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Evidence of the facts so uncertain, that these processes couldcontinue for a period ten times greater than thatmeasured all of our groups of sedimentary formations. But not only that, the present form of the earth's crust does not represent us anydata to determine the beginning of these processes, moreover, that somecircumstances allow us to assume that the beginning of this applies toimmeasurably distant past, is immeasurably far, evento the great geological periods - we have no shortage of evenpositive evidence gives us the right to take immeasurablethe remoteness of this beginning of Latest Geology was elevated to irrefutable truththese facts, which are incompatible with the belief that education and the destruction ofseams started at the time when he formed the Cambrian rockor even in any other recent period. To prove it,it will be enough to cite one fact from Siluria. Sir R. Murchison calculatesthe vertical thickness of Silurian strata in the Wallis ranges between 26000 and 27 000 feet, in other words, is approximately five milesif to this we add the vertical thickness of the Cambrian strata, onwhich are Silurian, in accordance with them in the bends and direction, we, believing the smallest numbers, you get a depth of approximately sevenmiles. All geologists accepted that this is a huge accumulation of layers shouldbeen going on slowly settling plane. These layers couldto lie one above the other in such a correct order, if the crust in thisthe place is not settled or continuously, or by intermittent, smalldepressions. But such a huge subsidence would occur if the earththe bark had no significant thickness of the Molten core of the earth constantlytends to take the form of a flattened spheroid correct any compressionits crust below the surface of equilibrium, and any elevation of the crust abovethis surface needs to meet a lot of resistance.
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