Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
Text
Text Image
Image
XML
Thumbnail overview
Document information
None
Concordance
Figures
Thumbnails
Page concordance
<
1 - 30
31 - 60
61 - 90
91 - 120
121 - 150
151 - 180
181 - 210
211 - 240
241 - 270
271 - 300
301 - 330
331 - 360
361 - 390
391 - 420
421 - 450
451 - 480
481 - 510
511 - 540
541 - 570
571 - 579
>
Scan
Original
421
422
423
424
425
426
427
428
429
430
431
432
433
434
435
436
437
438
439
440
441
442
443
444
445
446
447
448
449
450
<
1 - 30
31 - 60
61 - 90
91 - 120
121 - 150
151 - 180
181 - 210
211 - 240
241 - 270
271 - 300
301 - 330
331 - 360
361 - 390
391 - 420
421 - 450
451 - 480
481 - 510
511 - 540
541 - 570
571 - 579
>
page
|<
<
of 579
>
>|
<
archimedes
>
<
text
>
<
body
>
<
chap
>
<
p
type
="
main
">
<
s
id
="
s.002506
">
<
pb
pagenum
="
475
"
xlink:href
="
010/01/483.jpg
"/>
<
arrow.to.target
n
="
marg649
"/>
<
lb
/>
pore facti ſubduplicatam proportionem habeant al
<
lb
/>
titudinum eorum. </
s
>
</
p
>
<
p
type
="
margin
">
<
s
id
="
s.002507
">
<
margin.target
id
="
marg649
"/>
Cap. 11. gra
<
lb
/>
uia in fluido
<
lb
/>
velocitati
<
lb
/>
bus inæqua
<
lb
/>
libus ferri
<
lb
/>
debere.</
s
>
</
p
>
<
p
type
="
main
">
<
s
id
="
s.002508
">
<
emph
type
="
center
"/>
PROP. CCXXXI.
<
emph.end
type
="
center
"/>
</
s
>
</
p
>
<
p
type
="
main
">
<
s
id
="
s.002509
">
<
emph
type
="
center
"/>
<
emph
type
="
italics
"/>
Eorumdem conorum æquè altorum ſi vnius vertex, & al
<
lb
/>
terius baſis ſursùm ambo, vel deorsùm
<
expan
abbr
="
reſpiciõt
">reſpiciont</
expan
>
; parum
<
lb
/>
celeriùs feretur is, qui mucrone præcedente fertur.
<
emph.end
type
="
italics
"/>
<
emph.end
type
="
center
"/>
</
s
>
</
p
>
<
p
type
="
main
">
<
s
id
="
s.002510
">COmparari modò debent inter ſe duo coni æqua
<
lb
/>
les, ſimiles, & homogenei aqua leuiores, vel gra
<
lb
/>
uiores, ſed contrario ordine diſpoſiti, ſcilicèt ſi vnius
<
lb
/>
baſis
<
expan
abbr
="
deorsũ
">deorsum</
expan
>
reſpiciat, alterius baſis ſursùm vergat,
<
lb
/>
ſed ambo horizonti æquidiſtantes, atque temporibus
<
lb
/>
æqualibus ſemper infra aquæ libellam aſcendendo,
<
lb
/>
vel deſcendendo ferantur; aliquantum celeriùs mo
<
lb
/>
uebitur is, qui vertice præcedente mouetur; quia li
<
lb
/>
cet expulſio ſupremæ aquæ efficiatur ab exceſſu pon
<
lb
/>
deris aquæ ſiphonis ſupra pondus ligni aſcendentis,
<
lb
/>
& ab illius motu, cui veluti appendix ſubſequitur a
<
lb
/>
quæ ſupernæ migratio, nihilominus illa moueri de
<
lb
/>
bet, ergo ſi eius motus impedimentum patietur,
<
expan
abbr
="
cõ-ſequenter
">con
<
lb
/>
ſequenter</
expan
>
retardabitur aſcenſus ligni: modo negari
<
lb
/>
non poteſt reſiſtentia
<
expan
abbr
="
pendẽs
">pendens</
expan
>
ab ampla translatione,
<
lb
/>
& diſtractione lanuginis partium aquæ, & à confri
<
lb
/>
catione cum aſperitatibus ligni
<
expan
abbr
="
aſcendẽtis
">aſcendentis</
expan
>
; hæc pro
<
lb
/>
fectò magis retardare poſſe videtur baſim coni
<
expan
abbr
="
ſursũ
">ſursum</
expan
>
<
lb
/>
vergentem, quàm eius apicem, & hac de cauſa veri
<
lb
/>
ſimile videtur vt celeriùs conus ſursùm feratur quan
<
lb
/>
do eius vertex ſursùm reſpicit, quàm ſi inuerſo ordi
<
lb
/>
ne diſponatur, idemque in deſcenſu oſtendetur. </
s
>
</
p
>
<
p
type
="
main
">
<
s
id
="
s.002511
">Id quod dictum eſt de conis, verificatur etiam dę </
s
>
</
p
>
</
chap
>
</
body
>
</
text
>
</
archimedes
>