Handbook to the Matlick Tellurian Guide to Mathematical And Astronomical Geogra
Handbook to the Matlick Tellurian Guide to Mathematical And Astronomical Geogra
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In our eReader you can find the full English version of the book. Read Handbook to the Matlick Tellurian Guide to Mathematical And Astronomical Geogra 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 Handbook to the Matlick Tellurian Guide to Mathematical And Astronomical Geogra
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The tide now will neither rise so high, nor fall so low as at new or full Moon. The solar tides occur at regular inter- vals of twelve hours, but the Moon revolving eastward comes to a given meridian later and later each day and thus there will be a lunar tide on an average every twelve hours, and twenty-five minutes or fifty minutes later each day. The ponderous weight of such a great mass of water as constitutes a tide is not suddenly raised by the Moon's attraction, but yields slowly to the ...unseen force, so that the greatest effect is noticed after the Moon has passed. For this reason the highest point of the tide is, in the open ocean, 45 behind or oast of that body.
The Heights 1 of Tides in Different Parts of the World. The time is often essentially var ied by local influences as the direction of coasts and the peculiar shape of bays and mouths of rivers. If a place is situated on a large bay, with but a narrow strait connecting it with the sea, the tide will be longer in rising, as the bay has to fill up through a narrow gate.
What to read after Handbook to the Matlick Tellurian Guide to Mathematical And Astronomical Geogra?
You can find similar books in the "Read Also" column, or choose other free books by Isaac Newton Matlick to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The tide now will neither rise so high, nor fall so low as at new or full Moon. The solar tides occur at regular inter- vals of twelve hours, but the Moon revolving eastward comes to a given meridian later and later each day and thus there will be a lunar tide on an average every twelve hours, and twenty-five minutes or fifty minutes later each day. The ponderous weight of such a great mass of water as constitutes a tide is not suddenly raised by the Moon's attraction, but yields slowly to the ...unseen force, so that the greatest effect is noticed after the Moon has passed. For this reason the highest point of the tide is, in the open ocean, 45 behind or oast of that body.
The Heights 1 of Tides in Different Parts of the World. The time is often essentially var ied by local influences as the direction of coasts and the peculiar shape of bays and mouths of rivers. If a place is situated on a large bay, with but a narrow strait connecting it with the sea, the tide will be longer in rising, as the bay has to fill up through a narrow gate.
What to read after Handbook to the Matlick Tellurian Guide to Mathematical And Astronomical Geogra?
You can find similar books in the "Read Also" column, or choose other free books by Isaac Newton Matlick to read onlineMoreLess
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