CHAPTER V.

OTHER STONE COUNTY CAVES.

GENTRY CAVE.

The cave nearest to Galena, and the first visited by us, is Gentry Cave,

situated a mile and a half from town. We started in the mail coach, but

that vehicle met with a misfortune by no means unusual in that region,

the total wreck of a wheel. Having only that morning arrived from the

rich agricultural portion of the State where no surface rock can be

found, we were pleased enough with the prospect of a walk in such

charming spring weather, and set out with a cheerful certainty that the

rough place in the road would soon be passed. But the school of

experience is always open for the reception of new-comers and we were

admitted to full duty without question.

The topography was nearly as broken, in its way, as the natural "piking"

spread over it, and very beautiful with the dense forests lighted by the

slanting yellow rays of the afternoon sun. The way leads up to the

"ridge road" which is at length abandoned for no road at all, and

descending through the forest, more than half the distance down to the

James River flowing at the base of the hill, we come suddenly in view of

the cave entrance, which is probably one of the most magnificent pieces

of natural architecture ever seen.

Rounding a corner by a narrow path, we step onto a covered portico

ninety-seven feet long, with an average width of ten feet. The floor is

smooth and level, as also is the ceiling, which is nine feet above,

supported by handsomely carved pillars and rising in a gray cliff

projecting from the slope of the hill above, out to the brink of the

more abrupt descent to the water's edge ninety feet below. Between the

pillars are three large door-ways into the cave. The comparison

suggested is an Egyptian temple, and the idea is continued within, where

there are no chambers as in other caves; but instead, the entire

interior is a labyrinth of passages winding about in every direction

among an uncounted number of low massive pillars, some supporting a low

ceiling and others connected by high arches, the highest point being

estimated at sixty feet, but appearing to be more, because the enclosed

space rising to a dome is so narrow that the point of view is

necessarily directly underneath.

All exposed surfaces of pillars and walls inside the cave are of clay or

a soft porous rock having the same appearance, and are covered with

curious little raised markings like the indescribable designs of mixed

nothing generally known as "Persian patterns." This is, of course,

easily explained; the clay being the residuum from disintegrated

limestone, the markings described are the harder portions of the rock

remaining after particles of clay had been carried out by flowing water

while the disintegrating process was yet incomplete.

The Drinking Fountain is considered the great attraction of the cave,

and appears to have been fashioned to suggest a model for the handsome

soda fountains belonging to a later period. The water bowl is a large

depression worn in the top of a rock which seems to have been built into

the wall. In front it is five feet high and nine feet across, with

artistic corners approximately alike, and at the back ornamental carving

extends upward towards the ceiling with an opening through the wall at

the center. This opening is divided by a short column down which water

trickles to supply the bowl. The ceiling here is about thirty-five feet

high and most of the exposed surface is a blue-gray limestone. Only one

portion of Gentry Cave has received a deposit of dripstone and even that

is of limited extent, and located at the end of a narrow slippery

passage between high, slippery walls.

The fine entrance is of grey limestone in undisturbed horizontal strata,

and this is so plainly marked in the roof-supporting pillars as to give

them the appearance of having been prepared by skillful hands, in

several blocks, and afterwards arranged in place without the aid of

mortar. Unfortunately, all efforts to photograph this wonderful portico

have failed to give satisfaction--its position above the river being

such as to afford no point for the proper placing of the camera; but a

second visit made for the purpose of trying was far from being a loss,

and part of the reward consisted of finding among the sheltered rocks,

scarcely three feet above the floor, two humming birds' nests with their

treasure of small eggs, and our little companion who discovered them was

pleased to leave them untouched.

SUGAR TREE HOLLOW CAVE.

The name of this cave is due to the fact that the approach is through a

"hollow" well wooded with sugar maple trees. It is two miles from Galena

and the drive a beautiful one, as much of the way is through the forest

without a road, but with a charming little rushing, crooked stream of

clear, cold water: and in places the green slopes give way to mural

bluffs of grey limestone in undisturbed strata.

The entrance to the cave is through a hole about two feet high by three

in width, into which we went feet first and wiggled slowly down an

incline covered with broken rock, for a distance of fifteen feet, where

a standing depth is reached. A flat, straight, level ceiling extends

over the whole cave without any perceptible variation, and this is

bordered around its entire length and breadth with a heavy cornice of

dripstone, made very ornamental by the forms it assumes, and the

multitude of depending stalactites that fall as a fringe around the

walls. The line of contact between the cornice and ceiling is as clear

and strong as if both had been finished separately before the cornice

was put in place by skillful hands.

