presented as being worth
investigation. All are north of Tompkinsville, the county seat.
(1) A rock house in the conglomerate sandstone on the land of Dr. E.E.
Palmer, 7 miles north of Tompkinsville, shows smoke stains on the
ceiling, and some flint chips among the gravel and earth in front
where they have been exposed by water dripping over the face of the
cliff. There is, however, only 2 to 4 feet of space between the earth
floor and the roof, across the cave from side to side, a distance of
20 feet, and from the front to a point 10 feet back. From this rear
portion the earth slopes downward, parallel with the roof of the cave,
to the wall behind. The amount of descent could not be accurately
ascertained owing to the cramped space, but seems to be 5 or 6 feet.
At about that level on the outside a ledge was found on both sides of
the entrance and appears to continue across. If so, the earth covers
the part immediately in front of the cave. Neither tools nor men could
be found to do any trenching, but it is not probable the shelter was
ever high enough for a man to stand erect in, because most, or all, of
the floor earth must have come from the ceiling.
(2) A mile north of Dr. Palmer's is the McCreary Cave. The entrance is
from 60 to 70 feet across and the cavern reaches back fully a hundred
feet without any diminution of breadth. Two branches then start under
the hill. Each has been explored more than a mile. From each branch
flows a considerable brook. They unite near the entrance, sink into
the floor, and reappear as a strong spring 30 feet lower in the ravine
leading from the cave. The earth is not more than 3 feet deep near the
front. It becomes greater in amount farther back, but is wet
everywhere below the level of the running water, consequently no
excavation was practicable. Flood marks show that the whole floor,
except in places a strip along the side walls, is completely submerged
at times. On one side a rock ledge or shelf above reach of the water
is covered with dry loose earth from 1 to 3 feet deep. This has been
dug up in nearly every part by treasure seekers, but nothing of human
workmanship has ever been found.
(3) The Belcher Cave is 7 miles northwest of Tompkinsville. It is also
called Mill Cave, because a gristmill near the foot of the hill below
it is run by the outflowing stream. The entrance is wide and high; the
front chamber or vault is fully a hundred feet across each way. But
the bedrock
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