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- The cities and roads are where they are because of what the Fall Line is: a more or less invisible, small, underground cliff—an escarpment—that marks the old edge of the continent. On the Fall Line’s west side, the high side, are tough crystalline rocks; on the east side, the low side, are soft, easily moveable sediments.www.theatlantic.com/science/archive/2018/02/following-the-fall-line/553442/
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