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and form from one another; it was and is still an unpsychological violence to suppose in the human author of the narrative all possible knowledge of psychical and scientific secrets, and to lift him above the child-like views of his time concerning the things of this world. But it was by far the most fruitless undertaking to construct in detail from his words a picture of the real {308} circumstances of the creation and development of the world. Attempts of this kind have been often made; but they have produced nothing but dreams. And certainly the attempt to control and correct natural investigation by means of such dreams would be like trying to correct well-established facts of history by the prophecies of a still earlier period, or even to prove them false. But from the time when natural science, as it is at present, began to pay attention to the prehistoric history of the earth and even of the universe, such a comparison has been possible. It tells us, it is true, that the Biblical days' works did not follow each other in the course of earthly and cosmic developments in such a way, that the one began where the other ceased, but that they passed on in the long lines of their course, beside one another, and above one another. But looking upon their _meridian altitudes_, they nevertheless, where we are able to undertake certain geological comparisons, follow one another exactly in the same order in which the days follow one another in that Biblical record. The meridian altitude of the _third day_ (for here the certainty of geological knowledge first begins for us) has to be looked for where the continents are formed and the vegetable life preponderates on earth: and that is the _carboniferous period_. The meridian altitude of the _fourth day_ must have been reached where for the first time the covering of vapor and clouds of the earthly atmosphere permanently parted, and sun, moon, and stars became visible: and geology finds this time in the period which lies between the carboniferous period and the trias--in the _Permian period_, as it is called in England, in the _dyas_ of the {309} fossiliferous and of cupriferous slate and _Zechstein_, as we call it in Germany. The meridian altitude of the _fifth day_ has to be looked for where ocean-life, with its sauria and innumerable animals, gave its impress to organic life on earth, and the air was filled with inhabitants: geology calls such a time the _secondary period_ of
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