PART II.

ARISTARCHUS OF SAMOS.

We are told that Aristarchus of Samos was a pupil of Strato of

Lampsacus, a natural philosopher of originality, who succeeded

Theophrastus as head of the Peripatetic school in 288 or 287 B.C., and

held that position for eighteen years. Two other facts enable us to fix

Aristarchus’s date approximately. In 281–280 he made an observation

of the summer solstice; and the book in which he formulated his

heliocentric hypothesis was published before the date of Archimedes’s

_Psammites_ or _Sandreckoner_, a work written before 216 B.C.

Aristarchus therefore probably lived _circa_ 310–230 B.C., that is, he

came about seventy-five years later than Heraclides and was older than

Archimedes by about twenty-five years.

Aristarchus was called “the mathematician,” no doubt in order to

distinguish him from the many other persons of the same name; Vitruvius

includes him among the few great men who possessed an equally profound

knowledge of all branches of science, geometry, astronomy, music, etc.

“Men of this type are rare, men such as were in times past Aristarchus

of Samos, Philolaus and Archytas of Tarentum, Apollonius of Perga,

Eratosthenes of Cyrene, Archimedes and Scopinas of Syracuse, who

left to posterity many mechanical and gnomonic appliances which they

invented and explained on mathematical and natural principles.” That

Aristarchus was a very capable geometer is proved by his extant book,

_On the sizes and distances of the sun and moon_, presently to be

described. In the mechanical line he is credited with the invention of

an improved sun-dial, the so-called _scaphe_, which had not a plane but

a concave hemispherical surface, with a pointer erected vertically in

the middle, throwing shadows and so enabling the direction and height

of the sun to be read off by means of lines marked on the surface of

the hemisphere. He also wrote on vision, light, and colours. His views

on the latter subjects were no doubt largely influenced by the teaching

of Strato. Strato held that colours were emanations from bodies,

material molecules as it were, which imparted to the intervening air

the same colour as that possessed by the body. Aristarchus said that

colours are “shapes or forms stamping the air with impressions like

themselves as it were,” that “colours in darkness have no colouring,”

and that “light is the colour impinging on a substratum”.

THE HELIOCENTRIC HYPOTHESIS.

There is no doubt whatever that Aristarchus put forward the

heliocentric hypothesis. Ancient testimony is unanimous on the point,

and the first witness is Archimedes who was a younger contemporary of

Aristarchus, so that there is no possibility of a mistake. Copernicus

himself admitted that the theory was attributed to Aristarchus, though

this does not seem to be generally known. Copernicus refers in two

passages of his work, _De revolutionibus caelestibus_, to the opinions

of the ancients about the motion of the earth. In the dedicatory letter

to Pope Paul III he mentions that he first learnt from Cicero that one

Nicetas (i.e. Hicetas) had attributed motion to the earth, and that he

afterwards read in Plutarch that certain others held that opinion; he

then quotes the _Placita philosophorum_ according to which “Philolaus

the Pythagorean asserted that the earth moved round the fire in an

oblique circle in the same way as the sun and moon”. In Book I. c. 5 of

his work Copernicus alludes to the views of Heraclides, Ecphantus, and

Hicetas, who made the earth rotate about its own axis, and then goes on

to say that it would not be very surprising if any one should attribute

to the earth another motion besides rotation, namely, revolution in

an orbit in space: “atque etiam (terram) pluribus motibus vagantem et

unam ex astris Philolaus Pythagoricus sensisse fertur, Mathematicus non

vulgaris”. Here, however, there is no question of the earth revolving

round the sun, and there is no mention of Aristarchus. But Copernicus

did mention the theory of Aristarchus in a passage which he afterwards

suppressed: “Credibile est hisce similibusque causis Philolaum

mobilitatem terrae sensisse, quod etiam nonnulli Aristarchum Samium

ferunt in eadem fuisse sententia”.

It is desirable to quote the whole passage of Archimedes in which the

allusion to Aristarchus’s heliocentric hypothesis occurs, in order to

show the whole context.

