The Writings of Thomas Jefferson, Vol. 8 (of 9): Being His Autobiography, Correspondence, Reports, Messages, Addresses, and Other Writings, Official and PrivateJefferson, Thomas
History
The Writings of Thomas Jefferson, Vol. 8 (of 9): Being His Autobiography, Correspondence, Reports, Messages, Addresses, and Other Writings, Official and Private
Jefferson, Thomas
United States -- Politics and government -- 1775-1783; United States -- Politics and government -- 1783-1865
growth of shells unattached to animal bodies, would have been
that of his theory. But he has not established it. He has not
even left it on ground so respectable as to have rendered it an
object of inquiry to the _literati_ of his own country. Abandoning
this fact, therefore, the three hypotheses are equally unsatisfactory;
and we must be contented to acknowledge, that this
great phenomenon is as yet unsolved. Ignorance is preferable
to error; and he is less remote from the truth who believes nothing,
than he who believes what is wrong.
There is great abundance (more especially when you approach
the mountains) of stone, white, blue, brown, &c., fit for the chisel,
good mill-stone, such also as stands the fire, and slate stone. We
are told of flint, fit for gun-flints, on the Meherrin in Brunswick,
on the Mississippi between the mouth of the Ohio and Kaskaskia,
and on others of the western waters. Isinglass or mica is in
several places; loadstone also; and an Asbestos of a ligneous texture,
is sometimes to be met with.
Marle abounds generally. A clay, of which, like the Sturbridge
in England, bricks are made, which will resist long the
violent action of fire, has been found on Tuckahoe creek of
James' river, and no doubt will be found in other places. Chalk
is said to be in Botetourt and Bedford. In the latter county is some
earth believed to be gypseous. Ochres are found in various parts.
In the lime-stone country are many caves, the earthy floors
of which are impregnated with nitre. On Rich creek, a branch
of the Great Kanhaway, about sixty miles below the lead mines,
is a very large one, about twenty yards wide, and entering a hill
a quarter or half a mile. The vault is of rock, from nine to fifteen
or twenty feet above the floor. A Mr. Lynch, who gives
me this account, undertook to extract the nitre. Besides a coat
of the salt which had formed on the vault and floor, he found
the earth highly impregnated to the depth of seven feet in some
places, and generally of three, every bushel yielding on an average
three pounds of nitre. Mr. Lynch having made about ten
hundred pounds of the salt from it, consigned it to some others,
who have since made ten thousand pounds. They have done
this by pursuing the cave into the hill, never trying a second
time the earth they have once exhausted, to see how far or soon
it receives another impregnation. At least fifty of these caves
are worked on the Greenbriar. There are many of them known
on Cumberland river.
Public-domain text, read in full here on John Shaqi.
The Writings of Thomas Jefferson, Vol. 8 (of 9): Being His Autobiography, Correspondence, Reports, Messages, Addresses, and Other Writings, Official and Private — John Shaqi
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