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-The Project Gutenberg EBook of Comets and Meteors, by Daniel Kirkwood
-
-This eBook is for the use of anyone anywhere at no cost and with
-almost no restrictions whatsoever. You may copy it, give it away or
-re-use it under the terms of the Project Gutenberg License included
-with this eBook or online at www.gutenberg.org
-
-
-Title: Comets and Meteors
- Their phenomena in all ages; their mutual relations; and
- the theory of their origin.
-
-Author: Daniel Kirkwood
-
-Release Date: December 11, 2012 [EBook #41606]
-
-Language: English
-
-Character set encoding: ASCII
-
-*** START OF THIS PROJECT GUTENBERG EBOOK COMETS AND METEORS ***
-
-
-
-
-Produced by sp1nd and the Online Distributed Proofreading
-Team at http://www.pgdp.net (This file was produced from
-images generously made available by The Internet Archive)
-
-
-
-
-
-
-
-
-
- [Illustration: Fig. 1. THE SOLAR SYSTEM.
- _Frontispiece._]
-
-
-
-
- COMETS AND METEORS:
-
- THEIR PHENOMENA IN ALL AGES;
- THEIR MUTUAL RELATIONS;
- AND THE
- THEORY OF THEIR ORIGIN.
-
-
- BY
- DANIEL KIRKWOOD, LL.D.,
-
- PROFESSOR OF MATHEMATICS IN INDIANA UNIVERSITY,
- AND AUTHOR OF "METEORIC ASTRONOMY."
-
-
- [Illustration]
-
-
- PHILADELPHIA:
- J. B. LIPPINCOTT & CO.
- 1873.
-
-
-
-
- Entered according to Act of Congress, in the year 1873, by
- DANIEL KIRKWOOD, LL.D.,
- In the Office of the Librarian of Congress at Washington.
-
-
-
-
-PREFACE.
-
-
-The origin of meteoric astronomy, as a science, dates from the memorable
-star-shower of 1833. Soon after that brilliant display it was found that
-similar phenomena had been witnessed, at nearly regular intervals, in
-former times. This discovery led at once to another no less important,
-viz.: that the nebulous masses from which such showers are derived
-revolve about the sun in paths intersecting the earth's orbit. The
-theory that these meteor-clouds are but the scattered fragments of
-disintegrated comets was announced by several astronomers in 1867:--a
-theory confirmed in a remarkable manner by the shower of meteors from
-the _debris_ of Biela's comet on the 27th of November, 1872.
-
-To gratify the interest awakened in the public mind by the discoveries
-here named, is the main design of the following work. Among the subjects
-considered are, cometary astronomy; aerolites, with the phenomena
-attending their fall; the most brilliant star-showers of all ages; and
-the origin of comets, aerolites, and falling stars.
-
-It may be proper to remark that the language used by the writer in a
-volume[1] published several years since, and now nearly out of print,
-has been occasionally adopted in the following treatise.
-
-BLOOMINGTON, INDIANA, April, 1873.
-
- [1] Meteoric Astronomy.
-
-
-
-
-CONTENTS.
-
-
- PAGE.
- PREFACE 3
-
- CHAPTER I.
- A GENERAL VIEW OF THE SOLAR SYSTEM 9
-
- CHAPTER II.
- COMETS 13
- COMETS VISIBLE IN THE DAY-TIME 15
- PERIODIC COMETS 18
-
- CHAPTER III.
- COMETS WHOSE ELEMENTS INDICATE PERIODICITY, BUT
- WHOSE RETURNS HAVE NOT BEEN RECOGNIZED 31
-
- CHAPTER IV.
- OTHER REMARKABLE COMETS 39
-
- CHAPTER V.
- THE POSITION AND ARRANGEMENT OF COMETARY ORBITS 43
-
- CHAPTER VI.
- THE DISINTEGRATION OF COMETS 49
-
- CHAPTER VII.
- METEORIC STONES 57
-
- CHAPTER VIII.
- SHOOTING-STARS--METEORS OF NOVEMBER 14 69
-
- CHAPTER IX.
- OTHER METEORIC STREAMS 82
-
- CHAPTER X.