“You are aware [‘you’ being King Gelon] that ‘universe’ is the name

given by most astronomers to the sphere the centre of which is the

centre of the earth, while its radius is equal to the straight line

between the centre of the sun and the centre of the earth. This is the

common account as you have heard from astronomers. But Aristarchus

brought out _a book consisting of certain hypotheses_, wherein it

appears, as a consequence of the assumptions made, that the universe is

many times greater than the ‘universe’ just mentioned. His hypotheses

are that _the fixed stars and the sun remain unmoved, that the earth

revolves about the sun in the circumference of a circle, the sun lying

in the middle of the orbit_, and that the sphere of the fixed stars,

situated about the same centre as the sun, is so great that the circle

in which he supposes the earth to revolve bears such a proportion to

the distance of the fixed stars as the centre of the sphere bears to

its surface.”

The heliocentric hypothesis is here stated in language which leaves

no room for doubt about its meaning. The sun, like the fixed stars,

remains unmoved and forms the centre of a circular orbit in which the

earth moves round it; the sphere of the fixed stars has its centre at

the centre of the sun.

We have further evidence in a passage of Plutarch’s tract, _On the

face in the moon’s orb_: “Only do not, my dear fellow, enter an action

for impiety against me in the style of Cleanthes, who thought it was

the duty of Greeks to indict Aristarchus on the charge of impiety for

putting in motion the Hearth of the Universe, this being the effect of

his attempt to save the phenomena by supposing the heaven to remain at

rest and the earth to revolve in an oblique circle, while it rotates,

at the same time, about its own axis”.

Here we have the additional detail that Aristarchus followed

Heraclides in attributing to the earth the daily rotation about its

axis; Archimedes does not state this in so many words, but it is

clearly involved by his remark that Aristarchus supposed the fixed

stars as well as the sun to remain unmoved in space. A tract “Against

Aristarchus” is mentioned by Diogenes Laertius among Cleanthes’s works;

and it was evidently published during Aristarchus’s lifetime (Cleanthes

died about 232 B.C.).

We learn from another passage of Plutarch that the hypothesis of

Aristarchus was adopted, about a century later, by Seleucus, of

Seleucia on the Tigris, a Chaldæan or Babylonian, who also wrote on

the subject of the tides about 150 B.C. The passage is interesting

because it also alludes to the doubt about Plato’s final views. “Did

Plato put the earth in motion as he did the sun, the moon and the five

planets which he called the ‘instruments of time’ on account of their

turnings, and was it necessary to conceive that the earth ‘which is

globed about the axis stretched from pole to pole through the whole

universe’ was not represented as being (merely) held together and

at rest but as turning and revolving, as Aristarchus and Seleucus

afterwards maintained that it did, the former of whom stated this as

only a hypothesis, the latter as a definite opinion?”

No one after Seleucus is mentioned by name as having accepted the

doctrine of Aristarchus and, if other Greek astronomers refer to it,

they do so only to denounce it. Hipparchus, himself a contemporary of

Seleucus, definitely reverted to the geocentric system, and it was

doubtless his authority which sealed the fate of the heliocentric

hypothesis for so many centuries.

The reasons which weighed with Hipparchus were presumably the facts

that the system in which the earth revolved in a circle of which

the sun was the exact _centre_ failed to “save the phenomena,” and

in particular to account for the variations of distance and the

irregularities of the motions, which became more and more patent as

methods of observation improved; that, on the other hand, the theory

of epicycles did suffice to represent the phenomena with considerable

accuracy; and that the latter theory could be reconciled with the

immobility of the earth.

ON THE APPARENT DIAMETER OF THE SUN.

Archimedes tells us in the same treatise that “Aristarchus discovered

that the sun’s apparent size is about 1/720th part of the zodiac

circle”; that is to say, he observed that the angle subtended at the

earth by the diameter of the sun is about half a degree.

ON THE SIZES AND DISTANCES OF THE SUN AND MOON.

Archimedes also says that, whereas the ratio of the diameter of the sun

to that of the moon had been estimated by Eudoxus at 9 : 1 and by his

own father Phidias at 12 : 1, Aristarchus made the ratio greater than

18 : 1 but less than 20 : 1. Fortunately we possess in Greek the short

treatise in which Aristarchus proved these conclusions; on the other

matter of the apparent diameter of the sun Archimedes’s statement is

our only evidence.

