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This hypothetical explanation, which should be taken onlyin accordance with its true value, go to a more positivetestimony. Currently, geologists and physiogeography accepted thatThe earth was initially a molten mass of the substance. If it wasso really, the substance that was initially uniform in yourthe composition and strength of the movement of heated liquid had to berelatively homogeneous with respect to the temperature; it should be surrounded byatmosphere, consisting of elements of air and water, and part ofvarious other elements that turn into gases at high temperature.Slow cooling by radiation, is still constantlycontinuing in the sizes that it is impossible to determine, and, moreover, althoughoriginally far more rapid than now, but stillrequiring excessive time to produce somean abrupt change is cooling had to have a finalthe result of hardening the part that is most capable of separatewarmth is surface.
Although the lack of evidence, they are notable to point out the many phase, through which passed the existingtypes before reached its present state, or to reproducethose influences which were the cause of gradual changes, but they canto show that all existing species, both animal and vegetable,being placed in conditions different from their former conditions immediatelybegin to undergo some changes in its structure, prisposobleniethem to new conditions. It can be shown that these changes occur insubsequent generations until, until, finally, the new conditions will not becomenatural for them. These changes can be displayed on the cultivation of plantsdomashneye animals and different races of mankind. It can be shown thatthe degree of change thus occurred, are often - as, for example,in dogs - significant changes which provide the basis for the differencesspecies. It is possible to show (which is still a matter of debate), is there somethese modified forms are only varieties or separate species. Canshow also that the changes daily taking place in ourselves - a skill thatacquired by long practice, and the loss of it when practice ceases -the strengthening of the passions, is constantly satisfied, and the weakening of such thatsuppressed the development of any abilities, physical, moral andmentally, in proportion to its exercise, - all this is easily explained onthe basis of the same principle. Thus it is possible to show that in allorganic nature are known to alter the factor that supportersthe hypothesis admits a basis of these specific differences, factor,which, although it acts slowly, but may over time producesignificant changes, if that is conducive circumstances, factor,which for millions of years and under the influence of various conditionstaken by Geology, had, in all probability, to make knownthe amount changes.
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