- THE ORIGIN OF COMETS AND METEORS 94
-
-
-
-
-I.
-
-COMETS.
-
-
-
-
-COMETS AND METEORS.
-
-
-
-
-CHAPTER I.
-
-A GENERAL VIEW OF THE SOLAR SYSTEM.
-
-
-A descriptive treatise on COMETS and METEORS may properly be preceded by
-a brief general view of the _planetary_ system to which these bodies are
-related, and by which their motions, in direction and extent, are
-largely influenced.
-
-THE SOLAR SYSTEM consists of the sun, together with the planets, comets,
-and meteors which revolve around it as the centre of their motions. The
-sun is the great controlling orb of this system, and the source of light
-and heat to its various members. Its magnitude is one million three
-hundred thousand times greater than that of the earth, and it contains
-more than seven hundred times as much matter as all the planets put
-together.
-
-Mercury is the nearest planet to the sun; its mean distance being about
-35,400,000 miles. Its diameter is 3000 miles, and it completes its
-orbital revolution in 88 days.
-
-Venus, the next member of the system, is sometimes our morning and
-sometimes our evening star. Its magnitude is almost exactly the same as
-that of the earth. It revolves round the sun in 225 days.
-
-The earth is the third planet from the sun in the order of distance; the
-radius of its orbit being about 92,000,000 miles. It is attended by one
-satellite,--the moon,--the diameter of which is 2160 miles.
-
-Mars is the first planet exterior to the earth's orbit. It is
-considerably smaller than the earth, and has no satellite. It revolves
-round the sun in 687 days.
-
-_The Asteroids._--Since the commencement of the present century a
-remarkable zone of telescopic planets has been discovered immediately
-exterior to the orbit of Mars. These bodies are extremely small; some of
-them probably containing less matter than the largest mountains on the
-earth's surface. 131 members of the group are known at present, and the
-number is annually increasing.
-
-Jupiter, the first planet exterior to the asteroids, is nearly
-500,000,000 miles from the sun, and revolves round it in a little less
-than 12 years. This planet is 86,000 miles in diameter, and contains
-more than twice as much matter as all the other planets, primary and
-secondary, put together. Jupiter is attended by four moons or
-satellites.
-
-Saturn is the sixth of the principal planets in the order of distance.
-Its orbit is about 400,000,000 miles beyond that of Jupiter. This planet
-is attended by eight satellites, and is surrounded by three broad flat
-rings. Saturn is 73,000 miles in diameter, and its mass or quantity of
-matter is more than that of all the other planets except Jupiter.
-
-Uranus is at double the distance of Saturn, or nineteen times that of
-the earth. Its diameter is about 34,000 miles, and its period of
-revolution 84 years. It is attended by at least four satellites.
-
-Neptune is the most remote known member of the system; its distance
-being 2,800,000,000 miles. It is somewhat larger than Uranus; has
-certainly one satellite, and probably several more. Its period is about
-165 years. A cannon-ball flying outward from the sun at the uniform
-velocity of 500 miles per hour would not reach the orbit of Neptune in
-less than 639 years.
-
-These planets all move round the sun in the same direction,--from west
-to east. Their motions are nearly circular, and also nearly in the same
-plane. Their orbits, except that of Neptune, are represented in the
-frontispiece. It is proper to remark, however, that all representations
-of the solar system by maps and planetariums must give an exceedingly
-erroneous view either of the magnitudes or distances of its various
-members. If the earth, for instance, be denoted by a ball half an inch
-in diameter, the diameter of the sun, according to the same scale
-(16,000 miles to the inch), will be between four and five feet; that of
-the earth's orbit, about 1000 feet; while that of Neptune's orbit will
-be nearly six miles. To give an accurate representation of the solar
-system at a single view is therefore plainly impracticable.
