The netherworld of Mendip : $b explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhereBaker, Ernest A. (Ernest Albert)
Science
The netherworld of Mendip : $b explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhere
Baker, Ernest A. (Ernest Albert)
Caves; Mendip Hills (England)
At the time of my first serious attempt to explore the caves of
Cheddar, when our party contained Dr. Norman Sheldon, Mr. J. O.
Morland, and Mr. Harry Bamforth, two of whom have not since been able
to join us in Somerset, I had not the advantage of knowing Mr. H. E.
Balch, and we were utterly unaware of the great work he had been doing
in the cave region adjoining Wells. On the other hand, we received
invaluable assistance from the brothers Gough, who are not only
proprietors of show caves, but take a sincere interest in underground
exploration. Their father, who died in 1902, was the discoverer of the
caverns that bear his name, and was actively at work pushing his way
farther and farther into the rocky bosom of the hill up to the year of
his death, at a good old age.
[Illustration: STALAGMITE PILLARS IN GOUGH'S GREAT CAVERN.
_Photo by Gough, Cheddar._]
[Illustration: THE PILLARS OF SOLOMON'S TEMPLE, GOUGH'S CAVES, CHEDDAR.
_Photo by Gough, Cheddar._]
The Great Cavern was discovered in 1898. The parts open to visitors
extend in a generally easterly direction for some 600 yards, and
consist of natural chambers and passages, connected here and there
by artificial tunnels. We began work early in the morning, carrying
into the cavern a large quantity of ropes, ladders of wood and rope,
and plenty of illuminants, including a 2000-candle-power limelight,
which with its lens or condenser is one of the most valuable aids in
subterranean work. Many openings are seen overhead and in the walls
of the cavern as the visitor advances, some of which end abruptly,
whilst others lead into small grottos and galleries. One of the most
conspicuous chimneys, or perpendicular caves, has at its base a
peculiar staircase of stalagmitic basins, formed by the deposits of
a calcareous spring that is now dried up. These basins are known as
the "Fonts." Our conductors had been in the habit of climbing about
50 feet up this lofty chasm, over the crust of stalagmite, and a wire
rope had been fixed to assist visitors in ascending to a broad, deep
ledge. Above this point the rocks were much steeper. No one had ever
succeeded in seeing the top, and at first we thought it would be
impossible to ascend any higher without some sort of apparatus. We sent
for a ladder, and meanwhile Dr. Sheldon and I tried to clamber over
the jutting arch of rock that formed the first obstacle--a cave-pitch
in a gully or chimney we should call it in climbing parlance. To our
surprise, we succeeded in reaching the continuous channel or gutter
above it, which ascended at a high angle, with sheer walls to right
and left, and the other side of the huge shaft overhanging it. The
holds were shallow and slippery, and with one hand grasping a candle we
found the ordinary difficulties of a rock-climb multiplied enormously.
Half-way up my candle went out, but my companion was now well ahead,
and I groped my way after him with confidence. When a shout from below
Public-domain text, read in full here on John Shaqi.
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