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Ifsubsequently, a similar origin of the planets will be satisfactorily proved,it will serve as a striking explanation of those highly heterogeneousactions that produced the original homogeneous cause, but forour present purpose it is enough to point to the fact that bymutual attraction of particles of irregular nebulous mass in the resultturns out the condensation, rotation, heat and light. The conclusion arising fromhypothesis nebulous mass, there is the fact that the Earth had to be inthe red-hot state; and find whether or not the hypothesis of a nebulous mass, in anycase, this initial raskalennoi Land now proved the inductiveor if not proven, then at least brought to such a highthe degree of probability that is generally accepted geological doctrine.Let's look first of all on the astronomical properties of this oncemolten ball. The results of rotation are tapered at the polesform him the next day and night, and (under the influence of the moon and, to a lesserdegree the Sun) the tides, and atmospheric water. The inclination of hisaxis produces a simultaneous and consistent differences occurring inits surface, respectively, and so on. Thus, the reproductionaction obvious. We have already mentioned the various differentiations,dependent on the gradual cooling of the Earth, what are the formation of crusthardening gaseous elements, the precipitation of water, etc., here we are againaddress them actually, in order to indicate the simultaneousthe action of one causes reduction of heat. Pay, however, nowour attention to increased changes arising subsequently fromduration of action one of the reasons.
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