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Along each shoreline, wash off little by little waves are formedsand, silt and pebbles. This scree, covering neighbouring parts of the sea bottom,has each area its more or less sharp features,- defined property destroyed layers. In the English channel it is notthe same as in the Irish Strait; on the West coast of Ireland it is not the same,on the East, etc. In the mouth of each great river deposited sedimentdiffering more or less from the sediment other rivers of color and composition andforming where the red layers, where the yellow, where the brown, gray oroff-white. In addition to these various formations occurring in the river deltas andalong the coast, there are other, much more extensive and more sharplydifferent from one another. At the bottom of the Aegean sea's gathering in the presenttime layer of pteropod shells, which, no doubt, over time, formthe limestone rock. Several hundred thousand square miles of the ocean bottom betweenThe UK and North America is covered with a layer of chalk, and an extensivespace Pacific astrawtsa sediments of coral limestone. Thisway over the entire space of the globe is formed, and is currentlycountless layers of sharply differing from each other inlithology. Name at random any part of the seabed andask similar whether the precipitation is formed in it, with rainfall in any othera distant part of the sea bottom, and will almost certainly be no. Allthe probabilities are on the side not of identity, but rather diversity.
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