE.

The greater part of this parish is situated on granite, including

within its boundaries Roughtor and Brown Willy, the highest hills in

Cornwall, the latter being 1368 feet above the level of the sea. The

composition of this granite has been already noticed under the head of

Advent: it affords few varieties, which may be owing to its offering

few opportunities for examination.

The circumstance most attractive of attention is the great sterility

of this extensive district; some few contracted spots are indeed

brought into cultivation; some parts afford summer pasturage for

cattle, and others turf for fuel; but by far the greater portion of

the whole lies entirely unproductive. And this character belongs to

the whole insulated patch of granite more than ten miles in diameter;

and the church of St. Breward is the only one to be found on this

extensive surface of perhaps from forty to fifty thousand acres; while

nine churches are to be found on the granite district of the Land’s

End, where this substratum, departing from its usual qualities, gives

fertility to the soil.

The western extremity of this parish is fertile, resting on a peculiar

kind of slate, which possesses geological interest. It may be seen at

Combe, at Penrose, and at other places near the river Camel, and

appears to be a variety of mica slate, being composed of granular

felspar, interlaminated with mica. It contains beds of dark purple

felspar rock, very similar to that which abounds in the mining

district in the western part of the county. This micaceous slate

gradually passes into a thick lamellar rock, which extensively

disintegrates and becomes argillaceous, exactly resembling the stone

quarried for building at Bodmin.

[20] This is written in a different hand.

The Parochial History of Cornwall, Volume 1 (of 4) · 第 125 / 315 题