Dripstone covers the walls, which vary in height from one foot to twenty

feet, according to the irregularities of the floor, just as the width of

this one-room cave varies with the curves of the walls, which are

sweeping and graceful, the average being twenty-nine feet, but is much

greater at the entrance where the entire slope extends out beyond the

body of the cave. The length, from north to south, measures two hundred

and thirty-three feet exclusive of an inaccessible extension.

The south end of the cave rises by a steep slope to within a foot of the

ceiling with which it is connected by short but heavy columns of

dripstone, and another line of pillars of graduated height meets this

at right angles near the middle and ends in an immense stalagmite that

stands at the foot of the slope like a grand newel post.

There is no standing water in the cave, but everything is wet with drip,

and consequently the formation of onyx is actively progressing and the

south slope already mentioned shows a curious succession of changes in

cave affairs. By the slow action of acidulated waters, the grey

limestone deteriorated into a yellowish clay-bank, and now its particles

are being re-united into solid rock by the deposit of calcium carbonate

from the drip.

A careful test of the temperature of the atmosphere showed it to be

fifty-eight degrees.

PINE RUN CAVE.

This also is a small cave easily visited from Galena, being less than

two miles distant on the Marionville road. The entrance faces the road

and is on the same level, consequently it is one of the easiest to

visit. Just within is seen an opening in the ceiling, which we are told

is one of the two ways to an upper chamber whose chief attraction is a

dripstone piano, and the means of ascending is at hand in the form of a

Spanish ladder; but an attempt of that sort might even cause the new

woman to hesitate, and who hesitates is lost. The ascent was not made.

We advanced on a level with the road for a distance of perhaps twenty

feet, when the direction of the cave changed with a right angular turn

and we were in a straight gallery about two hundred and fifty feet long

and fifteen feet in width, the height gradually decreasing to about

three feet towards the upper end, where it widened out into a low but

broad chamber. The floor of this chamber is most beautiful. It is

composed of a series of connected calcite bowls whose beautifully fluted

rims are of regular and uniform height, and all are equally filled with

clear, still water. A great number of these basins are said to have been

destroyed by an ax in the hands of a poor witless creature for the

gratification of a burst of temper, and a magnificent stalagmitic

column, too heavy for one man to lift, lay detached and broken, in proof

that his body did not share the feebleness of his mind.

Beyond these basins is a low passage through which is found the second

entrance to the upper chamber, but the basins must be crossed in order

to reach it, and this is not an easy undertaking even when their water

supply is low, but in the early summer they are almost full.

There are said to be more than one hundred caves in Stone County, one of

which is supposed to be fully as large as Marble Cave, if not larger,

and is located in the southern part of the county but has not been

explored.

Mill Cave is in the northeast of the county, and at the entrance is a

saw mill which receives its working power from the cave stream. Inside

the cave there is a lake.

Hermit's Cave is a few miles from Galena, and is so named on account of

having been used as a dwelling by its former owner, who kept a coffin in

which he intended to place himself before the final summons, but was

overtaken by death in the forest and it was never used. He wrote sermons

on the rocks in his cave and one of these was afterwards removed.

Wolf's Den is also near Galena, and has been utilized as a sheep fold.

Wild Man's Cave is near Galena, and on account of the stories with which

people have been frightened, can only be visited by permission and with

a guard stationed at the entrance.

Reynard's Cave is four miles west of Galena on the farm of Dr. Fox, but

is so nearly filled up with dripstone that only crawling room remains.

The doctor's place is a fine locality for the collection of fossils.

At a distance of twelve miles from Galena there is said to be a fine

natural bridge, well worth a visit and sufficiently near Mill Cave for

both to be seen on the same trip.

In Bread Tray Mountain there is supposed to be a cave through which a

torrent rushes at times, that being the only way in which to explain the

strange thundering, roaring noise always heard after a storm, and never

at other times.

Besides being a wonderful cave region, and rich in the great abundance

and variety of native fruits and fine timber, Stone County has a vast

amount of mineral wealth, the heaviest deposits being zinc, lead and

iron, with some indications of silver, gold and copper, which have been

found but not in paying quantity. Already since the summer of 1896

several exceptionally pure bodies of zinc have been discovered, the

white ore of one recently opened deposit giving highly gratifying

indications as to extent. Prospecting may be said to have only commenced

in this very far from over-crowded region.

Cave Regions of the Ozarks and Black Hills · 第 5 / 16 章