The Jenolan Caves: An Excursion in Australian WonderlandCook, Samuel
History
The Jenolan Caves: An Excursion in Australian Wonderland
Cook, Samuel
Australia -- Description and travel; Caves; Jenolan Caves (N.S.W.)
That portion of the limestone dyke in which the caves are found runs six
miles north and south; and the Grand Arch and the Devil's Coach
House--the two principal "day caves"--are formed right through the
mountain, near the centre, in an easterly and westerly direction. On the
one side McEwan's Creek flows towards the Devil's Coach House, and on
the other side is a natural watercourse leading to the Grand Arch, which
is only a few yards distant from it. Bearing in mind how the
watercourses converge towards these two central caves, and with what
force, in times of heavy rain, the floods scour them, a good
understanding may be obtained of the mechanical causes of the enormous
excavations which excite amazement as well as admiration. If a visit be
paid in winter, when the frost is sharp and the ground is "hoar with
rime;" when every bough and every blade of grass is covered with
congealed dew and adorned with forms of crystallisation which rival the
rarest beauties of the caves; when rocks are split and crumbled by
sudden alternations of heat and cold; there will be abundant
illustration of the effect of water and light, and the variation of
temperature in causing geological transformation. Limestone is not
soluble in water without the addition of carbonic acid. An exploration
of the caves, however, shows that the mountains are not composed
entirely of limestone, but that other substances constitute part of
their bulk. The principal causes of the formation of the "day caves,"
the Grand Arch and the Devil's Coach House, are the mechanical action of
water and the variation of temperature. As regards the interior caves,
where night reigns supreme, chemical combination has played a more
important part. But the effect of water power is everywhere observable
in graceful contours, caused by continuous motion, or in stony
efflorescence, produced by intermittent humidity or dryness of the
atmosphere. The action of the former is the more marked and striking,
the latter more elaborate, and microscopically beautiful. The
hygrometric condition of the caves is recorded in lovely forms, which
lend enchantment to ornate bowers, sparkling grottoes, and fairy cities.
[Illustration: THE GRAND ARCH ENTRANCE.]
[Illustration: THE GRAND ARCH--LOOKING EAST.]
THE GRAND ARCH.
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