Aristarchus of Samos
Aristarchus of Samos
(ca. 310–230 b.c.)
Aristarchus is celebrated as being the first man to have propounded a heliocentric theory, eighteen centuries before Copernicus. He was born on the island of Samos, close by Miletus, cradle of Ionian science and philosophy. Little is known of Aristarchus’ subsequent habitation. He was a pupil of Strato of Lampsacos, third head of the Lyceum founded by Aristotle. It is more likely that he studied under Strato at Alexandria than at Athens after the latter’s assumption of the headship of the Lyceum in 287 b.c. Aristarchus’ approximate dates are determined by Ptolemy’s record (Syntaxis 3.2) of his observation of the summer solstice in 280 b.c. and by Archimedes’ account of his heliocentric theory in a treatise, The Sand-Reckoner, which Archimedes composed before 216 b.c. The sole surviving work of Aristarchus is the treatise On the Sizes and Distances of the Sun and Moon.
To his contemporaries Aristarchus was known as “the mathematician”; the epithet may merely have served to distinguish him from other men of the same name, although On Sizes and Distances is indeed the work of a highly competent mathematician. The Roman architect Vitruvius lists him with six other men of rare endowment who were expert in all branches of mathematics and who could apply their talents to practical purposes. Vitruvius also credits him with inventing the skaphē, a widely used sundial consisting of a hemispherical bowl with a needle erected vertically in the middle to cast shadows. Speculations as to why a reputable mathematician like Aristarchus should interest himself in the true physical orientation of the solar system thus appear to be idle. Some have pointed to the possible influence of Strato, who was known as “the physical philosopher.” There is no evidence however, to indicate that Aristarchus got his physical theories from Strato. A more likely assumption is that On Sizes and Distances gave him an appreciation of the relative sizes of the sun and earth and led him to propound a heliocentric system.
The beginnings of heliocentrism are traced to the early Pythagoreans, a religiophilosophical school that flourished in southern Italy in the fifth century b.c. Ancient tradition ascribed to Pythagoras (ca. 520 b.c.) the identification of the Morning Star and the Evening Star as the same body. Philolaus (ca. 440 b.c.) gave the earth, moon, sun, and planets an orbital motion about a central fire, which he called “the hearth of the universe.” According to another tradition, it was Hicetas, a contemporary of Philolaus, who first gave a circular orbit to the earth. Hicetas was also credited with maintaining the earth’s axial rotation and a stationary heavens. More reliable ancient authorities, however, associate the hypothesis of the earth’s diurnal rotation with Heraclides of Pontus, a pupil of Plato, who is a also explicitly credited with maintaining (ca. 340 b.c.) an epicyclic orbit of Venus—and presumably that of Mercury also—about the sun. Some Greek astronomer may have taken the next logical step toward developing a complete heliocentric hypothesis by proposing the theory advanced in modern times by Tycho Brahe, which placed the five visible planets in motion about the sun, and the sun, in turn, in motion about the earth. Several scholars have argued that such a step was indeed taken, the most notable being the Italian astronomer Schiaparelli, who ascribed the Tychonic system to Heraclides; but evidence of its existence in antiquity is lacking.
Ancient authorities are unanimous in attributing the heliocentric theory to Aristarchus. Archimedes, who lived shortly afterward, says that he published his views in a book or treatise in which the premises that he developed led to the conclusion that the universe is many times greater than the current conception of it. Archimedes, near the opening of The Sand-Reckoner, gives a summary statement of Aristarchus’ argument:
His hypotheses are that the fixed stars and the sun are stationary, that the earth is borne in a circular orbit about the sun, which lies in the middle of its orbit, and that the sphere of the fixed stars, having the same center as the sun, is so great in extent that the circle on which he supposes the earth to be borne has such a proportion to the distance of the fixed stars as the center of the sphere bears to its surface.
Plutarch (ca. a.d. 100) gives a similar brief account of Aristarchus’ hypothesis, stating specifically that the earth revolves along the ecliptic and that it is at the same time rotating on its axis.
After reporting Aristarchus’ views, Archimedes criticizes him for setting up a mathematically impossible proportion, pointing out that the center of the sphere has no magnitude and therefore cannot bear any ratio to the surface of the sphere. Archimedes intrudes the observation that the “universe,” as it is commonly conceived of by astronomers, is a sphere whose radius extends from the center of the sun to the center of the earth. Accordingly, as a mathematician he imputes to the mathematician Aristarchus a proportion that he feels is implicit in his statement, namely, that the ratio that the earth bears to the universe, as it is commonly conceived, is equal to the ratio that the sphere in which the earth revolves, in Aristarchus’ scheme, bears to the sphere of the fixed stars.
