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See also: Crawford county, See also: Indiana, U.S.A., 5 M
.
N.E. of Leavenworth, on the See also: Ohio See also: river, and 12 M. from See also: Corydon, the early territorial capital
.
The nearest railway station is Milltown, 9 M. distant
.
The cave is in a rugged region of high See also: limestone hills, in one of which its See also: main entrance is found, 220 ft. above the level of the Blue river, whose See also: original name, the See also: Wyandotte, was transferred to the cave by Governor See also: David See also: Wallace; it having previously been styled the See also: Mammoth Cave of Indiana, the See also: Epsom Salts Cave, and the Indiana Saltpetre Cave
.
The exact date of See also: discovery is not known; but early records show it to have been pre-empted by a Dr See also: Adams in 1812 for the manufacture of saltpetre, and his vats and hoppers are still to be seen
.
After the War of 1812 he relinquished his claim; and in 1819 the ground was bought from the
See also: United States See also: government by See also: Henry P
.
Roth-
See also: rock, whose heirs are its owners
.
The earliest account is in See also: Flint's Geography (1831); the first official report of it was by Dr R
.
T
.
See also: Brown (1831); and it was first mapped by the writer (1855), whose map was revised by
See also: John Collett,
See also: state geologist (1878)
.
No instrumental survey has been made, nor have all its intricate windings been explored
.
Its known passages aggregate more than 23 M. in length, and 144 places are named as noteworthy
.
The " Old Cave " contains the saltpetre See also: works, and ends in a remarkable chamber exactly 144 ft. long and 56 ft. wide, in which stands the Pillar of the Constitution, a stalagmitic See also: column perfectly cylindrical and 71 ft. in circumference, entirely composed of crystalline carbonate of lime (satin-spar), fluted and snow-See also: white
.
A cavity in the column was first claimed by H
.
C
.
Hovey as a prehistoric
See also: quarry, proved to be such by the stag horns and See also: boulder pounders found in its vicinity
.
Hiscareful estimate of the See also: rate of stalagmitic growth showed that limo years would have been needed to See also: form the lip now covering the incision
.
In the N. arm of the newer See also: part of the cave, opened in 185o, is an immense See also: room, styled Rothrock's See also: Cathedral, loon ft. in circumference and zoo ft. high, with a rugged central See also: hill 135 ft. high, surmounted by statuesque stalagmites, near which is another quarry of satin-spar with similar fragments, pounders and aboriginal
See also: relics
.
When Mr Hovey visited this cave in 1855 he found many See also: extinct torches, See also: charcoal embers, poles and pounders, as well = y as numerous footprints, in the soft nitreous See also: earth of certain avenues, which were See also: left by exploring parties previous to the coming of the white See also: man
.
In the Pillared Palace a number of large alabaster shafts had been thrown down and fragments carried away
.
Near by were so-called " bear-wallows," which proved to be the remains of an aboriginal workshop, where masses of flint were broken into rectangular blocks; and spalls and flint-chips en-cumber the floor and choke the passage-way
.
Milroy's See also: Temple is a magnificent room, 10o by 15o ft. in its dimensions
.
It contains many remarkable formations; and its display of helictites, or See also: twisted stalactites, is unsurpassed
.
As Wyandotte Cave has no large streams and few pools or springs, its See also: fauna and See also: flora are not extensive
.
Formerly bears, wolves and other See also: wild animals took See also: refuge in its fastnesses; and bats, rats, mice and salamanders are frequent visitors
.
See also: Blind crawfish (Cambarus pellucidus)inhabit the Crawsh Spring
.
Cave crickets (Hadenoecus subterraneus) abound
.
A dozen kinds of See also: insects, with a few varieties of See also: spiders, flies and See also: worms, See also: complete the meagre See also: list
.
The florae include mainly forms brought in from the
outside. See also: aaa,y See also: wake
For more full descriptions of Wyandotte Cave and its contents, see Hovey's Celebrated See also: American Caverns, pp
.
123-153; Indiana State See also: Geological Reports, by R
.
T Brown, E
.
T
.
See also: Cox, John Collett and W
.
S
.
Blatchley; and concerning cave fauna reports and papers by C
.
H
.
Eigenmann, professor of zoology, Indiana State University . (H . C . |
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