CHAPTER IX. THE ETHER AND PONDERABLE MATTER

James Clerk-Maxwell's conception of ether--Thomas Young and

"Luminiferous ether,"--Young's and Fresnel's conception of transverse

luminiferous undulations--Faraday's experiments pointing to the

existence of ether--Professor Lodge's suggestion of two ethers--Lord

Kelvin's calculation of the probable density of ether--The vortex theory

of atoms--Helmholtz's calculations in vortex motions--Professor

Tait's apparatus for creating vortex rings in the air---The ultimate

constitution of matter as conceived by Boscovich--Davy's speculations

as to the changes that occur in the substance of matter at different

temperatures--Clausius's and Maxwell's investigations of the

kinetic theory of gases--Lord Kelvin's estimate of the size of the

molecule--Studies of the potential energy of molecules--Action of gases

at low temperatures.

APPENDIX

A HISTORY OF SCIENCE

BOOK III. MODERN DEVELOPMENT OF THE PHYSICAL SCIENCES

With the present book we enter the field of the distinctively modern.

There is no precise date at which we take up each of the successive

stories, but the main sweep of development has to do in each case with

the nineteenth century. We shall see at once that this is a time both

of rapid progress and of great differentiation. We have heard almost

nothing hitherto of such sciences as paleontology, geology, and

meteorology, each of which now demands full attention. Meantime,

astronomy and what the workers of the elder day called natural

philosophy become wonderfully diversified and present numerous

phases that would have been startling enough to the star-gazers and

philosophers of the earlier epoch.

Thus, for example, in the field of astronomy, Herschel is able, thanks

to his perfected telescope, to discover a new planet and then to reach

out into the depths of space and gain such knowledge of stars and

nebulae as hitherto no one had more than dreamed of. Then, in rapid

sequence, a whole coterie of hitherto unsuspected minor planets is

discovered, stellar distances are measured, some members of the starry

galaxy are timed in their flight, the direction of movement of the solar

system itself is investigated, the spectroscope reveals the chemical

composition even of suns that are unthinkably distant, and a tangible

theory is grasped of the universal cycle which includes the birth and

death of worlds.

Similarly the new studies of the earth's surface reveal secrets of

planetary formation hitherto quite inscrutable. It becomes known that

the strata of the earth's surface have been forming throughout untold

ages, and that successive populations differing utterly from one another

have peopled the earth in different geological epochs. The entire point

of view of thoughtful men becomes changed in contemplating the history

of the world in which we live--albeit the newest thought harks back to

some extent to those days when the inspired thinkers of early Greece

dreamed out the wonderful theories with which our earlier chapters have

made our readers familiar.

In the region of natural philosophy progress is no less pronounced and

no less striking. It suffices here, however, by way of anticipation,

simply to name the greatest generalization of the century in physical

science--the doctrine of the conservation of energy.

I. THE SUCCESSORS OF NEWTON IN ASTRONOMY

HEVELIUS AND HALLEY

STRANGELY enough, the decade immediately following Newton was one of

comparative barrenness in scientific progress, the early years of the

eighteenth century not being as productive of great astronomers as the

later years of the seventeenth, or, for that matter, as the later years

of the eighteenth century itself. Several of the prominent astronomers

of the later seventeenth century lived on into the opening years of the

following century, however, and the younger generation soon developed

a coterie of astronomers, among whom Euler, Lagrange, Laplace, and

Herschel, as we shall see, were to accomplish great things in this field

before the century closed.

One of the great seventeenth-century astronomers, who died just before

the close of the century, was Johannes Hevelius (1611-1687), of Dantzig,

who advanced astronomy by his accurate description of the face and

the spots of the moon. But he is remembered also for having retarded

progress by his influence in refusing to use telescopic sights in his

observations, preferring until his death the plain sights long before

discarded by most other astronomers. The advantages of these telescope

sights have been discussed under the article treating of Robert Hooke,

but no such advantages were ever recognized by Hevelius. So great was

Hevelius's reputation as an astronomer that his refusal to recognize the

advantage of the telescope sights caused many astronomers to hesitate

before accepting them as superior to the plain; and even the famous

Halley, of whom we shall speak further in a moment, was sufficiently

in doubt over the matter to pay the aged astronomer a visit to test his

skill in using the old-style sights. Side by side, Hevelius and Halley

made their observations, Hevelius with his old instrument and Halley

with the new. The results showed slightly in the younger man's favor,

but not enough to make it an entirely convincing demonstration. The

explanation of this, however, did not lie in the lack of superiority

of the telescopic instrument, but rather in the marvellous skill of the

aged Hevelius, whose dexterity almost compensated for the defect of his

instrument. What he might have accomplished could he have been induced

to adopt the telescope can only be surmised.

Halley himself was by no means a tyro in matters astronomical at that

time. As the only son of a wealthy soap-boiler living near London, he

had been given a liberal education, and even before leaving college

made such novel scientific observations as that of the change in the

variation of the compass. At nineteen years of age he discovered a new

method of determining the elements of the planetary orbits which was a

distinct improvement over the old. The year following he sailed for the

Island of St, Helena to make observations of the heavens in the southern

hemisphere.

It was while in St. Helena that Halley made his famous observation

of the transit of Mercury over the sun's disk, this observation being

connected, indirectly at least, with his discovery of a method of

determining the parallax of the planets. By parallax is meant the

apparent change in the position of an object, due really to a change in

the position of the observer. Thus, if we imagine two astronomers making

observations of the sun from opposite sides of the earth at the same

time, it is obvious that to these observers the sun will appear to be

at two different points in the sky. Half the angle measuring this

difference would be known as the sun's parallax. This would depend,

then, upon the distance of the earth from the sun and the length of

the earth's radius. Since the actual length of this radius has been

determined, the parallax of any heavenly body enables the astronomer to

determine its exact distance.

The parallaxes can be determined equally well, however, if two observers

are separated by exactly known distances, several hundreds or thousands

of miles apart. In the case of a transit of Venus across the sun's

disk, for example, an observer at New York notes the image of the planet

moving across the sun's disk, and notes also the exact time of this

observation. In the same manner an observer at London makes similar

observations. Knowing the distance between New York and London, and

the different time of the passage, it is thus possible to calculate the

difference of the parallaxes of the sun and a planet crossing its disk.

The idea of thus determining the parallax of the planets originated, or

at least was developed, by Halley, and from this phenomenon he thought

it possible to conclude the dimensions of all the planetary orbits. As

we shall see further on, his views were found to be correct by later

astronomers.

In 1721 Halley succeeded Flamsteed as astronomer royal at the Greenwich

Observatory. Although sixty-four years of age at that time his activity

in astronomy continued unabated for another score of years. At Greenwich

he undertook some tedious observations of the moon, and during those

observations was first to detect the acceleration of mean motion. He

was unable to explain this, however, and it remained for Laplace in the

closing years of the century to do so, as we shall see later.

Halley's book, the Synopsis Astronomiae Cometicae, is one of the most

valuable additions to astronomical literature since the time of Kepler.

He was first to attempt the calculation of the orbit of a comet, having

revived the ancient opinion that comets belong to the solar system,

moving in eccentric orbits round the sun, and his calculation of the

orbit of the comet of 1682 led him to predict correctly the return of

that comet in 1758. Halley's Study of Meteors.

Like other astronomers of his time he was greatly puzzled over the

well-known phenomena of shooting-stars, or meteors, making many

observations himself, and examining carefully the observations of other

astronomers. In 1714 he gave his views as to the origin and composition

of these mysterious visitors in the earth's atmosphere. As this

subject will be again referred to in a later chapter, Halley's views,

representing the most advanced views of his age, are of interest.

"The theory of the air seemeth at present," he says, "to be perfectly

well understood, and the differing densities thereof at all altitudes;

for supposing the same air to occupy spaces reciprocally proportional to

the quantity of the superior or incumbent air, I have elsewhere proved

that at forty miles high the air is rarer than at the surface of

the earth at three thousand times; and that the utmost height of the

atmosphere, which reflects light in the Crepusculum, is not fully

forty-five miles, notwithstanding which 'tis still manifest that some

sort of vapors, and those in no small quantity, arise nearly to that

height. An instance of this may be given in the great light the society

had an account of (vide Transact. Sep., 1676) from Dr. Wallis, which was

seen in very distant counties almost over all the south part of England.

Of which though the doctor could not get so particular a relation as was

requisite to determine the height thereof, yet from the distant places

it was seen in, it could not but be very many miles high.

"So likewise that meteor which was seen in 1708, on the 31st of July,

between nine and ten o'clock at night, was evidently between forty and

fifty miles perpendicularly high, and as near as I can gather, over

Shereness and the buoy on the Nore. For it was seen at London moving

horizontally from east by north to east by south at least fifty degrees

high, and at Redgrove, in Suffolk, on the Yarmouth road, about twenty

miles from the east coast of England, and at least forty miles to the

eastward of London, it appeared a little to the westward of the south,

suppose south by west, and was seen about thirty degrees high, sliding

obliquely downward. I was shown in both places the situation thereof,

which was as described, but could wish some person skilled in

astronomical matters bad seen it, that we might pronounce concerning its

height with more certainty. Yet, as it is, we may securely conclude

that it was not many more miles westerly than Redgrove, which, as I

said before, is about forty miles more easterly than London. Suppose it,

therefore, where perpendicular, to have been thirty-five miles east

from London, and by the altitude it appeared at in London--viz., fifty

degrees, its tangent will be forty-two miles, for the height of the

meteor above the surface of the earth; which also is rather of the

least, because the altitude of the place shown me is rather more than

less than fifty degrees; and the like may be concluded from the altitude

it appeared in at Redgrove, near seventy miles distant. Though at this

very great distance, it appeared to move with an incredible velocity,

darting, in a very few seconds of time, for about twelve degrees of

a great circle from north to south, being very bright at its first

appearance; and it died away at the east of its course, leaving for some

time a pale whiteness in the place, with some remains of it in the track

where it had gone; but no hissing sound as it passed, or bounce of an

explosion were heard.

