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From inorganic bodies striking example is the old, longlying core. His cover is formed from a layer into the layer of rust. Thisthe layer thickens from year to year may be as long as the process is notreaches the phase in which the outer surface of the nucleus loses from rain andwind the same as the inside of the kernel gets from the futurethe oxidation of iron. When large mineral masses, stones, boulders, rocksgenerally find some action of the surrounding conditions, itseen only by the destruction of the surface, for example from freezing of absorbedwater: this fact, although rather mechanical than chemical, also illustratesthe essential truth. Sometimes there is therefore "a rolling stone". On the surface of the stoneformed more loose in its consistency layers, each of which hasthe greatest thickness in the more open places, quickly disintegrates under the action ofweathering and thus gives the mass of the shape is more rounded thanbefore, finally, being on the convex surface, it is easy to putin motion. But of all possible examples, maybe the most wonderfulone that can be seen on the West Bank of the Nile in Filah where the outerpart of a granite ridge 100 feet high turned over time incollection valuearray masses, varying from the yard and up to 6-8 feetdiameter.
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