Modern scholars have generally supposed that Aristarchus did not intend to have his proportion interpreted as a mathematical statement, that instead he was using an expression conventional with Greek mathematical cosmographers—“having the relation of a point”—merely to indicate the minuteness of the earth’s orbit and the vastness of the heavens. Sir Thomas Heath points to similar expressions in the works of Euclid, Geminus, Ptolemy, and Cleomedes, and in the second assumption of Aristarchus’ extant treatise On Sizes and Distances (see below). Heath feels that Archimedes’ interpretation was arbitrary and sophistical and that Aristarchus introduced the statement to account for the inability to observe stellar parallax from an orbiting earth. Neugebauer defends the proportion that Archimedes ascribes to Aristarchus,
r: Re = Re: Rf,
as mathematically sound and providing finite dimensions for the sphere of the fixed stars: the earth’s radius (r) is so small in comparison with the sun’s distance (Re) that no daily parallax of the sun is discernible for determining Re; according to Aristarchus’hypothesis, the earth moves in an orbit whose radius is Re and no annual parallax of the fixed stars is discernible.
Why did the Greeks, after evolving a heliocentric hypothesis in gradual steps over a period of two centuries, allow it to fall into neglect almost immediately? Only one man, Seleucus of Seleucia (ca. 150 b.c.), is known to have embraced Aristarchus’ views. The common attitude of deploring the “abandonment” of the heliocentric theory as a “retrogressive step” appears to be unwarranted when it is realized that the theory, however bold and ingenious it is to be regarded, never attracted much attention in antiquity. Aristarchus’ system was the culmination of speculations about the physical nature of the universe that began with the Ionian philosophers of the sixth century, and it belongs to an age that was passing away. The main course of development of Greek astronomy was mathematical, not physical, and the great achievements were still to come—the exacting demonstrations and calculations of Apollonius of Perga, Hipparchus, and Ptolemy. These were based upon a geocentric orientation.
To a mathematician the orientation is of no consequence; in fact it is more convenient to construct a system of epicycles and eccentrics to account for planetary motions from a geocentric orientation. A heliocentric hypothesis neatly explained some basic phenomena, such as the stations and retrogradations of superior planets; but a circular orbit for the earth, about a sun in the exact center, failed to account for precise anomalies, such as the inequality of the seasons. In explanation of this inequality, Hipparchus determined the eccentricity of the earth’s position as 1/24 of the radius of the sun’s circle and he fixed the line of absides in the direction of longitude 65° 30’. Ptolemy adopted Hipparchus’ solar data without change, unaware that the sun’s orbit describes a revolving eccentric, the shift being 32’ in a century. The Arab astronomer al-Battānī (a.d. 858–929) discovered this shift. Epicyclic constructions had two advantages over eccentric constructions: they were applicable to inferior as well as superior planets and they palpably demonstrated planetary stations and retrograde motions. By the time of Apollonius it was understood that an equivalent eccentric system could be constructed for every epicyclic system. Henceforth, combinations of epicycles and eccentrics were introduced, all from a geocentric orientation. Aristarchus, too, had used a geocentric orientation in calculating the sizes and distances of the sun and moon.
It is not hard to account for the lack of interest in the heliocentric theory. The Zeitgeist of the new Hellenistic age was set and characterized by the abstruse erudition of the learned scholars and the precise researches of the astronomers, mathematicians, and anatomists working at the library and museum of Alexandria. Accurate instruments in use at Alexandria were giving astronomers a better appreciation of the vast distance of the sun. Putting the earth in orbit about the sun would lead to the expectation that some variation in the position of the fixed stars would be discernible at opposite seasons. Absence of displacement would presuppose a universe of vast proportions. The more precise the observations, the less inclined were the astronomers at Alexandria to accept an orbital motion of the earth. It is the opinion of Heath that Hipparchus (ca. 190–120 b.c.) usually regarded as the greatest of Greek astronomers, in adopting the geocentric orientation “sealed. the fate of the heliocentric hypothesis for so many centuries.”