"It may deserve the honorable society's thoughts, how so great a

quantity of vapor should be raised to the top of the atmosphere, and

there collected, so as upon its ascension or otherwise illumination, to

give a light to a circle of above one hundred miles diameter, not much

inferior to the light of the moon; so as one might see to take a pin

from the ground in the otherwise dark night. 'Tis hard to conceive what

sort of exhalations should rise from the earth, either by the action

of the sun or subterranean heat, so as to surmount the extreme cold

and rareness of the air in those upper regions: but the fact is

indisputable, and therefore requires a solution."

From this much of the paper it appears that there was a general belief

that this burning mass was heated vapor thrown off from the earth in

some mysterious manner, yet this is unsatisfactory to Halley, for after

citing various other meteors that have appeared within his knowledge, he

goes on to say:

"What sort of substance it must be, that could be so impelled and

ignited at the same time; there being no Vulcano or other Spiraculum of

subterraneous fire in the northeast parts of the world, that we ever yet

heard of, from whence it might be projected.

"I have much considered this appearance, and think it one of the hardest

things to account for that I have yet met with in the phenomena of

meteors, and I am induced to think that it must be some collection of

matter formed in the aether, as it were, by some fortuitous concourse

of atoms, and that the earth met with it as it passed along in its orb,

then but newly formed, and before it had conceived any great impetus of

descent towards the sun. For the direction of it was exactly opposite to

that of the earth, which made an angle with the meridian at that time

of sixty-seven gr., that is, its course was from west southwest to east

northeast, wherefore the meteor seemed to move the contrary way. And

besides falling into the power of the earth's gravity, and losing its

motion from the opposition of the medium, it seems that it descended

towards the earth, and was extinguished in the Tyrrhene Sea, to the

west southwest of Leghorn. The great blow being heard upon its first

immersion into the water, and the rattling like the driving of a cart

over stones being what succeeded upon its quenching; something like this

is always heard upon quenching a very hot iron in water. These facts

being past dispute, I would be glad to have the opinion of the learned

thereon, and what objection can be reasonably made against the above

hypothesis, which I humbly submit to their censure."(1)

These few paragraphs, coming as they do from a leading

eighteenth-century astronomer, convey more clearly than any comment the

actual state of the meteorological learning at that time. That this ball

of fire, rushing "at a greater velocity than the swiftest cannon-ball,"

was simply a mass of heated rock passing through our atmosphere, did not

occur to him, or at least was not credited. Nor is this surprising when

we reflect that at that time universal gravitation had been but recently

discovered; heat had not as yet been recognized as simply a form of

motion; and thunder and lightning were unexplained mysteries, not to

be explained for another three-quarters of a century. In the chapter on

meteorology we shall see how the solution of this mystery that puzzled

Halley and his associates all their lives was finally attained.

BRADLEY AND THE ABERRATION OF LIGHT

Halley was succeeded as astronomer royal by a man whose useful additions

to the science were not to be recognized or appreciated fully until

brought to light by the Prussian astronomer Bessel early in the

nineteenth century. This was Dr. James Bradley, an ecclesiastic, who

ranks as one of the most eminent astronomers of the eighteenth century.

His most remarkable discovery was the explanation of a peculiar motion

of the pole-star, first observed, but not explained, by Picard a

century before. For many years a satisfactory explanation was sought

unsuccessfully by Bradley and his fellow-astronomers, but at last he was

able to demonstrate that the stary Draconis, on which he was making his

observations, described, or appeared to describe, a small ellipse.

If this observation was correct, it afforded a means of computing the

aberration of any star at all times. The explanation of the physical

cause of this aberration, as Bradley thought, and afterwards

demonstrated, was the result of the combination of the motion of light

with the annual motion of the earth. Bradley first formulated this

theory in 1728, but it was not until 1748--twenty years of continuous

struggle and observation by him--that he was prepared to communicate the

results of his efforts to the Royal Society. This remarkable paper is

thought by the Frenchman, Delambre, to entitle its author to a place in

science beside such astronomers as Hipparcbus and Kepler.

Bradley's studies led him to discover also the libratory motion of the

earth's axis. "As this appearance of Draconis indicated a diminution

of the inclination of the earth's axis to the plane of the ecliptic,"

he says; "and as several astronomers have supposed THAT inclination to

diminish regularly; if this phenomenon depended upon such a cause, and

amounted to 18" in nine years, the obliquity of the ecliptic would, at

that rate, alter a whole minute in thirty years; which is much

faster than any observations, before made, would allow. I had reason,

therefore, to think that some part of this motion at the least, if not

the whole, was owing to the moon's action upon the equatorial parts of

the earth; which, I conceived, might cause a libratory motion of

the earth's axis. But as I was unable to judge, from only nine years

observations, whether the axis would entirely recover the same position

that it had in the year 1727, I found it necessary to continue my

observations through a whole period of the moon's nodes; at the end of

which I had the satisfaction to see, that the stars, returned into the

same position again; as if there had been no alteration at all in the

inclination of the earth's axis; which fully convinced me that I had

guessed rightly as to the cause of the phenomena. This circumstance

proves likewise, that if there be a gradual diminution of the obliquity

of the ecliptic, it does not arise only from an alteration in the

position of the earth's axis, but rather from some change in the plane

of the ecliptic itself; because the stars, at the end of the period

of the moon's nodes, appeared in the same places, with respect to the

equator, as they ought to have done, if the earth's axis had retained

the same inclination to an invariable plane."(2)

FRENCH ASTRONOMERS

Meanwhile, astronomers across the channel were by no means idle. In

France several successful observers were making many additions to the

already long list of observations of the first astronomer of the Royal

Observatory of Paris, Dominic Cassini (1625-1712), whose reputation

among his contemporaries was much greater than among succeeding

generations of astronomers. Perhaps the most deserving of these

successors was Nicolas Louis de Lacaille (1713-1762), a theologian who

had been educated at the expense of the Duke of Bourbon, and who, soon

after completing his clerical studies, came under the patronage of

Cassini, whose attention had been called to the young man's interest in

the sciences. One of Lacaille's first under-takings was the remeasuring

of the French are of the meridian, which had been incorrectly measured

by his patron in 1684. This was begun in 1739, and occupied him for

two years before successfully completed. As a reward, however, he was

admitted to the academy and appointed mathematical professor in Mazarin

College.

In 1751 he went to the Cape of Good Hope for the purpose of determining

the sun's parallax by observations of the parallaxes of Mars and Venus,

and incidentally to make observations on the other southern hemisphere

stars. The results of this undertaking were most successful, and were

given in his Coelum australe stelligerum, etc., published in 1763. In

this he shows that in the course of a single year he had observed some

ten thousand stars, and computed the places of one thousand nine hundred

and forty-two of them, measured a degree of the meridian, and made

many observations of the moon--productive industry seldom equalled in

a single year in any field. These observations were of great service to

the astronomers, as they afforded the opportunity of comparing the stars

of the southern hemisphere with those of the northern, which were being

observed simultaneously by Lelande at Berlin.

Lacaille's observations followed closely upon the determination of an

absorbing question which occupied the attention of the astronomers in

the early part of the century. This question was as to the shape of the

earth--whether it was actually flattened at the poles. To settle this

question once for all the Academy of Sciences decided to make the

actual measurement of the length of two degrees, one as near the pole

as possible, the other at the equator. Accordingly, three astronomers,

Godin, Bouguer, and La Condamine, made the journey to a spot on the

equator in Peru, while four astronomers, Camus, Clairaut, Maupertuis,

and Lemonnier, made a voyage to a place selected in Lapland. The result

of these expeditions was the determination that the globe is oblately

spheroidal.

A great contemporary and fellow-countryman of Lacaille was Jean Le Rond

d'Alembert (1717-1783), who, although not primarily an astronomer, did

so much with his mathematical calculations to aid that science that

his name is closely connected with its progress during the eighteenth

century. D'Alembert, who became one of the best-known men of science of

his day, and whose services were eagerly sought by the rulers of Europe,

began life as a foundling, having been exposed in one of the markets of

Paris. The sickly infant was adopted and cared for in the family of a

poor glazier, and treated as a member of the family. In later years,

however, after the foundling had become famous throughout Europe, his

mother, Madame Tencin, sent for him, and acknowledged her relationship.

It is more than likely that the great philosopher believed her story,

but if so he did not allow her the satisfaction of knowing his belief,

declaring always that Madame Tencin could "not be nearer than a

step-mother to him, since his mother was the wife of the glazier."

D'Alembert did much for the cause of science by his example as well

as by his discoveries. By living a plain but honest life, declining

magnificent offers of positions from royal patrons, at the same time

refusing to grovel before nobility, he set a worthy example to other

philosophers whose cringing and pusillanimous attitude towards persons

of wealth or position had hitherto earned them the contempt of the upper

classes.

His direct additions to astronomy are several, among others the

determination of the mutation of the axis of the earth. He also

determined the ratio of the attractive forces of the sun and moon,

which he found to be about as seven to three. From this he reached the

conclusion that the earth must be seventy times greater than the moon.

The first two volumes of his Researches on the Systems of the World,

published in 1754, are largely devoted to mathematical and astronomical

problems, many of them of little importance now, but of great interest

to astronomers at that time.