It is noteworthy that in Aristarchus’s extant treatise _On the sizes

and distances of the sun and moon_ there is no hint of the heliocentric

hypothesis, while the apparent diameter of the sun is there assumed to

be, not ½°, but the very inaccurate figure of 2°. Both circumstances

are explained if we assume that the treatise was an early work written

before the hypotheses described by Archimedes were put forward. In the

treatise Aristarchus finds the ratio of the diameter of the sun to the

diameter of the earth to lie between 19 : 3 and 43 : 6; this would

make the volume of the sun about 300 times that of the earth, and it

may be that the great size of the sun in comparison with the earth, as

thus brought out, was one of the considerations which led Aristarchus

to place the sun rather than the earth in the centre of the universe,

since it might even at that day seem absurd to make the body which was

so much larger revolve about the smaller.

There is no reason to doubt that in his heliocentric system Aristarchus

retained the moon as a satellite of the earth revolving round it as

centre; hence even in his system there was one _epicycle_.

The treatise _On sizes and distances_ being the only work of

Aristarchus which has survived, it will be fitting to give here a

description of its contents and special features.

The style of Aristarchus is thoroughly classical as befits an able

geometer intermediate in date between Euclid and Archimedes, and his

demonstrations are worked out with the same rigour as those of his

predecessor and successor. The propositions of Euclid’s _Elements_ are,

of course, taken for granted, but other things are tacitly assumed

which go beyond what we find in Euclid. Thus the transformations of

ratios defined in Euclid, Book V, and denoted by the terms _inversely_,

_alternately_, _componendo_, _convertendo_, etc., are regularly

used in dealing with _unequal_ ratios, whereas in Euclid they are

only used in proportions, i.e. cases of _equality_ of ratios. But

the propositions of Aristarchus are also of particular mathematical

interest because the ratios of the sizes and distances which have

to be calculated are really trigonometrical ratios, sines, cosines,

etc., although at the time of Aristarchus trigonometry had not been

invented, and no reasonably close approximation to the value of π,

the ratio of the circumference of any circle to its diameter, had

been made (it was Archimedes who first obtained the approximation

22/7). Exact calculation of the trigonometrical ratios being therefore

impossible for Aristarchus, he set himself to find upper and lower

limits for them, and he succeeded in locating those which emerge in

his propositions within tolerably narrow limits, though not always

the narrowest within which it would have been possible, even for him,

to confine them. In this species of approximation to trigonometry he

tacitly assumes propositions comparing the ratio between a greater

and a lesser _angle_ in a figure with the ratio between two _straight

lines_, propositions which are formally proved by Ptolemy at the

beginning of his _Syntaxis_. Here again we have proof that textbooks

containing such propositions existed before Aristarchus’s time, and

probably much earlier, although they have not survived.

Aristarchus necessarily begins by laying down, as the basis for his

treatise, certain assumptions. They are six in number, and he refers

to them as _hypotheses_. We cannot do better than quote them in full,

along with the sentences immediately following, in which he states the

main results to be established in the treatise:--

[HYPOTHESES.]

1. _That the moon receives its light from the sun._

2. _That the earth is in the relation of a point and centre to the

sphere in which the moon moves._

3. _That, when the moon appears to us halved, the great circle which

divides the dark and the bright portions of the moon is in the

direction of our eye._

4. _That, when the moon appears to us halved, its distance from the sun

is then less than a quadrant by one-thirtieth of a quadrant._

5. _That the breadth of the (earth’s) shadow is (that) of two moons._

6. _That the moon subtends one-fifteenth part of a sign of the zodiac._

We are now in a position to prove the following propositions:--

1. _The distance of the sun from the earth is greater than eighteen

times, but less than twenty times, the distance of the moon (from the

earth)_; this follows from the hypothesis about the halved moon.

2. _The diameter of the sun has the same ratio (as aforesaid) to the

diameter of the moon._

3. _The diameter of the sun has to the diameter of the earth a ratio

greater than that which 19 has to 3, but less than that which 43 has to

6_; this follows from the ratio thus discovered between the distances,

the hypothesis about the shadow, and the hypothesis that the moon

subtends one-fifteenth part of a sign of the zodiac.

