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Cooling of the Earth causesa it compression. This is what initially formed the crustimmediately becomes too broad for the tapering of the core andinability to support itself, inevitably emulates the core. Butspheroidal shell of gap to achieve contact withinside it less spheroidal body - she needs to get wrinkledlike wrinkles the skin of the Apple, when its content is reducedby evaporation. As cooling increases, the bark becomesthicker, the wrinkles produced by this compression must increase, increasing,finally, to hills and mountains, and the latter mountain system, formed in thisby the way, should not only be higher, as we see it, but long asand we also see it. Thus, leaving aside other changingstrength, we see a large heterogeneity of surface has arisen from onecauses loss of heat, the heterogeneity, the analogy which a telescopeshows us on the surface of Mars and which opens in a slightly differentform on the moon, where the activity of water and air did not take place. But we havemore to pay attention to another kind of heterogeneity at the earth's surface,depending on similar and simultaneous causes. While the crust was stillthin, not only the elevation, by its compression, had to beminor, but and depressions between these elevations hadgreater evenness to lie on under them liquid spheroid; and the water inthose Arctic and Antarctic countries, where it first condensed, mustwas distributed evenly.
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