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Meanwhile, the influence of this desire to take "local" events for the overallstill so much comments in geological speculations, that even the mostcautious people can't seem to completely get rid of it. 158visit their Grounds of Geology sir Charles Lyell says: "Based on the fact that in England a group of red marl andred Sandstone, containing salt and gypsum, which lies between liason andcoal formation, the geologists felt entitled to refer to the sameperiod all strata of red marl and Sandstone with the admixture of salt or gypsum,coming across not only in different parts of Europe, but in North America, Peru, India, the salt deserts of Asia and Africa, in short, in all parts of thelight... in Vain they argued, pointing to the improbability of the hypothesis,assuming all the flowing waters of the globe at the same time onceconcluded used red. But finally the rashness of this conclusion,attributing equal antiquity with all the layers of redmarl and Sandstone, was enough to convict the discovery that, even in Europethese strata belong to many different epochs." But, despite the fact that in this place and in others who Express the samethe idea of sir Charles Lyell rebelled against outlined here views himselfhe did not seem to have freed him. Although he has a positiverejects the old hypothesis that the whole space of the globe the samecontinuous layers lie on one another in the correct order, likethe petals of the bulb, however, he writes as though geologicthe "system" really followed one after another in that order.
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