The first assumption is Anaxagoras’s discovery. The second assumption

is no doubt an exaggeration; but it is made in order to avoid having

to allow for the fact that the phenomena as seen by an observer on the

surface of the earth are slightly different from what would be seen

if the observer’s eye were at the centre of the earth. Aristarchus,

that is, takes the earth to be like a point in order to avoid the

complication of parallax.

The meaning of the third hypothesis is that the plane of the great

circle in question passes through the point where the eye of the

observer is situated; that is to say, we see the circle _end on_, as it

were, and it looks like a straight line.

Hypothesis 4. If S be the sun, M the moon and E the earth, the triangle

SME is, at the moment when the moon appears to us halved, right-angled

at M; and the hypothesis states that the angle at E in this triangle is

87°, or, in other words, the angle MSE, that is, the angle subtended

at the sun by the line joining M to E, is 3°. These estimates are

decidedly inaccurate, for the true value of the angle MES is 89° 50′,

and that of the angle MSE is therefore 10′. There is nothing to show

how Aristarchus came to estimate the angle MSE at 3°, and none of his

successors seem to have made any direct estimate of the size of the

angle.

The assumption in Hypothesis 5 was improved upon later. Hipparchus made

the ratio of the diameter of the circle of the earth’s shadow to the

diameter of the moon to be, not 2, but 2½ at the moon’s mean distance

at the conjunctions; Ptolemy made it, at the moon’s greatest distance,

to be inappreciably less than 2⅗.

The sixth hypothesis states that the diameter of the moon subtends at

our eye an angle which is 1/15th of 30°, i.e. 2°, whereas Archimedes,

as we have seen, tells us that Aristarchus found the angle subtended

by the diameter of the sun to be ½° (Archimedes in the same tract

describes a rough instrument by means of which he himself found that

the diameter of the sun subtended an angle less than 1/164th, but

greater than 1/200th of a right angle). Even the Babylonians had, many

centuries before, arrived at 1° as the apparent angular diameter of the

sun. It is not clear why Aristarchus took a value so inaccurate as 2°.

It has been suggested that he merely intended to give a specimen of the

calculations which would have to be made on the basis of more exact

experimental observations, and to show that, for the solution of the

problem, one of the data could be chosen almost arbitrarily, by which

proceeding he secured himself against certain objections which might

have been raised. Perhaps this is too ingenious, and it may be that, in

view of the difficulty of working out the geometry if the two angles in

question are very small, he took 3° and 2° as being the smallest with

which he could conveniently deal. Certain it is that the _method_ of

Aristarchus is perfectly correct and, if he could have substituted the

true values (as we know them to-day) for the inaccurate values which he

assumes, and could have carried far enough his geometrical substitute

for trigonometry, he would have obtained close limits for the true

sizes and distances.

The book contains eighteen propositions. Prop. 1 proves that we can

draw one cylinder to touch two equal spheres, and one cone to touch two

unequal spheres, the planes of the circles of contact being at right

angles to the axis of the cylinder or cone. Next (Prop. 2) it is shown

that, if a lesser sphere be illuminated by a greater, the illuminated

portion of the former will be greater than a hemisphere. Prop. 3

proves that the circle in the moon which divides the dark and the

bright portions (we will in future, for short, call this “the dividing

circle”) is least when the cone which touches the sun and the moon

has its vertex at our eye. In Prop. 4 it is shown that the dividing

circle is not perceptibly different from a great circle in the moon.

If CD is a diameter of the dividing circle, EF the parallel diameter

of the parallel great circle in the moon, O the centre of the moon,

A the observer’s eye, FDG the great circle in the moon the plane of

which passes through A, and G the point where OA meets the latter great

circle, Aristarchus takes an arc of the great circle GH on one side of

G, and another GK on the other side of G, such that GH = GK = ½ (the

arc FD), and proves that the angle subtended at A by the arc HK is less

than 1/44°; consequently, he says, the arc would be imperceptible at

A even in that position, and _a fortiori_ the arc FD (which is nearly

in a straight line with the tangent AD) is quite imperceptible to the

observer at A. Hence (Prop. 5), when the moon appears to us halved, we

can take the plane of the great circle in the moon which is parallel to

the dividing circle as passing through our eye. (It is tacitly assumed

in Props. 3, 4, and throughout, that the diameters of the sun and moon

respectively subtend the same angle at our eye.) The proof of Prop.