The intellectual world at large was also idsinclined to accept Aristarchus’ orientation. Aristotle’s doctrine of “natural places,” which assigned to earth a position at the bottom or center among the elements comprising the universe, and his plausible “proofs” of a geocentric orientation, carried great weight in later antiquity, even with the mathematician Ptolemy. Religious minds were reluctant to relinquish the central position of man’s adobe. According to Plutarch, Cleanthes, the second head of the Stoic school (263–232 b.c.), thought that Aristarchus ought to be indicted on a charge of impiety for putting the earth in motion. Astrology, a respectable science in the eyes of many leading intellectuals, was enjoying an extraordinary vogue after its recent introduction. Its doctrines and findings were also based upon a geocentric orientation.
It is interesting to note in passing that Copernicus’ disappointment at being anticipated by Aristarchus has recently come to light. Copernicus deliberately suppressed a statement acknowledging his awareness of Aristarchus’ theory; the statement, deleted from the autograph copy of the De revolutionibus, appears in a footnote in the Thorn edition (1873) of that work. Elsewhere Copernicus tells of his search for classical precedents for his novel ideas about the heavens and of his finding in Plutarch the views of Philolaus, Heraclides, and Ecphantus; but he omits mention of the clear statement about Aristarchus’ theory that appears a few pages earlier. Lastly, Copernicus’ almost certain acquaintance with Archimedes’ The Sand-Reckoner, the work containing our best account of Aristarchus’ theory, has recently been pointed out.
His accomplishments as an astronomer have tended to detract attention from Aristarchus’ attainments as a mathematician. Flourishing a generation after Euclid and a generation before Archimedes, Aristarchus was capable of the same sort of rigorous and logical geometrical demonstrations that distinguished the work of those famous mathematicians. On Sizes and Distances marks the first attempt to determine astronomical distances and dimensions by mathematical deductions based upon a set of assumptions. His last assumption assigns a grossly excessive estimate to the apparent angular diameter of the moon (2°). We are told by Archimedes in The Sand-Reckoner that Aristarchus discovered the sun’s apparent angular diameter to be 1/720 part of the zodiac circle (1/2°), a close and respectable estimate. Aristarchus uses a geocentric orientation in On Sizes and Distances and concludes that the sun’s volume is over 300 times greater than the earth’s volume. For these reasons it is generally assumed that the treatise was an early work, antedating his heliocentric hypothesis.
Aristarchus argues that at the precise moment of the moon’s quadrature, when it is half-illuminated, angle SME is a right angle; angle SEM can be measured by observation; therefore it is possible to deduce angle MSE and to determine the ratio of the distance of the moon to the distance of the sun (Figure 1). Two obvious difficulties are involved in his procedures: the determination with any exactitude (1) of the time of the moon’s dichotomy and (2) of the measurement of angle SEM. A slight inaccuracy in either case would lead to a grossly inaccurate result. Aristarchus assumes angle SEM to be 87°, when in actuality it is more than 89° 50’, and he derives a distance for the sun of 18 to 20 times greater than the moon’s distance (actually nearly 400 times greater). His mathematical procedures are sound, but his observational data are so crude as to make it apparent that Aristarchus was interested here in mathematical demonstrations and not in physical realities.
Aristarchus’ treatise begins with six assumptions:
(1) That the moon receives its light from the sun.
(2) That the earth has the relation of a point and center to the sphere of the moon.
(3) That when the moon appears to us to be exactly
at the half the great circle dividing the light and dark portions of the moon is in line with the observer’s eye.
(4) That when the moon appears to us to be at the half its distance from the sun is less than a quadrant by 1/30 part of a quadrant (87°).
(5)That the breadth of the earth’s shadow (during eclipses) is that of two moons.
(6) That the moon subtends 1/15 part of a sign of the zodiac (2°).
He then states that he is in a position to prove three propositions:
(1)The distance of the sun from the earth is more than eighteen times but less than twenty times the moon’s distance (from the earth); this is based on the assumption about the halved moon.
(2) The diameter of the sun has the same ratio to the diameter of the moon (i.e., assuming that the sun and moon have the same apparent angular diameter).
(3)The diameter of the sun has to the diametre of the earth a ratio greater than 19:3, but less than 43:6; this deduction follows from the ratio between the distances thus discovered, from the assumption about the shadow, and from the assumption that the moon subtends 1/15 part of a sign of the zodiac.
