LEM. I. Quantities, and the ratios of quantities, which in any finite time converge continually to equality, and before that time approach nearer the one to the other than by any given difference, become ultimately equal. If you deny it; suppose them to be ultimately unequal, and let D be their ultimate difference. Therefore they cannot approach nearer to equality than by that given difference D; which is against the supposition.

Concerning the meaning of this lemma philosophers are not agreed; and unhappily it is the very fundamental position on which the whole of the system rests. Many objections have been raised to it by people who

5 G 2

supposed

equal and contrary loss and gain, remain in equilibrio. Let the original motion of A have been twelve, then A having received a contrary action equal to six, six degrees of its motion will be destroyed or in equilibrio; consequently, a motive force as six will remain to A towards the south, and B will be in equilibrio, or at rest. A will then endeavour to move with six degrees, or half its original motion, and B will remain at rest as before. A and B being equal masses, by the laws of communication three degrees of motion will be communicated to B, or A with its six degrees will act with three, and B will re-act also with three. B then will act on A from south to north equal to three, while it is acted upon or resisted by A from north to south, equal also to three, and B will remain at rest as before; A will also have its six degrees of motion reduced to one half by the contrary action of B, and only three degrees of motion will remain to A, with which it will yet endeavour to move; and finding B still at rest, the same process will be repeated till the whole motion of A is reduced to an infinitely small quantity, B all the while remaining at rest, and there will be no communication of motion from A to B, which is contrary to experience.

Let a body, A, whose mass is twelve, at rest, be impinged upon first by B, having a mass as twelve, and a velocity as four, making a momentum of 48; and secondly by C, whose mass is six, and velocity eight, making a momentum of 48 equal to B, the three bodies being inelastic. In the first case, A will become possessed of a momentum of 24, and 24 will remain to B; and, in the second case, A will become possessed of a momentum of 32, and 16 will remain to C, both bodies moving with equal velocities after the shock, in both cases, by the laws of percussion. It is required to know, if in both cases A resists equally, and if B and C act equally? if the actions and resistances are equal, how does A in one case destroy 24 parts of B's motion, and in the other case 32 parts of C's motion, by an equal resistance? And how does B communicate in one case 24 degrees of motion, and C 32, by equal actions? If the actions and resistances are unequal, it is asked how the same mass can resist differently to bodies impinging upon it with equal momenta, and how bodies possessed of equal momenta can exert different actions, it being admitted that bodies resist proportional to their masses, and that their power of overcoming resistance is proportional to their momenta?

It is incumbent on those who maintain the doctrine of universal re-action, to free it from these difficulties and apparent contradictions.

Newtonian supposed themselves capable of understanding it. They Philosophy say, that it is impossible we can come to an end of any infinite series, and therefore that the word ultimate can in this case have no meaning. In some cases the lemma is evidently false. Thus, suppose there are two quantities of matter A and B, the one containing half a pound, and the other a third part of one. Let both be continually divided by 2; and though their ratio, or the proportion of the one to the other, doth not vary, yet the difference between them perpetually becomes less, as well as the quantities themselves, until both the difference and quantities themselves become less than any assignable quantity: yet the difference will never totally vanish, nor the quantities become equal, as is evident from the two following series:

