"The past year has given to us the new [minor] planet Astraea; it has done more--it has given us the probable prospect of another.
We see it as Columbus saw America from the sh.o.r.es of Spain. Its movements have been felt trembling along the far-reaching line of our a.n.a.lysis with a certainty hardly inferior to ocular demonstration."
It was about time to begin to look for it. So the Astronomer-Royal thought on reading Leverrier"s paper. But as the national telescope at Greenwich was otherwise occupied, he wrote to Professor Challis, at Cambridge, to know if he would permit a search to be made for it with the Northumberland Equatoreal, the large telescope of Cambridge University, presented to it by one of the Dukes of Northumberland.
Professor Challis said he would conduct the search himself; and shortly commenced a leisurely and dignified series of sweeps round about the place a.s.signed by theory, cataloguing all the stars which he observed, intending afterwards to sort out his observations, compare one with another, and find out whether any one star had changed its position; because if it had it must be the planet. He thus, without giving an excessive time to the business, acc.u.mulated a host of observations, which he intended afterwards to reduce and sift at his leisure.
The wretched man thus actually saw the planet twice--on August 4th and August 12th, 1846--without knowing it. If only he had had a map of the heavens containing telescopic stars down to the tenth magnitude, and if he had compared his observations with this map as they were made, the process would have been easy, and the discovery quick. But he had no such map. Nevertheless one was in existence: it had just been completed in that country of enlightened method and industry--Germany. Dr.
Bremiker had not, indeed, completed his great work--a chart of the whole zodiac down to stars of the tenth magnitude--but portions of it were completed, and the special region where the new planet was expected happened to be among the portions already just done. But in England this was not known.
Meanwhile, Mr. Adams wrote to the Astronomer-Royal several additional communications, making improvements in his theory, and giving what he considered nearer and nearer approximations for the place of the planet.
He also now answered quite satisfactorily, but too late, the question about the radius vector sent to him months before.
Let us return to Leverrier. This great man was likewise engaged in improving his theory and in considering how best the optical search could be conducted. Actuated, probably, by the knowledge that in such matters as cataloguing and mapping Germany was then, as now, far ahead of all the other nations of the world, he wrote in September (the same September as Sir John Herschel delivered his eloquent address at Southampton) to Berlin. Leverrier wrote, I say, to Dr. Galle, head of the Observatory at Berlin, saying to him, clearly and decidedly, that the new planet was now in or close to such and such a position, and that if he would point his telescope to that part of the heavens he would see it; and, moreover, that he would be able to tell it from a star by its having a sensible magnitude, or disk, instead of being a mere point.
Galle got the letter on the 23rd of September, 1846. That same evening he did point his telescope to the place Leverrier told him, and he saw the planet that very night. He recognized it first by its appearance. To his practised eye it did seem to have a small disk, and not quite the same aspect as an ordinary star. He then consulted Bremiker"s great star chart, the part just engraved and finished, and sure enough on that chart there was no such star there. Undoubtedly it was the planet.
The news flashed over Europe at the maximum speed with which news could travel at that date (which was not very fast); and by the 1st of October Professor Challis and Mr. Adams heard it at Cambridge, and had the pleasure of knowing that they were forestalled, and that England was out of the race.
It was an unconscious race to all concerned, however. Those in France knew nothing of the search going on in England. Mr. Adams"s papers had never been published; and very annoyed the French were when a claim was set up on his behalf to a share in this magnificent discovery.
Controversies and recriminations, excuses and justifications, followed; but the discussion has now settled down. All the world honours the bright genius and mathematical skill of Mr. Adams, and recognizes that he first solved the problem by calculation. All the world, too, perceives clearly the no less eminent mathematical talents of M.
Leverrier, but it recognizes in him something more than the mere mathematician--the man of energy, decision, and character.
LECTURE XVI
COMETS AND METEORS
We have now considered the solar system in several aspects, and we have pa.s.sed in review something of what is known about the stars. We have seen how each star is itself, in all probability, the centre of another and distinct solar system, the const.i.tuents of which are too dark and far off to be visible to us; nothing visible here but the central sun alone, and that only as a twinkling speck.
