Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
When these lands were taken into cultivation little or no
attention was paid to the direction of the furrows and rows
of corn and cotton; most commonly the plowing was done
“up-hill and down,” so that the “dead-furrow” afforded
a ready opportunity for the formation of washes cutting
into the subsoil, during the torrential rains sometimes
falling during the summers. Even when filled with soil by
plowing, these washes would frequently re-open during rains,
shedding the soil in a muddy flood upon the lower lands. The
washing-away of the surface soil, thus brought about, of
course diminished the production of the higher lands, which
were then commonly “turned out” and left without cultivation
or care of any kind. The crusted surface shed the rain water
into the old furrows, and the latter were quickly deepened
and widened into gullies—“red washes”—whose presence
rendered any resumption of cultivation difficult. In the
course of a few years the soil-stratum of brown loam was
penetrated into the loose or loosely cemented sand which
underlies it almost everywhere, and is very readily washed
away. Soon the water, gaining yearly in volume, undercut the
loam stratum so as to cause it to “cave” into gullies in
huge masses, which with the sand were carried into the
valleys adjacent, filling the beds of the streams so as to
cause their flow to disappear under the flood of sand. As
the evil progressed, large areas of uplands were denuded
completely of their loam or culture stratum, leaving nothing
but bare, arid sand, wholly useless for cultivation; while
the valleys were little better, the native vegetation having
been destroyed and only hardy weeds finding nourishment on
the sandy surface.
[Illustration: FIG. 40a.—Erosion in Mississippi Table Lands, causing
destruction of agricultural value both of Uplands and Valleys. (McGee,
12th Ann. Rept. U. S. G. S., 1890-91.)]
In this manner whole sections, and in some portions of the
State whole townships of the best class of uplands have
been transformed into sandy wastes, hardly reclaimable by
any ordinary means, and wholly changing the industrial
conditions of entire counties; whose county seats even in
some instances had to be changed, the old town and site
having, by the same destructive agencies, literally “gone
down hill.” This destruction of lands was greatly aggravated
by the civil war, during which, and for some time after,
large areas of lands once under cultivation were left to the
mercy of the elements.
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