\begin{array}{cccccccccccc} \frac{1}{2} & \frac{1}{4} & \frac{1}{8} & \frac{1}{16} & \frac{1}{32} & \frac{1}{64} & \frac{1}{128} & \frac{1}{256} & \frac{1}{512} & \frac{1}{1024} & \frac{1}{2048} & \frac{1}{4096} & \frac{1}{8192} & \frac{1}{16384} & \frac{1}{32768} & \frac{1}{65536} & \frac{1}{131072} & \frac{1}{262144} & \frac{1}{524288} & \frac{1}{1048576} & \frac{1}{2097152} & \frac{1}{4194304} & \frac{1}{8388608} & \frac{1}{16777216} & \frac{1}{33554432} & \frac{1}{67108864} & \frac{1}{134217728} & \frac{1}{268435456} & \frac{1}{536870912} & \frac{1}{1073741824} & \frac{1}{2147483648} & \frac{1}{4294967296} & \frac{1}{8589934592} & \frac{1}{17179869184} & \frac{1}{34359738368} & \frac{1}{68709476736} & \frac{1}{137418953472} & \frac{1}{274837906944} & \frac{1}{549675813888} & \frac{1}{1099351627776} & \frac{1}{2198703255552} & \frac{1}{4397406511104} & \frac{1}{8794813022208} & \frac{1}{17589626044416} & \frac{1}{35179252088832} & \frac{1}{70358504177664} & \frac{1}{140717008355328} & \frac{1}{281434016710656} & \frac{1}{562868033421312} & \frac{1}{1125736066842624} & \frac{1}{2251472133685248} & \frac{1}{4502944267370496} & \frac{1}{9005888534740992} & \frac{1}{18011777069481984} & \frac{1}{36023554138963968} & \frac{1}{72047108277927936} & \frac{1}{144094216555855872} & \frac{1}{288188433111711744} & \frac{1}{576376866223423488} & \frac{1}{1152753732446846976} & \frac{1}{2305507464893693952} & \frac{1}{4611014929787387904} & \frac{1}{9222029859574775808} & \frac{1}{18444059719149551616} & \frac{1}{36888119438299103232} & \frac{1}{73776238876598206464} & \frac{1}{147552477753196412928} & \frac{1}{295104955506392825856} & \frac{1}{590209911012785651712} & \frac{1}{1180419822025571303424} & \frac{1}{2360839644051142606848} & \frac{1}{4721679288102285213696} & \frac{1}{9443358576204570427392} & \frac{1}{18886717152409140854784} & \frac{1}{37773434304818281709568} & \frac{1}{75546868609636563419136} & \frac{1}{151093737219273126838272} & \frac{1}{302187474438546253676544} & \frac{1}{604374948877092507353088} & \frac{1}{1208749897754185014706176} & \frac{1}{2417499795508370029412352} & \frac{1}{4834999591016740058824704} & \frac{1}{9669999182033480117649408} & \frac{1}{19339998364066960235298816} & \frac{1}{38679996728133920470597632} & \frac{1}{773599934562678409411951648} & \frac{1}{1547199869125356818823903296} & \frac{1}{3094399738250713637647806592} & \frac{1}{6188799476501427275295613184} & \frac{1}{12377598953002854550591226368} & \frac{1}{24755197906005709101182452736} & \frac{1}{49510395812011418202364905472} & \frac{1}{99020791624022836404729810944} & \frac{1}{198041583248045672809459621888} & \frac{1}{396083166496091345618919243776} & \frac{1}{792166332992182691237838487552} & \frac{1}{1584332665984365382475676975104} & \frac{1}{3168665331968730764951353950208} & \frac{1}{6337330663937461529902707900416} & \frac{1}{12674661327874923059805415800832} & \frac{1}{25349322655749846119610831601664} & \frac{1}{50698645311499692239221663203328} & \frac{1}{101397290622999384478443326406656} & \frac{1}{202794581245998768956886652913312} & \frac{1}{405589162491997537913773305826624} & \frac{1}{811178324983995075827546611653248} & \frac{1}{1622356649967990151655093223306496} & \frac{1}{3244713299935980303310186446612992} & \frac{1}{6489426599871960606620372893225984} & \frac{1}{12978853199743921213240745786451968} & \frac{1}{25957706399487842426481491572903936} & \frac{1}{51915412798975684852962983145807872} & \frac{1}{103830825597951369705925966291615744} & \frac{1}{207661651195902739411851932583231488} & \frac{1}{415323302391805478823703865166462976} & \frac{1}{830646604783610957647407730332925952} & \frac{1}{1661293209567221915294815460665851904} & \frac{1}{3322586419134443830589630921331703808} & \frac{1}{6645172838268887661179261842663407616} & \frac{1}{13290345676537775322358523685326832} & \frac{1}{26580691353075550644717047370653664} & \frac{1}{53161382706151101289434094741307328} & \frac{1}{106322765412302202578868189482614656} & \frac{1}{21264553082460440515773637896522912} & \frac{1}{42529106164920881031547275793045824} & \frac{1}{85058212329841762063094551586091648} & \frac{1}{170116424659683524126189103172183296} & \frac{1}{340232849319367048252378206344366592} & \frac{1}{68046569863873409650475641268873296} & \frac{1}{13609313972774681930095128253776} & \frac{1}{27218627945549363860190256507552} & \frac{1}{54437255891098727720380513015104} & \frac{1}{108874511782197455440761026030208} & \frac{1}{217749023564394910881522052060416} & \frac{1}{435498047128789821763044104120832} & \frac{1}{870996094257579643526088208241664} & \frac{1}{17419921885151592870521764164832} & \frac{1}{34839843770303185741043528329664} & \frac{1}{69679687540606371482087056659328} & \frac{1}{139359375081212742964174113318656} & \frac{1}{278718750162425485928348226637312} & \frac{1}{557437500324850971856696453274624} & \frac{1}{1114875000649701943713392906549248} & \frac{1}{2229750001299403887426785813098496} & \frac{1}{4459500002598807774853571626196992} & \frac{1}{8919000005197615549707143252393984} & \frac{1}{17838000000395231099414286504787968} & \frac{1}{35676000000790462198828573009575936} & \frac{1}{71352000001580924397657146019151872} & \frac{1}{142704000003161848795314292038233744} & \frac{1}{285408000006333697590628584076467488} & \frac{1}{570816000001267395181257168152934976} & \frac{1}{1141632000002534790362514336305869952} & \frac{1}{2283264000005069580725028670611739904} & \frac{1}{4566528000010139161450057341223479808} & \frac{1}{9133056000020278322900114682446959616} & \frac{1}{18266112000040556645800229364893918208} & \frac{1}{36532224000081113291600458729787836416} & \frac{1}{73064448000162226583200917559575672832} & \frac{1}{146128896000324453166401835119151345664} & \frac{1}{2922577920006489063328036702383026912} & \frac{1}{5845155840012978126656073404766052224} & \frac{1}{11690311680025956253312146809532104448} & \frac{1}{23380623360051912506624293019064208896} & \frac{1}{46761246720103825013248586038128417792} & \frac{1}{93522493440207650026497172076256835584} & \frac{1}{187044986880415300052994344152513671168} & \frac{1}{374089973760830600105988688305027442336} & \frac{1}{748179947521661200211977376610054884672} & \frac{1}{1496359895043322400423954753220109689344} & \frac{1}{2992719790086644800847909506440219378688} & \frac{1}{5985439580173289601695819012880438757376} & \frac{1}{1197087916034657920339163802576087554752} & \frac{1}{2394175832069315840678327605152175109088} & \frac{1}{4788351664138631681356655210304350208176} & \frac{1}{9576703328277263362713310420