-
-THE ZODIACAL LIGHT.--This term was first applied by Dominic Cassini, in
-1683, to a faint nebulous aurora, somewhat resembling the milky way,
-apparently of a conical or lenticular form, having its base toward the
-sun and its axis nearly in the direction of the ecliptic. The most
-favorable time for observing it is when its axis is most nearly
-perpendicular to the horizon. This, in our latitudes, occurs in March,
-for the evening, and in October, for the morning. The angular distance
-of its vertex from the sun is frequently seventy or eighty degrees,
-while sometimes, though rarely (except within the tropics), it exceeds
-even one hundred degrees. It was noticed in the latter part of the 16th
-century by Tycho Brahe. The first accurate description of the phenomenon
-was given, however, by Cassini. This astronomer supposed the appearance
-to be produced by the blended light of innumerable bodies too small to
-be separately observed,--a theory still very generally accepted. In
-other words, the zodiacal light is probably a swarm of infinitesimal
-planets; the greater part of the cluster being interior to Mercury's
-orbit.
-
-The distances between the different members of our planetary system,
-vast as they may seem, sink into insignificance when compared with the
-intervals which separate us from the so-called fixed stars. _Alpha
-Centauri_, the nearest of those twinkling luminaries, is 7000 times more
-distant than Neptune from the sun. Even light itself, which moves
-185,000 miles in a second, is more than three years in traversing the
-mighty interval.
-
-
-
-
-CHAPTER II.
-
-COMETS.
-
-
-The term _comet_--which signifies literally a _hairy star_--may be
-applied to all bodies that revolve about the sun in very eccentric
-orbits. The sudden appearance, vast dimensions, and extraordinary aspect
-of these celestial wanderers, together with their rapid and continually
-varying motions, have never failed to excite the attention and wonder of
-all observers. Nor is it surprising that in former times, when the
-nature of their orbits was wholly unknown, they should have been looked
-upon as omens of impending evil, or messengers of an angry Deity. Even
-now, although modern science has reduced their motions to the domain of
-law, determined approximately their orbits, and assigned in a number of
-instances their periods, the interest awakened by their appearance is in
-some respects still unabated.
-
-The special points of dissimilarity between planets and comets are the
-following:--The former are dense, and, so far as we know, solid bodies;
-the latter are many thousand times rarer than the earth's atmosphere.
-The planets _all_ move from west to east; many comets revolve in the
-opposite direction. The planetary orbits are but slightly inclined to
-the plane of the ecliptic; those of comets may have any inclination
-whatever. The planets are observed in all parts of their orbits;
-comets, only in those parts nearest the sun.
-
-The larger comets are attended by a _tail_, or train of varying
-dimensions, extending generally in a direction opposite to that of the
-sun. The more condensed part, from which the tail proceeds, is called
-the _nucleus_; and the nebulous envelope immediately surrounding the
-nucleus is sometimes termed the _coma_. These different parts are seen
-in Fig. 2, which represents the great comet of 1811.
-
-[Illustration: Fig. 2. THE GREAT COMET OF 1811.]
-
-Zeno, Democritus, and other Greek philosophers held that comets were
-produced by the collection of several stars into clusters. Aristotle
-taught that they were formed by exhalations, which, rising from the
-earth's surface, ignited in the upper regions of the atmosphere. This
-hypothesis, through the great influence of its author, was generally
-received for almost two thousand years. Juster views, however, were
-entertained by the celebrated Seneca, who maintained that comets ought
-to be ranked among the permanent works of nature, and that their
-disappearance was not an extinction, but simply a passing beyond the
-reach of our vision. The observations of Tycho Brahe first established
-the fact that comets move through the planetary spaces far beyond the
-limits of our atmosphere. The illustrious Dane, however, supposed them
-to move in circular orbits. Kepler, on the other hand, was no less in
-error in considering their paths to be rectilinear. James Bernoulli
-supposed comets to be the satellites of a very remote planet, invisible
-on account of its great distance,--such satellites being seen only in
-the parts of their orbits nearest the earth. Still more extravagant
-was the hypothesis of Descartes, who held that they were originally
-fixed stars, which, having gradually lost their light, could no longer
-retain their positions, but were involved in the vortices of the
-neighboring stars, when such as were thus brought within the sphere of
-the sun's illuminating power again became visible.
