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Going into great details, we findfirst, that the geologists of the present time instead to considerflushing soil is produced by rain and rivers, as the only reasoncontributing to the smoothing of the continents and producing the irregularities of the earthsurface, the flushing of a particular cause of these irregularities,further, we find that new layers formed on the bottom of the sea, areproducts not only the river of rain, but partly occur fromthe actions of waves and tides on the shore. Second, we see thatGolonova the idea of raising the soil by the action of underground forces not onlymodified equating these underground forces those forces thatoperate in an ordinary earthquake, but is even of the neweststudies that in addition increases the earth's surface the same way happenand down her that as a local enhancement, and the universal, continental,belong to the same category as all these changes are, in allprobability investigation ongoing subsidence of the crust inthe cooling and Contracting nucleus. Finally, third, we see that in addition to thesethe main two opposing figures of modern Geology recognizes anothera few other minor influences what, for example, the impact of glaciersand icy mountains, the impact of coral polyps, the impact of protozoa with siliceous orcalcareous shell, each of these effects, no matter how insignificant they areseem, is able to produce graduallysignificant changes in the earth's surface. So, the latest progress of Geologystill further pushed us away from the original ideas. Instead of onecatastrophic causes, acting once everywhere, as taughtWerner, is one common causes of constant, who had met after a longtime opposition from catastrophic causes likeimagine Gotten, we recognize now the action several reasons, whichall more or less common and constant. To explain the phenomena presentedthe crust of the earth, we no longer resort to hypothetical effects, but everyday more clearly see that these phenomena came from the forces, very similar to thethose operating in the present time - from the forces acting ininfinitely varied combinations in the continuation immeasurably long periodstime.
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