608700403328} & \frac{1}{19153406656554526725426620841217400806656} & \frac{1}{38306813313109053450853241682434801613312} & \frac{1}{7661362662621810690170648336486960322664} & \frac{1}{15322725325243621380341296672973920645328} & \frac{1}{30645450650487242760682593345947840126656} & \frac{1}{61290901300974485521365186691895680253312} & \frac{1}{122581802601948971042730373383791360506624} & \frac{1}{245163605203897942085460746767582720101328} & \frac{1}{490327210407795884170921493535165440202656} & \frac{1}{980654420815591768341842987070330880405312} & \frac{1}{1961308841631183536683685974140661760810624} & \frac{1}{3922617683262367073367371948281323521621248} & \frac{1}{784523536652473414673474389656264704322496} & \frac{1}{1569047073304946829346948779312529408644992} & \frac{1}{3138094146609893658693897558625058809289984} & \frac{1}{6276188293219787317387795117250117678579808} & \frac{1}{12552376586439574634775590234500235357159616} & \frac{1}{2510475317287914926955118046900047071430032} & \frac{1}{5020950634575829853910236093800094042860064} & \frac{1}{10041901269151659707820472187600188087400128} & \frac{1}{20083802538303319415640944375200376017400256} & \frac{1}{4016760507660663883128188875040075203400512} & \frac{1}{803352101532132776625637775008015068000256} & \frac{1}{1606704203064265553251275550016030136000512} & \frac{1}{32134084061285311065025511000320602720000256} & \frac{1}{6426816812257062213005102200064012013440000512} & \frac{1}{12853633624514124426010204400128024026880000256} & \frac{1}{25707267249028248852020408800256048053760000512} & \frac{1}{514145344980564977040408176005120960107520000256} & \frac{1}{10282906899611299540808163520051201920215040000512} & \frac{1}{20565813799222599081616327040051203840430080000256} & \frac{1}{41131627598445198163232654080051207680860160000512} & \frac{1}{82263255196890396326465308160051215361720320000256} & \frac{1}{164526510393780792652930616320051230723440640000512} & \frac{1}{329053020787561585305861232640051261446880320000256} & \frac{1}{65810604157512317061172246528005121228976640000512} & \frac{1}{131621208315024634122344493056005122457952320000256} & \frac{1}{263242416630049268244688986112005124915904640000512} & \frac{1}{526484833260098536489377972224005129831809280000256} & \frac{1}{1052969666520197072978755944448005121966368560000512} & \frac{1}{2105939333040394145957511888896005123933367120000256} & \frac{1}{4211878666080788291915023777792005127866734240000512} & \frac{1}{8423757332161576583830047555584005121573468480000256} & \frac{1}{16847514664323153167660095111168005123146937920000512} & \frac{1}{33695029328646306335320190222336005126293875840000256} & \frac{1}{67390058657292612670640380444672005121258775680000512} & \frac{1}{134780117314585225341280760889344005122517551360000256} & \frac{1}{269560234629170450682561521778688005125035102720000512} & \frac{1}{539120469258340901365123043557376005121007025440000256} & \frac{1}{107824093851668180273024711071464005122014050080000512} & \frac{1}{21564818770333636054604942214292800512402800000256} & \frac{1}{43129637540667272109209884428585600512805600000512} & \frac{1}{862592750813345442184197688571712005121611200000256} & \frac{1}{1725185501626690884368395377143424005123222400000512} & \frac{1}{345037100325338176873679075428684800512644480000256} & \frac{1}{6900742006506763537473581508573696005121288960000512} & \frac{1}{13801484013013527074947163017157392005122577920000256} & \frac{1}{27602968026027054149894326034314784005125155840000512} & \frac{1}{55205936052054108299788652068629568005121031680000256} & \frac{1}{110411872104108216599577304137259136005122063360000512} & \frac{1}{220823744208216433199154608274518272005124126720000256} & \frac{1}{441647488416432866398309216549036544005128253440000512} & \frac{1}{8832949768328657327966184330980730880051216506880000256} & \frac{1}{17665899536657314655932368661961461760051233013760000512} & \frac{1}{35331799073314629311864737323922923520051266027520000256} & \frac{1}{70663598146629258623729474647845843200512132055040000512} & \frac{1}{14132719629325851724745894929569168640051226410080000256} & \frac{1}{282654392586517034494917898591383360051252820160000512} & \frac{1}{5653087851730340689898357971827667200512105640320000256} & \frac{1}{1130617570346068137979671594365532800512211280000512} & \frac{1}{2261235140692136275959343188731065600512422560000256} & \frac{1}{4522470281384272551918686377462131200512845120000512} & \frac{1}{90449405627685451038373727549242624005121690240000256} & \frac{1}{180898811255370902076747455098485248005123380480000512} & \frac{1}{361797622510741804153494910196970496005126760960000256} & \frac{1}{7235952450214836083069898203939409920051213521920000512} & \frac{1}{1447190490042967216613979640787880960051227043840000256} & \frac{1}{2894380980085934433227959281575761920051254087680000512} & \frac{1}{57887619601718688664559185631515238400512108175360000256} & \frac{1}{115775239203437377329118371263030476800512216350720000512} & \frac{1}{23155047840687475465823674252606095360051243270080000256} & \frac{1}{46310095681374950931647348505212090720051286540160000512} & \frac{1}{926201913627499018632946970104241804800512173090240000256} & \frac{1}{185240382725499803726589394020848380800512346180480000512} & \frac{1}{370480765450999607453178788040696761600512692360960000256} & \frac{1}{7409615309019992149063575760813935232005121444609920000512} & \frac{1}{1481923061803998429812715152162987046400512288921920000256} & \frac{1}{2963846123607996859625430304325974092800512577843840000512} & \frac{1}{59276922472159937192508606086519480768005121155687680000256} & \frac{1}{118553844944319874385017212133038941536005122311375360000512} & \frac{1}{2371076898886397487700344242660778830720051246227520000256} & \frac{1}{474215379777279497540068848532155766080051292455040000512} & \frac{1}{948430759554558995080137697064311532160051218490080000256} & \frac{1}{1896861519109117990160275394128623064320051236980080000512} & \frac{1}{3793723038218235980320550788257246048640051273960160000256} & \frac{1}{7587446076436471960641101576514492092800512147920320000512} & \frac{1}{15174892152872943921202203153028984185600512295840320000256} & \frac{1}{3034978430574588784240440630605796836800512591680320000512} & \frac{1}{60699568611491775684808812612115936736005121183360320000256} & \frac{1}{121399137222983551369617625224231873472005122366720320000512} & \frac{1}{2427982744459671027392352504484636688005124733440320000256} & \frac{1}{4855965488919342054784705008969273376005129466880320000512} & \frac{1}{971193097783868