-
-
-_Comets visible in the daytime._
-
-Comets of extraordinary brilliancy have sometimes been seen during the
-daytime. At least thirteen authentic instances of this phenomenon have
-been recorded in history. The first was the comet which appeared about
-the year 43 B.C., just after the assassination of Julius Caesar. The
-Romans called it the _Julium Sidus_, and regarded it as a celestial
-chariot sent to convey the soul of Caesar to the skies. It was seen two
-or three hours before sunset, and continued visible for eight successive
-days. The great comet of 1106, described as an object of terrific
-splendor, was seen simultaneously with the sun, and in close proximity
-to it. Dr. Halley supposed this and the Julian comet to have been
-previous visits of the great comet of 1680. In the year 1402 two comets
-appeared,--one about the middle of February, the other in June,--both of
-which were visible while the sun was above the horizon. One was of such
-magnitude and brilliancy that the nucleus and even the tail could be
-seen at midday. The comet of 1472, one of the most splendid recorded in
-history, was visible in full daylight, when nearest the earth, on the
-21st of January. This comet, according to Laugier, moves very nearly in
-the plane of the ecliptic, its inclination being less than two degrees.
-Its least distance from our globe was only 3,300,000 miles. The comet of
-1532, supposed by some to be identical with that of 1661, was also
-visible in full sunshine. The apparent magnitude of its nucleus was
-three times greater than that of Jupiter. The comet of 1577 was seen
-with the naked eye by Tycho Brahe before sunset. It was by observations
-on this body that Aristotle's doctrine in regard to the origin, nature,
-and distance of comets was proved to be erroneous. It was simultaneously
-observed by Tycho at Oranienberg, and Thaddeus Hagecius at Prague; the
-points of observation being more than 400 miles apart, and nearly on the
-same meridian. The comet was found to have no sensible diurnal parallax;
-in other words, its apparent place in the heavens was the same to each
-observer, which could not have been the case had the comet been less
-distant than the moon. The comet which passed its perihelion on the 8th
-of November, 1618, was distinctly seen by Marsilius when the sun was
-above the horizon. The great comet of 1744 was seen without the aid of a
-glass at one o'clock in the afternoon,--only five hours after its
-perihelion passage. The diameter of this body was nearly equal to that
-of Jupiter. It had _six_ tails, the greatest length of which was about
-30,000,000 miles, or nearly one-third of the distance of the earth from
-the sun. The spaces between the tails were as dark as the rest of the
-heavens, while the tails themselves were bordered with a luminous edging
-of great beauty.
-
-The great comet of 1843 was distinctly visible to the naked eye, at
-noon, on the 28th of February. It appeared as a brilliant body, within
-less than two degrees from the sun. This comet passed its perihelion on
-the 27th of February, at which time its distance from the sun's surface
-was only about one-fourth of the moon's distance from the earth. This is
-the nearest approach to the sun ever made by any known comet. The
-velocity of the body in perihelion was about 1,280,000 miles an hour, or
-nearly nineteen times that of the earth in its orbit. The apparent
-length of its tail was sixty-five degrees, and its true length
-150,000,000 miles. The first comet of 1847, discovered by Mr. Hind, was
-also seen near the sun on the day of its perihelion passage. That
-discovered by Klinkerfues on the 10th of June, 1853, and which passed
-its perihelion on the 1st of September, was seen at Olmutz in the
-daytime, August 31, when only twelve degrees from the sun. After passing
-its perihelion, it was again observed, _at noon_, on the 2d, 3d, and 4th
-of September. Finally, the great comet of 1861 was seen before sunset,
-on Monday evening, July 1, by Rev. Henry W. Ballantine, of Bloomington,
-Indiana. It was again detected on the following evening just as the sun
-was in the horizon.
-
-Besides the thirteen comets which we have enumerated, at least four
-others have been seen in the daytime; all, however, under peculiar
-circumstances. Seneca relates that during a great solar eclipse, 63
-years before our era, a large comet was observed not far from the sun.
-"Philostorgius says that on the 19th of July, A.D. 418, when the sun
-was eclipsed and stars were visible, a great comet, in the form of a
-cone, was discovered near that luminary, and was afterwards observed
-during the nights."[2] The comet which passed its perihelion on the 18th
-of November, 1826, was observed by both Gambart and Flaugergues to
-transit the solar disk,--the least distance of the nucleus from the
-sun's surface being about 2,000,000 miles. The second comet of 1819 and
-the comet of 1823 are both known in like manner to have passed between
-the sun and the earth. Unfortunately, however, the transits were not
-observed.
