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Rambles in the Mammoth Cave, during the Year 1844 - By a Visiter by Alexander Clark Bullitt
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admiration. Some of the formations in the avenue, have been
denominated by Professor Locke, oulophilites, or curled leafed stone;
and in remarking upon them, he says, "They are unlike any thing yet
discovered; equally beautiful for the cabinet of the amateur, and
interesting to the geological philosopher." And I, although a wanderer
myself in various climes, and somewhat of a mineralogist withal, have
never seen or heard of such. Apprehensive that I might, in attempting
to describe much that I have seen, color too highly, I will, in lieu
thereof, offer the remarks of an intelligent clergyman, extracted from
the New York Christian Observer, of a recent date: "The most
imaginative poet never conceived or painted a palace of such exquisite
beauty and loveliness, as Cleveland's Cabinet, into which you now
pass. Were the wealth of princes bestowed on the most skilful
lapidaries, with the view of rivaling the splendors of this single
chamber, the attempt would be vain. How then can I hope to give you a
conception of it? You must see it; and you will then feel that all
attempt at description, is futile." The Cabinet was discovered by Mr.
Patten, of Louisville, and Mr. Craig, of Philadelphia, accompanied by
the guide Stephen, and extends in nearly a direct line about one and a
half miles, (the guides say two miles.) It is a perfect arch, of fifty
feet span, and of an average height of ten feet in the centre--just
high enough to be viewed with ease in all its parts. It is incrusted
from end to end with the most beautiful formations, in every variety
of form. The base of the whole, is carbonate (sulphate) of lime, in
part of dazzling whiteness, and perfectly smooth, and in other places
crystallized so as to glitter like diamonds in the light. Growing from
this, in endlessly diversified forms, is a substance resembling
selenite, translucent and imperfectly laminated. It is most probably
sulphate of lime, (a gypsum,) combined with sulphate of magnesia. Some
of the crystals bear a striking resemblance to branches of celery, and
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