A book of the west. Volume 1, Devon : $b being an introduction to Devon and CornwallBaring-Gould, S. (Sabine)
History
A book of the west. Volume 1, Devon : $b being an introduction to Devon and Cornwall
Baring-Gould, S. (Sabine)
Devon (England)
The ancients were not such fools as we take them to have been. They
did condescend to consider the capabilities and the disadvantages
of their building material before employing it. The "old men,"
when they constructed a wall of granite, always gave it two faces,
and filled in with rubble between. By this means the rain did
not drive through, although they did not employ mortar; and the
ancient tenement houses on the moor are dry as snuff. But the modern
architect insists on having the walls built throughout with lime,
in courses, and the rain enters by these as by aqueducts. Then,
to remedy the evil, the whole face of the house is tarred over or
cemented, with what result to the prospect may well be conceived.
The granite, though pervious, is so to a very limited extent when
compared with limestone, and through a granite country there are
no springs that issue from subterranean reservoirs. All the rain
that falls on the surface runs off superficially, but not all at
once, for on the granite lie enormous beds of peat, the growth and
decomposition of moor plants through vast ages. These beds of peat
are like sponges; they absorb the rain, retain it, and slowly give
it up during the summer. In limestone districts the making of a
river goes on within the bowels of the mountain, but in a granite
district it takes place on its outside. Remove the beds of turf
and peat, and there will be torrents after a shower, and then dry
torrent beds.
To north and south of the equator of the moor lie vast tracts of bog
in which the rivers are nursed, and without which they could not be.
No visitor can realise what Dartmoor really is in the economy of
nature as the mother of the Devonshire rivers till he has visited
either Cranmere Pool, or the ridge on the south, where are the meres
from which spring the Avon, the Erme, the Yealm, and the Plym.
The granite being of unequal hardness, its constituent crystals
become separated by the action of the weather into an incoherent
gravel, which in Cornwall is called growan. The process may be seen
in full activity on any tor. Sometimes water lodges on a slab, and
finding a soft spot begins to decompose it; then, when this is the
case, the wind swirls the water about, and with it the grit is spun
round and round, and this continues the work of disintegration, and
finally a rock basin is produced.
Of these rock basins some fine samples exist: that on Caistor Rock
has had to be railed round, to prevent sheep from falling in and
being drowned. Mis Tor has another, the Devil's Frying-pan. There
are plenty of them to be seen in all conditions, from the rude
beginning to the complete bowl.
At one time it was supposed that they were Druidical vessels
employed for lustration, and archæologists talked long and learnedly
concerning them. But what is quite certain is that they were
produced by Nature unassisted.
Public-domain text, read in full here on John Shaqi.
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