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)
miles and reappear in Castleton, 600 feet beneath. Whether they unite
into one or two large streams, which form considerable chambers and
caverns in the inaccessible region beyond the farthest known parts of
Speedwell and Peak Caverns, is an interesting question, that tempts one
to answer boldly in the affirmative, since the action of underground
streams in Somerset and Yorkshire seems to justify the assumption, if
we take into account the extent of the vertical joints eaten away by
the water in its descent of 600 feet, and the effects of periodical
floods. In Somerset, in a situation exactly similar, two caves of 600
feet fall and 2000 feet horizontal measurement have recently been
discovered by opening similar swallet-holes. Is there any hope of
finding such hypothetical cavern or caverns here by exploring, and if
necessary opening artificially, any of the swallets between Perryfoot
and Giant's Hole? The investigations recently carried out by a friend
and myself do not make us hopeful that if there are such caverns they
will ever be made accessible.
We began our work at Giant's Hole, which opens in the bottom of a
little gorge between Peak's Hill and Middle Hill. The brooklet that
runs in at the cave mouth was very low, and we passed almost dryshod
over the rough stones that cover the stream-bed for some 60 feet.
Giant's Hole has an arched entrance about seven feet high, and the
first part of the cave retains the same form. Then the walls contract,
and the cave takes the shape of a deep and narrow canyon, cut through
solid rock, with the stream coursing along at the bottom over little
falls and waterslides and through pools that are not easy to pass
without a wetting. One hundred and fifty feet from the entrance to the
cave is a lofty rift, near the top of which an upper gallery turns
west, the general direction of the main passage being southerly.
Passing this, we followed the stream downhill for another fifty or
sixty yards, and were then brought to a standstill by a partial choke.
At this point a quantity of stones and gravel comes within two feet of
the roof, and the water is dammed back in a pool a foot deep, so that
there is barely a foot of clear space between water and roof.
Public-domain text, read in full here on John Shaqi.
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