Casati, Paolo, Terra machinis mota : dissertationes geometricae, mechanicae physicae hydrostaticae
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              enim terra vniuerſa intrà aquam demerſą
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              deliteſceret. </s>
              <s>Prætereà quamuis totius terreæ
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              portionis in aquâ exiſtentis grauitas minuere­
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              tur, ſegmenti tamen vltra Vniuerſi cen­
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              trum poſiti grauitas imminuta vel auctą
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              nihil iuuaret, cùm motui illa non repugnet,
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              dum deſcendit: ideò ſolùm ſegmenti ſupe­
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              rioris pars aquis immerſa attendenda eſſet:
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              atque adeò quò magis terræ centrum ab vni­
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              uerſi centro remoueretur, eò augeretur ma­
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              gis pondus, quia plus terrenæ molis ex aquis
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              extaret. </s>
              <s>Neque enim aliud terræ conringe­
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              ret, quâm ſolido cuilibet corpori, quod ex
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              humore in vaſe extrahitur, cuius maior mo­
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              les emergit ex aquâ, quàm ſit moles aquæ
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              accurrentis ad replendum ſpatium à corpo­
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              re ſolido relictum. </s>
              <s>Quia ſcilicet ſi aqua ma­
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              neret in eâdem ſuperficie, nec deprimere­
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              tur, ſolidi tanta moles emergeret, quanta eſt
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              moles, quæ relinquit ſpatium intra aquam:
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              ſed quoniam aqua infra illam ſuperficiem̨
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              deprimitur, quam priùs conſtituebat, & re­
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              linquit aliam prætereà ſolidi partem ab aquâ
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              immunem, ideò moles, quæ ex aquâ emer­
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              git, maior eſt mole aquæ accurrentis ad re­
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              plendum ſpatium relictum à corpore eleua­
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              to. </s>
              <s>Sic in vaſe HX, corpus AB totum in­
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              trà aquam, cuius ſuperficies ſit CD, ſi ex-</s>
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