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In the stacking order of layers one above the other found similarvariety. Each area of the earth's surface has its own historyincreases, decreases, and periods of peace; and the story is quite differentchronologically with the history of any other region. River deltas are deposited inpresent at the formation of very different periods, some onvery ancient, the other modern. Meanwhile, in the same place settled grouplayers with several hundred feet of thickness, in another place, the donkey oneonly the layer of fine silt. Meanwhile, as one region of the earth's crust remainingover a long period of time over the ocean surface, is notno change, except for those that occur from weathering;another area of the crust has traces of various changes of level,caused the formation of different masses of talus, located layers.If at all possible to make any conclusion on the basis ofthe ongoing processes, we have to come to thatthe conclusion that not only is everywhere the order of the layers one over the othervaries more or less from the order you place them in other areas, butin each area there are groups of formations, which in many otherareas not at all relevant members.
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