Salusbury, Thomas
,
Mathematical collections and translations (Tome I)
,
1667
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other eminent aereal alteration that might occaſion the ſame; of
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which diſturbance of the Air we ought to make great account
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in other accidents, and to take it for a third and accidental
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cauſe, able to alter very much the obſervation of the effects
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pending on the ſecondary and more eſſential cauſes. </
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>And it is
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not to be doubted, but that impetuous windes, continuing to
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blow, for example, from the Eaſt, they ſhall retein the Waters
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and prohibit the reflux or ebbing; whereupon the ſecond and
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third reply of the flux or tide overtaking the former, at the
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hours prefixed, they will ſwell very high; and being thus born
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up for ſome dayes, by the ſtrength of the Winds, they ſhall riſe
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more than uſual, making extraordinary inundations.</
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>We ought alſo, (and this ſhall ſerve for a ſeventh Probleme)
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to take notice of another cauſe of motion dependant on the
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great abundance of the Waters of great Rivers that diſcharge </
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themſelves into Seas of no great capacity, whereupon in the
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Straits or
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Boſphori
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that communicate with thoſe Seas, the Waters
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are ſeen to run always one way: as it happeneth in the
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an Boſphorus
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below
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Conſtantinople,
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where the water alwayes
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runneth from the
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Black-Sea,
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towards the
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Propontis
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: For in the
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ſaid
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Black-Sea
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by reaſon of its ſhortneſſe, the principal cauſes
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of ebbing and flowing are but of ſmall force. </
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>But, on the
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trary, very great Rivers falling into the ſame, thoſe huge
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fluxions of water being to paſſe and diſgorge themſelves by the
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the Straight, the ^{*}courſe is there very notable and alwayes
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wards the South. </
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>Where moreover we ought to take notice, that
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the ſaid Straight or Channel, albeit very narrow, is not ſubject
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to perturbations, as the Straight of
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Soilla
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and
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Carybdis
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; for that
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that hath the
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Black-Sea
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above towards the North, and the
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pontis,
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the
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Ægean,
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and the
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Mediterranean
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Seas joyned unto it,
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though by a long tract towards the South; but now, as we have
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obſerved, the Seas, though of never ſo great length, lying North
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and South, are not much ſubject to ebbings and flowings; but
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becauſe the
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Sicilian
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Straight is ſituate between the parts of the
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Mediterrane diſtended for a long tract or diſtance from Weſt to
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Eaſt, that is, according to the courſe of the fluxes and refluxes,
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therefore in this the agitations are very great; and would be
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much more violent between
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Hercules Pillars,
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in caſe the
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Straight of
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Gibraltar
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did open leſſe; and thoſe of the Straight of
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Magellanes
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are reported to be extraordinary violent.</
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The cauſe why,
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in ſome narrow
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Channels, we ſee
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the Sea-waters run
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alwayes one way.
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* Or current.</
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<
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>This is what, for the preſent, cometh into my mind to ſay unto
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you about the cauſes of this firſt period diurnal of the Tide, and
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its various accidents, touching which, if you have any thing to
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offer, you may let us hear it, that ſo we may afterwards
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ceed to the other two periods, monethly and annual.</
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