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

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    <archimedes>
      <text>
        <body>
          <chap>
            <p type="main">
              <s>
                <pb xlink:href="018/01/104.jpg" pagenum="90"/>
              terminus, vnde terrena
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                <figure id="id.018.01.104.1.jpg" xlink:href="018/01/104/1.jpg" number="26"/>
                <lb/>
              ſemidiameter cognoſci­
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              tur, non tamen ipſa ſe­
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              midiameter AG eſt ter­
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              tius analogiæ terminus,
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              ſed potius conflatum ex
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              DC, CB: latus enim v­
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              num trianguli rectan­
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              guli eſt medium propor­
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              tionale inter differentiam
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              hypothenuſæ ac reliqui lateris, & eorum ag­
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              gregatum: ac proinde vt AD ad DB, itą
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              DB ad DCB. </s>
              <s>Quare ex inuento tertio ter­
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              mino debuiſſet datam altitudinem DA de­
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              mere, & reſiduum bifariam diuiſum dediſ­
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              ſet quæſitam ſemidiametrum AC. </s>
              <s>Hinc
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              rectè dicebas arcum illum pro rectâ lineâ
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              parùm Geometricè aſſumptum. </s>
            </p>
            <p type="margin">
              <s>
                <margin.target id="note44"/>
                <emph type="italics"/>
              XXXXIV
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              Quarta me­
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              thodus in­
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              neniendi ter­
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              ra ſemidia­
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              metrum.
                <emph.end type="italics"/>
              </s>
            </p>
            <p type="main">
              <s>
                <emph type="italics"/>
              Gal.
                <emph.end type="italics"/>
              </s>
              <s> Nunquam hominem potui à con­
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              ceptâ ſententiâ reuocare, niſi vbi eum iuſſi
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              rem rotam in praxim deducere. </s>
              <s>Statuimus
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              primùm extra omnem controuerſiam poſi­
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              tum videri, in decernendâ Phyſici horizon­
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              tis amplitudine non incertam ædium aut
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              montium altitudinem eſſe ſpectandam, ſed
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              eam ex communi vulgarique hominum ma­
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              gnitudine definiendam. </s>
              <s>Quandoquidem </s>
            </p>
          </chap>
        </body>
      </text>
    </archimedes>
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