Rambles in the Mammoth Cave, during the Year 1844 - By a Visiter by Alexander Clark Bullitt
page 64 of 70 (91%)
page 64 of 70 (91%)
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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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