Galilei, Galileo, The systems of the world, 1661

Table of figures

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              tions; the one is its riſing and falling alternately towards the
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              one and other extremity; the other is its moving and running, to
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              ſo ſpeak, Horizontally forwards and backwards. </s>
              <s>Which two
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              ferent motions differently reſide in divers parts of the Water:
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              for its extream parts are thoſe which moſt eminently riſe and fall;
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              thoſe in the middle never abſolutely moving upwards and
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              wards, of the reſt ſucceſſively thoſe that are neereſt to the
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              treams riſe and fall proportionally more than the remote: but on
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              the contrary, touching the other progreſſive motion forwards
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              and backwards, the middle parts move notably, going and
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              turning, and the waters that are in the extream parts gain no
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              ground at all; ſave onely in caſe that in their riſing they
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              flow their banks, and break forth of their firſt channel and
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              ceptacle; but where there is the obſtacle of banks to keep them
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              in, they onely riſe and fall; which yet hindereth not the waters
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              in the middle from fluctuating to and again; which likewiſe
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              the other parts do in proportion, undulating more or leſſe,
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              according as they are neerer or more remote from the
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              Water riſeth &
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              falleth in the
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              tream parts of the
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              Veſſel, and runneth
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              to and fro in the
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              midst.
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              An accident of
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              the Earths motions
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              impoſſible to be
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              duced to practice
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              by art.
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              <s>The fifth particular accident ought the more attentively to be
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              conſidered, in that it is impoſſible to repreſent the effect
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              of by an experiment or example; and the accident is this. </s>
              <s>In
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              the veſſels by us framed with art, and moved, as the
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              named Bark, one while more, and another while leſſe ſwiftly,
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              the acceleration and retardation is imparted in the ſame manner
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              to all the veſſel, and to every part of it; ſo that whilſt
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              v. </s>
              <s>g.
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              the
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              Bark forbeareth to move, the parts precedent retard no more
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              than the ſubſequent, but all equally partake of the ſame
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              tardment; and the ſelf-ſame holds true of the acceleration,
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              namely, that conferring on the Bark a new cauſe of
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              ter velocity, the Prow and Poop both accelerate in one and
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              the ſame manner. </s>
              <s>But in huge great veſſels, ſuch as are the very
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              long bottomes of Seas, albeit they alſo are no other than
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              tain cavities made in the ſolidity of the Terreſtrial Globe,
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              it alwayes admirably happeneth, that their extreams do not
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              unitedly equall, and at the ſame moments of time increaſe
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              and diminiſh their motion, but it happeneth that when one of its
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              extreames hath, by vertue of the commixtion of the two
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              Motions, Diurnal, and Annual, greatly retarded its velocity,
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              the other extream is animated with an extream ſwift motion.
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              <s>Which for the better underſtanding of it we will explain,
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              ſuming a Scheme like to the former; in which if we do but
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              poſe a tract of Sea to be long,
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              v. </s>
              <s>g.
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              a fourth part, as is the arch
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              B C [
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              in Fig.
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              2.] becauſe the parts B are, as hath been already
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              declared, very ſwift in motion, by reaſon of the union of the
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              two motions diurnal and annual, towards one and the ſame way, </s>
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