But between our solar system and these other suns--between each of these suns and all the rest--there exist vast empty s.p.a.ces, apparently devoid of matter.
We have now to ask, Are these s.p.a.ces really empty? Is there really nothing in s.p.a.ce but the nebulae, the suns, their planets, and their satellites? Are all the bodies in s.p.a.ce of this gigantic size? May there not be an infinitude of small bodies as well?
The answer to this question is in the affirmative. There appears to be no special size suited to the vastness of s.p.a.ce; we find, as a matter of fact, bodies of all manner of sizes, ranging by gradations from the most tremendous suns, like Sirius, down through ordinary suns to smaller ones, then to planets of all sizes, satellites still smaller, then the asteroids, till we come to the smallest satellite of Mars, only about ten miles in diameter, and weighing only some billion tons--the smallest of the regular bodies belonging to the solar system known.
But, besides all these, there are found to occur other ma.s.ses, not much bigger and some probably smaller, and these we call comets when we see them. Below these, again, we find ma.s.ses varying from a few tons in weight down to only a few pounds or ounces, and these when we see them, which is not often, we call meteors or shooting-stars; and to the size of these meteorites there would appear to be no limit: some may be literal grains of dust. There seems to be a regular gradation of size, therefore, ranging from Sirius to dust; and apparently we must regard all s.p.a.ce as full of these cosmic particles--stray fragments, as it were, perhaps of some older world, perhaps going to help to form a new one some day. As Kepler said, there are more "comets" in the sky than fish in the sea. Not that they are at all crowded together, else they would make a cosmic haze. The transparency of s.p.a.ce shows that there must be an enormous proportion of clear s.p.a.ce between each, and they are probably much more concentrated near one of the big bodies than they are in interstellar s.p.a.ce.[30] Even during the furious hail of meteors in November 1866 it was estimated that their average distance apart in the thickest of the shower was 35 miles.
Consider the nature of a meteor or shooting-star. We ordinarily see them as a mere streak of light; sometimes they leave a luminous tail behind them; occasionally they appear as an actual fire-ball, accompanied by an explosion; sometimes, but very seldom, they are seen to drop, and may subsequently be dug up as a lump of iron or rock, showing signs of rough treatment by excoriation and heat. These last are the meteorites, or siderites, or aerolites, or bolides, of our museums. They are popularly spoken of as thunderbolts, though they have nothing whatever to do with atmospheric electricity.
[Ill.u.s.tration: FIG. 95.--Meteorite.]
They appear to be travelling rocky or metallic fragments which in their journey through s.p.a.ce are caught in the earth"s atmosphere and instantaneously ignited by the friction. Far away in the depths of s.p.a.ce one of these bodies felt the attracting power of the sun, and began moving towards him. As it approached, its speed grew gradually quicker and quicker continually, until by the time it has approached to within the distance of the earth, it whizzes past with the velocity of twenty-six miles a second. The earth is moving on its own account nineteen miles every second. If the two bodies happened to be moving in opposite directions, the combined speed would be terrific; and the faintest trace of atmosphere, miles above the earth"s surface, would exert a furious grinding action on the stone. A stream of particles would be torn off; if of iron, they would burn like a shower of filings from a firework, thus forming a trail; and the ma.s.s itself would be dissipated, shattered to fragments in an instant.
[Ill.u.s.tration: FIG. 96.--Meteor stream crossing field of telescope.]
[Ill.u.s.tration: FIG. 97.--Diagram of direction of earth"s...o...b..tal motion, showing that after midnight, _i.e._ between midnight and noon, more asteroids are likely to be swept up by any locality than between noon and midnight. [From Sir R.S. Ball.]]
