Excursions in the County of Cornwall: Comprising a Concise Historical and Topographical Delineation of the Principal Towns and Villages, Together With Descriptions of the Residences of the Nobility and Gentry, Remains of Antiquity, and Every Other Interesting Object of Curiosity — John Shaqi
Excursions in the County of Cornwall: Comprising a Concise Historical and Topographical Delineation of the Principal Towns and Villages, Together With Descriptions of the Residences of the Nobility and Gentry, Remains of Antiquity, and Every Other Interesting Object of CuriosityStockdale, Frederick Wilton Litchfield
History
Excursions in the County of Cornwall: Comprising a Concise Historical and Topographical Delineation of the Principal Towns and Villages, Together With Descriptions of the Residences of the Nobility and Gentry, Remains of Antiquity, and Every Other Interesting Object of Curiosity
Stockdale, Frederick Wilton Litchfield
Cornwall (England : County) -- Description and travel; Cornwall (England : County) -- History
Another species of stone very prevalent in Cornwall, is distinguished by
the name of _Killas_. It is a schistus, and forms the most considerable
substratum in the county. It varies in texture and colour, some being
hard, others more pliable and laniated, and of a blueish yellow, and
ferrugineous brown; but either forms an excellent material for building.
The worst sort of stone found in Cornwall, is an opaque whitish debased
crystal, generally called spar, and lies loose on the surface of the
ground, in almost every parish. It is, however, useful for making fences
and for repairing the roads.
On the north and south coasts of the county, there are several _Slate
Quarries_, the slate from which is generally adopted for the roofing of
houses; but the best species is found in the celebrated quarry of
_Delabole_ near Camelford, which is said to produce the finest and
largest slates in England.—“The quarry is about 300 yards long, 100
broad, and upwards of 40 fathoms deep. The slate is first met with about
three feet below the surface of the ground, in a loose shattery state,
with short and frequent fissures, the _laminæ_ of unequal thickness, but
not horizontal.—Thus it continues to the depth of 10 or 12 fathoms, when
a more firm and useful stone is procured, the largest pieces of which
are used for flat pavements. This is called the _top-stone_, and
continues for 10 fathoms, after which the quality improves with
increasing depth, till at the 24th from the surface, the workmen arrive
at the most superior kind, called the _bottom-stone_.—The colour is
grey-blue, and the texture is so close, that it will sound like a piece
of metal. The masses are separated from the rock by wedges driven by
sledges of iron, and contain from five to 14 superficial square feet of
stone. As soon as this mass is freed by one man, another stone cutter,
with a strong wide chisel and mallet, is ready to cleave it to its
proper thinness, which is usually about one eighth of an inch; the
pieces are generally from a foot square, to two feet long, by one wide,
but the flakes are sometimes large enough for tables and tomb
stones.”[3]
Public-domain text, read in full here on John Shaqi.
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