Newtonian Philosophy. In his succeeding lemmas, Sir Isaac goes on to prove, in a manner similar to the above, that the ultimate ratios of the sine, chord, and tangent of arcs infinitely diminished, are ratios of equality, and therefore that in all our reasonings about these we may safely use the one for the other:—that the ultimate form of evanescent triangles made by the arc, chord, and tangent, is that of similitude, and their ultimate ratio is that of equality; and hence, in reasonings about ultimate ratios, we may safely use these triangles for each other, whether made with the sine, the arc, or the tangent.—He then shows some properties of the ordinates of curvilinear figures; and proves that the spaces which a body describes by any finite force urging it, whether that force is determinate and immutable, or is continually augmented or continually diminished, are, in the very beginning of the motion, one to the other in the duplicate ratio of the powers. And, lastly, Having added some demonstrations concerning the evanescence of angles of contact, he proceeds to lay down the mathematical part of his system, and which depends on the following theorems:

THEOR. I. The areas which revolving bodies describe by radii drawn to an immoveable centre of force, lie in the same immoveable planes, and are proportional to the times in which they are described.—For, suppose the time to be divided into equal parts, and in the first part of that time, let the body by its innate force describe the right line AB (fig. 2.); in the second part of that time, the same would, by LAW 1. if not hindered, proceed directly to c along the line B \equiv AB; so that by the radii AS, BS, cS, drawn to the centre, the equal areas ASB, BSc, would be described. But, when the body is arrived at B, suppose the centripetal force acts at once with a great impulse, and turning aside the body from the right line Bc, compels it afterwards to continue its motion along the right line BC. Draw cC parallel to BS, meeting BC in C; and at the end of the second part of the time, the body, by Cor. 1. of the Laws, will be found in C, in the same plane with the triangle ASB. Join SC; and because SB and cC are parallel, the triangle SBC will be equal to the triangle SBC, and therefore also to the triangle SAB. By the like argument, if the centripetal force acts successively in C, D, E, &c. and makes the body in each single particle of time to describe the right lines CD, DE, EF, &c. they will all lie in the same plane; and the triangle SCD will be equal to the triangle SBC, and SDE to SCD, and SEF to SDE. And therefore, in equal times, equal areas are described in one immoveable plane; and, by composition, any sums SADS, SAES, of those areas are, one to the other, as the times in which they are described. Now, let the number of those triangles be augmented, and their size diminished in infinitum; and then, by the preceding lemmas, their ultimate perimeter ADF will be a curve line: and therefore the centripetal force by which the body is perpetually drawn back from the tangent of this curve will act continually; and any described areas SADS, SAES, which are always proportional to the times of description, will, in this case also, be proportional to those times. Q. E. D.

COR. 1. The velocity of a body attracted towards an immoveable centre, in spaces void of resistance, is reciprocally as the perpendicular let fall from that centre

on the right line which touches the orbit. For the velocities in these places, A, B, C, D, E, are as the Newtonian Philosophy. bases AB, BC, DE, EF, of equal triangles; and these bases are reciprocally as the perpendiculars let fall upon them.

COR. 2. If the chords AB, BC, of two arcs, successively described in equal times by the same body, in spaces void of resistance, are completed into a parallelogram ABCV, and the diagonal BV of this parallelogram, in the position which it ultimately acquires when those arcs are diminished in infinitum, is produced both ways, it will pass through the centre of force.

COR. 3. If the chords AB, BC, and DE, EF, of arcs described in equal times, in spaces void of resistance, are completed into the parallelograms ABCV, DEFZ, the forces in B and E are one to the other in the ultimate ratio of the diagonals BV, EZ, when those arcs are diminished in infinitum. For the motions BC and EF of the body (by Cor. 1. of the Laws), are compounded of the motions Bc, BV and Ef, EZ; but BV and EZ, which are equal to Cc and Ff, in the demonstration of this proposition, were generated by the impulses of the centripetal force in B and E, and are therefore proportional to those impulses.

COR. 4. The forces by which bodies, in spaces void of resistance, are drawn back from rectilinear motions, and turned into curvilinear orbits, are one to another as the versed sines of arcs described in equal times; which versed sines tend to the centre of force, and bisect the chords when these arcs are diminished to infinity. For such versed sines are the halves of the diagonals mentioned in Cor. 3.

COR. 5. And therefore those forces are to the force of gravity, as the said versed sines to the versed sines perpendicular to the horizon of those parabolic arcs which projectiles describe in the same time.

COR. 6. And the same things do all hold good (by Cor. 5. of the laws) when the planes in which the bodies are moved, together with the centres of force, which are placed in those planes, are not at rest, but move uniformly forward in right lines.

THEOR. II. Every body that moves in any curve line described in a plane, and, by a radius drawn to a point either immoveable or moving forward with a uniform rectilinear motion, describes about that point areas proportional to the times, is urged by a centripetal force directed to that point.

CASE I. For every body that moves in a curve line is (by Law 1.) turned aside from its rectilinear course by the action of some force that impels it; and that force by which the body is turned off from its rectilinear course, and made to describe in equal times the least equal triangles SAB, SBC, SCD, &c. about the immoveable point S, (by Prop. 40. E. 1. and Law 2.) acts in the place B according to the direction of a line parallel to C; that is, in the direction of the line BS; and in the place C according to the direction of a line parallel to dD, that is, in the direction of the line CS, &c.; and therefore acts always in the direction of lines tending to the immoveable point S. Q. E. D.

CASE II. And (by Cor. 5. of the laws) it is indifferent whether the superficies in which a body describes a curvilinear figure be quiescent, or moves together with the body, the figure described, and its point S, uniformly forward in right lines.

COR.

COR. 1. In non-resisting spaces or mediums, if the areas are not proportional to the times, the forces are not directed to the point in which the radii meet; but deviate therefrom in consequentia, or towards the parts to which the motion is directed, if the description of the areas is accelerated; but in antecedentia if retarded.

COR. 2. And even in resisting mediums, if the description of the areas is accelerated, the directions of the forces deviate from the point in which the radii meet, towards the parts to which the motion tends.

A body may be urged by a centripetal force compounded of several forces. In which case the meaning of the proposition is, that the force which results out of all tends to the point S. But if any force acts perpetually in the direction of lines perpendicular to the described surface, this force will make the body to deviate from the plane of its motion, but will neither augment nor diminish the quantity of the described surface; and is therefore not to be neglected in the composition of forces.

THEOR. III. Every body that, by a radius drawn to the centre of another body, howsoever moved, describes areas about that centre proportional to the times, is urged by a force compounded of the centripetal forces tending to that other body, and of all the accelerative force by which that other body is impelled.—The demonstration of this is a natural consequence of the theorem immediately preceding.

Hence, if the one body L, by a radius drawn to the other body T, describes areas proportional to the times, and from the whole force by which the first body L is urged, (whether that force is simple, or, according to Cor. 2. of the laws, compounded of several forces), we subtract that whole accelerative force by which the other body is urged; the whole remaining force by which the first body is urged will tend to the other body T, as its centre.

And vice versa, if the remaining force tends nearly to the other body T, those areas will be nearly proportional to the times.

If the body L, by a radius drawn to the other body T, describes areas, which, compared with the times, are very unequal, and that other body T be either at rest, or moves uniformly forward in a right line, the action of the centripetal force tending to that other body T is either none at all, or it is mixed and combined with very powerful actions of other forces; and the whole force compounded of them all, if they are many, is directed to another (immoveable or moveable) centre. The same thing obtains when the other body is actuated by any other motion whatever; provided that centripetal force is taken which remains after subtracting that whole force acting upon that other body T.

Because the equable description of areas indicates that a centre is respected by that force with which the body is most affected, and by which it is drawn back from its rectilinear motion, and retained in its orbit, we may always be allowed to use the equable description of

areas as an indication of a centre about which all circular motion is performed in free spaces. Newtonian
Philosophy.

