Salusbury, Thomas, Mathematical collections and translations (Tome I), 1667
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              it hath not been likewiſe with a perfect curioſity inquired, what
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              its courſe is thorow the particular arches of the Zodiack. </s>
              <s>That
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              therefore the Earth and Moon in running through the Zodiack,
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              that is round the Grand Orb, do ſomewhat accellerate at the
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              Moons change, and retard at its full, ought not to be doubted;
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              for that the ſaid difference is not manifeſt, which cometh to be
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              unobſerved upon two accounts; Firſt, Becauſe it hath not been
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              lookt for. </s>
              <s>Secondly, Becauſe that its poſſible it may not be very
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              great. </s>
              <s>Nor is there any need that it ſhould be great, for the
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              ducing the effect that we ſee in the alteration of the greatneſs of
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              ebbings and flowings. </s>
              <s>For not onely thoſe alterations, but the
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                <arrow.to.target n="marg812"/>
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              Tides themſelves are but ſmall matters in reſpect of the grandure
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              of the ſubjects on which they work; albeit that to us, and to our
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              littleneſs they ſeem great. </s>
              <s>For the addition or ſubduction of
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              one degree of velocity where there are naturally 700, or 1000,
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              can be called no great alteration, either in that which conferreth
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              it, or in that Which receiveth it: the Water of our Mediterrane
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              carried about by the diurnal revolution, maketh about 700 miles
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              an hour, (which is the motion common to the Earth and to it, and
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              therefore not perceptible to us) & that which we ſenſibly diſcern
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              to be made in the ſtreams or currents, is not at the rate of full one
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              mile an hour, (I ſpeak of the main Seas, and not of the Straights)
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              and this is that which altereth the firſt, naturall, and grand
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              tion; and this motion is very great in reſpect of us, and of Ships:
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              for a Veſſel that in a ſtanding Water by the help of Oares can
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              make
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              v. </s>
              <s>g.
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              three miles an hour, in that ſame current will row
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              twice as far with the ſtream as againſt it: A notable difference
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              in the motion of the Boat, though but very ſmall in the motion
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              of the Sea, which is altered but its ſeven hundredth part. </s>
              <s>The
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              like I ſay of its riſing, and falling one, two, or three feet; and
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              ſcarcely four or five in the utmoſt bounds of a ſtreight, two
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              ſand, or more miles long, and where there are depths of hundreds
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              of feet; this alteration is much leſs than if in one of the Boats
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              that bring us freſh Water, the ſaid Water upon the arreſt of the
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              Boat ſhould riſe at the Prow the thickneſs of a leaf. </s>
              <s>I conclude
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              therefore that very ſmall alterations in reſpect of the immenſe
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              greatneſs, and extraordinary velocity of the Seas, is ſufficient to
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              make therein great mutations in relation to our ſmallneſs, and to
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              our accidents.</s>
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            <p type="margin">
              <s>
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                <emph type="italics"/>
              Many things
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              may remain as yet
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              unobſerved in
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              ſtronomy.
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              Saturn
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              for its
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              ſlowneſs, and
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              cury
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              for its
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              neſs of appearing
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              were amongſt thoſe
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              that were laſt
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              ſerved.
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              </s>
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            <p type="margin">
              <s>
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                <emph type="italics"/>
              Particular
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              ctures of the Orbs
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              of the Planets not
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              yet well reſolved.
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              </s>
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            <p type="margin">
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                <emph type="italics"/>
              The Sun
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              eth one half of the
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              Zodiack nine days
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              ſooner than the
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              other.
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              </s>
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            <p type="margin">
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                <emph type="italics"/>
              The Moons
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              tion principally
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              ſought in the
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              count of Eclipſes.
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              </s>
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            <p type="margin">
              <s>
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                <emph type="italics"/>
              Ebbings and
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              flowings are petty
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              things in
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              ſon of the vaſtneſs
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              of Seas, and of the
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              velocity of the
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              tion of the
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              ſtrial Globe.
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              </s>
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              <s>SAGR. </s>
              <s>I am fully ſatisfied as to this particular; it remains to
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              declare unto us how thoſe additions and ſubſtractions derived
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              from the diurnal
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              Vertigo
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              are made one while greater, and
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              ther while leſſer; from which alterations you hinted that the
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              nual period of the augmentations and diminutions of the
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              bings and flowings did depend.</s>
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