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

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            <p type="main">
              <s>
                <pb xlink:href="018/01/225.jpg" pagenum="211"/>
              altitudine OS, eſt vt ſuperficies vaſis minus
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              ſuperficie ſolidi VY ad ipſam ſuperficiem ſo­
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              lidi; igitur VK eleuatio ſolidi ad KN depreſ­
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              ſionem aquæ eſt vt ſuperficies vaſis maioris
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              minùs ſuperficie ſolidi ad ipſam ſuperficiem
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              ſolidi VY: & componendo vt VN corporis
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              emerſio ad KN aquæ depreſſionem, ita ſu­
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              perficies vaſis maioris ad ſuperficiem ſolidi
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              VY. </s>
              <s>Eâdem methodo oſtenditur HA eleua­
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              tionem ſolidi ad AG depreſſionem aquæ eſſe,
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              vt eſt ſuperficies vaſis minoris minùs ſuper­
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              ficie ſolidi HT ad ipſam ſuperficiem ſolidi: &
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              componendo vt HG ad GA, ita ſuperficies
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              vaſis minoris ad ſuperficiem ſolidi HT. </s>
            </p>
            <figure id="id.018.01.225.1.jpg" xlink:href="018/01/225/1.jpg" number="46"/>
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              <s>Quoniam igitur vt ſuperficies vaſis maio­
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              ris ad ſuperficiem minoris, ita GA ad NK;
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              ſi eſſet VK ad HA vt GA ad NK, iam eſſet vt
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              VK ad HA ita ſuperficies vaſis maioris ad ſu­</s>
            </p>
          </chap>
        </body>
      </text>
    </archimedes>
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