Borelli, Giovanni Alfonso, De motionibus naturalibus a gravitate pendentibus, 1670

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1
verò in deſcenſu aqua ſubiecta expulſa ex I curuo iti­
nere ſurſum fluit per ZF vſque ad E denuò renouatur
libra horizontalis, comparanturque inter ſe ſaxum B
D cum aqua collaterali in nouo ſitu horizontali de­
preſſiori exiſtente, igitur denuò eadem proportione
diſſecta libra imaginaria horizontali, fune-pendulum
æquale priori eadem vi flectetur deorsum, deſcendetque
centrum grauitatis eius motu perpendiculari ad hori­
zontem quòuſque ad fundum vaſis ſaxum pertingat.
Cap. 2. dę
momentis
grauium in
fluido inna­
tantium
Cap. 2. de
momentis
grauium in
fluido inna­
tantium
PROP. X.
Idipſum contingit, ſed inuerſo ordine cum corpus de­
merſum minùs graue aqua collaterali fueris.
SI poſtea priſma BD fuerit ligneum, & minùs gra­
ue ſpecie quam aqua AH, tunc ijſdem manen­
tibus ſolummodò centrum grauitatis communis Y
cadet ad partes aquæ inter Q & P, & proindè vniuer­
ſum graue compoſitum ex aqua, & ligno vim faciet
impellendo deorſum centrum gra­
14[Figure 14]
uitatis Y, & ideò vehementiùs con­
primetur
aqua ſubiecta HDVS,
hæc verò ob eius continuitatem
& naturam conſiſtentem, quæ preſ­
ſioni non cedit, neceſſariò impel­
letur versùs I, & ſic vim faciet ſur­
ſum exprimendo ligni ſuperficiem DC; at dum lignum
aſcendit, oportet vt expellat è ſuo loco incumbentem
aquam E, quæ tranſuerſali & obliquo motu perduce-

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