Hovey's Handbook of the Mammoth Cave of Kentucky: A Practical Guide to the Regulation RoutesHovey, Horace Carver
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Hovey's Handbook of the Mammoth Cave of Kentucky: A Practical Guide to the Regulation Routes
Hovey, Horace Carver
Mammoth Cave (Ky.)
Advancing through Audubon Avenue, we soon find the roof and floor
approaching to form what is called Bunker Hill, around which we pass by
a narrow defile. The Mushroom Beds attract our attention, to which we
have already referred as having cost far more than they ever returned by
way of profit, although the idea itself is feasible.
Above a floor encumbered by debris hang formations needing an
explanation. Limpid drops trickle through the roof, saturated with
bicarbonate of lime. The supply of water is constant, but so meager as
to drip instead of flow; and as the dripping goes on each drop lays down
its load as a ring slight enough for a fairy’s finger. Ring follows ring
till a pendant is formed like a pipestem. The pipestems thicken to the
size of candles, and often grow as large as tree-trunks. Occasionally
they broaden into elegant drapery, or are twisted into fantastic shapes.
All these stone icicles are called “stalactites.”
Such lime-laden drops as fall splash about and on evaporation deposit,
not rings, but films thin as tissue-paper, building up stalagmites that
are solid from their base upwards. Often these downward and upward
growths meet as stately shafts, like the pillar named the Sentinel,
which guards Olive’s Bower a few steps beyond it.
The general term “dripstone” is conveniently applied to all these
deposits, and their finer varieties are known to the mineralogist as
“oriental alabaster.” A central stalactite in Olive’s Bower is very
large and cone-shaped, amid many smaller ones. Below is a rampart,
looking over which we see, some twenty feet below, a limpid pool that
reflects the overhanging formations. Before leaving the subject of
dripstone it should be remarked that, chemically regarded, it is simply
the hard carbonate, not the bicarbonate, as is often alleged; the latter
being an unstable compound, readily changing on any change of its
conditions.
The pit which arrests our progress beyond Olive’s Bower might, if
explored, prove this locality to be connected with White’s Cave, whose
features it resembles. On returning to the Rotunda we again inspect the
historic relics of the War of 1812, and mark the grooves cut in the
limestone walls by the hubs of the primitive cart-wheels that were
slowly drawn along by oxen to collect the nitrous earth for the
saltpeter vats. We notice that the bottoms of these vats were made of
small logs halved and grooved and laid in layers on supports; the lower
layer with its grooved surface up, to receive the second layer in
reversed position, making a method for conveying the lye into
reservoirs, whence it was pumped out to the crystallization troughs. Dr.
Call was the first to direct attention to this ingenious device.
Public-domain text, read in full here on John Shaqi.
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