Another great contemporary of D'Alembert, whose name is closely

associated and frequently confounded with his, was Jean Baptiste Joseph

Delambre (1749-1822). More fortunate in birth as also in his educational

advantages, Delambre as a youth began his studies under the celebrated

poet Delille. Later he was obliged to struggle against poverty,

supporting himself for a time by making translations from Latin, Greek,

Italian, and English, and acting as tutor in private families. The

turning-point of his fortune came when the attention of Lalande was

called to the young man by his remarkable memory, and Lalande soon

showed his admiration by giving Delambre certain difficult astronomical

problems to solve. By performing these tasks successfully his future as

an astronomer became assured. At that time the planet Uranus had just

been discovered by Herschel, and the Academy of Sciences offered as the

subject for one of its prizes the determination of the planet's orbit.

Delambre made this determination and won the prize--a feat that brought

him at once into prominence.

By his writings he probably did as much towards perfecting modern

astronomy as any one man. His History of Astronomy is not merely a

narrative of progress of astronomy but a complete abstract of all the

celebrated works written on the subject. Thus he became famous as an

historian as well as an astronomer.

LEONARD EULER

Still another contemporary of D'Alembert and Delambre, and somewhat

older than either of them, was Leonard Euler (1707-1783), of Basel,

whose fame as a philosopher equals that of either of the great

Frenchmen. He is of particular interest here in his capacity of

astronomer, but astronomy was only one of the many fields of science in

which he shone. Surely something out of the ordinary was to be expected

of the man who could "repeat the AEneid of Virgil from the beginning

to the end without hesitation, and indicate the first and last line of

every page of the edition which he used." Something was expected, and he

fulfilled these expectations.

In early life he devoted himself to the study of theology and the

Oriental languages, at the request of his father, but his love of

mathematics proved too strong, and, with his father's consent, he

finally gave up his classical studies and turned to his favorite study,

geometry. In 1727 he was invited by Catharine I. to reside in St.

Petersburg, and on accepting this invitation he was made an associate

of the Academy of Sciences. A little later he was made professor of

physics, and in 1733 professor of mathematics. In 1735 he solved a

problem in three days which some of the eminent mathematicians would not

undertake under several months. In 1741 Frederick the Great invited him

to Berlin, where he soon became a member of the Academy of Sciences and

professor of mathematics; but in 1766 he returned to St. Petersburg.

Towards the close of his life he became virtually blind, being obliged

to dictate his thoughts, sometimes to persons entirely ignorant of the

subject in hand. Nevertheless, his remarkable memory, still further

heightened by his blindness, enabled him to carry out the elaborate

computations frequently involved.

Euler's first memoir, transmitted to the Academy of Sciences of Paris

in 1747, was on the planetary perturbations. This memoir carried off the

prize that had been offered for the analytical theory of the motions of

Jupiter and Saturn. Other memoirs followed, one in 1749 and another in

1750, with further expansions of the same subject. As some slight

errors were found in these, such as a mistake in some of the formulae

expressing the secular and periodic inequalities, the academy proposed

the same subject for the prize of 1752. Euler again competed, and won

this prize also. The contents of this memoir laid the foundation for

the subsequent demonstration of the permanent stability of the planetary

system by Laplace and Lagrange.

It was Euler also who demonstrated that within certain fixed limits

the eccentricities and places of the aphelia of Saturn and Jupiter are

subject to constant variation, and he calculated that after a lapse

of about thirty thousand years the elements of the orbits of these two

planets recover their original values.

II. THE PROGRESS OF MODERN ASTRONOMY

A NEW epoch in astronomy begins with the work of William Herschel, the

Hanoverian, whom England made hers by adoption. He was a man with a

positive genius for sidereal discovery. At first a mere amateur in

astronomy, he snatched time from his duties as music-teacher to grind

him a telescopic mirror, and began gazing at the stars. Not content with

his first telescope, he made another and another, and he had such genius

for the work that he soon possessed a better instrument than was ever

made before. His patience in grinding the curved reflective surface was

monumental. Sometimes for sixteen hours together he must walk steadily

about the mirror, polishing it, without once removing his hands.

Meantime his sister, always his chief lieutenant, cheered him with her

presence, and from time to time put food into his mouth. The telescope

completed, the astronomer turned night into day, and from sunset to

sunrise, year in and year out, swept the heavens unceasingly, unless

prevented by clouds or the brightness of the moon. His sister sat always

at his side, recording his observations. They were in the open air,

perched high at the mouth of the reflector, and sometimes it was so cold

that the ink froze in the bottle in Caroline Herschel's hand; but the

two enthusiasts hardly noticed a thing so common-place as terrestrial

weather. They were living in distant worlds.

The results? What could they be? Such enthusiasm would move mountains.

But, after all, the moving of mountains seems a liliputian task compared

with what Herschel really did with those wonderful telescopes. He moved

worlds, stars, a universe--even, if you please, a galaxy of universes;

at least he proved that they move, which seems scarcely less wonderful;

and he expanded the cosmos, as man conceives it, to thousands of times

the dimensions it had before. As a mere beginning, he doubled the

diameter of the solar system by observing the great outlying planet

which we now call Uranus, but which he christened Georgium Sidus,

in honor of his sovereign, and which his French contemporaries, not

relishing that name, preferred to call Herschel.

This discovery was but a trifle compared with what Herschel did later

on, but it gave him world-wide reputation none the less. Comets and

moons aside, this was the first addition to the solar system that had

been made within historic times, and it created a veritable furor of

popular interest and enthusiasm. Incidentally King George was flattered

at having a world named after him, and he smiled on the astronomer, and

came with his court to have a look at his namesake. The inspection

was highly satisfactory; and presently the royal favor enabled the

astronomer to escape the thraldom of teaching music and to devote his

entire time to the more congenial task of star-gazing.

Thus relieved from the burden of mundane embarrassments, he turned with

fresh enthusiasm to the skies, and his discoveries followed one another

in bewildering profusion. He found various hitherto unseen moons of our

sister planets; he made special studies of Saturn, and proved that this

planet, with its rings, revolves on its axis; he scanned the spots on

the sun, and suggested that they influence the weather of our earth; in

short, he extended the entire field of solar astronomy. But very soon

this field became too small for him, and his most important researches

carried him out into the regions of space compared with which the span

of our solar system is a mere point. With his perfected telescopes he

entered abysmal vistas which no human eve ever penetrated before, which

no human mind had hitherto more than vaguely imagined. He tells us that

his forty-foot reflector will bring him light from a distance of "at

least eleven and three-fourths millions of millions of millions of

miles"--light which left its source two million years ago. The smallest

stars visible to the unaided eye are those of the sixth magnitude; this

telescope, he thinks, has power to reveal stars of the 1342d magnitude.

But what did Herschel learn regarding these awful depths of space and

the stars that people them? That was what the world wished to know.

Copernicus, Galileo, Kepler, had given us a solar system, but the stars

had been a mystery. What says the great reflector--are the stars points

of light, as the ancients taught, and as more than one philosopher of

the eighteenth century has still contended, or are they suns, as others

hold? Herschel answers, they are suns, each and every one of all the

millions--suns, many of them, larger than the one that is the centre of

our tiny system. Not only so, but they are moving suns. Instead of

being fixed in space, as has been thought, they are whirling in gigantic

orbits about some common centre. Is our sun that centre? Far from it.

Our sun is only a star like all the rest, circling on with its attendant

satellites--our giant sun a star, no different from myriad other stars,

not even so large as some; a mere insignificant spark of matter in an

infinite shower of sparks.

Nor is this all. Looking beyond the few thousand stars that are visible

to the naked eye, Herschel sees series after series of more distant

stars, marshalled in galaxies of millions; but at last he reaches a

distance beyond which the galaxies no longer increase. And yet--so he

thinks--he has not reached the limits of his vision. What then? He has

come to the bounds of the sidereal system--seen to the confines of the

universe. He believes that he can outline this system, this universe,

and prove that it has the shape of an irregular globe, oblately

flattened to almost disklike proportions, and divided at one edge--a

bifurcation that is revealed even to the naked eye in the forking of the

Milky Way.

This, then, is our universe as Herschel conceives it--a vast galaxy

of suns, held to one centre, revolving, poised in space. But even

here those marvellous telescopes do not pause. Far, far out beyond the

confines of our universe, so far that the awful span of our own system

might serve as a unit of measure, are revealed other systems, other

universes, like our own, each composed, as he thinks, of myriads of

suns, clustered like our galaxy into an isolated system--mere islands of

matter in an infinite ocean of space. So distant from our universe are

these now universes of Herschel's discovery that their light reaches

us only as a dim, nebulous glow, in most cases invisible to the unaided

eye. About a hundred of these nebulae were known when Herschel began

his studies. Before the close of the century he had discovered about

two thousand more of them, and many of these had been resolved by his

largest telescopes into clusters of stars. He believed that the farthest

of these nebulae that he could see was at least three hundred thousand

times as distant from us as the nearest fixed star. Yet that nearest

star--so more recent studies prove--is so remote that its light,

travelling one hundred and eighty thousand miles a second, requires

three and one-half years to reach our planet.

As if to give the finishing touches to this novel scheme of cosmology,

Herschel, though in the main very little given to unsustained

theorizing, allows himself the privilege of one belief that he cannot

call upon his telescope to substantiate. He thinks that all the myriad

suns of his numberless systems are instinct with life in the human

sense. Giordano Bruno and a long line of his followers had held that

some of our sister planets may be inhabited, but Herschel extends

the thought to include the moon, the sun, the stars--all the heavenly

bodies. He believes that he can demonstrate the habitability of our own

sun, and, reasoning from analogy, he is firmly convinced that all the

suns of all the systems are "well supplied with inhabitants." In this,

as in some other inferences, Herschel is misled by the faulty physics

of his time. Future generations, working with perfected instruments, may

not sustain him all along the line of his observations, even, let alone

his inferences. But how one's egotism shrivels and shrinks as one grasps

the import of his sweeping thoughts!