4 assumes as known the equivalent of the proposition in trigonometry

that, if each of the angles α, β is not greater than a right angle, and

α > β, then

tan α / tan β > α/β > sin α / sin β.

Prop. 6 proves that the moon’s orbit is “lower” (i.e. smaller) than

that of the sun, and that, when the moon appears to us halved, it

is distant less than a quadrant from the sun. Prop. 7 is the main

proposition in the treatise. It proves that, on the assumptions made,

the distance of the sun from the earth is greater than eighteen times,

but less than twenty times, the distance of the moon from the earth.

The proof is simple and elegant and should delight any mathematician;

its two parts depend respectively on the geometrical equivalents of the

two inequalities stated in the formula quoted above, namely,

tan α / tan β > α/β > sin α / sin β,

where α, β are angles not greater than a right angle and α > β.

Aristarchus also, in this proposition, cites 7/5 as an approximation by

defect to the value of √2, an approximation found by the Pythagoreans

and quoted by Plato. The trigonometrical equivalent of the result

obtained in Prop. 7 is

1/18 > sin 3° > 1/20.

Prop. 8 states that, when the sun is totally eclipsed, the sun and moon

are comprehended by one and the same cone which has its vertex at our

eye. Aristarchus supports this by the arguments (1) that, if the sun

overlapped the moon, it would not be totally eclipsed, and (2) that,

if the sun fell short (i.e. was more than covered), it would remain

totally eclipsed for some time, which it does not (this, he says,

is manifest from observation). It is clear from this reasoning that

Aristarchus had not observed the phenomenon of an _annular_ eclipse of

the sun; and it is curious that the first mention of an annular eclipse

seems to be that quoted by Simplicius from Sosigenes (second century,

A.D.), the teacher of Alexander Aphrodisiensis.

It follows (Prop. 9) from Prop. 8 that the diameters of the sun

and moon are in the same ratio as their distances from the earth

respectively, that is to say (Prop. 7) in a ratio greater than 18 : 1

but less than 20 : 1. Hence (Prop. 10) the volume of the sun is more

than 5832 times and less than 8000 times that of the moon.

By the usual geometrical substitute for trigonometry Aristarchus proves

in Prop. 11 that the diameter of the moon has to the distance between

the centre of the moon and our eye a ratio which is less than 2/45ths

but greater than 1/30th. Since the angle subtended by the moon’s

diameter at the observer’s eye is assumed to be 2°, this proposition is

equivalent to the trigonometrical formula

1/45 > sin 1° > 1/60.

Having proved in Prop. 4 that, so far as our perception goes, the

dividing circle in the moon is indistinguishable from a great circle,

Aristarchus goes behind perception and proves in Prop. 12 that the

diameter of the dividing circle is less than the diameter of the moon

but greater than 89/90ths of it. This is again because half the angle

subtended by the moon at the eye is assumed to be 1° or 1/90th of a

right angle. The proposition is equivalent to the trigonometrical

formula

1 > cos 1° > 89/90.

We come now to propositions which depend on Hypothesis 5 that “the

breadth of the earth’s shadow is that of two moons”. Prop. 13 is about

the diameter of the circular section of the cone formed by the earth’s

shadow at the place where the moon passes through it in an eclipse,

and it is worth while to notice the extreme accuracy with which

Aristarchus describes the diameter in question. It is with him “the

straight line subtending the portion intercepted within the earth’s

shadow of the circumference of the circle in which the extremities of

the diameter of the circle dividing the dark and the bright portions in

the moon move.” Aristarchus proves that the length of the straight line

in question has to the diameter of the moon a ratio less than 2 but

greater than 88 : 45, and has to the diameter of the sun a ratio less

than 1 : 9 but greater than 22 : 225. The ratio of the straight line to

the diameter of the moon is, in point of fact, 2 cos² 1° or 2 sin² 89°,

and Aristarchus therefore proves the equivalent of

2 > 2 cos² 1° > ½(89/45)² or 7921/4050.

He then observes (without explanation) that 7921/4050 > 88/45 (an

approximation easily obtained by developing 7921/4050 as a continued

fraction (= 1 + (1    1    1)/(1 + 21 + 2))); his result is therefore

equivalent to

1 > cos² 1° > 44/45.

