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)
It is easy to wander back in imagination and bring the state of things
that existed visibly before the mind's eye: to watch the unwieldy
Mammoth or the great Rhinoceros rolling its huge bulk along; to see the
pack of cowardly Hyænas or Wolves hounding some worn-out Bison to its
death, over the awful cliff close by their den, which purpose effected,
they themselves rushed headlong down the steep slope hard by, to fight
and wrangle over the shattered carcass of their prey; or to see the
Lion lying in wait by the peaceful stream in the little valley for the
noble Elk or timid Deer to come for its accustomed drink; and then to
behold savage Man, with his weapons of flint or bone, when out on his
hunting expeditions, arriving at this peaceful valley, and there for
a while making his quarters in the Den, and lighting his fires at the
entrance to scare the wild beasts from their lair.[1]
[1] Only a few years since, three cows were driven over the cliff by
several unruly dogs, and of course were instantly killed. Thus was the
tragedy of long ago re-enacted.
How long ago this state of things existed is a matter for geological
calculation. Suffice it that the earliest historical records show us
no wild beasts existing in the land except Bears and Wolves, along
with the Red Deer which is with us to this day. Now there is no sign
at Wookey Hole of the time when the Bear and Wolf alone remained and
all else had become extinct from the land. There is no trace whatever
in the Hyæna Den of the pottery which we find in the entrance of the
great cave. Without a doubt, the latest deposits here are vastly older
than the most ancient deposits there. The commingling of northern,
temperate, and southern forms gives evidence of oscillations in
temperature such as demand a vast time to have taken place. Yet the
whole of these remains accumulated between the time when the entrance
to the Den was left exposed by the gradual destruction and retreat
of the cliff face up the valley, and the infilling and choking of the
entrance by the accumulating gravel which eventually blocked it. It is
only within the last few years that the gravel arch which was first
formed, and then undermined in the search after bones, has collapsed,
revealing the true configuration of the cavern. Here we must again
postulate a great antiquity for our caverns, since these deposits exist
in what is really an insignificant fragment of the great cavern, and
are only an incidental part of the material which an exposed cavity
is sure to receive. But when purely geological evidences are taken
into account, the demand for time becomes still more imperative. The
subterranean Axe occupies, as its present channel, vast chambers formed
by the excavation of thousands of tons of the hard Conglomerate, great
halls over 70 feet in height and of fine proportions. The process which
formed these is still at work enlarging them, till in the course of
Public-domain text, read in full here on John Shaqi.
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