Continuing his observations of the innumerable nebulae, Herschel is led

presently to another curious speculative inference. He notes that some

star groups are much more thickly clustered than others, and he is

led to infer that such varied clustering tells of varying ages of the

different nebulae. He thinks that at first all space may have been

evenly sprinkled with the stars and that the grouping has resulted from

the action of gravitation.

"That the Milky Way is a most extensive stratum of stars of various

sizes admits no longer of lasting doubt," he declares, "and that our sun

is actually one of the heavenly bodies belonging to it is as evident. I

have now viewed and gauged this shining zone in almost every direction

and find it composed of stars whose number... constantly increases and

decreases in proportion to its apparent brightness to the naked eye.

"Let us suppose numberless stars of various sizes, scattered over an

indefinite portion of space in such a manner as to be almost equally

distributed throughout the whole. The laws of attraction which no doubt

extend to the remotest regions of the fixed stars will operate in such a

manner as most probably to produce the following effects:

"In the first case, since we have supposed the stars to be of various

sizes, it will happen that a star, being considerably larger than its

neighboring ones, will attract them more than they will be attracted by

others that are immediately around them; by which means they will be,

in time, as it were, condensed about a centre, or, in other words, form

themselves into a cluster of stars of almost a globular figure, more

or less regular according to the size and distance of the surrounding

stars....

"The next case, which will also happen almost as frequently as the

former, is where a few stars, though not superior in size to the rest,

may chance to be rather nearer one another than the surrounding ones,...

and this construction admits of the utmost variety of shapes....

"From the composition and repeated conjunction of both the foregoing

formations, a third may be derived when many large stars, or combined

small ones, are spread in long, extended, regular, or crooked rows,

streaks, or branches; for they will also draw the surrounding stars, so

as to produce figures of condensed stars curiously similar to the former

which gave rise to these condensations.

"We may likewise admit still more extensive combinations; when, at the

same time that a cluster of stars is forming at the one part of

space, there may be another collection in a different but perhaps not

far-distant quarter, which may occasion a mutual approach towards their

own centre of gravity.

"In the last place, as a natural conclusion of the former cases, there

will be formed great cavities or vacancies by the retreating of the

stars towards the various centres which attract them."(1)

Looking forward, it appears that the time must come when all the suns

of a system will be drawn together and destroyed by impact at a common

centre. Already, it seems to Herschel, the thickest clusters have

"outlived their usefulness" and are verging towards their doom.

But again, other nebulae present an appearance suggestive of an opposite

condition. They are not resolvable into stars, but present an almost

uniform appearance throughout, and are hence believed to be composed of

a shining fluid, which in some instances is seen to be condensed at the

centre into a glowing mass. In such a nebula Herschel thinks he sees a

sun in process of formation.

THE NEBULAR HYPOTHESIS OF KANT

Taken together, these two conceptions outline a majestic cycle of world

formation and world destruction--a broad scheme of cosmogony, such as

had been vaguely adumbrated two centuries before by Kepler and in

more recent times by Wright and Swedenborg. This so-called "nebular

hypothesis" assumes that in the beginning all space was uniformly filled

with cosmic matter in a state of nebular or "fire-mist" diffusion,

"formless and void." It pictures the condensation--coagulation, if

you will--of portions of this mass to form segregated masses, and the

ultimate development out of these masses of the sidereal bodies that we

see.

Perhaps the first elaborate exposition of this idea was that given by

the great German philosopher Immanuel Kant (born at Konigsberg in 1724,

died in 1804), known to every one as the author of the Critique of Pure

Reason. Let us learn from his own words how the imaginative philosopher

conceived the world to have come into existence.

"I assume," says Kant, "that all the material of which the globes

belonging to our solar system--all the planets and comets--consist, at

the beginning of all things was decomposed into its primary elements,

and filled the whole space of the universe in which the bodies formed

out of it now revolve. This state of nature, when viewed in and by

itself without any reference to a system, seems to be the very simplest

that can follow upon nothing. At that time nothing has yet been formed.

The construction of heavenly bodies at a distance from one another,

their distances regulated by their attraction, their form arising out of

the equilibrium of their collected matter, exhibit a later state.... In

a region of space filled in this manner, a universal repose could last

only a moment. The elements have essential forces with which to put

each other in motion, and thus are themselves a source of life. Matter

immediately begins to strive to fashion itself. The scattered elements

of a denser kind, by means of their attraction, gather from a sphere

around them all the matter of less specific gravity; again, these

elements themselves, together with the material which they have united

with them, collect in those points where the particles of a still denser

kind are found; these in like manner join still denser particles, and

so on. If we follow in imagination this process by which nature fashions

itself into form through the whole extent of chaos, we easily perceive

that all the results of the process would consist in the formation of

divers masses which, when their formation was complete, would by the

equality of their attraction be at rest and be forever unmoved.

"But nature has other forces in store which are specially exerted when

matter is decomposed into fine particles. They are those forces by which

these particles repel one another, and which, by their conflict with

attractions, bring forth that movement which is, as it were, the lasting

life of nature. This force of repulsion is manifested in the elasticity

of vapors, the effluences of strong-smelling bodies, and the diffusion

of all spirituous matters. This force is an uncontestable phenomenon of

matter. It is by it that the elements, which may be falling to the point

attracting them, are turned sideways promiscuously from their movement

in a straight line; and their perpendicular fall thereby issues in

circular movements, which encompass the centre towards which they were

falling. In order to make the formation of the world more distinctly

conceivable, we will limit our view by withdrawing it from the infinite

universe of nature and directing it to a particular system, as the

one which belongs to our sun. Having considered the generation of this

system, we shall be able to advance to a similar consideration of the

origin of the great world-systems, and thus to embrace the infinitude of

the whole creation in one conception.

"From what has been said, it will appear that if a point is situated in

a very large space where the attraction of the elements there situated

acts more strongly than elsewhere, then the matter of the elementary

particles scattered throughout the whole region will fall to that point.

The first effect of this general fall is the formation of a body at this

centre of attraction, which, so to speak, grows from an infinitely

small nucleus by rapid strides; and in the proportion in which this mass

increases, it also draws with greater force the surrounding particles

to unite with it. When the mass of this central body has grown so great

that the velocity with which it draws the particles to itself with great

distances is bent sideways by the feeble degree of repulsion with which

they impede one another, and when it issues in lateral movements which

are capable by means of the centrifugal force of encompassing the

central body in an orbit, then there are produced whirls or vortices

of particles, each of which by itself describes a curved line by the

composition of the attracting force and the force of revolution that had

been bent sideways. These kinds of orbits all intersect one another,

for which their great dispersion in this space gives place. Yet these

movements are in many ways in conflict with one another, and they

naturally tend to bring one another to a uniformity--that is, into a

state in which one movement is as little obstructive to the other as

possible. This happens in two ways: first by the particles limiting

one another's movement till they all advance in one direction; and,

secondly, in this way, that the particles limit their vertical movements

in virtue of which they are approaching the centre of attraction, till

they all move horizontally--i. e., in parallel circles round the sun as

their centre, no longer intercept one another, and by the centrifugal

force becoming equal with the falling force they keep themselves

constantly in free circular orbits at the distance at which they move.

The result, finally, is that only those particles continue to move in

this region of space which have acquired by their fall a velocity, and

through the resistance of the other particles a direction, by which they

can continue to maintain a FREE CIRCULAR MOVEMENT....

"The view of the formation of the planets in this system has the

advantage over every other possible theory in holding that the origin

of the movements, and the position of the orbits in arising at that same

point of time--nay, more, in showing that even the deviations from the

greatest possible exactness in their determinations, as well as the

accordances themselves, become clear at a glance. The planets are formed

out of particles which, at the distance at which they move, have exact

movements in circular orbits; and therefore the masses composed out of

them will continue the same movements and at the same rate and in the

same direction."(2)

It must be admitted that this explanation leaves a good deal to be

desired. It is the explanation of a metaphysician rather than that of

an experimental scientist. Such phrases as "matter immediately begins to

strive to fashion itself," for example, have no place in the reasoning

of inductive science. Nevertheless, the hypothesis of Kant is a

remarkable conception; it attempts to explain along rational lines

something which hitherto had for the most part been considered

altogether inexplicable.

But there are various questions that at once suggest themselves which

the Kantian theory leaves unanswered. How happens it, for example, that

the cosmic mass which gave birth to our solar system was divided into

several planetary bodies instead of remaining a single mass? Were the

planets struck from the sun by the chance impact of comets, as Buffon

has suggested? or thrown out by explosive volcanic action, in accordance

with the theory of Dr. Darwin? or do they owe their origin to some

unknown law? In any event, how chanced it that all were projected in

nearly the same plane as we now find them?

LAPLACE AND THE NEBULAR HYPOTHESIS

It remained for a mathematical astronomer to solve these puzzles. The

man of all others competent to take the subject in hand was the French

astronomer Laplace. For a quarter of a century he had devoted his

transcendent mathematical abilities to the solution of problems of

motion of the heavenly bodies. Working in friendly rivalry with his

countryman Lagrange, his only peer among the mathematicians of the age,

he had taken up and solved one by one the problems that Newton left

obscure. Largely through the efforts of these two men the last lingering

doubts as to the solidarity of the Newtonian hypothesis of universal

gravitation had been removed. The share of Lagrange was hardly less than

that of his co-worker; but Laplace will longer be remembered, because

he ultimately brought his completed labors into a system, and,

incorporating with them the labors of his contemporaries, produced

in the Mecanique Celeste the undisputed mathematical monument of the

century, a fitting complement to the Principia of Newton, which it

supplements and in a sense completes.

