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In Aberdeen granite are often found lumpsunmelted gneiss, finally, we ourselves can attest to thatLoch Sunart represent abundant evidence that granitethis area, when it was molten, contained not quitemolten boulders of sedimentary rocks. And that's not all. Fifty years agoago believed that all the granite rocks of primitive, or existed beforeany of the sedimentary formations, but is currently "very difficultto specify at least one of the granite mass, with respect to which it would be possibleon the basis of evidence to say that it is the most ancient of all knownlayers, enclosing fossils". In short, manythe evidence clearly show that all the layers of sediments can throughcontact with molten substance that make up the core of the globe,or at least only through proximity to the substance to be completelymelted or only partially melted or strained to the extentwhat is needed to produce fusion of the particles and that, depending onthe temperature to which they were heated, and the circumstances under whichthey cool down, they take the form of the granite, the porphyry, the ladder, gneiss, it is some other rocks. Next, we can clearly see that, thoughlayers of different ancient times, were subjected to that kind of change, theless more likely to have changed the most ancient strata, as because theycommonly lying nearer to the center of the fire action, and because theyhas been longer subjected to this action. It is evident, therefore, that sedimentarystrata, the antiquity of which goes beyond the known limit, unlikely to befind in unconverted condition, and the strata more ancient than thesethe latter probably was in the old days, molten. So, if withinlast time that lasted an indefinite period of time, acted the sameforces - water and fire, which are in force at the present time, andthe state of the earth's crust could be the same as it is to us now. Weyou do not have any data on the basis of which could decide the exactthe limits of the period in which occurred the formation and destructionlayers.
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