-
- [2] Hind.
-
-A few cometary orbits are hyperbolas, more ellipses, and a still greater
-number parabolas. Comets moving in ellipses remain permanently within
-the limits of solar influence. Others, however, visit our system but
-once, and then pass off to wander indefinitely in the sidereal spaces.
-
-
-_Comets of known periodicity._
-
-I. Halley's Comet.
-
-As comets are subject to great changes of appearance, one can never be
-identified by any description of its magnitude, brilliancy, etc., at the
-time of a previous return. This can be done only by a comparison of
-orbits. If, for example, we find the elements of an orbit very nearly
-corresponding in every particular with those of a former comet, there is
-a degree of probability, amounting almost to certainty, that the two
-are identical. Sir Isaac Newton, in his _Principia_, published shortly
-after the appearance of the comet of 1682, explained how the periods of
-those mysterious visitors might thus be ascertained, thus directing the
-attention of astronomers to the subject. Dr. Halley soon after undertook
-a thorough discussion of all the recorded cometary observations within
-his reach. In the course of his investigations he discovered that the
-path of the comet observed by Kepler in 1607 coincided almost exactly
-with that of the one which passed its perihelion in 1682. Hence he
-concluded that they were the same. He found also that the comet of 1531,
-whose course had been particularly observed by Apian, moved in the same
-path. The interval between the consecutive appearances being nearly 76
-years, Halley announced this as the time of the comet's revolution, and
-boldly predicted its return in 1758 or 1759. The law of universal
-gravitation had at this time just been discovered and announced. But
-although its application to the determination of planetary and cometary
-perturbations had not been developed, Halley was well aware that the
-attractive influence of Jupiter and Saturn might accelerate or retard
-the motion of the comet, so as to produce a considerable variation in
-its period. During the interval from 1682 to 1759, the application of
-the higher mathematics to problems in physical astronomy had been
-studied with eminent success. The disturbing effect of the two large
-planets, Jupiter and Saturn, was computed with almost incredible labor
-by Clairaut, Lalande, and Madame Lepaute. The result as announced by
-Clairaut to the Academy of Sciences in November, 1758, was that the
-period must be 618 days longer than that immediately preceding, and that
-the comet accordingly would pass its perihelion about the 13th of April,
-1759. It was stated, however, that, being pressed for want of time, they
-had neglected certain quantities which might somewhat affect the result.
-The comet, in fact, passed its perihelion in March, within less than a
-month of the predicted time. When it is considered that the attraction
-of the earth was not taken into the account, and that Uranus, whose
-influence must have been sensible, had not then been discovered, this
-must certainly be regarded as a remarkable approximation.
-
-But during the next interval of 76 years the theory of planetary
-perturbations had been more perfectly developed. The masses of Jupiter
-and Saturn had been determined with greater accuracy, and Uranus had
-been added to the known members of the planetary system. A nearer
-approximation to the exact time of the comet's perihelion passage in
-1835 was therefore to be expected. Prizes were offered by two of the
-learned societies of Europe--the Academy of Sciences at Turin, and the
-French Institute--for the most perfect discussion of its motions. That
-of the former was awarded to Damoiseau,--that of the latter to
-Pontecoulant. The times assigned by these distinguished mathematicians
-for the comet's perihelion passage were very nearly the same, and
-differed but a few days from the true time. Had the present received
-mass of Jupiter been used in the calculations, Pontecoulant, it is
-believed, would not have been in error as much as 24 hours. It may be
-proper to remark that, during the entire period from 1759 to 1835, the
-position of Neptune was such that it could produce no considerable
-effect on the motion of the comet.
-
-This interesting object will again return about 1911.
-
-The visit of 1531 was the earliest that Halley succeeded in determining
-with any degree of certainty. Peter Apian, by whom it was at that time
-observed, was the first European to ascertain the fact that, as a
-general thing, the tails of comets are turned from the sun.[3] To
-confirm this discovery, he carefully followed the body in its progress
-through the constellations. By means of his recorded observations Halley
-was enabled to identify this comet with that of 1607 and 1682. The great
-comet of 1456 he _conjectured_ to be the same, from the date of its
-appearance. Pingre subsequently confirmed this suspicion by a careful
-examination of the few trustworthy records that could be collected from
-the writers of that period.