In the closing years of the eighteenth century Laplace took up the

nebular hypothesis of cosmogony, to which we have just referred, and

gave it definite proportions; in fact, made it so thoroughly his own

that posterity will always link it with his name. Discarding the crude

notions of cometary impact and volcanic eruption, Laplace filled up the

gaps in the hypothesis with the aid of well-known laws of gravitation

and motion. He assumed that the primitive mass of cosmic matter which

was destined to form our solar system was revolving on its axis even at

a time when it was still nebular in character, and filled all space to

a distance far beyond the present limits of the system. As this vaporous

mass contracted through loss of heat, it revolved more and more swiftly,

and from time to time, through balance of forces at its periphery, rings

of its substance were whirled off and left revolving there, subsequently

to become condensed into planets, and in their turn whirl off minor

rings that became moons. The main body of the original mass remains in

the present as the still contracting and rotating body which we call the

sun.

Let us allow Laplace to explain all this in detail:

"In order to explain the prime movements of the planetary system,"

he says, "there are the five following phenomena: The movement of the

planets in the same direction and very nearly in the same plane; the

movement of the satellites in the same direction as that of the planets;

the rotation of these different bodies and the sun in the same

direction as their revolution, and in nearly the same plane; the slight

eccentricity of the orbits of the planets and of the satellites; and,

finally, the great eccentricity of the orbits of the comets, as if their

inclinations had been left to chance.

"Buffon is the only man I know who, since the discovery of the true

system of the world, has endeavored to show the origin of the planets

and their satellites. He supposes that a comet, in falling into the sun,

drove from it a mass of matter which was reassembled at a distance in

the form of various globes more or less large, and more or less removed

from the sun, and that these globes, becoming opaque and solid, are now

the planets and their satellites.

"This hypothesis satisfies the first of the five preceding phenomena;

for it is clear that all the bodies thus formed would move very nearly

in the plane which passed through the centre of the sun, and in the

direction of the torrent of matter which was produced; but the four

other phenomena appear to be inexplicable to me by this means. Indeed,

the absolute movement of the molecules of a planet ought then to be in

the direction of the movement of its centre of gravity; but it does not

at all follow that the motion of the rotation of the planets should be

in the same direction. Thus the earth should rotate from east to west,

but nevertheless the absolute movement of its molecules should be

from east to west; and this ought also to apply to the movement of the

revolution of the satellites, in which the direction, according to the

hypothesis which he offers, is not necessarily the same as that of the

progressive movement of the planets.

"A phenomenon not only very difficult to explain under this hypothesis,

but one which is even contrary to it, is the slight eccentricity of the

planetary orbits. We know, by the theory of central forces, that if

a body moves in a closed orbit around the sun and touches it, it also

always comes back to that point at every revolution; whence it follows

that if the planets were originally detached from the sun, they would

touch it at each return towards it, and their orbits, far from being

circular, would be very eccentric. It is true that a mass of matter

driven from the sun cannot be exactly compared to a globe which touches

its surface, for the impulse which the particles of this mass receive

from one another and the reciprocal attractions which they exert among

themselves, could, in changing the direction of their movements, remove

their perihelions from the sun; but their orbits would be always most

eccentric, or at least they would not have slight eccentricities except

by the most extraordinary chance. Thus we cannot see, according to

the hypothesis of Buffon, why the orbits of more than a hundred comets

already observed are so elliptical. This hypothesis is therefore

very far from satisfying the preceding phenomena. Let us see if it is

possible to trace them back to their true cause.

"Whatever may be its ultimate nature, seeing that it has caused or

modified the movements of the planets, it is necessary that this cause

should embrace every body, and, in view of the enormous distances which

separate them, it could only have been a fluid of immense extent.

In order to have given them an almost circular movement in the same

direction around the sun, it is necessary that this fluid should

have enveloped the sun as in an atmosphere. The consideration of the

planetary movements leads us then to think that, on account of excessive

heat, the atmosphere of the sun originally extended beyond the orbits of

all the planets, and that it was successively contracted to its present

limits.

"In the primitive condition in which we suppose the sun to have been, it

resembled a nebula such as the telescope shows is composed of a nucleus

more or less brilliant, surrounded by a nebulosity which, on condensing

itself towards the centre, forms a star. If it is conceived by analogy

that all the stars were formed in this manner, it is possible to imagine

their previous condition of nebulosity, itself preceded by other states

in which the nebulous matter was still more diffused, the nucleus being

less and less luminous. By going back as far as possible, we thus

arrive at a nebulosity so diffused that its existence could hardly be

suspected.

"For a long time the peculiar disposition of certain stars, visible

to the unaided eye, has struck philosophical observers. Mitchell

has already remarked how little probable it is that the stars in the

Pleiades, for example, could have been contracted into the small

space which encloses them by the fortuity of chance alone, and he has

concluded that this group of stars, and similar groups which the skies

present to us, are the necessary result of the condensation of a nebula,

with several nuclei, and it is evident that a nebula, by continually

contracting, towards these various nuclei, at length would form a group

of stars similar to the Pleiades. The condensation of a nebula with two

nuclei would form a system of stars close together, turning one upon

the other, such as those double stars of which we already know the

respective movements.

"But how did the solar atmosphere determine the movements of the

rotation and revolution of the planets and satellites? If these bodies

had penetrated very deeply into this atmosphere, its resistance would

have caused them to fall into the sun. We can therefore conjecture that

the planets were formed at their successive limits by the condensation

of a zone of vapors which the sun, on cooling, left behind, in the plane

of his equator.

"Let us recall the results which we have given in a preceding chapter.

The atmosphere of the sun could not have extended indefinitely. Its

limit was the point where the centrifugal force due to its movement

of rotation balanced its weight. But in proportion as the cooling

contracted the atmosphere, and those molecules which were near to them

condensed upon the surface of the body, the movement of the rotation

increased; for, on account of the Law of Areas, the sum of the areas

described by the vector of each molecule of the sun and its atmosphere

and projected in the plane of the equator being always the same, the

rotation should increase when these molecules approach the centre of the

sun. The centrifugal force due to this movement becoming thus larger,

the point where the weight is equal to it is nearer the sun. Supposing,

then, as it is natural to admit, that the atmosphere extended at some

period to its very limits, it should, on cooling, leave molecules behind

at this limit and at limits successively occasioned by the increased

rotation of the sun. The abandoned molecules would continue to revolve

around this body, since their centrifugal force was balanced by their

weight. But this equilibrium not arising in regard to the atmospheric

molecules parallel to the solar equator, the latter, on account of their

weight, approached the atmosphere as they condensed, and did not cease

to belong to it until by this motion they came upon the equator.

"Let us consider now the zones of vapor successively left behind. These

zones ought, according to appearance, by the condensation and mutual

attraction of their molecules, to form various concentric rings of vapor

revolving around the sun. The mutual gravitational friction of each ring

would accelerate some and retard others, until they had all acquired the

same angular velocity. Thus the actual velocity of the molecules most

removed from the sun would be the greatest. The following cause would

also operate to bring about this difference of speed. The molecules

farthest from the sun, and which by the effects of cooling and

condensation approached one another to form the outer part of the ring,

would have always described areas proportional to the time since the

central force by which they were controlled has been constantly directed

towards this body. But this constancy of areas necessitates an increase

of velocity proportional to the distance. It is thus seen that the same

cause would diminish the velocity of the molecules which form the inner

part of the ring.

"If all the molecules of the ring of vapor continued to condense without

disuniting, they would at length form a ring either solid or fluid. But

this formation would necessitate such a regularity in every part of the

ring, and in its cooling, that this phenomenon is extremely rare; and

the solar system affords us, indeed, but one example--namely, in the

ring of Saturn. In nearly every case the ring of vapor was broken into

several masses, each moving at similar velocities, and continuing to

rotate at the same distance around the sun. These masses would take

a spheroid form with a rotatory movement in the direction of the

revolution, because their inner molecules had less velocity than the

outer. Thus were formed so many planets in a condition of vapor. But

if one of them were powerful enough to reunite successively by its

attraction all the others around its centre of gravity, the ring of

vapor would be thus transformed into a single spheroidical mass of

vapor revolving around the sun with a rotation in the direction of its

revolution. The latter case has been that which is the most common, but

nevertheless the solar system affords us an instance of the first case

in the four small planets which move between Jupiter and Mars; at least,

if we do not suppose, as does M. Olbers, that they originally formed a

single planet which a mighty explosion broke up into several portions

each moving at different velocities.

