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M

E

e

H

( he difb nce of ::

40000

miles

(rom

the

eUl h's

centre, ¡nd

of

~ 3.}OCO

miles

{fOl11 t11l:

cent re of gravity

oC

lhe

c.lrth

and moon, lo does thl! earth go roum!

,he

(.tOle

centre of

gr.l\'ity r;:very month

¿ l

lhe ddUnce of 6000 miles

flOOl

it

j

lh

tt " .

Irom

H

tO lhe cent r< of lhe e.u-li\.

I

OW ::'5

tbe c.anh is

(in

r!Juan

numbcrs)

Seoo mile:!>

111

diamcter.

it

15

pllio

lholt tU

(id..:

neXt l he m OOn is

ooly

:2000 m iles

{1 0m

the:

comm·,n

cen,lc

of gra",ity of lhe;:

canh am.I

moon ; its cenue

6000

miles d,UaOt

thercfroOl

j

and iu

f.lrth.::{l

{¡de (,om

lhe O1oon 10aoo .

Thcrl!fore

lhe cen–

trirug.tl

furces

of thefe pans

are

as

2 000 , 6 0 00.

and

10000

j

thal ¡s, lhe

centrifugal

force of any

IÍde:

oC

the

c:\rth, when

il 1$

lurned from tbe moon. is

f¡ve

times as

grt :u

:as

when

it

as

lurncd

lowards the moon

And as

Ih< moon', .." .tlion (e" prelt by the nu,"be.

6000)

at

lhe

~arth'5

cenue kccps (he

can h

(ronl

fi ying OUt of this

monthly circ1e, 1t muU

ue

grcO\tcr than

lhe ccntriruga{

force

oC

' he w;ttcrs on the Cicle

" t'XI

hcr; and conCcqucnt–

Jy.

h~r

grc,llcr

degrt c of

attratllon 011

th:tt f¡de is fuffi–

cient

lO

rair~

ltrcm ; UUI as her

attr.tt'

bon on lhe oppoCitc

!idc is IcCs

th.ln

lhe centrifugal force of {he water there,

lhe exccr, of this

fo rce

i5

fufficicnt 10

raiCe

lhe

water

jufi

a.

high on the oppofite fideo- To prove this ex–

pcrimenl.lly, Iel Ihe bJr

DC

(fig

10 )

wilh il5 fur–

niture be fixcd upon the whirlmg board of the ma-

hine (6g. , ..) by pu!!tiog the pio

P

ioto Ihe ceo"e of

,he board; which pio 1S in lhe centre of gravity of lhe

whole bar with

its

thrce balls

~.f,g.

and moon M.

N ow,

ir

lhe:

whirling board and bar be (urned

no\V

Iy

round by Ihe '\lÍoch, uotil tbe

b. 1I /

hang. over

fhe c('ntre

of

the c:rde, as

In

fig.

I 1.

lhe b.tll

g

will be

I:<pt toward. Ih< muoo by Ihe heal'iefi \Veigh,

p,

(6g" 9')

~nd

the b,,1I

r,

00

aCCOLlnt of

ttS

trcater centnfugal force,

. od Ihe

Idr..

weiglll

r ,

will fly off.s Car tOIhe olbor fide

QS

in

lig.

1.2.

Ano fo,

whilll

the machine 1S kept (Uro·

; n&, lhe balls

r

:md

g

\Viii

hang o\"er the cuds of ,he

d –

lipfis

IJ.~.

So Ih I the « r.triCug_1(orce of the ball e " ill

c xcecd

,h¡:

moon's auraéllon

jurt

as much

as

her au rae·

'tion excecds Ihe centrifugal force of Ihe

hall

g,

whilfi

hcr attraé\ion

juH

bdl¡nccs the centr,

fug.ll

force

of

the

b~1I

/t

and mAkes

il

kcep

in

in

circ.l..: . And ht:nce it

i5

cvidcnt th,u Ihe lides mua rife

to

equal Leights at the

(a.me

time on oppofi,c

Cid

es of lhe e.\rlh . T his expcri·

rnc:nt,

10

Ihe bcll of my kr.o·" !cdgc , is ent¡rely ne\V.

Fronl the principies lhus dl.tbliflled .

it

is cvident that

lhe can h moycs round Ihe: fu n, and oot Ihe fun round Ihe

~anh :

(ur lhe

centrifug.tl

l3.w

\l.ill uc:ycr

.lIow

a gre¡ t

body

10

mO'lle roond a fmi\1I one in

al\y

orbit what ver;

cfpcciollly when

\\,le

lind. that if

a

fruall boJy

mo'! s

round

a

~rtat

onc, lhe great ODe mufi alf.l

mo\'c

round the corn o

mon cenue

of

~ra, it)'

belween tht'm

( \\'0.

.'\nd

it

is

wcll

known.

tla t

the q'lantity of

nuucr in

Ih~

foo 15

= l7000

times

as

gr..:at as lhe

qU.lnu t)'

of mJ.ttcr

In

lh..: e-·_nh.

N ow,

as

the Cun's

dil\.m-.:.:

f:o~n

lhe

t ..

nh

is at

h:,!;

~

- 81.000.000

of miles.

ii

\\'C di,;de th.H

Jl!hnce

by

? 'l7000,

\/ole

0, ..11

}¡ we. onl)'

;Si

fo..

lhe

n·lol'.Jer of nules

Ih1.t

the. ctntre

of

I!rolvity b t\Yeco

,he

fUD

;md

c::lrth

is

d tlhnl from the fo n's centre

J\n,l

<lS

lhe fun's

f.·:ni,Jia–

meter

is

T

of

a d.:grec,

Wh:Cll.

