Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 1 of 2]Weld, Isaac
History
Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 1 of 2]
Weld, Isaac
Canada -- Description and travel -- Early works to 1800; United States -- Description and travel -- Early works to 1800
It has already been mentioned, that the predominant soil to the eastward
of the Blue Ridge is a red earth, and that it is always a matter of some
difficulty to lay down a piece of land in grass, on account of the
rains, which are apt to wash away the seeds, together with the mould on
the surface. In Bottetourt County, on the contrary, the soil consists
chiefly of a rich brown mould, and throws up white clover spontaneously.
To have a rich meadow, it is only necessary to leave a piece of ground
to the hand of nature for one year. Again, on the eastern side of the
Blue Mountains, scarcely any limestone is to be met with; on the
opposite one, a bed of it runs entirely through the country, so that by
some it is emphatically called the limestone county. In sinking wells,
they have always to dig fifteen or twenty feet through a solid rock to
get at the water.
[Sidenote: INSECTS.]
Another circumstance may also be mentioned, as making a material
difference between the country on one side of the Blue Ridge and that on
the other, namely, that behind the mountains the weevil is unknown. The
weevil is a small insect of the moth kind, which deposits its eggs in
the cavity of the grain, and particularly in that of wheat; and if the
crops are stacked or laid up in the barn in sheaves, these eggs are
there hatched, and the grain is in consequence totally destroyed. To
guard against this in the lower parts of Virginia, and the other states
where the weevil is common, they always thresh out the grain as soon as
the crops are brought in, and leave it in the chaff, which creates a
degree of heat sufficient to destroy the insect, at the same time that
it does not injure the wheat. This insect has been known in America but
a very few years; according to the general opinion, it originated on the
eastern shore of Maryland, where a person, in expectation of a great
rise in the price of wheat, kept over all his crops for the space of six
years, when they were found full of these insects; from thence they have
spread gradually over different parts of the country. For a considerable
time the Patowmac River formed a barrier to their progress, and while
the crops were entirely destroyed in Maryland, they remained secure in
Virginia; but these insects at last found their way across the river.
The Blue Mountains at present serve as a barrier, and secure the country
to the westward from their depredations[24].
Footnote 24:
Public-domain text, read in full here on John Shaqi.
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