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Meanwhile, the view that geological "system" is widespread, asuntenable, as first considered by us, it is equally absurd, ifto consider it a priori, and equally inconsistent with the facts. Although knowngroup of formations, classed together under the heading of oolitic, maybeto be distributed over more than one layerfrom this group, however, it is sufficient to examine the circumstances of its deposition,to ensure that the oolitic group, as well as each of the individualits constituent formations, has purely local origin and that are unlikely tocan exist in any other location group, it iscorresponding in its signs and the time of its inception andthe end. The formation of such groups requires the area of subsidence, inwhich were dumped layers that make up the group. Each area of subsidencemust be limited; and to assume that somewhere inanother place there are groups of layers that are completely consistent with thosewhich is known as the oolitic, would be to assume thatmodern each other areas of the subsidence occurred exactly the sameprocesses. We have no reason to believe it is and have allreason to believe the opposite. None of the modern geologists nodare to say that in modern each other's areas of subsidencethe whole space of the globe, there may be conditions thatrequired for the formation of oolite; every geologist will tell you thatthe respective groups of formations required in other places will in allprobability, present a completely different mineral characteristics. Moreover, notonly the phenomena occurring in these modern each other areassubsidence would be more or less different in essence, but barelythere are at least two such cases in which these phenomena would coincide inthe time of its beginning and end. The assumption that separate parts of the earththe surface can start to settle at the same time and to cease to settle, tooat the same time, is faced by a large preponderance of probabilities, and meanwhileonly this kind of coincidence could produce the corresponding to each othergroup layers.
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