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

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              GB, & aquam OMRS deſcendentem eſſę
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              maiorem aquâ CDFE deſcendente. </s>
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              <s>Nam ſi KV non eſt maior quàm AH,
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              ergo aut æqualis, aut minor. </s>
              <s>Sit æqualis: er­
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              go quia HG & VN æquales ſunt ex hypothe­
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              ſi, & VK ipſi HA æqualis dicitur, etiam
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              reliquæ KN & AG, hoc eſt OS & CE, æqua­
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              les ſunt: ergo aquæ OMRS & CDFE æqua­
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              lem habentes altitudinem ſunt inter ſe vt
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              baſes, hoc eſt vt ſuperficies OM & CD. </s>
              <s>At­
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              qui ſuperficies OM maior eſt ſuperficie CD,
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              ergo aqua OMRS maior eſt quàm aquą
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              CDFE: ſed aqua deſcendens eſt æqualis mo­
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              li corporis NL, quæ replebat ſpatium reli­
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              ctum; igitur maior eſt moles NL quàm GB:
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              eſt autem NL æqualis parti eleuatæ VO, &
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              GB æqualis eſt parti eleuatæ HC, ergo VO
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              maior eſt moles
                <expan abbr="quãm">quàm</expan>
              HC: hæ verò moles
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              VO & HC ſunt vt altitudines, quia ex hypo­
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              theſi data ſolida ſunt æqualia, ſimilia, & ſi­
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              militer poſita; ergo maior eſt altitudo KV
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              quam altitudo AH. </s>
            </p>
            <p type="main">
              <s>Quod ſi KV dicatur minor quàm AH
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              ergo ex æqualibus VN, HG, demptis inæ­
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              qualibus, remanet KN maior quam AG,
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              hoc eſt OS maior quam CE: aqua igitur
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              OMRS maiorem habens baſim ac maiorem
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              altitudinem, quam aqua CDFE, maior quo­</s>
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