"According to our hypothesis, the comets are strangers to our planetary

system. In considering them, as we have done, as minute nebulosities,

wandering from solar system to solar system, and formed by the

condensation of the nebulous matter everywhere existent in profusion in

the universe, we see that when they come into that part of the heavens

where the sun is all-powerful, he forces them to describe orbits either

elliptical or hyperbolic, their paths being equally possible in all

directions, and at all inclinations of the ecliptic, conformably to what

has been observed. Thus the condensation of nebulous matter, by which

we have at first explained the motions of the rotation and revolution

of the planets and their satellites in the same direction, and in nearly

approximate planes, explains also why the movements of the comets escape

this general law."(3)

The nebular hypothesis thus given detailed completion by Laplace is a

worthy complement of the grand cosmologic scheme of Herschel. Whether

true or false, the two conceptions stand as the final contributions

of the eighteenth century to the history of man's ceaseless efforts to

solve the mysteries of cosmic origin and cosmic structure. The world

listened eagerly and without prejudice to the new doctrines; and that

attitude tells of a marvellous intellectual growth of our race. Mark the

transition. In the year 1600, Bruno was burned at the stake for teaching

that our earth is not the centre of the universe. In 1700, Newton was

pronounced "impious and heretical" by a large school of philosophers

for declaring that the force which holds the planets in their orbits

is universal gravitation. In 1800, Laplace and Herschel are honored for

teaching that gravitation built up the system which it still controls;

that our universe is but a minor nebula, our sun but a minor star, our

earth a mere atom of matter, our race only one of myriad races peopling

an infinity of worlds. Doctrines which but the span of two human lives

before would have brought their enunciators to the stake were now

pronounced not impious, but sublime.

ASTEROIDS AND SATELLITES

The first day of the nineteenth century was fittingly signalized by the

discovery of a new world. On the evening of January 1, 1801, an Italian

astronomer, Piazzi, observed an apparent star of about the eighth

magnitude (hence, of course, quite invisible to the unaided eye), which

later on was seen to have moved, and was thus shown to be vastly nearer

the earth than any true star. He at first supposed, as Herschel had

done when he first saw Uranus, that the unfamiliar body was a comet; but

later observation proved it a tiny planet, occupying a position in space

between Mars and Jupiter. It was christened Ceres, after the tutelary

goddess of Sicily.

Though unpremeditated, this discovery was not unexpected, for

astronomers had long surmised the existence of a planet in the wide

gap between Mars and Jupiter. Indeed, they were even preparing to make

concerted search for it, despite the protests of philosophers, who

argued that the planets could not possibly exceed the magic number

seven, when Piazzi forestalled their efforts. But a surprise came

with the sequel; for the very next year Dr. Olbers, the wonderful

physician-astronomer of Bremen, while following up the course of Ceres,

happened on another tiny moving star, similarly located, which soon

revealed itself as planetary. Thus two planets were found where only one

was expected.

The existence of the supernumerary was a puzzle, but Olbers solved it

for the moment by suggesting that Ceres and Pallas, as he called his

captive, might be fragments of a quondam planet, shattered by internal

explosion or by the impact of a comet. Other similar fragments, he

ventured to predict, would be found when searched for. William Herschel

sanctioned this theory, and suggested the name asteroids for the tiny

planets. The explosion theory was supported by the discovery of another

asteroid, by Harding, of Lilienthal, in 1804, and it seemed clinched

when Olbers himself found a fourth in 1807. The new-comers were named

Juno and Vesta respectively.

There the case rested till 1845, when a Prussian amateur astronomer

named Hencke found another asteroid, after long searching, and opened a

new epoch of discovery. From then on the finding of asteroids became a

commonplace. Latterly, with the aid of photography, the list has been

extended to above four hundred, and as yet there seems no dearth in the

supply, though doubtless all the larger members have been revealed. Even

these are but a few hundreds of miles in diameter, while the smaller

ones are too tiny for measurement. The combined bulk of these minor

planets is believed to be but a fraction of that of the earth.

Olbers's explosion theory, long accepted by astronomers, has been

proven open to fatal objections. The minor planets are now believed to

represent a ring of cosmical matter, cast off from the solar nebula

like the rings that went to form the major planets, but prevented

from becoming aggregated into a single body by the perturbing mass of

Jupiter.

The Discovery of Neptune

As we have seen, the discovery of the first asteroid confirmed a

conjecture; the other important planetary discovery of the nineteenth

century fulfilled a prediction. Neptune was found through scientific

prophecy. No one suspected the existence of a trans-Uranian planet till

Uranus itself, by hair-breadth departures from its predicted orbit, gave

out the secret. No one saw the disturbing planet till the pencil of the

mathematician, with almost occult divination, had pointed out its place

in the heavens. The general predication of a trans-Uranian planet was

made by Bessel, the great Konigsberg astronomer, in 1840; the analysis

that revealed its exact location was undertaken, half a decade later,

by two independent workers--John Couch Adams, just graduated senior

wrangler at Cambridge, England, and U. J. J. Leverrier, the leading

French mathematician of his generation.

Adams's calculation was first begun and first completed. But it had one

radical defect--it was the work of a young and untried man. So it found

lodgment in a pigeon-hole of the desk of England's Astronomer Royal, and

an opportunity was lost which English astronomers have never ceased to

mourn. Had the search been made, an actual planet would have been seen

shining there, close to the spot where the pencil of the mathematician

had placed its hypothetical counterpart. But the search was not made,

and while the prophecy of Adams gathered dust in that regrettable

pigeon-hole, Leverrier's calculation was coming on, his tentative

results meeting full encouragement from Arago and other French savants.

At last the laborious calculations proved satisfactory, and, confident

of the result, Leverrier sent to the Berlin observatory, requesting that

search be made for the disturber of Uranus in a particular spot of the

heavens. Dr. Galle received the request September 23, 1846. That very

night he turned his telescope to the indicated region, and there, within

a single degree of the suggested spot, he saw a seeming star, invisible

to the unaided eye, which proved to be the long-sought planet,

henceforth to be known as Neptune. To the average mind, which finds

something altogether mystifying about abstract mathematics, this was a

feat savoring of the miraculous.

Stimulated by this success, Leverrier calculated an orbit for an

interior planet from perturbations of Mercury, but though prematurely

christened Vulcan, this hypothetical nursling of the sun still haunts

the realm of the undiscovered, along with certain equally hypothetical

trans-Neptunian planets whose existence has been suggested by "residual

perturbations" of Uranus, and by the movements of comets. No other

veritable additions of the sun's planetary family have been made in our

century, beyond the finding of seven small moons, which chiefly attest

the advance in telescopic powers. Of these, the tiny attendants of our

Martian neighbor, discovered by Professor Hall with the great Washington

refractor, are of greatest interest, because of their small size and

extremely rapid flight. One of them is poised only six thousand

miles from Mars, and whirls about him almost four times as fast as he

revolves, seeming thus, as viewed by the Martian, to rise in the west

and set in the east, and making the month only one-fourth as long as the

day.

The Rings of Saturn

The discovery of the inner or crape ring of Saturn, made simultaneously

in 1850 by William C. Bond, at the Harvard observatory, in America,

and the Rev. W. R. Dawes in England, was another interesting optical

achievement; but our most important advances in knowledge of Saturn's

unique system are due to the mathematician. Laplace, like his

predecessors, supposed these rings to be solid, and explained their

stability as due to certain irregularities of contour which Herschel

bad pointed out. But about 1851 Professor Peirce, of Harvard, showed

the untenability of this conclusion, proving that were the rings such as

Laplace thought them they must fall of their own weight. Then Professor

J. Clerk-Maxwell, of Cambridge, took the matter in hand, and his

analysis reduced the puzzling rings to a cloud of meteoric particles--a

"shower of brickbats"--each fragment of which circulates exactly as if

it were an independent planet, though of course perturbed and jostled

more or less by its fellows. Mutual perturbations, and the disturbing

pulls of Saturn's orthodox satellites, as investigated by Maxwell,

explain nearly all the phenomena of the rings in a manner highly

satisfactory.

After elaborate mathematical calculations covering many pages of his

paper entitled "On the Stability of Saturn's Rings," he summarizes his

deductions as follows:

"Let us now gather together the conclusions we have been able to draw

from the mathematical theory of various kinds of conceivable rings.

"We found that the stability of the motion of a solid ring depended

on so delicate an adjustment, and at the same time so unsymmetrical a

distribution of mass, that even if the exact conditions were fulfilled,

it could scarcely last long, and, if it did, the immense preponderance

of one side of the ring would be easily observed, contrary to

experience. These considerations, with others derived from the

mechanical structure of so vast a body, compel us to abandon any theory

of solid rings.

"We next examined the motion of a ring of equal satellites, and found

that if the mass of the planet is sufficient, any disturbances produced

in the arrangement of the ring will be propagated around it in the form

of waves, and will not introduce dangerous confusion. If the satellites

are unequal, the propagations of the waves will no longer be regular,

but disturbances of the ring will in this, as in the former case,

produce only waves, and not growing confusion. Supposing the ring to

consist, not of a single row of large satellites, but a cloud of evenly

distributed unconnected particles, we found that such a cloud must

have a very small density in order to be permanent, and that this is

inconsistent with its outer and inner parts moving with the same angular

velocity. Supposing the ring to be fluid and continuous, we found that

it will be necessarily broken up into small portions.

"We conclude, therefore, that the rings must consist of disconnected

particles; these must be either solid or liquid, but they must be

independent. The entire system of rings must, therefore, consist either

of a series of many concentric rings each moving with its own velocity

and having its own system of waves, or else of a confused multitude of

revolving particles not arranged in rings and continually coming into

collision with one another.

"Taking the first case, we found that in an indefinite number of

possible cases the mutual perturbations of two rings, stable in

themselves, might mount up in time to a destructive magnitude, and that

such cases must continually occur in an extensive system like that of

Saturn, the only retarding cause being the irregularity of the rings.

"The result of long-continued disturbance was found to be the

spreading-out of the rings in breadth, the outer rings pressing outward,

while the inner rings press inward.

"The final result, therefore, of the mechanical theory is that the only

system of rings which can exist is one composed of an indefinite number

of unconnected particles, revolving around the planet with different

velocities, according to their respective distances. These particles

may be arranged in series of narrow rings, or they may move through one

another irregularly. In the first case the destruction of the system

will be very slow, in the second case it will be more rapid, but there

may be a tendency towards arrangement in narrow rings which may retard

the process.