The next propositions are the equivalents of more complicated

trigonometrical formulæ. Prop. 14 is an auxiliary proposition to Prop.

15. The diameter of the shadow dealt with in Prop. 13 divides into two

parts the straight line joining the centre of the earth to the centre

of the moon, and Prop. 14 shows that the whole length of this line is

more than 675 times the part of it terminating in the centre of the

moon. With the aid of Props. 7, 13, and 14 Aristarchus is now able,

in Prop. 15, to prove another of his main results, namely, that the

diameter of the sun has to the diameter of the earth a ratio greater

than 19 : 3 but less than 43 : 6. In the second half of the proof he

has to handle quite large numbers. If A be the centre of the sun, B the

centre of the earth, and M the vertex of the cone formed by the earth’s

shadow, he proves that MA : AB is greater than (10125 × 7087) : (9146

× 6750) or 71755875 : 61735500, and then adds, without any word of

explanation, that the latter ratio is greater than 43 : 37. Here again

it is difficult not to see in 43 : 37 the continued fraction 1 +

11/(6+6); and although we cannot suppose that the Greeks could actually

develop 71755875/61735500 or 21261/18292 as a continued fraction (in

_form_), “we have here an important proof of the employment by the

ancients of a method of calculation, the theory of which unquestionably

belongs to the moderns, but the first applications of which are too

simple not to have originated in very remote times” (Paul Tannery).

The remaining propositions contain no more than arithmetical inferences

from the foregoing. Prop. 16 is to the effect that the volume of the

sun has to the volume of the earth a ratio greater than 6859 : 27 but

less than 79507 : 216 (the numbers are the cubes of those in Prop.

15); Prop. 17 proves that the diameter of the earth is to that of the

moon in a ratio greater than 108 : 43 but less than 60 : 19 (ratios

compounded of those in Props. 9 and 15), and Prop. 18 proves that the

volume of the earth is to that of the moon in a ratio greater than

1259712 : 79507 but less than 216000 : 6859.

ARISTARCHUS ON THE YEAR AND “GREAT YEAR”.

Aristarchus is said to have increased by 1/1623rd of a day Callippus’s

figure of 365¼ days as the length of the solar year, and to have given

2484 years as the length of the Great Year or the period after which

the sun, the moon and the five planets return to the same position

in the heavens. Tannery has shown reason for thinking that 2484 is a

wrong reading for 2434 years, and he gives an explanation which seems

convincing of the way in which Aristarchus arrived at 2434 years as

the length of the Great Year. The Chaldæan period of 223 lunations was

well known in Greece. Its length was calculated to be 6585⅓ days, and

in this period the sun was estimated to describe 10⅔° of its circle in

addition to 18 sidereal revolutions. The Greeks used the period called

by them _exeligmus_ which was three times the period of 223 lunations

and contained a whole number of days, namely, 19756, during which the

sun described 32° in addition to 54 sidereal revolutions. It followed

that the number of days in the sidereal year was--

19756/(54 + 32/360) = 19756/(54 + 4/45) = (45 × 19756)/2434

= 889020/2434 = 365¼ + 3/4868.

Now 4868/3 = 1623 - ⅓, and Aristarchus seems to have merely replaced

3/4868 by the close approximation 1/1623. The calculation was, however,

of no value because the estimate of 10⅔° over 18 sidereal revolutions

seems to have been an approximation based merely on the difference

between 6585⅓ days and 18 years of 365¼ days, i.e. 6574½ days; thus

the 10⅔° itself probably depended on a solar year of 365¼ days, and

Aristarchus’s evaluation of it as 365¼ 1/1623 was really a sort of

circular argument like the similar calculation of the length of the

year made by Œnopides of Chios.

LATER IMPROVEMENTS ON ARISTARCHUS’S FIGURES.

