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. ”