"We are not able to ascertain by observation the constitution of the two

outer divisions of the system of rings, but the inner ring is certainly

transparent, for the limb of Saturn has been observed through it. It is

also certain that though the space occupied by the ring is transparent,

it is not through the material parts of it that the limb of Saturn is

seen, for his limb was observed without distortion; which shows that

there was no refraction, and, therefore, that the rays did not pass

through a medium at all, but between the solar or liquid particles of

which the ring is composed. Here, then, we have an optical argument

in favor of the theory of independent particles as the material of

the rings. The two outer rings may be of the same nature, but not

so exceedingly rare that a ray of light can pass through their whole

thickness without encountering one of the particles.

"Finally, the two outer rings have been observed for two hundred years,

and it appears, from the careful analysis of all the observations of M.

Struve, that the second ring is broader than when first observed, and

that its inner edge is nearer the planet than formerly. The inner ring

also is suspected to be approaching the planet ever since its discovery

in 1850. These appearances seem to indicate the same slow progress of

the rings towards separation which we found to be the result of theory,

and the remark that the inner edge of the inner ring is more distinct

seems to indicate that the approach towards the planet is less rapid

near the edge, as we had reason to conjecture. As to the apparent

unchangeableness of the exterior diameter of the outer ring, we must

remember that the outer rings are certainly far more dense than the

inner one, and that a small change in the outer rings must balance a

great change in the inner one. It is possible, however, that some of the

observed changes may be due to the existence of a resisting medium.

If the changes already suspected should be confirmed by repeated

observations with the same instruments, it will be worth while to

investigate more carefully whether Saturn's rings are permanent or

transitory elements of the solar system, and whether in that part of

the heavens we see celestial immutability or terrestrial corruption

and generation, and the old order giving place to the new before our

eyes."(4)

Studies of the Moon

But perhaps the most interesting accomplishments of mathematical

astronomy--from a mundane standpoint, at any rate--are those that refer

to the earth's own satellite. That seemingly staid body was long ago

discovered to have a propensity to gain a little on the earth, appearing

at eclipses an infinitesimal moment ahead of time. Astronomers were

sorely puzzled by this act of insubordination; but at last Laplace and

Lagrange explained it as due to an oscillatory change in the earth's

orbit, thus fully exonerating the moon, and seeming to demonstrate the

absolute stability of our planetary system, which the moon's misbehavior

had appeared to threaten.

This highly satisfactory conclusion was an orthodox belief of celestial

mechanics until 1853, when Professor Adams of Neptunian fame, with whom

complex analyses were a pastime, reviewed Laplace's calculation, and

discovered an error which, when corrected, left about half the moon's

acceleration unaccounted for. This was a momentous discrepancy, which at

first no one could explain. But presently Professor Helmholtz, the great

German physicist, suggested that a key might be found in tidal friction,

which, acting as a perpetual brake on the earth's rotation, and

affecting not merely the waters but the entire substance of our planet,

must in the long sweep of time have changed its rate of rotation. Thus

the seeming acceleration of the moon might be accounted for as actual

retardation of the earth's rotation--a lengthening of the day instead of

a shortening of the month.

Again the earth was shown to be at fault, but this time the moon could

not be exonerated, while the estimated stability of our system, instead

of being re-established, was quite upset. For the tidal retardation is

not an oscillatory change which will presently correct itself, like the

orbital wobble, but a perpetual change, acting always in one direction.

Unless fully counteracted by some opposing reaction, therefore (as

it seems not to be), the effect must be cumulative, the ultimate

consequences disastrous. The exact character of these consequences was

first estimated by Professor G. H. Darwin in 1879. He showed that tidal

friction, in retarding the earth, must also push the moon out from the

parent planet on a spiral orbit. Plainly, then, the moon must formerly

have been nearer the earth than at present. At some very remote period

it must have actually touched the earth; must, in other words, have been

thrown off from the then plastic mass of the earth, as a polyp buds out

from its parent polyp. At that time the earth was spinning about in a

day of from two to four hours.

Now the day has been lengthened to twenty-four hours, and the moon has

been thrust out to a distance of a quarter-million miles; but the end is

not yet. The same progress of events must continue, till, at some remote

period in the future, the day has come to equal the month, lunar tidal

action has ceased, and one face of the earth looks out always at the

moon with that same fixed stare which even now the moon has been brought

to assume towards her parent orb. Should we choose to take even greater

liberties with the future, it may be made to appear (though some

astronomers dissent from this prediction) that, as solar tidal action

still continues, the day must finally exceed the month, and lengthen out

little by little towards coincidence with the year; and that the moon

meantime must pause in its outward flight, and come swinging back on a

descending spiral, until finally, after the lapse of untold aeons, it

ploughs and ricochets along the surface of the earth, and plunges to

catastrophic destruction.

But even though imagination pause far short of this direful culmination,

it still is clear that modern calculations, based on inexorable tidal

friction, suffice to revolutionize the views formerly current as to the

stability of the planetary system. The eighteenth-century mathematician

looked upon this system as a vast celestial machine which had been in

existence about six thousand years, and which was destined to run on

forever. The analyst of to-day computes both the past and the future of

this system in millions instead of thousands of years, yet feels well

assured that the solar system offers no contradiction to those laws of

growth and decay which seem everywhere to represent the immutable order

of nature.

COMETS AND METEORS

Until the mathematician ferreted out the secret, it surely never could

have been suspected by any one that the earth's serene attendant,

"That orbed maiden, with white fire laden,

Whom mortals call the moon,"

could be plotting injury to her parent orb. But there is another

inhabitant of the skies whose purposes have not been similarly free from

popular suspicion. Needless to say I refer to the black sheep of the

sidereal family, that "celestial vagabond" the comet.

Time out of mind these wanderers have been supposed to presage war,

famine, pestilence, perhaps the destruction of the world. And little

wonder. Here is a body which comes flashing out of boundless space into

our system, shooting out a pyrotechnic tail some hundreds of millions of

miles in length; whirling, perhaps, through the very atmosphere of the

sun at a speed of three or four hundred miles a second; then darting off

on a hyperbolic orbit that forbids it ever to return, or an elliptical

one that cannot be closed for hundreds or thousands of years; the tail

meantime pointing always away from the sun, and fading to nothingness as

the weird voyager recedes into the spatial void whence it came. Not many

times need the advent of such an apparition coincide with the outbreak

of a pestilence or the death of a Caesar to stamp the race of comets as

an ominous clan in the minds of all superstitious generations.

It is true, a hard blow was struck at the prestige of these alleged

supernatural agents when Newton proved that the great comet of 1680

obeyed Kepler's laws in its flight about the sun; and an even harder

one when the same visitant came back in 1758, obedient to Halley's

prediction, after its three-quarters of a century of voyaging but in

the abyss of space. Proved thus to bow to natural law, the celestial

messenger could no longer fully, sustain its role. But long-standing

notoriety cannot be lived down in a day, and the comet, though proved a

"natural" object, was still regarded as a very menacing one for

another hundred years or so. It remained for the nineteenth century to

completely unmask the pretender and show how egregiously our forebears

had been deceived.

The unmasking began early in the century, when Dr. Olbers, then the

highest authority on the subject, expressed the opinion that

the spectacular tail, which had all along been the comet's chief

stock-in-trade as an earth-threatener, is in reality composed of

the most filmy vapors, repelled from the cometary body by the sun,

presumably through electrical action, with a velocity comparable to that

of light. This luminous suggestion was held more or less in abeyance for

half a century. Then it was elaborated by Zollner, and particularly by

Bredichin, of the Moscow observatory, into what has since been regarded

as the most plausible of cometary theories. It is held that comets

and the sun are similarly electrified, and hence mutually repulsive.

Gravitation vastly outmatches this repulsion in the body of the comet,

but yields to it in the case of gases, because electrical force varies

with the surface, while gravitation varies only with the mass. From

study of atomic weights and estimates of the velocity of thrust of

cometary tails, Bredichin concluded that the chief components of the

various kinds of tails are hydrogen, hydrocarbons, and the vapor of

iron; and spectroscopic analysis goes far towards sustaining these

assumptions.

But, theories aside, the unsubstantialness of the comet's tail has been

put to a conclusive test. Twice during the nineteenth century the

earth has actually plunged directly through one of these threatening

appendages--in 1819, and again in 1861, once being immersed to a depth

of some three hundred thousand miles in its substance. Yet nothing

dreadful happened to us. There was a peculiar glow in the atmosphere,

so the more imaginative observers thought, and that was all. After such

fiascos the cometary train could never again pose as a world-destroyer.

But the full measure of the comet's humiliation is not yet told. The

pyrotechnic tail, composed as it is of portions of the comet's actual

substance, is tribute paid the sun, and can never be recovered. Should

the obeisance to the sun be many times repeated, the train-forming

material will be exhausted, and the comet's chiefest glory will have

departed. Such a fate has actually befallen a multitude of comets which

Jupiter and the other outlying planets have dragged into our system and

helped the sun to hold captive here. Many of these tailless comets were

known to the eighteenth-century astronomers, but no one at that time

suspected the true meaning of their condition. It was not even known how

closely some of them are enchained until the German astronomer Encke,

in 1822, showed that one which he had rediscovered, and which has

since borne his name, was moving in an orbit so contracted that it must

complete its circuit in about three and a half years. Shortly afterwards

another comet, revolving in a period of about six years, was discovered

by Biela, and given his name. Only two more of these short-period comets

were discovered during the first half of last century, but latterly they

have been shown to be a numerous family. Nearly twenty are known

which the giant Jupiter holds so close that the utmost reach of their

elliptical tether does not let them go beyond the orbit of Saturn. These

aforetime wanderers have adapted themselves wonderfully to planetary

customs, for all of them revolve in the same direction with the planets,

and in planes not wide of the ecliptic.