It may interest the reader to know how far Aristarchus’s estimates of

sizes and distances were improved upon by later Greek astronomers. We

are not informed how large he conceived the earth to be; but Archimedes

tells us that “some have tried to prove that the circumference of

the earth is about 300,000 stades and not greater,” and it may be

presumed that Aristarchus would, like Archimedes, be content with this

estimate. It is probable that it was Dicaearchus who (about 300 B.C.)

arrived at this value, and that it was obtained by taking 24° (1/15th

of the whole meridian circle) as the difference of latitude between

Syene and Lysimachia (on the same meridian) and 20,000 stades as the

actual distance between the two places. Eratosthenes, born a few years

after Archimedes, say 284 B.C., is famous for a better measurement of

the earth which was based on scientific principles. He found that at

noon at the summer solstice the sun threw no shadow at Syene, whereas

at the same hour at Alexandria (which he took to be on the same

meridian) a vertical stick cast a shadow corresponding to 1/50th of the

meridian circle. Assuming then that the sun’s rays at the two places

are parallel in direction, and knowing the distance between them to

be 5000 stades, he had only to take 50 times 5000 stades to get the

circumference of the earth. He seems, for some reason, to have altered

250,000 into 252,000 stades, and this, according to Pliny’s account

of the kind of stade used, works out to about 24,662 miles, giving

for the diameter of the earth a length of 7850 miles, a surprisingly

close approximation, however much it owes to happy accidents in the

calculation.

Eratosthenes’s estimates of the sizes and distances of the sun and moon

cannot be restored with certainty in view of the defective state of

the texts of our authorities. We are better informed of Hipparchus’s

results. In the first book of a treatise on sizes and distances

Hipparchus based himself on an observation of an eclipse of the sun,

probably that of 20th November in the year 129 B.C., which was exactly

total in the region about the Hellespont, whereas at Alexandria about

⅘ths only of the diameter was obscured. From these facts Hipparchus

deduced that, if the radius of the earth be the unit, the least

distance of the moon contains 71, and the greatest 83 of these units,

the mean thus containing 77. But he reverted to the question in the

second book and proved “from many considerations” that the mean

distance of the moon is 67⅓ times the radius of the earth, and also

that the distance of the sun is 2490 times the radius of the earth.

Hipparchus also made the size (meaning thereby the solid content) of

the sun to be 1880 times that of the earth, and the size of the earth

to be 27 times that of the moon. The cube root of 1880 being about 12⅓,

the diameters of the sun, earth and moon would be in the ratio of the

numbers 12⅓, 1, ⅓. Hipparchus seems to have accepted Eratosthenes’s

estimate of 252,000 stades for the circumference of the earth.

It is curious that Posidonius (135–51 B.C.), who was much less of an

astronomer, made a much better guess at the distance of the sun from

the earth. He made it 500,000,000 stades. As he also estimated the

circumference of the earth at 240,000 stades, we may take the diameter

of the earth to be, according to Posidonius, about 76,400 stades;

consequently, if _D_ be that diameter, Posidonius made the distance of

the sun to be equal to 6545_D_ as compared with Hipparchus’s 1245_D_.

Ptolemy does not mention Hipparchus’s figures. His own estimate of

the sun’s distance was 605_D_, so that Hipparchus was far nearer the

truth. But Hipparchus’s estimate remained unknown and Ptolemy’s held

the field for many centuries; even Copernicus only made the distance

of the sun 750 times the earth’s diameter, and it was not till 1671–3

that a substantial improvement was made; observations of Mars carried

out in those years by Richer enabled Cassini to conclude that the sun’s

parallax was about 9·5″ corresponding to a distance between the sun

and the earth of 87,000,000 miles.

Ptolemy made the distance of the moon from the earth to be 29½ times

the earth’s diameter, and the diameter of the earth to be 3⅖ times that

of the moon. He estimated the diameter of the sun at 18⅘ times that of

the moon and therefore about 5½ times that of the earth, a figure again

much inferior to that given by Hipparchus.

BIBLIOGRAPHY.

On the astronomy of the early Greek philosophers much information is

given by Aristotle (especially in the _De Caelo_); for Aristotle was

fortunately in the habit of stating the views of earlier thinkers as

a preliminary to enunciating his own. Apart from what we learn from

Aristotle, we are mainly dependent on the fragmentary accounts of

the opinions of philosophers which were collected in the _Doxographi

Graeci_ of Hermann Diels (Berlin, 1879), to which must be added, for

the period before Socrates, _Die Fragmente der Vorsokratiker_ by the

same editor (2nd edition, with index, 1906–10, 3rd edition, 1912).

