| Edmond Halley, Royal Society (Great Britain) - 1705 - 390 pages
.....;u; fition, and that it would be always high Water under the Poles, and low Water every where, wider the ^Equinoctial : And therefore the nearer the Moon approaches the Poles, the lefs is the agitation of the Ocean, which is of all the greateft, when the Moon is in the &.-. quinodial, or fartheft... | |
| Royal Society (Great Britain) - 1705 - 398 pages
...that it would be always high Water under the Poles, and low Water every where under the .Equino&ial : And therefore the nearer the Moon approaches the Poles, the lefs is the agitation of the Ocean, which is of all the greateft, when the Moon is in the Rquino&ial, or fartheft... | |
| Royal Society (Great Britain) - 1722 - 956 pages
...it would be always High- water under the Poles , and Low-water eveiy where under the ÄLquinoclial : And therefore the nearer the Moon approaches the PoleS) the lefs is the Agitation of the Ocean, which is of all the greateft, when the Moon is in the JEquinouial, or farthcft... | |
| Regnault (Père, Noël) - 1731 - 492 pages
...— a •.:,:v •• ?.<. . fixt Pofition, and that it would be always highWater under the Polesj and low Water every where under the /Equinoctial :...nearer the Moon approaches the Poles, the lefs' is the Agitation of the Ocean, which is of all the greateft, when the Moon is in the /Equino€lial, or fartheft... | |
| Sir Richard Phillips - 1830 - 728 pages
...that the spheroid would have a fixed position, and that it would be always high water under the poles, and low water every where under the equinoctial ; and, therefore, the nearer the moon approaches to the poles, the less is the agitation of the ocean, which is the greatest of all, when the moon is... | |
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