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
The first abounds in the high lands, and consists of a light, moory,
black earth, intermixed with small particles of granite or gravel. The
earthy parts of this are so exceedingly light, that in a dry summer, as
Dr. Borlase observes, the sun quickly exhales its moisture, and in a wet
summer or winter, much of the vegetable soil is washed from the tilled
grounds. This soil is in general very productive, and fit for any kind
of grain. The shelfy or slaty soil is far the most prevalent, and is
distinguished by this name from having a large proportion of the
schistus, or rotten slaty matter mixed with the light loam, of which its
soil is composed. With sand and more viscuous earths, it makes an
excellent compost, and produces great crops of wheat and barley. In
congenial situations, barley has frequently been sown, reaped, and
threshed, in less than nine weeks. This soil is not unfrequently mixed
with _quartz_, provincially called _spar_, and according as this
prevails, its value is lessened. When a dun or ironstone is found, it is
considered a fortunate circumstance, being a certain indication of the
incumbent soil.
Of the _Loamy Soils_, there are many very rich and fertile patches,
interpersed in different parts of the county; and the low grounds,
declivities, banks of the rivers and town-lands are composed of them.
Some of these are incumbent on a subsoil of clay, and partake more or
less of it in their composition. With respect to _Clays_, Cornwall
presents endless varieties; good bricks are made from some of them, and
in the parish of Lelant, there is an excellent species for making
furnaces and ovens. A clay of a slaty nature, but soapy to the touch, is
found near Liskeard, and has fertilizing powers; but the Serpentine,
with veins of _steatite_, near the Lizard, is the most curious of all
the earthy substances found in Cornwall, although very little of it has
been used for some years in the porcelain manufactures. Large quantities
of a fine white clay, found in the parish of St. Stephen near St.
Austell, is exported annually, and is now become an important article of
commerce.
The mineralogical substances of Cornwall are more abundant than any
other county in England, and the variety and beauty of them affords an
abundant source for the scientific enquirer. Of the stones most entitled
to precedence, is the _granite_, or _moor stone_, which abounds in great
quantities in almost every part of the county. Granite is an aggregate
of _felspar_, _quartz_, and _mica_, and is found of different colours
and texture. Most of the churches and gentlemen’s seats in the county
are built with this stone, also the Waterloo Bridge in London, and which
was exported at a very great expense. It is frequently cut into pillars,
as supporters to buildings, and is very serviceable as gate posts,
bridges over rivers, rollers, troughs, and many other purposes.
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