The doxographic data and the fragments for the period from Thales to

Empedocles were translated and explained by Paul Tannery in _Pour

l’histoire de la Science Hellène_ (Paris, 1887). A History of Astronomy

was written by Eudemus of Rhodes, a pupil of Aristotle; this is lost,

but a fair number of fragments are preserved by later writers. Of the

theory of concentric spheres we have a short account in Aristotle’s

_Metaphysics_, but a more elaborate and detailed description is

contained in Simplicius’s commentary on the _De Caelo_; Simplicius

quotes largely from Sosigenes the Peripatetic (second century A.D.) who

drew upon Eudemus.

There are a number of valuable histories of Greek astronomy. In German

we have Schaubach, _Geschichte der griechischen Astronomie bis auf

Eratosthenes_, 1809; R. Wolf, _Geschichte der Astronomie_, 1877;

and two admirable epitomes (1) by Siegmund Günther in Windelband’s

_Geschichte der alten Philosophie_ (Iwan von Müller’s _Handbuch der

klassischen Altertumswissenschaft_, Vol. V, Pt. 1), 2nd edition, 1894,

and (2) by Friedrich Hultsch in Pauly-Wissowa’s _Real-Encyclopädie der

classischen Altertumswissenschaft_ (Art. Astronomie in Vol. II, 2,

1896).

In French, besides the great work of Delambre, _Histoire de

l’astronomie ancienne_, 1817, we have the valuable studies of Paul

Tannery in _Recherches sur l’histoire de l’astronomie ancienne_, 1893,

and Pierre Duhem, _Le Système du Monde_, Vol. I, 1913.

In English, reference may be made to Sir G. Cornewall Lewis, _An

Historical Survey of the Astronomy of the Ancients_, 1863; J. L. E.

Dreyer, _History of the Planetary Systems from Thales to Kepler_,

Cambridge, 1906; and the historical portion of Sir Thomas Heath’s

_Aristarchus of Samos, the ancient Copernicus_, Oxford, 1913.

Aristarchus’s treatise _On the Sizes and Distances of the Sun and

Moon_ first appeared in a Latin translation by George Valla in 1488

and 1498, and next in a Latin translation by Commandinus (1572). The

_editio princeps_ of the Greek text was brought out by John Wallis,

Oxford, 1688, and was reprinted in _Johannis Wallis Opera Mathematica_,

1693–1699, Vol. III, in both cases along with Commandinus’s

translation. In 1810 there appeared an edition by the Comte de Fortia

d’Urban, _Histoire d’Aristarque de Samos_ ... including the Greek text

and Commandinus’s translation but without figures; a French translation

by Fortia d’Urban followed in 1823. The treatise was translated into

German by A. Nokk in 1854. Finally, Sir Thomas Heath’s work above cited

contains a new Greek text with English translation and notes.

CHRONOLOGY.

(_Approximate where precise dates are not known._)

B.C.

624–547 Thales.

610–546 Anaximander.

585–526 Anaximenes.

572–497 Pythagoras.

born 516 or 514 Parmenides.

(possibly 540).

500–428 Anaxagoras.

494–434 Empedocles.

5th century { Œnopides of Chios.

{ Philolaus.

427–347 Plato.

408–355 Eudoxus.

388–315 Heraclides of Pontus.

384–322 Aristotle.

370–300 Callippus.

310–230 Aristarchus of Samos.

287–212 Archimedes.

284–203 Eratosthenes.

265–190 Apollonius of Perga.

3rd century Aratus.

fl. 150 Hipparchus.

135–51 Posidonius.

A.D.

50–125 Plutarch.

100–178 Ptolemy.

ABERDEEN: THE UNIVERSITY PRESS

Transcriber’s Notes

Punctuation and spelling were made consistent when a predominant

preference was found in this book; otherwise they were not changed.

Simple typographical errors were corrected. One unbalanced parenthesis

was remedied.

Italics are indicated by _underscores_.

End of Project Gutenberg's The Copernicus of Antiquity, by Thomas Little Heath

The Copernicus of Antiquity (Aristarchus of Samos) · 第 4 / 4 章