Then follow eighteen propositions containing the demonstrations. Heath has edited and translated the complete Greek text, together with Pappus’ comments on the treatise, in his Aristarchus of Samos (pp.352–414), and presents a summary account of the treatise in A History of Greek Mathematics (Vol. II).
Anticipating trigonometric methods that were to come. Aristarchus was the first to develop geometric procedures for approximating the sines of small angles. He deals with angles expressed as fractions of right angles and ratios of the sides of triangles, determining limits between which actual values lie. In Proposition 7, demonstrating that the distance of the sun is more than eighteen times but less than twenty times the distance of the moon, which would be expressed trigonometrically 1/18 > sin 3° > 1/20, he uses in his proof certain inequalities that he assumes to be known and accepted. These may be expressed trigonometrically. If α and β are acute angles and α > β, then
tanα/tanβ > α/β > sinα/sinβ.
If Aristarchus had had a correct measurement of the angle SEM—89 5/6° instead of 87°—his result would have been nearly correct. A century later Hipparchus was able to obtain a very close approximation of the moon’s distance, expressed in terms of earth radii, by measuring the earth’s shadow during lunar eclipses; but an appreciation of the vast distance of the sun had to wait upon the development of modern precision instruments.
Other dimensions deduced by Aristarchus in his treatise, all of them grossly underestimated because of his poor observational data, are:
(Prop. 10) The sun has to the moon a ratio greater than 5,832: I but less than 8,000: 1.
(Prop. 11) The diameter of the moon is less than 2/45 but greater than 1/30 of the distance of the centre of the moon from the observre.
(Prop. 16) The sun has to the earth a ratio greater than 6,859:27 but less than 79,507:216.
(Prop. 17) The diameter of the earth is to the diameter of the moon in a ratio greater than 108:43 but less than 60:19.
(Prop. 18) The earth is to the moon in a ratio greater than 1,259,712: 79,507 but less than 216,000:6,859.
Thomas W. Africa, “Copernicus’ Relation to Aristarchus and Pythagoras,” in Isis, 52 (1961), 403–409; Angus Armitage, Copernicus, the Founder of Modern Astronomy (London, 1938); John L. E. Dreyer, A History of the Planetary Systems from Thales to Kepler (Cambridge, England, 1906; repr., New York, 1953); Pierre Duhem, Le système du monde, Vols. I-II (Paris, 1954); Sir Thomas Heath, Aristarchus of Samos (Oxford, 1913) and A History of Greek Mathematics, 2 vols. (Oxford, 1921); Otto Neugebauer, “Archimedes and Aristarchus,” in Isis. 39 (1942), 4–6; Giovanni V. Schiaparelli, “Origine del sistema planetario eliocentrico presso i Greci,” in Memorie del’Istituto lombardodi scienze e lettere, 18 (1898), asc. 5; and William H. Stahl, “The Greek Heliocentric Theory and Its Abandonment.” in Transactions of the Amerrican Philological Association, 77 (1945), 321–332.
William H. Stahl
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Aristarchus of Samos
Aristarchus of Samos
The Greek astronomer Aristarchus of Samos (ca. 310-230 B.C.) hypothesized that the earth revolves yearly about the sun and daily rotates about its own axis. He attempted to determine the relative sizes and distances of the sun, moon, and earth.
Born on the island of Samos, Aristarchus studied at Athens in the Lyceum under Straton of Lampsacus, who was the head of the Peripatetic school from 288/287 to 270/269 B.C.
Though Aristarchus is known to have written on problems of vision, light, and color, his primary work was in astronomy, specifically on the interrelations of the sun, moon, and earth. With respect to their relative positions he pointed out that, mathematically, one can imagine the earth rotating about the sun as easily as the sun about the earth; all that is required is a vastly increased radius of the sphere of the fixed stars and the daily rotation of the earth about its own axis rather than the rotation of the sphere of the fixed stars. Though all serious astronomers in antiquity and the Middle Ages would have realized the mathematical equivalence of the geocentric and heliocentric hypotheses (and many do refer to it), arguments from physics compelled them to accept geocentricity, as Aristarchus himself does in his sole surviving book. Only with the abandonment of Aristotelian physics could the heliocentric hypothesis attain credibility.
