Introduction to Science
Introduction to Science
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In our eReader you can find the full English version of the book. Read Introduction to Science 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 Introduction to Science
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E. , upon the velocity of its rotation. The earth, as we know it, is almost perfectly rigid. We still speak of the "crust of the earth " as if its surface only were solid and its contents molten, but this theory has been abandoned. Physicists hold now that the earth is solid to its core, except for patches of molten lava. At any rate, it is so nearly rigid that any deformation by centrifugal force or return towards sphericity owing to the diminution of cen- trifugal force, is out of the questio...n. The earth has the THE AGE OF THE EARTH 67 shape which it assumed when it first became cool enough to solidify. It is, as we have said, an oblate spheroid, but the difference in length between the axis joining the poles and the axis passing from one side of the equator to the other is much smaller than the contemplation of most models of the globe would lead one to suppose. The equatorial axis is only seventeen miles longer than the polar axis. Therefore it cannot have been spinning much faster when it first became solid than it does now.
What to read after Introduction to Science?
You can find similar books in the "Read Also" column, or choose other free books by Alex Hill to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
E. , upon the velocity of its rotation. The earth, as we know it, is almost perfectly rigid. We still speak of the "crust of the earth " as if its surface only were solid and its contents molten, but this theory has been abandoned. Physicists hold now that the earth is solid to its core, except for patches of molten lava. At any rate, it is so nearly rigid that any deformation by centrifugal force or return towards sphericity owing to the diminution of cen- trifugal force, is out of the questio...n. The earth has the THE AGE OF THE EARTH 67 shape which it assumed when it first became cool enough to solidify. It is, as we have said, an oblate spheroid, but the difference in length between the axis joining the poles and the axis passing from one side of the equator to the other is much smaller than the contemplation of most models of the globe would lead one to suppose. The equatorial axis is only seventeen miles longer than the polar axis. Therefore it cannot have been spinning much faster when it first became solid than it does now.
What to read after Introduction to Science?
You can find similar books in the "Read Also" column, or choose other free books by Alex Hill to read onlineMoreLess
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