Scribners Magazine volume 3
Scribners Magazine volume 3
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In our eReader you can find the full English version of the book. Read Scribners Magazine volume 3 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 Scribners Magazine volume 3
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We are, therefore, driven to another hypothesis which is entirely satisfactoiy. It was long ago suggested, though it has not been pre- sented in a perfectly clear form in our popular treatises on the subject. This explanation may be stated in a few words : When . Deposits of rocky matter are laid down upon the sea-floor, they con- tain a good deal of water. Such de- posits are never entirely compact ; there are numerous little spaces between the grains of sand or mud, in or between ' the fossil... shells and other animal re- mains, which form in most places a part of the strata as they are made. We see how large an element water is in such beds if we take up a portion of the miad from the bottom of any pool. It is probable that, on the average, this en- closed water amoimts, at the time when the deposits are made, to as much as from five to fifteen per cent, of the mass. At first this imprisoned water is at the or- dinary temperature of the sea-floor, and so has no tendency to break out of its cells ; but in the course of the geologic ages, a great many thousand feet of strata are slowly accumvilated above the original level, aU charged in the same way with a portion of the fluid in which they were laid down.
What to read after Scribners Magazine volume 3?
You can find similar books in the "Read Also" column, or choose other free books by Edward L Edward Livermore Burlingame to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
We are, therefore, driven to another hypothesis which is entirely satisfactoiy. It was long ago suggested, though it has not been pre- sented in a perfectly clear form in our popular treatises on the subject. This explanation may be stated in a few words : When . Deposits of rocky matter are laid down upon the sea-floor, they con- tain a good deal of water. Such de- posits are never entirely compact ; there are numerous little spaces between the grains of sand or mud, in or between ' the fossil... shells and other animal re- mains, which form in most places a part of the strata as they are made. We see how large an element water is in such beds if we take up a portion of the miad from the bottom of any pool. It is probable that, on the average, this en- closed water amoimts, at the time when the deposits are made, to as much as from five to fifteen per cent, of the mass. At first this imprisoned water is at the or- dinary temperature of the sea-floor, and so has no tendency to break out of its cells ; but in the course of the geologic ages, a great many thousand feet of strata are slowly accumvilated above the original level, aU charged in the same way with a portion of the fluid in which they were laid down.
What to read after Scribners Magazine volume 3?
You can find similar books in the "Read Also" column, or choose other free books by Edward L Edward Livermore Burlingame to read onlineMoreLess
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