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

Table of figures

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                <pb xlink:href="018/01/143.jpg" pagenum="129"/>
              ſingulis cursûs velocitatem incitarent re­
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              mitterentque, aut etiam ſuum in caput re­
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              laberentur; id quod nondum licuit obſerua­
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              re. </s>
              <s>Præterquam quod vix dixeris, quo mo­
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              uente tellus viciſſim commearet, citrà fabu­
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              larum figmenta. </s>
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              <s>At ſi contingere poſſet, vt machinarum </s>
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              ope telluris centrum ex V in T transferretur,
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              fluminis GL aqua ex G reflueret in L, & in
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              eundem alueum ſe inſinuaret mare vſquę
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              dum tota aquæ ſuperficies continua in ſphæ­
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              ram inflexa conſiſteret, cum non haberet,
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              quò deſcenderet. </s>
              <s>Hinc illud fit, quod cum
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              maria omnia (niſi fortè Caſpium velis exci­
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              pere, cui tamen per ſubterraneos cuniculos
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              cum Ponto Euxino communio eſt) ſibi in­
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              uicem continuata iunctaque ſint, terrâ in
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              partem vnam translatâ, aquæ ferè omnes in
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              oppoſitam recederent, vel per patentem al­
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              ueum dilabentes, vel etiam exundantes:
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              idem quippe tunc aquarum conceptaculis
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              contingeret, ac ſi nunc vas liquore quaſi
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              plenum magis & magis inclinaretur, totus
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              enim demùm liquor effunderetur. </s>
              <s>Quarè
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              vniuerſa ferè aqua ſuperiorem locum relin­
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              quens in H conflueret eò velociùs, quò lon­
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              giùs telluris centrum T recederet ab V cen­
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              tro grauium ſeu vniuerſi. </s>
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