Scientific American Supplement, No. 401, September 8, 1883Various
Science
Scientific American Supplement, No. 401, September 8, 1883
Various
Science -- Periodicals
at a depth of three hundred feet they attained a thickness of three or
four inches. Upon examination, it was found that a yellow wax could be
made of a portion of this substance, and at once a substitute for wax
was manufactured.
The discovery caused an excitement like the oil fever of 1865 in
America. A large number of leases were made. When I saw the wells of
Pennsylvania, in 1879, there were more than two thousand. The owner
of the land received one-fourth of the product, and the miners
three-fourths. In the petroleum region, the leases at first were whole
farms, then they were reduced to 20, then 10, then 5, and at last to 1
acre, which is a square of 209 feet.
But in the ozokerite region of Poland, where everything is done on a
small scale, when compared with like enterprises in this country, the
leases were on tracts thirty-two feet square. These were so small that
the surface was not large enough to contain the earth that had to be
raised to sink the shaft; consequently the earth had to be transported
to a distance, and, when I saw it, there was a mound sixty or seventy
feet high. Its weight had become so great that it caused a sinking
of the earth, and endangered the shafts to such an extent that the
government ordered its removal to a distance and its deposit on ground
that was not undermined. The shafts are four feet square, and the sides
are supported by timbers six inches through, which leaves a shaft three
feet square. The miner digs the well or shaft just as we dig our water
wells, and the dirt and rock are hoisted up in a bucket by a rope and
windlass. But one man can work in the shaft at a time. For many years
no water was found; but, as there is a deposit of petroleum under the
ozokerite, at a depth of six hundred feet from the surface, the miners
were troubled with gas. This is got rid of by blowing a current of fresh
air from a rotary fan through a pipe extending down the shaft as fast as
the curbing of timber is put in place. The ozokerite is embedded in a
very stiff blue clay for a depth of several hundred feet; below, it is
interlaid with rock. [Specimens of crude and manufactured ozokerite were
on exhibition, through the kindness of Dr. J. S. Newberry.]
Public-domain text, read in full here on John Shaqi.
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