-
- [3] The Chinese, however, as appears from Biot's researches, had
- observed the same fact 700 years earlier. See Humboldt's Cosmos,
- vol. iv. (Bohn's ed.), p. 544.
-
-From the earlier descriptions of this comet we infer that its brilliancy
-is gradually diminishing. In 1456 its tail, which was slightly curved
-like a sword or sabre, extended two-thirds of the distance from the
-horizon to the zenith. The appearance of such an object, in a grossly
-superstitious age, excited throughout Europe the utmost consternation.
-The Moslems had just taken Constantinople, and were threatening to
-advance westward into Europe. Pope Calixtus III., regarding the comet as
-confederate with the Turk, ordered prayers to be offered three times a
-day for deliverance from both. The alarm, however, was of short
-duration. Within ten days of its appearance the comet reached its
-perihelion. Receding from the sun, the sword-like form began to diminish
-in brilliancy and extent; and finally, to the great relief of Europe, it
-entirely disappeared.
-
-The perihelion passage of 1456 was, until recently, the earliest known.
-It was shown by Laugier, however, in 1843, that among the notices of
-comets extracted by Edward Biot from the Chinese records, were
-observations of a body in 1378, which was undoubtedly the comet of
-Halley. Further researches among these annals enabled the same
-astronomer to recognize two ancient returns, one in 760, the other in
-451. Still more recently the distinguished English astronomer, Mr. Hind,
-has traced back the returns to the year 11 B.C. He remarks, however,
-that previous to that epoch, "the Chinese descriptions of comets are too
-vague to aid us in tracing any more ancient appearances," and that
-"European writers of these remote times render us no assistance." Let us
-now inquire whether the comet had probably made any former approach to
-the sun in an orbit nearly identical with the present. It is well known
-that the modern period of this body is considerably less than the
-ancient. Thus, the mean period since A.D. 1456 has been 75.88 years;
-while from 11 B.C. to 1456 A.D. it was 77.27 years. In determining the
-approximate dates of former returns, the ancient period should evidently
-be employed. Now, it is a remarkable fact that of more than 70
-comets,[4] or objects supposed to be comets, whose appearance was
-recorded during the six centuries immediately preceding the year 11
-B.C., but one--that of 166 B.C.--was observed at a date corresponding
-nearly to that of a former return of Halley's comet. Of this object it
-is merely recorded that "a torch was seen in the heavens." Whether this
-was a comet or some other phenomenon, it is impossible to determine. But
-as the comet of Halley was more brilliant in ancient than in modern
-times, it seems highly improbable that seven _consecutive_ returns of so
-conspicuous an object should have been unrecorded, especially as twelve
-comets per century[5] were observed during the same period. It would
-appear, therefore, that the perihelion passage of 11 B.C. was in fact
-the first ever made by the comet, or at least the first in an orbit
-nearly the same as the present.
-
- [4] See the Catalogues of Chambers and Williams.
-
- [5] The average number.
-
-The motion of Halley's comet is retrograde. The point of its nearest
-approach to the sun is situated within the orbit of Venus. Its greatest
-distance from the centre of the system is nearly twice that of Uranus,
-or 36 times that of the earth. The comet is, consequently, subject to
-great changes of temperature. When nearest the sun its light and heat
-are almost four times greater than the earth's; when most remote, they
-are 1200 times less. In the former position, the sun would appear much
-larger than to us; in the latter, his apparent diameter would not
-greatly exceed that of Jupiter, as viewed from the earth. It would be
-difficult to conjecture what the consequences might be, were our planet
-transported to either of these extremes of the cometary path. In the
-perihelion, the waters of the ocean would undoubtedly be reduced to a
-state of vapor; in the aphelion, they would be solidified by
-congelation.
-
-
-II. Encke's Comet.
