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Dirt: The Erosion of Civilizations - Kootenay Local Agricultural Society

Dirt: The Erosion of Civilizations - Kootenay Local Agricultural Society

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more than three thousand years and then increased four- to fivefold when<br />

land clearance reached the crest <strong>of</strong> the range around 1880.<br />

Slavery wasn’t the only reason that erosion was a bigger problem in the<br />

South than in the North. Bare fields were particularly vulnerable to erosion<br />

in the South because rainfall intensities could reach up to one and a half<br />

inches per hour and the frozen ground and snow cover in the North<br />

allowed for little erosion during winter storms. In addition, the South’s<br />

topography is carved into rougher slopes than the gentle contours <strong>of</strong><br />

glacier-sculpted New England.<br />

<strong>Erosion</strong> continued to degrade the South after the Civil War. After surveying<br />

regional erosion problems in the southern Appalachians from 1904<br />

to 1907 for the U.S. Geological Survey, Leonidas Chalmers Glenn described<br />

farming practices little changed from colonial days.<br />

When first cleared, the land is usually planted in corn for about two<br />

or three years, is then for two or three years put in small grain ...and<br />

then back into corn for several years. Unless it is well cared for the land<br />

has by this time become poor, for it has lost its original humus. <strong>The</strong><br />

soil has become less porous and less able to absorb the rainfall and erosion<br />

begins. Means are rarely taken to prevent or check this erosion,<br />

so it increases rapidly and the field is soon abandoned and a new one<br />

cleared. ...Many fields are worn out and abandoned before the trees<br />

girdled in its clearing have all fallen. <strong>The</strong>n new grounds are usually<br />

cleared beside the abandoned field and the same destructive process<br />

is repeated.<br />

It took a few hundred years, but agricultural clearing was finally reaching<br />

into the remotest uplands <strong>of</strong> the region in a process much like what happened<br />

in Greece, Italy, and France. “In some places it was found that the<br />

entire surface wore away slowly, each heavy rain removing a thin layer or<br />

sheet <strong>of</strong> material, so that the fertile soil layer gradually wore thin and poor<br />

and the field was at last abandoned as worn out. ...Sheet-wash erosion is<br />

so slow and gradual that some farmers fail to recognize it and believe that<br />

their soils have deteriorated through exhaustion <strong>of</strong> the fertility, whereas<br />

they have slowly and almost imperceptibly worn away to the subsoil.” 29<br />

By the early 1900s more than five million acres <strong>of</strong> formerly cultivated<br />

land in the South lay idle because <strong>of</strong> the detrimental effects <strong>of</strong> soil erosion.<br />

When the government began to support aggressive soil conservation<br />

efforts in the 1930s, the new U.S. Soil Conservation Service did not <strong>of</strong>fer<br />

w estward hoe 141

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