Alluvium

Definition and stakes

Portrait of Sir Charles Lyell Sir Charles Lyell,  A Manual of Elementary Geology

“ It is not so easy as may at first appear to draw a clear line of distinction between the fixed rocks, or regular strata (rocks in situ or in place) , and alluvium. If the bed of a torrent or river be dried up, we call the gravel, sand, and mud left in their channels, or whatever, during floods, they may have scattered over the neighbouring plains, alluvium. The very same materials carried into a lake, where they become sorted by water and arranged in more distinct layers, especially if they inclose the remains of plants, shells, or other fossils, are termed regular strata. ”
Source: Gutenberg

Thomas Thomson,  Western Himalaya and Tibet

“ Where platforms of alluvium occupy the lateral ravines, they attain a very great thickness, seldom less than two hundred feet, and occasionally at least twice as much. They are generally cut off in steep cliffs by the river, beautifully showing the structure of the alluvium. In the sections of these masses of boulders and clay, I several times observed that the strata, instead of being horizontal, were highest in the middle and sloped gently downwards on either side. ”
Source: Gutenberg

J. A. Munk,  Arizona Sketches

“ In many of the canons where water flows continuously, effects are produced that are exactly the opposite of those ascribed to water erosion. Instead of the running water cutting deeper into the earth it has partly filled the canon with alluvium, thereby demonstrating nature's universal leveling process. ”
Source: Gutenberg

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