Even if the earth were moving laterally, the same thing would occur. But if earth and stone happened to be moving in the same direction, there would be only the differential velocity of seven miles a second; and though this is in all conscience great enough, yet there might be a chance for a residue of the nucleus to escape entire destruction, though it would be sc.r.a.ped, heated, and superficially molten by the friction; but so much of its speed would be rubbed out of it, that on striking the earth it might bury itself only a few feet or yards in the soil, so that it could be dug out. The number of those which thus reach the earth is comparatively infinitesimal. Nearly all get ground up and dissipated by the atmosphere; and fortunate it is for us that they are so. This bombardment of the exposed face of the moon must be something terrible.[31]
Thus, then, every shooting-star we see, and all the myriads that we do not and cannot see because they occur in the day-time, all these bright flashes or streaks, represent the death and burial of one of these flying stones. It had been careering on its own account through s.p.a.ce for untold ages, till it meets a planet. It cannot strike the actual body of the planet--the atmosphere is a sufficient screen; the tremendous friction reduces it to dust in an instant, and this dust then quietly and leisurely settles down on to the surface.
Evidence of the settlement of meteoric dust is not easy to obtain in such a place as England, where the dust which acc.u.mulates is seldom of a celestial character; but on the snow-fields of Greenland or the Himalayas dust can be found; and by a Committee of the British a.s.sociation distinct evidence of molten globules of iron and other materials appropriate to aerolites has been obtained, by the simple process of collecting, melting, and filtering long exposed snow.
Volcanic ash may be mingled with it, but under the microscope the volcanic and the meteoric const.i.tuents have each a distinctive character.
The quant.i.ty of meteoric material which reaches the earth as dust must be immensely in excess of the minute quant.i.ty which arrives in the form of lumps. Hundreds or thousands of tons per annum must be received; and the accretion must, one would think, in the course of ages be able to exert some influence on the period of the earth"s rotation--the length of the day. It is too small, however, to have been yet certainly detected. Possibly, it is altogether negligible.
It has been suggested that those stones which actually fall are not the true cosmic wanderers, but are merely fragments of our own earth, cast up by powerful volcanoes long ago when the igneous power of the earth was more vigorous than now--cast up with a speed of close upon seven miles a second; and now in these quiet times gradually being swept up by the earth, and so returning whence they came.
I confess I am unable to draw a clear distinction between one set and the other. Some falling stars may have had an origin of this sort, but certainly others have not; and it would seem very unlikely that one set only should fall bodily upon the earth, while the others should always be rubbed to powder. Still, it is a possibility to be borne in mind.
We have spoken of these cosmic visitors as wandering ma.s.ses of stone or iron; but we should be wrong if we a.s.sociated with the term "wandering"
any ideas of lawlessness and irregularity of path. These small lumps of matter are as obedient to the law of gravity as any large ones can be.
They must all, therefore, have definite orbits, and these orbits will have reference to the main attracting power of our system--they will, in fact, be nearly all careering round the sun.
Each planet may, in truth, have a certain following of its own. Within the limited sphere of the earth"s predominant attraction, for instance, extending some way beyond the moon, we may have a number of satellites that we never see, all revolving regularly in elliptic orbits round the earth. But, comparatively speaking, these satellite meteorites are few.
The great bulk of them will be of a planetary character--they will be attendant upon the sun.
It may seem strange that such minute bodies should have regular orbits and obey Kepler"s laws, but they must. All three laws must be as rigorously obeyed by them as by the planets themselves. There is nothing in the smallness of a particle to excuse it from implicit obedience to law. The only consequence of their smallness is their inability to perturb others. They cannot appreciably perturb either the planets they approach or each other. The attracting power of a lump one million tons in weight is very minute. A pound, on the surface of such a body of the same density as the earth, would be only pulled to it with a force equal to that with which the earth pulls a grain. So the perturbing power of such a ma.s.s on distant bodies is imperceptible. It is a good thing it is so: accurate astronomy would be impossible if we had to take into account the perturbations caused by a crowd of invisible bodies.
Astronomy would then approach in complexity some of the problems of physics.