;u ro

h1 eu

.1

,I¡lhnce

",$

thl t

of the fun.

nlUn

b:

ro !

c.Cs

dHn 3S

I

~oo

mih.s,

ir

11".

be illd

ti

by

35 7. lhe q"cli.c¡ will be lo6S';.

A

N

1

e

s,

43

which OICWS th:u lhe common C\!ntre of cravity js

withio

lhe

body of

lhe

fun . and 1S only lhe loG8.,. part of

bis

felH1di3melcr from his centre toward his fudue:.

AII

globul...r

bodics~

whofc pan s

c.tn

yt<:ld . and \\hich

do nOI tum on their 3XCS, mun be perfea fpheres, be...

caufe

311

pJ.n s of thci r furfaces are equall y

attr~tlcd

lO ...

ward their centres. But all fuch globcs which do turo

on their

axes~

will be

obl.He

fpheroids; that is, their

furf3ces

\Viii

be higher. or ranher from che

c~ntre,

io.

\he eql1:u orial {h an

in

thc polar regions. For.

as

the

e–

qualortal pans move quickcrt. they mun llave the grear–

en

centrifug:ll force ; and will therefore rccede

fanhe(~

from the: axis of motion. T hus,

if

twO circular hoops

AI:I

. od

CD ,

(Plate

CVII. 6g.

l .) m. de IhiD .od Be""

ible, and cro!ling one anolher al rigl'ot angles, be lurned

round lheir

axis

EF

by me:ans of the winch

111,

the whe:cl

11,

and pinion

o,

and the axis be loofe in the pole or in–

lerCeaíon e, lhe middle paru

A,B,e,D

will Cwell out fo

as tO firike ag. infl Ihe (id.. of Ihe frame

al

F and G,

ir

the

pole~,

in únking

·10

lhe pin

E, b(

nOI flopt

by

it (roal

fiokiog farlher:

Co

1041

Ihe \Vhole wil! ' ppe.r of an ov.1

6-

go re~

lhe: equatorial diameler being confider...bly longer lhan

the polar. T hal our eanh

is

of this

figure~

is

dt lUon–

firable from ¡ (tu..) meafur(ment ?f (ome degrees on

its

furface. which are found

tO

be

lon~el

in lhe frigid

zon~s

than in lhe tOrrid : and the difference is (ound to be

fuch as prove lhe eauh's equ;u oTlal diarncler lo be

35

miles longer tluo its axis .-Since lhen, lhe eanh

is

high ...

er at lhe equalor than at lhe

pole:s~

lhe fea, ·which Jike

0111

othcr 8uids naturally runs downward (or towards the

pl ace5 which clre ne:aren Ihe earth's ce:otre) \Vould

run

towarcls the polar regions. and leave the (quatorial parts

d ry. if the

centrjfuga~

{orce of fhe w:oIter, which carried

it

lO

thof~

pans, and fo raifcd them, did not de(ain and

kecp it from ruoniDg back .gain loward. Ibe poles

oE

!he

earth.

0/ ,he M uhan;cal

PD'tUU',

I'T

\Ve conriJer lodies

in

motion, and compare theDl

tOAclhrr. we may do this

eilh~r

with refpeét lO the

quan.

I¡ties of m: tter

\h~y conta;n~

or the vclocities wilh' which

lhey

al~

mot"c:d

T he

heavi~r

any body

¡S,

lhe greater

is the po\\'cr requircd

eith~r

tOmove it or .tO flop

ltS

mo–

lion : ól:od at!,ain,

lhe

f",i(ler

h

mO\Tes, the greatcr is

its

force,

So

lhat

the ·\Vhol~

1JJonlr nlmn

or qoantilY offorcc

of a

mo\'in~

body

is

lhe rerule

of

its quantity of mauee

muh ipl:ed by lhe velocity with which it is

move-d.

And

when

th~

produéls ¡rilins. (ro",

the

nluhiplication of

tbe

p.lrdcular qu..ntitics of IUJtter in any

1\"0

bOlhn by lheir

rcfpc:éhve \' I:)cities arl! I!q ual, the

n!oll},ml a

or eotire

forces are ro

100.

Thu. , Cuppo(e

1

booy, which we {hall

call A,

lO

wei~h

';0

pounds, 3nd to rnove al lhe rate of

two mil s in

él

m:nutc

j

and another body, which

\Ve

(hall

ctlJ

S ,

lO \'oCigh onl)" rour poun¿s, and

10

move

20

miles

in a

nur-u·e ; the entire forces "'¡Ih

\1,

hich the(e l WO

b.Jdi~s

wodd Hnke

againfi

any

obOacle v:ould be cqua.!

lO

t aeh

otha. and lhc:rdorc it \\'ould require ( qua) powers

tn flop them.

For

40

muhiplit"d by

2

glves

80,

the force

of thc hoJy A and 20 muhiplied by 4 givc. 80. Ihe

force of Ih. b<>ly

1:1.

V uo Ihis caCy princi 1: dCP:Dds !he whole of me–

d lolOics :