At Cornell
At Cornell
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In our eReader you can find the full English version of the book. Read At Cornell Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book At Cornell
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These layers of rock salt are nearly pure, and there can not, therefore, have been much sediment brought in by streams at this time; more- over, if there had been many streams, their waters would have sweetened and freshened the sea waters sufficiently to prevent precipitation of the salt. It is logical, then, to conclude that the climate of that period for this region was arid, so that little water found its way from the land into. The sea.
But this condition, though of long duration, for ther...e are layers of solid salt, two hundred and fifty- eight feet in thickness, underlying Ithaca, eventually changed; a more humid climate followed, and, at the same time, the bottom of the inland sea began a slow subsidence, the rate of which seems to have kept pace very nearly with the rate at which the enlarged streams now supplied sediment and spread this sediment in layers over the bottom. This pro- cess continued with slight variations, until more than two thousand five hundred feet in thickness (the depth from the level of the Cornell campus to the salt), of shales, sandstones and limestones had accumulated.
What to read after At Cornell?
You can find similar books in the "Read Also" column, or choose other free books by O D Von Oscar Diedrich Engeln to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
These layers of rock salt are nearly pure, and there can not, therefore, have been much sediment brought in by streams at this time; more- over, if there had been many streams, their waters would have sweetened and freshened the sea waters sufficiently to prevent precipitation of the salt. It is logical, then, to conclude that the climate of that period for this region was arid, so that little water found its way from the land into. The sea.
But this condition, though of long duration, for ther...e are layers of solid salt, two hundred and fifty- eight feet in thickness, underlying Ithaca, eventually changed; a more humid climate followed, and, at the same time, the bottom of the inland sea began a slow subsidence, the rate of which seems to have kept pace very nearly with the rate at which the enlarged streams now supplied sediment and spread this sediment in layers over the bottom. This pro- cess continued with slight variations, until more than two thousand five hundred feet in thickness (the depth from the level of the Cornell campus to the salt), of shales, sandstones and limestones had accumulated.
What to read after At Cornell?
You can find similar books in the "Read Also" column, or choose other free books by O D Von Oscar Diedrich Engeln to read onlineMoreLess
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