Flagg's The Far West, 1836-1837, part 1Flagg, Edmund
History
Flagg's The Far West, 1836-1837, part 1
Flagg, Edmund
Illinois -- Description and travel; Mississippi River Valley -- Description and travel; Missouri -- Description and travel
of eighty feet in height. The appearance is striking, standing, as it
does, distinct from anything of a kindred character for miles above
and for some distance below. Passing several fine farms, which sweep
down to the water's edge, a second range of cliffs are discovered,
similar to those described in altitude and aspect; but near the base,
through the dark cypresses skirting the water, is perceived the ragged
entrance to a large cavernous fissure, penetrating the bluff, and
designated by the name of "Rock-Inn-Cave."[36] It is said to have
received this significant appellation from emigrants, who were
accustomed to tarry with their families for weeks at the place when
detained by stress of weather, stage of the river, or any other
circumstance unfavourable to their progress.
It was near noon of a beautiful day when the necessary orders for
landing were issued to the pilot, and our boat rounded up to the low
sand-beach just below this celebrated cavern. As we strolled along the
shore beneath "the precipitous, black, jagged rocks" overhanging the
winding and broken pathway towards the entrance, we could not but
consider its situation wild and rugged enough to please the rifest
fancy. The entrance, {43} at first view, is exceedingly imposing; its
broad massive forehead beetling over the visiter for some yards before
he finds himself within. The mouth of the cavern looks out upon the
stream rushing along at the base of the cliff, and is delightfully
shaded by a cluster of cypresses, rearing aloft their huge shafts,
almost concealed in the luxuriant ivy-leaves clinging to their bark.
The entrance is formed into a semi-elliptical arch, springing boldly
to the height of forty feet from a heavy bench of rock on either side,
and eighty feet in width at the base, throwing over the whole a
massive roof of uniform concavity, verging to a point near the centre
of the cave. Here may be seen another opening of some size, through
which trickles a limpid stream, and forming an entrance to a second
chamber, said to be more extensive than that below. The extreme length
of this cavern is given by Schoolcraft[37] as one hundred and sixty
feet, the floor, the roof, and the walls gradually tapering to a
point. The rock is a secondary limestone, abounding with testacea and
petrifactions, a fine specimen of which I struck from the ledge while
the rest of our party were recording their names among the thousand
dates and inscriptions with which the walls are defaced.
Public-domain text, read in full here on John Shaqi.
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