See also:WYANDOTTE See also:CAVE
, a See also:cave in Jennings township, See also:Crawford See also: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 See also:early territorial See also: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 See also:Blue river, whose See also:original name, the See also:Wyandotte, was transferred to the cave by See also: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 See also: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
- ADAMS, ANDREW LEITH (1827-1882)
- ADAMS, CHARLES FRANCIS (1807-1886)
- ADAMS, HENRY (1838— )
- ADAMS, HENRY CARTER (1852— )
- ADAMS, HERBERT (i858— )
- ADAMS, HERBERT BAXTER (1850—1901)
- ADAMS, JOHN (1735–1826)
- ADAMS, JOHN QUINCY (1767-1848)
- ADAMS, SAMUEL (1722-1803)
- ADAMS, THOMAS (d. c. 1655)
- ADAMS, WILLIAM (d. 162o)
Adams in 1812 for the manufacture of saltpetre, and his vats and hoppers are still to be seen
.
After the See also: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
- HENRY (1129-1195)
- HENRY (c. 1108-1139)
- HENRY (c. 1174–1216)
- HENRY (Fr. Henri; Span. Enrique; Ger. Heinrich; Mid. H. Ger. Heinrich and Heimrich; O.H.G. Haimi- or Heimirih, i.e. " prince, or chief of the house," from O.H.G. heim, the Eng. home, and rih, Goth. reiks; compare Lat. rex " king "—" rich," therefore " mig
- HENRY, EDWARD LAMSON (1841– )
- HENRY, JAMES (1798-1876)
- HENRY, JOSEPH (1797-1878)
- HENRY, MATTHEW (1662-1714)
- HENRY, PATRICK (1736–1799)
- HENRY, PRINCE OF BATTENBERG (1858-1896)
- HENRY, ROBERT (1718-1790)
- HENRY, VICTOR (1850– )
- HENRY, WILLIAM (1795-1836)
Henry P
.
See also:Roth-See also:rock, whose heirs are its owners
.
The earliest See also:account is in See also:Flint's See also:Geography (1831); the first See also:official See also:report of it was by Dr R
.
T
.
See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
Brown (1831); and it was first mapped by the writer (1855), whose See also: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. See also:long and 56 ft. wide, in which stands the See also:Pillar of the Constitution, a stalagmitic See also:column perfectly cylindrical and 71 ft. in circumference, entirely composed of crystalline carbonate of See also:lime (satin-spar), fluted and See also:snow-See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
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 See also: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 See also:lip now covering the incision
.
In the N. See also: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
- HILL (0. Eng. hyll; cf. Low Ger. hull, Mid. Dutch hul, allied to Lat. celsus, high, collis, hill, &c.)
- HILL, A
- HILL, AARON (1685-175o)
- HILL, AMBROSE POWELL
- HILL, DANIEL HARVEY (1821-1889)
- HILL, DAVID BENNETT (1843–1910)
- HILL, GEORGE BIRKBECK NORMAN (1835-1903)
- HILL, JAMES J
- HILL, JOHN (c. 1716-1775)
- HILL, MATTHEW DAVENPORT (1792-1872)
- HILL, OCTAVIA (1838– )
- HILL, ROWLAND (1744–1833)
- HILL, SIR ROWLAND (1795-1879)
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 See also:Palace a number of large See also:alabaster shafts had been thrown down and fragments carried away
.
Near by were so-called " See also: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 See also: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 See also: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 See also: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, See also:professor of See also:zoology, Indiana State University
.
(H
.
C
.
End of Article: