Casati, Paolo, Terra machinis mota : dissertationes geometricae, mechanicae physicae hydrostaticae

Table of figures

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              Idemque dę
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              cæteris eſto iu­
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              dicium; nulla
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              ſiquidem repe­
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              riri poſſet a­
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              quarum con­
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              gregatio, quæ
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              tellure transla­
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              tâ, ſe aliam in
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              non
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              conglobaret,
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              altioribus par­
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              tibus in inferiorem locum delapſis.
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              LXII
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              Noua hypo­
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              theſis mari­
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              ni æstus in­
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              dicatur, ſed
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              non proba­
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              tur.
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              Gal.
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              <s> Ignoſce, quæſo, interpellanti. </s>
              <s>Ne­
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              ſcio quam mihi inijcis ſuſpicionem nouæ
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              hypotheſis, qua citra omnem telluris verti­
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              ginem ſiuè in orbe annuo, ſiuè circa ſuum
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              axem, marinus æſtus explicari poſſet: ſi ni­
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              mirum terræ centrum lento ac tenui motu
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              vltro citroque commeans centro grauium
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              congrueret ſolùm in medio fluxu aut reflu­
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              xu. </s>
              <s>Si enim T accedat ad V, aqua incipit
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              ex S refluere verſus M, vbi aqua ſemper au­
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              getur, quò magis centrum T recedit ab V
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              in X: iterumque fluit ex M in O, cum cen­
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              trum ab X recedens in V & in T ſua per
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              veſtigia eò remeat, vnde diſceſſit, ſeruatâ­
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              que in motu reciprocando conſtantiâ, al­</s>
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