THEOR. IV. The centripetal forces of bodies which by equable motions describe different circles, tend to the centres of the same circles; and are one to the other as the squares of the arcs described in equal times applied to the radii of circles.—For these forces tend to the centres of the circles, (by Theor. 2. and Cor. 2. Theor. 1.) and are to one another as the versed sines of the least arcs described in equal times (by Cor. 4. Theor. 1.), that is, as the squares of the same arcs applied to the diameters of the circles, by one of the lemmas; and therefore, since those arcs are as arcs described in any equal times, and the diameters are as the radii, the forces will be as the squares of any arcs described in the same time, applied to the radii of the circles. Q. E. D.

COR. 1. Therefore, since those arcs are as the velocities of the bodies, the centripetal forces are in a ratio compounded of the duplicate ratio of the velocities directly, and of the simple ratio of the radii inversely.

COR. 2. And since the periodic times are in a ratio compounded of the ratio of the radii directly, and the ratio of the velocities inversely; the centripetal forces are in a ratio compounded of the ratio of the radii directly, and the duplicate ratio of the periodic times inversely.

COR. 3. Whence, if the periodic times are equal, and the velocities therefore as the radii, the centripetal forces will be equal among themselves; and the contrary.

COR. 4. If the periodic times and the velocities are both in the subduplicate ratio of the radii, the centripetal forces will be equal among themselves; and the contrary.

COR. 5. If the periodic times are as the radii, and therefore the velocities equal, the centripetal forces will be reciprocally as the radii; and the contrary.

COR. 6. If the periodic times are in the sesquiplicate ratio of the radii, and therefore the velocities reciprocally in the subduplicate ratio of the radii, the centripetal forces will be in the duplicate ratio of the radii inversely; and the contrary.

COR. 7. And universally, if the periodic time is as any power R^n of the radius R, and therefore the velocity reciprocally as the power R^{n-1} of the radius, the centripetal force will be reciprocally as the power R^{1-n} of the radius; and the contrary.

COR. 8. The same things all hold concerning the times, the velocities, and forces, by which bodies describe the similar parts of any similar figures, that have their centres in a similar position within those figures, as appears by applying the demonstrations of the preceding cases to those. And the application is easy, by only substituting the equable description of areas in the place of equable motion, and using the distances of the bodies from the centres instead of the radii.

COR. 9. From the same demonstration it likewise follows, that the arc which a body uniformly revolving in a circle by means of a given centripetal force describes in any time, is a mean proportional between the diameter of the circle, and the space which the same body, falling by the same given force, would descend through in the same given time.

Newtonian Philosophy. "By means of the preceding proposition and its corollaries (says Sir Isaac), we may discover the proportion of a centripetal force to any other known force, such as that of gravity. For if a body by means of its gravity revolves in a circle concentric to the earth, this gravity is the centripetal force of that body. But from the descent of heavy bodies, the time of one entire revolution, as well as the arc described in any given time, is given (by Cor. 9. of this theorem). And by such propositions Mr Huygens, in his excellent book De Horologio Oscillatorio, has compared the force of gravity with the centrifugal forces of revolving bodies.

The preceding proposition may also be demonstrated in the following manner. In any circle suppose a polygon to be inscribed of any number of sides. And if a body, moved with a given velocity along the sides of the polygon, is reflected from the circle at the several angular points; the force with which, at every reflection it strikes the circle, will be as its velocity: and therefore the sum of the forces, in a given time, will be as that velocity and the number of reflections conjointly; that is (if the species of the polygon be given), as the length described in that given time, and increased or diminished in the ratio of the same length to the radius of the circle; that is, as the square of that length applied to the radius; and therefore, if the polygon, by having its sides diminished in infinitum, coincides with the circle, as the square of the arc described in a given time applied to the radius. This is the centrifugal force, with which the body impels the circle; and to which the contrary force, wherewith the circle continually repels the body towards the centre, is equal.

On these principles hangs the whole of Sir Isaac Newton's mathematical philosophy. He now shows how to find the centre to which the forces impelling any body are directed, having the velocity of the body given: and finds the centrifugal force to be always as the versed sine of the nascent arc directly, and as the square of the time inversely; or directly as the square of the velocity, and inversely as the chord of the nascent arc. From these premises he deduces the method of finding the centripetal force directed to any given point when the body revolves in a circle; and this whether the central point is near or at an immense distance; so that all the lines drawn from it may be taken for parallels. The same thing he shows with regard to bodies revolving in spirals, ellipses, hyperbolas, or parabolas.—Having the figures of the orbits given, he shows also how to find the velocities and moving powers; and, in short, solves all the most difficult problems relating to the celestial bodies with an astonishing degree of mathematical skill. These problems and demonstrations are all contained in the first book of the Principia: but to give an account of them here would far exceed our limits; neither would many of them be intelligible, excepting to first-rate mathematicians.

In the second book, Sir Isaac treats of the properties of fluids, and their powers of resistance: and here he lays down such principles as entirely overthrow the doctrine of Des Cartes's vortices, which was the fashionable system in his time. In the third book, he begins particularly to treat of the natural phenomena, and apply them to the mathematical principles formerly demonstrated; and, as a necessary preliminary to this part,

he lays down the following rules for reasoning in natural philosophy.

1. We are to admit no more causes of natural things than such as are both true and sufficient to explain their natural appearances.

2. Therefore to the same natural effects we must always assign, as far as possible, the same causes.

3. The qualities of bodies which admit neither intension or remission of degrees, and which are found to belong to all bodies within the reach of our experiments, are to be esteemed the universal qualities of all bodies whatsoever.

4. In experimental philosophy, we are to look upon propositions collected by general induction from phenomena as accurately or very nearly true, notwithstanding any contrary hypotheses that may be imagined, till such time as other phenomena occur, by which they may either be made more accurate, or liable to exceptions.