Following many predecessors in the 6th to 4th century (Cleostratus, Meton, Eudoxus, and Callippus), Aristarchus tried to fix a "Great Year"—a period in which integer numbers of days, solar years, and the various kinds of months would occur exactly. His Great Year of 2,434 solar years contains 45 exeligmi, and each exeligmus contains three periods in which the period-relation holds: 223 synodic months = 239 anomalistic months = 242 draconic months. Neither the exeligmus nor its third (both Babylonian period-relations) contains an integer number of years, though the exeligmus has an integer number of days. The 45 exeligmi of Aristarchus's Great Year are based on the following period-relations: 30,105 synodic months = 32,265 anomalistic months = 32,670 draconic months = 32,539 sidereal months = 889,020 days = 2,434 solar years.
Relative Sizes of the Sun and Moon
In his treatise On the Sizes and Distances of the Sun and Moon, using Euclid's laws of proportions, Aristarchus seeks to define the limits of the ratios of the sizes and distances of the sun, moon, and earth to each other. He uses the situation of a lunar eclipse, assuming that the diameters of the sun and moon are each 2° and the diameter of the disk of the cone of the earth's shadow at the distance of the moon is 4°; thus he uses a diameter of both sun and moon that is about four times what it should be (in another lost work he gave a more correct value of 0:30°) and ignores the variation in the distance and apparent diameter of the moon.
He arrives at the conclusions that the distance of the sun from the earth is between 18 and 20 times that of the moon from the earth, that the diameter of the sun is between 19/3 and 43/6 times the diameter of the earth and the diameter of the earth between 108/43 and 60/19 times the diameter of the moon, and that the diameter of the moon is between 1/30 and 2/45 of the distance of the moon from the earth. Though these results are not correct, their limitations are largely imposed by the state of the mathematics available to Aristarchus, though the erroneous estimate of the moon's diameter contributes. The method was more fully developed and fruitfully applied by Hipparchus a century later.
Influence of Aristarchus
Aristarchus is often called the "Copernicus of antiquity." In a sense this is true, though the identification need not be taken as being in praise of either man. Both realized, as did many others, that a heliocentric system is equivalent to a geocentric system as far as the observed celestial phenomena are concerned; and both were willing, as others were not, to propound this mathematical hypothesis without reference to current theories of physics, and in particular to the laws of motion. Aristarchus wrote when Aristotelian physics and Platonic cosmology were both gaining acceptance and there was no one willing, or perhaps able, to construct an adequate alternative theory embodying his cosmology.
Copernicus was followed by many who questioned and eventually, with the help of new instruments and improved observational methods, disproved Aristotelian physics. The failure of Aristarchus and the success of Copernicus had less to do with their individual merits than with the intellectual milieu in which their views were expounded. In any case, Aristarchus's attempt to measure solar and lunar distance had a far greater influence on his successors than did his heliocentric theory.
The standard work on Aristarchus is Sir Thomas L. Heath, Aristarchus of Samos, the Ancient Copernicus (1913; reprinted, 1981). A chapter on Aristarchus appears in J.L.E. Dreyer, A History of Astronomy: From Thales to Kepler (1905; rev. ed. 1953). Discussions of his life and work appear in George Sarton's scholarly A History of Science: Hellenistic Science and Culture in the Last Three Centuries B.C. (1959) and in Benjamin Farrington's popularly written Greek Science: Its Meaning for Us (1949; rev. ed. 1961). See also Marshall Claggett, Greek Science in Antiquity (1955), and Giorgio de Santillana, The Origins of Scientific Thought: From Anaximander to Proclus, 600 B.C. to 300 A.D. (1961). □
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Aristarchus of Samos
Aristarchus of Samos (ăr´Ĭstär´kəs, ăr´Ĭstär´kəs, sā´mŏs), fl. c.310 BC–c.230 BC, Greek astronomer and mathematician of the Alexandrian school. He is said to have been the first to propose a heliocentric or sun-centered theory of the universe. Of his writings only a treatise, The Sizes and Distances of the Sun and Moon, remains. The procedures he followed in this treatise were highly original; his calculation of the moon's distance was incorrect, but he derived a more correct value for the solar year. The treatise does not mention his conclusion that the earth moves around the sun and that the sun is at rest, but statements by Archimedes and Copernicus indicate that he held this theory. Other conclusions in which he seems to have anticipated later scientists are that the sun is larger than the earth, that the earth rotates upon its axis causing day and night, and that its axis is inclined to the plane of the ecliptic, causing the change of seasons.
See T. L. Heath, Aristarchus of Samos (1913, repr. 1981).
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Aristarchus of Samos
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