Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
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dente infrà ſupremam hy
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drargyri libellam DE, tunc
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ſublato digito mercurius
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profluet ab orificio C quo
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uſque altitudo FB extantis
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hydrargyri ſupra libellam̨
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DE ſit pedum duorum, &
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quadrantis, vel vnius cubi
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ti, & quadrantis, nec vlte
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rius hydrargyrum grauiſſi
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mum deſcendit ſemperque
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ad eamdem altitudinem̨
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perſeuerat, licèt inclinetur
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fiſtula, ſcilicèt ducta recta FG parallela horizonti
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ſummitas hydrargyri ad eamdem horizontalem
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FG perueniet quomodocumque fiſtula inclinetur.
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<
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cauſam quoque huius effectus indagauit, animaduer
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tit enim nos in infima profunditate oceani aerei de
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merſos eſſe, & ſicuti maris aqua vndique fundum̨
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comprimit per lineas horizonti perpendiculares, ſeù
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directas verſus centrum telluris, ſic quoque in oceano
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aereo niſus eius grauitatis exercetur perpendiculari
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tèr ſupra horizontis planum, vnde concipi debent cy
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lindri aerei perpendicularitèr ſuperficiem hydrargy
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ri DE ſupremam comprimentes; quia verò eadem̨
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libella mercurij DE comprimitur quoque in ſitu B à
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ſuperficie baſis B mercurialis cylindri FB efforma
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tur veluti libra, vel ſipho, quæ numquam quieſcit, ni-</
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