The phenomena first considered are, 1. That the satellites of Jupiter, by radii drawn to the centre of their primary, describe areas proportional to the times of their description; and that their periodic times, the fixed stars being at rest, are in the sesquiplicate ratio of their distances from its centre. 2. The same thing is likewise observed of the phenomena of Saturn. 3. The five primary planets, Mercury, Venus, Mars, Jupiter, and Saturn, with their several orbits encompass the sun. 4. The fixed stars being supposed at rest, the periodic times of the five primary planets, and of the earth, about the sun, are in the sesquiplicate proportion of their mean distances from the sun. 5. The primary planets, by radii drawn to the earth, describe areas no ways proportionable to the times: but the areas which they describe by radii drawn to the sun are proportional to the times of description. 6. The moon, by a radius drawn to the centre of the earth, describes an area proportional to the time of description. All these phenomena are undeniable from astronomical observations, and are explained at large under the article ASTRONOMY. The mathematical demonstrations are next applied by Sir Isaac Newton in the following propositions:

PROP. I. The forces by which the satellites of Jupiter are continually drawn off from rectilinear motions, and retained in their proper orbits, tend to the centre of that planet; and are reciprocally as the squares of the distances of those satellites from that centre. The former part of this proposition appears from Theor. 2. or 3. and the latter from Cor. 6. of Theor. 5.; and the same thing we are to understand of the satellites of Saturn.

PROP. II. The forces by which the primary planets are continually drawn off from rectilinear motions, and retained in their proper orbits, tend to the sun; and are reciprocally as the squares of the distances from the sun's centre. The former part of this proposition is manifest from Phenomenon 5. just mentioned, and from Theor. 2.; the latter from Phenomenon 4. and Cor. 6. of Theor. 4. But this part of the proposition is with great accuracy deducible from the quiescence of the aphelion points. For a very small aberration from the reciprocal duplicate proportion would produce a motion of the apsides, sensible in every single revolution, and in many of them enormously great.

PROP. III. The force by which the moon is retained in

Newtonian in its orbit, tends towards the earth; and is reciprocally as the square of the distance of its place from the centre of the earth. The former part of this proposition is evident from Phenom. 5. and Theor. 2.; the latter from Phenom. 6. and Theor. 2. or 3. It is also evident from the very slow motion of the moon's apogee; which, in every single revolution, amounting but to 3^{\circ} 3' \text{ in consequentia}, may be neglected: and this more fully appears from the next proposition.

PROP. IV. The moon gravitates towards the earth, and by the force of gravity is continually drawn off from a rectilinear motion, and retained in its orbit.—The mean distance from the moon to the earth in the syzgies, in semidiameters of the latter, is about 60\frac{1}{2}. Let us assume the mean distance of 60 semidiameters in the syzgies; and suppose one revolution of the moon in respect of the fixed stars to be completed in 27^{\text{d}} 7^{\text{h}} 43^{\text{m}}, as astronomers have determined; and the circumference of the earth to amount to 123,249,600 Paris feet. Now, if we imagine the moon, deprived of all motion, to be let go, so as to descend towards the earth with the impulse of all that force by which it is retained in its orbit, it will, in the space of one minute of time, describe in its fall 15\frac{1}{2} Paris feet. For the versed sine of that arc which the moon, in the space of one minute of time, describes by its mean motion at the distance of 60 semidiameters of the earth, is nearly 15\frac{1}{2} Paris feet; or more accurately, 15 feet one inch and one line \frac{1}{2}. Wherefore since that force, in approaching to the earth, increases in the reciprocal duplicate proportion of the distance; and, upon that account, at the surface of the earth, is 60 \times 60 times greater than that at the moon; a body in our regions, falling with that force, ought, in the space of one minute of time, to describe 60 \times 60 \times 15\frac{1}{2} Paris feet; and in the space of one second of time to describe 15\frac{1}{2} of those feet; or, more accurately, 15 feet 1 inch 1 line \frac{1}{2}. And with this very force we actually find that bodies here on earth do really descend.—For a pendulum oscillating seconds in the latitude of Paris, will be three Paris feet and 8\frac{1}{2} lines in length, as Mr Huygens has observed. And the space which a heavy body describes by falling one second of time, is to half the length of the pendulum in the duplicate ratio of the circumference of the circle to its diameter; and is therefore 15 Paris feet 1 inch 1 line \frac{1}{2}. And therefore the force by which the moon is retained in its orbit, becomes at the very surface of the earth, equal to the force of gravity which we observe in heavy bodies there. And therefore (by Rule 1. and 2.) the force by which the moon is retained in its orbit is that very same force which we commonly call gravity. For were gravity another force different from that, then bodies descending to the earth with the joint impulse of both forces would fall with a double velocity, and, in the space of one second of time, would describe 30\frac{1}{2} Paris feet; altogether against experience.

The demonstration of this proposition may be more diffusely explained after the following manner: Suppose several moons to revolve about the earth, as in the system of Jupiter or Saturn, the periodic times of those moons would (by the argument of induction) observe the same law which Kepler found to obtain among the planets; and therefore their centripetal forces would be reciprocally as the squares of the distances

from the centre of the earth, by Prop. I. Now, if Newtonian the lowest of these were very small, and were so near Philosophy. the earth as almost to touch the tops of the highest mountains, the centripetal force thereof, retaining it in its orbit, would be very nearly equal to the weights of any terrestrial bodies that should be found upon the tops of these mountains; as may be known from the foregoing calculation. Therefore, if the same little moon should be deserted by its centrifugal force that carries it through its orbit, it would descend to the earth; and that with the same velocity as heavy bodies do actually descend with upon the tops of those very mountains, because of the equality of forces that oblige them both to descend. And if the force by which that lowest moon would descend were different from that of gravity, and if that moon were to gravitate towards the earth, as we find terrestrial bodies do on the tops of mountains, it would then descend with twice the velocity, as being impelled by both these forces conspiring together. Therefore, since both these forces, that is, the gravity of heavy bodies, and the centripetal forces of the moons, respect the centre of the earth, and are similar and equal between themselves, they will (by Rule 1. and 2.) have the same cause. And therefore the force which retains the moon in its orbit, is that very force which we commonly call gravity; because otherwise, this little moon at the top of a mountain must either be without gravity, or fall twice as swiftly as heavy bodies use to do.

Having thus demonstrated that the moon is retained in its orbit by its gravitation towards the earth, it is easy to apply the same demonstration to the motions of the other secondary planets, and of the primary planets round the sun, and thus to show that gravitation prevails throughout the whole creation; after which, Sir Isaac proceeds to show from the same principles that the heavenly bodies gravitate towards each other, and contain different quantities of matter, or have different densities in proportion to their bulks.

PROP. V. All bodies gravitate towards every planet; and the weights of bodies towards the same planet, at equal distances from its centre, are proportional to the quantities of matter they contain.

