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Thus it cannot be denied that the masses which today form our highest mountains were originally in
Thus it cannot be denied that the masses which today form our highest mountains were originally in
Thus it cannot be denied that the masses which today form our highest mountains were originally in
Thus it cannot be denied that the masses which today form our highest mountains were originally in
Thus it cannot be denied that the masses which today form our highest mountains were originally in
Thus it cannot be denied that the masses which today form our highest mountains were originally in
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Georges Cuvier:
The traces of upheavals become more impressive when one moves a little higher, when one gets even cGeorges Cuvier:
The older the layers, the more each of them is uniform over a great extent; the newer the layers, tGeorges Cuvier:
The lowest and most level land areas show us, especially when we dig there to very great depths, noGeorges Cuvier:
The appearance of the bones of quadrupeds, especially those of complete bodies in the strata, tellsGeorges Cuvier:
Secondly, the nature of the revolutions which have altered the surface of the earth must have had aGeorges Cuvier:
My object will be, first, to show by what connections the history of the fossil bones of land animaGeorges Cuvier:
Moreover, it thus follows that not a great deal of time was needed for the large animals of the thrGeorges Cuvier:
Hence the same instant which killed the animals froze the country where they lived. This event wasGeorges Cuvier:
But the revolutions and changes which are responsible for the present state of the earth are not liGeorges Cuvier:
It is evident that one cannot say anything demonstrable about the problem before having resolved th