But though we may be convinced from the facts of gravitation that these meteoric stones, and all other bodies flying through s.p.a.ce near our solar system, must be constrained by the sun to obey Kepler"s laws, and fly round it in some regular elliptic or hyperbolic orbit, what chance have we of determining that orbit? At first sight, a very poor chance, for we never see them except for the instant when they splash into our atmosphere; and for them that instant is instant death. It is unlikely that any escape that ordeal, and even if they do, their career and orbit are effectually changed. Henceforward they must become attendants on the earth. They may drop on to its surface, or they may duck out of our atmosphere again, and revolve round us unseen in the clear s.p.a.ce between earth and moon.
Nevertheless, although the problem of determining the original orbit of any given set of shooting-stars before it struck us would seem nearly insoluble, it has been solved, and solved with some approach to accuracy; being done by the help of observations of certain other bodies. The bodies by whose help this difficult problem has been attacked and resolved are comets. What are comets?
I must tell you that the scientific world is not entirely and completely decided on the structure of comets. There are many floating ideas on the subject, and some certain knowledge. But the subject is still, in many respects, an open one, and the ideas I propose to advocate you will accept for no more than they are worth, viz. as worthy to be compared with other and different views.
Up to the time of Newton, the nature of comets was entirely unknown.
They were regarded with superst.i.tious awe as fiery portents, and were supposed to be connected with the death of some king, or with some national catastrophe.
Even so late as the first edition of the _Principia_ the problem of comets was unsolved, and their theory is not given; but between the first and the second editions a large comet appeared, in 1680, and Newton speculated on its appearance and behaviour. It rushed down very close to the sun, spun half round him very quickly, and then receded from him again. If it were a material substance, to which the law of gravitation applied, it must be moving in a conic section with the sun in one focus, and its radius vector must sweep out equal areas in equal times. Examining the record of its positions made at observatories, he found its observed path quite accordant with theory; and the motion of comets was from that time understood. Up to that time no one had attempted to calculate an orbit for a comet. They had been thought irregular and lawless bodies. Now they were recognized as perfectly obedient to the law of gravitation, and revolving round the sun like everything else--as members, in fact, of our solar system, though not necessarily permanent members.
But the orbit of a comet is very different from a planetary one. The excentricity of its...o...b..t is enormous--in other words, it is either a very elongated ellipse or a parabola. The comet of 1680, Newton found to move in an orbit so nearly a parabola that the time of describing it must be reckoned in hundreds of years at the least. It is now thought possible that it may not be quite a parabola, but an ellipse so elongated that it will not return till 2255. Until that date arrives, however, uncertainty will prevail as to whether it is a periodic comet, or one of those that only visit our system once. If it be periodic, as suspected, it is the same as appeared when Julius Caesar was killed, and which likewise appeared in the years 531 and 1106 A.D. Should it appear in 2255, our posterity will probably regard it as a memorial of Newton.
[Ill.u.s.tration: FIG. 98.--Parabolic and elliptic orbits. The _a b_ (visible) portions are indistinguishable.]
The next comet discussed in the light of the theory of gravitation was the famous one of Halley. You know something of the history of this.
Its period is 75-1/2 years. Halley saw it in 1682, and predicted its return in 1758 or 1759--the first cometary prediction. Clairaut calculated its return right within a month (p. 219). It has been back once more, in 1835; and this time its date was correctly predicted within three days, because Ura.n.u.s was now known. It was away at its furthest point in 1873. It will be back again in 1911.
[Ill.u.s.tration: FIG. 99.--Orbit of Halley"s comet.]
Coming to recent times, we have the great comets of 1843 and of 1858, the history of neither being known. Quite possibly they arrived then for the first time. Possibly the second will appear again in 3808. But besides these great comets, there are a mult.i.tude of telescopic ones, which do not show these striking features, and have no gigantic tail.
Some have no tail at all, others have at best a few insignificant streamers, and others show a faint haze looking like a microscopic nebula.
All these comets are of considerable extent--some millions of miles thick usually, and yet stars are clearly visible through them. Hence they must be matter of very small density; their tails can be nothing more dense than a filmy mist, but their nucleus must be something more solid and substantial.
[Ill.u.s.tration: FIG. 100.--Various appearances of Halley"s comet when last seen.]