It has been confirmed by many experiments, that all sorts of heavy bodies (allowance being made for the inequality of retardation by some small resistance of the air), descend to the earth from equal heights in equal times; and that equality of times we may distinguish to a great accuracy by the help of pendulums. Sir Isaac Newton tried the thing in gold, silver, lead, glass, sand, common salt, wood, water, and wheat. He provided two wooden boxes, round and equal, filled the one with wood, and suspended an equal weight of gold in the centre of oscillation of the other. The boxes hanging by equal threads of 11 feet, made a couple of pendulums, perfectly equal in weight and figure, and equally receiving the resistance of the air. And placing the one by the other, he observed them to play together forwards and backward, for a long time, with equal vibrations. And therefore the quantity of matter in the gold was to the quantity of matter in the wood, as the action of the motive force (or vis motrix) upon all the gold, to the action of the same upon all the wood; that is, as the weight

Newtonian weight of the one to the weight of the other. And Philosophy, the like happened in the other bodies. By these experiments, in bodies of the same weight, he could manifestly have discovered a difference of matter less than the thousandth part of the whole, had any such been. But without all doubt, the nature of gravity towards the planets, is the same as towards the earth. For should we imagine our terrestrial bodies removed to the orb of the moon, and there, together with the moon, deprived of all motion, to be let go, so as to fall together towards the earth; it is certain from what we have demonstrated before, that in equal times, they would describe equal spaces with the moon, and of consequence are to the moon in quantity of matter, as their weights to its weight. Moreover, since the satellites of Jupiter perform their revolutions in times which observe the sesquiplicate proportion of their distances from Jupiter's centre, their accelerative gravities towards Jupiter will be reciprocally as the squares of their distances from Jupiter's centre; that is, equal at equal distances. And therefore, these satellites, if supposed to fall towards Jupiter from equal heights, would describe equal spaces in equal times, in like manner as heavy bodies do on our earth. And by the same argument if the circumsolar planets were supposed to be let fall at equal distances from the sun, they would, in their descent towards the sun, describe equal spaces in equal times. But forces, which equally accelerate unequal bodies, must be as those bodies: that is to say, the weights of the planets towards the sun must be as their quantities of matter. Further, That the weights of Jupiter and his satellites towards the sun are proportional to the several quantities of their matter, appears from the exceeding regular motions of the satellites. For if some of the bodies were more strongly attracted to the sun in proportion to their quantity of matter than others, the motions of the satellites would be disturbed by that inequality of attraction. If, at equal distances from the sun, any satellite, in proportion to the quantity of its matter, did gravitate towards the sun, with a force greater than Jupiter in proportion to his, according to any given proportion, suppose d to e; then the distance between the centres of the sun and of the satellite's orbit would be always greater than the distance between the centres of the sun and of Jupiter nearly in the subduplicate of that proportion. And if the satellite gravitated towards the sun with a force less in the proportion of e to d, the distance of the centre of the satellite's orbit from the sun would be less than the distance of the centre of Jupiter's orbit from the sun in the subduplicate of the same proportion. Therefore, if, at equal distances from the sun, the accelerative gravity of any satellite towards the sun were greater or less than the accelerative gravity of Jupiter towards the sun but by \frac{1}{2} part of the whole gravity; the distance of the centre of the satellite's orbit from the sun would be greater or less than the distance of Jupiter from the sun by \frac{1}{2} part of the whole distance; that is, by a fifth part of the distance of the utmost satellite from the centre of Jupiter; an eccentricity of the orbit which would be very sensible. But the orbits of the satellites are concentric to Jupiter; therefore the accelerative gravities of Jupiter, and of all its satellites, towards the sun, are equal among themselves. And by the same argument, the weight of Saturn and of his sat-

tellites towards the sun, at equal distances from the sun, are as their several quantities of matter; and the Newtonian weights of the moon and of the earth towards the sun, are either none, or accurately proportional to the masses of matter which they contain.

But further, the weights of all the parts of every planet towards any other planet are one to another as the matter in the several parts. For if some parts gravitate more, others less, than in proportion to the quantity of their matter; then the whole planet, according to the sort of parts with which it most abounds, would gravitate more or less than in proportion to the quantity of matter in the whole. Nor is it of any moment whether these parts are external or internal. For if, as an instance, we should imagine the terrestrial bodies with us to be raised up to the orb of the moon, to be there compared with its body; if the weights of such bodies were to the weights of the external parts of the moon as the quantities of matter in the one and in the other respectively, but to the weights of the internal parts in a greater or less proportion; then likewise the weights of those bodies would be to the weight of the whole moon in a greater or less proportion; against what we have showed above.

COR. 1. Hence the weights of bodies do not depend upon their forms and textures. For if the weights could be altered with the forms, they would be greater or less, according to the variety of forms in equal matter; altogether against experience.

COR. 2. Universally, all bodies about the earth gravitate towards the earth; and the weights of all, at equal distances from the earth's centre, are as the quantities of matter which they severally contain. This is the quality of all bodies within the reach of our experiments; and therefore (by Rule 3.) to be affirmed of all bodies whatsoever. If ether, or any other body, were either altogether void of gravity, or were to gravitate less in proportion to its quantity of matter; then, because (according to Aristotle, Des Cartes, and others) there is no difference betwixt that and other bodies, but in mere form of matter, by a successive change from form to form, it might be changed at last into a body of the same condition with those which gravitate most in proportion to their quantity of matter; and, on the other hand, the heaviest bodies, acquiring the first form of that body, might by degrees quite lose their gravity. And therefore the weights would depend upon the forms of bodies, and with those forms might be changed, contrary to what was proved in the preceding corollary.

COR. 3. All spaces are not equally full. For if all spaces were equally full, then the specific gravity of the fluid which fills the region of the air, on account of the extreme density of the matter, would fall nothing short of the specific gravity of quicksilver or gold, or any other the most dense body, and therefore, neither gold, nor any other body, could descend in air. For bodies do not descend in fluids, unless they are specifically heavier than the fluids. And if the quantity of matter in a given space can by any rarefaction be diminished, what should hinder a diminution to infinity?

COR. 4. If all the solid particles of all bodies are of the same density, nor can be rarefied without pores, a void space or vacuum must be granted. [By bodies

Newtonian of the same density, our author means those whose vires Philosophy. inertiae are in the proportion of their bulks.]

PROB. VI. That there is a power of gravity tending to all bodies, proportional to the several quantities of matter which they contain.

That all the planets mutually gravitate one towards another, we have proved before: as well as that the force of gravity towards every one of them, considered apart, is reciprocally as the square of the distance of places from the centre of the planet. And thence it follows that the gravity tending towards all the planets is proportional to the matter which they contain.

