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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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14<br />

replaced through weathering <strong>of</strong> fresh rock, the soil, the landscape, and<br />

whole plant communities evolve together because <strong>of</strong> their mutual interdependence<br />

on the balance between soil erosion and soil production.<br />

Such interactions are apparent even in the form <strong>of</strong> the land itself. Bare<br />

angular hillslopes characterize arid regions where the ability <strong>of</strong> summer<br />

thunderstorms to remove soil chronically exceeds soil production. In wetter<br />

regions where rates <strong>of</strong> soil production can keep up with soil erosion, the<br />

form <strong>of</strong> rounded hills reflects soil properties instead <strong>of</strong> the character <strong>of</strong><br />

underlying rocks. So arid landscapes where soil forms slowly tend to have<br />

angular hillslopes, whereas humid and tropical lands typically have gentle,<br />

rolling hills.<br />

skin <strong>of</strong> the earth<br />

<strong>Erosion</strong><br />

Weathering<br />

Figure 1. <strong>The</strong> thickness <strong>of</strong> hillslope soils represents the balance<br />

between their erosion and the weathering <strong>of</strong> rocks that produces<br />

soil.

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