GEOLOGY, BY DR. BOASE.

The northern corner of this parish is situated on granite, resembling

that of Gulval in every respect, except as to one variety abounding in

mica. Much of this stone may be seen in the more ancient houses at

Penzance. The spot, however, from whence this stone was procured, is

no longer known. A difference of opinion is indeed entertained as to

whether it was gotten from blocks near the surface, or from a bed that

has been exhausted; but all are agreed as to the district from whence

it came; and it is universally known by the name of Ludgvan stone. The

property of cleaving evenly into regular blocks, eminently possessed

by this species of granite, makes it valuable for building purposes;

and this property is clearly derived from the even arrangement of the

scale of mica in which it abounds.

Between the granite and the sea-shore a considerable portion of the

schistose rocks is covered by a marsh, and by banks of sand. These

rocks are made up of compact felspar, sometimes nearly pure, at others

intimately united with hornblend or actynolite; they are traversed by

courses or dykes of felspar porphyry, as may be seen on the sea-shore.

[2] Extracted from an “Account of certain Hill Castles, near

the Land’s End in Cornwall,” by William Cotton, Esq. F.S.A.

printed in the Archæologia, vol. XXII. where a plan and

section of Castle-an-Dinas will be found, taken with greater

care than that in Lysons’s Cornwall. In the Gentleman’s

Magazine, LXXII. p. 393, are engravings of two stone weights

found within the inner circle of this fortress. The weight

of one was seventeen pounds and a half; and that of the

other three pounds one ounce.

LUXILIAN, or LUXULIAN.

The Parochial History of Cornwall, Volume 3 (of 4) · 第 77 / 434 题