Moreover, since all the parts of any planet A gravitate towards any other planet B, and the gravity of every part is to the gravity of the whole as the matter of the part to the matter of the whole; and (by Law 3.) to every action corresponds an equal re-action: therefore the planet B will, on the other hand, gravitate towards all the parts of the planet A; and its gravity towards any one part will be to the gravity towards the whole, as the matter of the part to the matter of the whole. Q. E. D.

COR. 1. Therefore the force of gravity towards any whole planet, arises from, and is compounded of, the forces of gravity towards all its parts. Magnetic and electric attractions afford us examples of this. For all attraction towards the whole arises from the attractions towards the several parts. The thing may be easily understood in gravity, if we consider a greater planet as formed of a number of lesser planets, meeting together in one globe. For hence it would appear that the force of the whole must arise from the forces of the component parts. If it be objected, that, according to this law, all bodies with us must mutually gravitate one towards another, whereas no such gravitation anywhere appears; it is answered, that, since the gravitation towards these bodies is to the gravitation towards the whole earth, as these bodies are to the whole earth, the gravitation towards them must be far less than to fall under the observation of our senses. [The experiments with regard to the attraction of mountains, however, have now further elucidated this point.]

COR. 2. The force of gravity towards the several equal particles of any body, is reciprocally as the square of the distance of places from the particles.

PROB. VII. In two spheres mutually gravitating each towards the other, if the matter, in places on all sides round about and equidistant from the centres, is similar; the weight of either sphere towards the other will be reciprocally as the square of the distance between their centres.

For the demonstration of this, see the Principia, Book I. Prop. lxxv. and lxxvi.

COR. 1. Hence we may find and compare together the weights of bodies towards different planets. For the weights of bodies revolving in circles about planets are as the diameters of the circles directly, and the squares of their periodic times reciprocally; and their weights at the surfaces of the planets, or at any other distances from their centres, are (by this prop.) greater or less, in the reciprocal duplicate proportion of the distances. Thus from the periodic times of Venus, revolving about the sun, in 224d. 16\frac{1}{2}h.; of the outmost circumjovial satellite revolving about Jupiter, in

16d. 16\frac{1}{2}h.; of the Huygenian satellite about Saturn Newtonian in 15d. 22\frac{1}{2}h.; and of the moon about the earth in Philosophy. 27d. 7h. 43\frac{1}{2}; compared with the mean distance of Venus from the sun, and with the greatest heliocentric elongations of the outmost circumjovial satellite from Jupiter's centre, 8' 16"; of the Huygenian satellite from the centre of Saturn, 3' 4"; and of the moon from the earth, 10' 33"; by computation our author found, that the weight of equal bodies, at equal distances from the centres of the sun, of Jupiter, of Saturn, and of the earth, towards the sun, Jupiter, Saturn, and the earth, were one to another as 1067, 1071, and 10787 respectively. Then, because as the distances are increased or diminished, the weights are diminished or increased in a duplicate ratio; the weights of equal bodies towards the sun, Jupiter, Saturn, and the earth, at the distances 10000, 997, 791, and 109, from their centres, that is, at their very superficies, will be as 10000, 943, 529, and 435 respectively.

COR. 2. Hence likewise we discover the quantity of matter in the several planets. For their quantities of matter are as the forces of gravity at equal distances from their centres, that is, in the sun, Jupiter, Saturn, and the earth, as 1, 1067, 1071, and 10787, respectively. If the parallax of the sun be taken greater or less than 10' 30", the quantity of matter in the earth must be augmented or diminished in the triplicate of that proportion.

COR. 3. Hence also we find the densities of the planets. For (by Prop. lxxii. Book I.) the weights of equal and similar bodies towards similar spheres, are, at the surfaces of those spheres, as the diameters of the spheres. And therefore the densities of dissimilar spheres are as those weights applied to the diameters of the spheres. But the true diameters of the sun, Jupiter, Saturn, and the earth, were one to another as 10000, 997, 791, and 109; and the weights towards the same, as 10000, 943, 529, and 435 respectively; and therefore their densities are as 120, 94\frac{1}{2}, 67, and 400. The density of the earth, which comes out by this computation, does not depend upon the parallax of the sun, but it is determined by the parallax of the moon, and therefore is here truly defined. The sun therefore is a little denser than Jupiter, and Jupiter than Saturn, and the earth four times denser than the sun; for the sun, by its great heat, is kept in a sort of a rarefied state. The moon also is denser than the earth.

COR. 4. The smaller the planets are, they are ceteris paribus, of so much the greater density. For so the powers of gravity on their several surfaces come nearer to equality. They are likewise, ceteris paribus, of the greater density as they are nearer to the sun. So Jupiter is more dense than Saturn, and the earth than Jupiter. For the planets were placed at different distances from the sun, that, according to their degrees of density, they might enjoy a greater or less proportion of the sun's heat. Our water, if it were converted as far as the orb of Saturn, would be converted into ice, and in the orb of Mercury would quickly fly away in vapour. For the light of the sun, to which its heat is proportional, is seven times denser in the orb of Mercury than with us: and by the thermometer Sir Isaac found, that a sevenfold heat of our summer sun will make water boil. Nor are we to doubt, that

Newtonian that the matter of Mercury is adapted to its heat, and Philosophy, is therefore more dense than the matter of our earth; since, in a denser matter, the operations of nature require a stronger heat.

It is shown in the scholium of Prop. xxii. Book II. of the Principia, that, at the height of 200 miles above the earth, the air is more rare than it is at the superficies of the earth, in the ratio of 30 to 0,000,000,000,000,3998, or as 75,000,000,000,000 to 1 nearly. And hence the planet Jupiter, revolving in a medium of the same density with that superior air, would not lose by the resistance of the medium the 100000th part of its motion in 1000000 years. In the spaces near the earth, the resistance is produced only by the air, exhalations, and vapours. When these are carefully exhausted by the air pump from under the receiver, heavy bodies fall within the receiver with perfect freedom, and without the least sensible resistance; gold itself, and the lightest down, let fall together, will descend with equal velocity; and though they fall through a space of four, six, and eight feet, they will come to the bottom at the same time; as appears from experiments that have often been made. And therefore the celestial regions being perfectly void of air and exhalations, the planets and comets meeting no sensible resistance in those spaces, will continue their motions through them for an immense space of time.