Checked in their proud hyperbolic sweep, made captive in a planetary

net, deprived of their trains, these quondam free-lances of the heavens

are now mere shadows of their former selves. Considered as to mere

bulk, they are very substantial shadows, their extent being measured in

hundreds of thousands of miles; but their actual mass is so slight that

they are quite at the mercy of the gravitation pulls of their captors.

And worse is in store for them. So persistently do sun and planets tug

at them that they are doomed presently to be torn into shreds.

Such a fate has already overtaken one of them, under the very eyes of

the astronomers, within the relatively short period during which these

ill-fated comets have been observed. In 1832 Biela's comet passed quite

near the earth, as astronomers measure distance, and in doing so created

a panic on our planet. It did no greater harm than that, of course, and

passed on its way as usual. The very next time it came within telescopic

hail it was seen to have broken into two fragments. Six years later

these fragments were separated by many millions of miles; and in 1852,

when the comet was due again, astronomers looked for it in vain. It had

been completely shattered.

What had become of the fragments? At that time no one positively knew.

But the question was to be answered presently. It chanced that just at

this period astronomers were paying much attention to a class of bodies

which they had hitherto somewhat neglected, the familiar shooting-stars,

or meteors. The studies of Professor Newton, of Yale, and Professor

Adams, of Cambridge, with particular reference to the great

meteor-shower of November, 1866, which Professor Newton had predicted

and shown to be recurrent at intervals of thirty-three years, showed

that meteors are not mere sporadic swarms of matter flying at random,

but exist in isolated swarms, and sweep about the sun in regular

elliptical orbits.

Presently it was shown by the Italian astronomer Schiaparelli that

one of these meteor swarms moves in the orbit of a previously observed

comet, and other coincidences of the kind were soon forthcoming. The

conviction grew that meteor swarms are really the debris of comets; and

this conviction became a practical certainty when, in November, 1872,

the earth crossed the orbit of the ill-starred Biela, and a shower of

meteors came whizzing into our atmosphere in lieu of the lost comet.

And so at last the full secret was out. The awe-inspiring comet, instead

of being the planetary body it had all along been regarded, is really

nothing more nor less than a great aggregation of meteoric particles,

which have become clustered together out in space somewhere, and which

by jostling one another or through electrical action become luminous. So

widely are the individual particles separated that the cometary body as

a whole has been estimated to be thousands of times less dense than the

earth's atmosphere at sea-level. Hence the ease with which the comet may

be dismembered and its particles strung out into streaming swarms.

So thickly is the space we traverse strewn with this cometary dust

that the earth sweeps up, according to Professor Newcomb's estimate, a

million tons of it each day. Each individual particle, perhaps no larger

than a millet seed, becomes a shooting-star, or meteor, as it burns to

vapor in the earth's upper atmosphere. And if one tiny planet sweeps

up such masses of this cosmic matter, the amount of it in the entire

stretch of our system must be beyond all estimate. What a story it tells

of the myriads of cometary victims that have fallen prey to the sun

since first he stretched his planetary net across the heavens!

THE FIXED STARS

When Biela's comet gave the inhabitants of the earth such a fright in

1832, it really did not come within fifty millions of miles of us. Even

the great comet through whose filmy tail the earth passed in 1861 was

itself fourteen millions of miles away. The ordinary mind, schooled to

measure space by the tiny stretches of a pygmy planet, cannot grasp the

import of such distances; yet these are mere units of measure compared

with the vast stretches of sidereal space. Were the comet which hurtles

past us at a speed of, say, a hundred miles a second to continue its

mad flight unchecked straight into the void of space, it must fly on its

frigid way eight thousand years before it could reach the very nearest

of our neighbor stars; and even then it would have penetrated but a

mere arm's-length into the vistas where lie the dozen or so of sidereal

residents that are next beyond. Even to the trained mind such distances

are only vaguely imaginable. Yet the astronomer of our century has

reached out across this unthinkable void and brought back many a secret

which our predecessors thought forever beyond human grasp.

A tentative assault upon this stronghold of the stars was being made

by Herschel at the beginning of the century. In 1802 that greatest of

observing astronomers announced to the Royal Society his discovery that

certain double stars had changed their relative positions towards one

another since he first carefully charted them twenty years before.

Hitherto it had been supposed that double stars were mere optical

effects. Now it became clear that some of them, at any rate, are

true "binary systems," linked together presumably by gravitation and

revolving about one another. Halley had shown, three-quarters of a

century before, that the stars have an actual or "proper" motion in

space; Herschel himself had proved that the sun shares this motion

with the other stars. Here was another shift of place, hitherto quite

unsuspected, to be reckoned with by the astronomer in fathoming sidereal

secrets.

Double Stars

When John Herschel, the only son and the worthy successor of the great

astronomer, began star-gazing in earnest, after graduating senior

wrangler at Cambridge, and making two or three tentative professional

starts in other directions to which his versatile genius impelled him,

his first extended work was the observation of his father's double

stars. His studies, in which at first he had the collaboration of Mr.

James South, brought to light scores of hitherto unrecognized pairs, and

gave fresh data for the calculation of the orbits of those longer

known. So also did the independent researches of F. G. W. Struve,

the enthusiastic observer of the famous Russian observatory at the

university of Dorpat, and subsequently at Pulkowa. Utilizing data

gathered by these observers, M. Savary, of Paris, showed, in 1827, that

the observed elliptical orbits of the double stars are explicable by

the ordinary laws of gravitation, thus confirming the assumption that

Newton's laws apply to these sidereal bodies. Henceforth there could be

no reason to doubt that the same force which holds terrestrial objects

on our globe pulls at each and every particle of matter throughout the

visible universe.

The pioneer explorers of the double stars early found that the systems

into which the stars are linked are by no means confined to single

pairs. Often three or four stars are found thus closely connected into

gravitation systems; indeed, there are all gradations between binary

systems and great clusters containing hundreds or even thousands of

members. It is known, for example, that the familiar cluster of the

Pleiades is not merely an optical grouping, as was formerly supposed,

but an actual federation of associated stars, some two thousand five

hundred in number, only a few of which are visible to the unaided eve.

And the more carefully the motions of the stars are studied, the more

evident it becomes that widely separated stars are linked together into

infinitely complex systems, as yet but little understood. At the same

time, all instrumental advances tend to resolve more and more seemingly

single stars into close pairs and minor clusters. The two Herschels

between them discovered some thousands of these close multiple systems;

Struve and others increased the list to above ten thousand; and Mr.

S. W. Burnham, of late years the most enthusiastic and successful of

double-star pursuers, added a thousand new discoveries while he was

still an amateur in astronomy, and by profession the stenographer of a

Chicago court. Clearly the actual number of multiple stars is beyond all

present estimate.

The elder Herschel's early studies of double stars were undertaken in

the hope that these objects might aid him in ascertaining the actual

distance of a star, through measurement of its annual parallax--that

is to say, of the angle which the diameter of the earth's orbit would

subtend as seen from the star. The expectation was not fulfilled. The

apparent shift of position of a star as viewed from opposite sides of

the earth's orbit, from which the parallax might be estimated, is so

extremely minute that it proved utterly inappreciable, even to the

almost preternaturally acute vision of Herschel, with the aid of any

instrumental means then at command. So the problem of star distance

allured and eluded him to the end, and he died in 1822 without seeing

it even in prospect of solution. His estimate of the minimum distance of

the nearest star, based though it was on the fallacious test of apparent

brilliancy, was a singularly sagacious one, but it was at best a

scientific guess, not a scientific measurement.

The Distance of the Stars

Just about this time, however, a great optician came to the aid of the

astronomers. Joseph Fraunhofer perfected the refracting telescope,

as Herschel had perfected the reflector, and invented a wonderfully

accurate "heliometer," or sun-measurer. With the aid of these

instruments the old and almost infinitely difficult problem of star

distance was solved. In 1838 Bessel announced from the Konigsberg

observatory that he had succeeded, after months of effort, in detecting

and measuring the parallax of a star. Similar claims had been made often

enough before, always to prove fallacious when put to further test; but

this time the announcement carried the authority of one of the greatest

astronomers of the age, and scepticism was silenced.

Nor did Bessel's achievement long await corroboration. Indeed, as so

often happens in fields of discovery, two other workers had almost

simultaneously solved the same problem--Struve at Pulkowa, where the

great Russian observatory, which so long held the palm over all others,

had now been established; and Thomas Henderson, then working at the

Cape of Good Hope, but afterwards the Astronomer Royal of Scotland.

Henderson's observations had actual precedence in point of time, but

Bessel's measurements were so much more numerous and authoritative that

he has been uniformly considered as deserving the chief credit of the

discovery, which priority of publication secured him.

By an odd chance, the star on which Henderson's observations were made,

and consequently the first star the parallax of which was ever measured,

is our nearest neighbor in sidereal space, being, indeed, some ten

billions of miles nearer than the one next beyond. Yet even this nearest

star is more than two hundred thousand times as remote from us as the

sun. The sun's light flashes to the earth in eight minutes, and to

Neptune in about three and a half hours, but it requires three and a

half years to signal Alpha Centauri. And as for the great majority of

the stars, had they been blotted out of existence before the Christian

era, we of to-day should still receive their light and seem to see them

just as we do. When we look up to the sky, we study ancient history;

we do not see the stars as they ARE, but as they WERE years, centuries,

even millennia ago.

A History of Science — Volume 3 · 第 9 / 13 章