-
-It was formerly supposed that all comets have their aphelia far beyond
-the limits of the planetary system. In 1818, however, a small comet was
-discovered by Pons, the orbit of which was subsequently found to be
-wholly interior to that of Jupiter. Its elements were presented by
-Bouvard, in 1819, to the Board of Longitude at Paris. The form and
-position of the orbit were immediately found to correspond with those of
-a comet observed by several astronomers in 1805. The different
-appearances were consequently regarded as returns of the same body. Its
-elliptic orbit was calculated by Encke, who found its period to be only
-about three years and four months. Its perihelion is within the orbit of
-Mercury; its aphelion, between the asteroids and the orbit of Jupiter.
-
-Encke's comet is invisible to the naked eye, except in very favorable
-circumstances; it has no tail; its motion, like that of the planets, is
-from west to east; and its orbit is inclined about 13 deg. to the ecliptic.
-
-A comparison of the successive periods of this interesting object has
-led to the discovery that its time of revolution is gradually
-diminishing; a fact regarded by Encke and other astronomers as
-indicating the existence of an ethereal medium.
-
-
-III. Biela's Comet.
-
-The discovery of Encke's comet of short period was followed, in 1826, by
-that of another, whose revolution is completed in about six years and
-eight months. It was observed on the 27th of February, by M. Biela, an
-Austrian officer; accordingly it has since been known as _Biela's
-comet_. On computing its elements and comparing them with those of
-former comets, it was found to have been observed in 1772 and 1805.
-Damoiseau having calculated the dimensions of the comet's elliptic path
-and the time of its return, announced as the result of his computations
-the remarkable fact that the orbits of the earth and comet intersect
-each other, and that the comet would cross the earth's path on the 29th
-of October, 1832. This produced no little alarm among the uneducated,
-especially in France. Even some journalists are said to have predicted
-the destruction of our globe by a collision with the comet. When the
-latter, however, passed the point of intersection at the predicted time,
-the earth was at a distance of 50,000,000 miles.
-
-At the return of 1845-6, Biela's comet exhibited a most remarkable
-appearance. Instead of a single comet, it appeared as two distinct
-bodies moving together side by side, at a distance from each other
-somewhat less than that of the moon from the earth. Astronomers,
-anxious to determine whether the cometary fragments had continued
-separate during an entire revolution, awaited the next return with no
-ordinary interest. The _two_ bodies appeared at the predicted time
-(September, 1852); their distance apart having increased to 1,250,000
-miles. In 1859 the comet, on account of its proximity to the sun,
-entirely escaped detection. At the return in 1865-6 the position of the
-object was quite favorable for observation, yet the search of
-astronomers was again unsuccessful. In 1872 the body escaped detection
-both in Europe and America. One fragment was seen, however, at Madras,
-India, on the mornings of the 2d and 3d of December,--several weeks
-after its perihelion passage. The comet's non-appearance in 1866 and its
-greatly diminished magnitude in 1872 leave no room to doubt its
-progressive dissolution. This subject will again be referred to in
-discussing the phenomena of meteoric showers.
-
-
-IV. Faye's Comet.
-
-On the 22d of November, 1843, M. Faye, of the Paris Observatory,
-discovered a comet, which was shown by Dr. Goldschmidt to revolve in an
-elliptic orbit, the perihelion of which is exterior to the orbit of
-Mars, and the aphelion immediately beyond that of Jupiter. The
-eccentricity is, therefore, less than that of any other comet previously
-discovered. Its period is about 7 years and 5 months.
-
-It is possible that a comet moving in a parabola or hyperbola, with the
-sun in the focus, may be thrown into an elliptic orbit by the disturbing
-influence of Jupiter or one of the other large planets. The celebrated
-Leverrier undertook to determine whether the comet of Faye had in this
-manner been recently fixed as a permanent member of the solar system. He
-found that it could not have been so introduced since 1747, and,
-consequently, that it must have completed at least thirteen revolutions
-before its discovery.
-
-This comet has been observed at each return from 1843 to the present
-time.
-
-
-V. De Vico's Comet.
-
-On the 22d of August, 1844, De Vico, of Rome, discovered a comet whose
-orbit is included between those of the earth and Jupiter. Its period is
-1996 days, or about 5-1/2 years. This body, from some cause,--perhaps a
-gradual dissolution,--has not been observed at any subsequent return.
-
-
-VI. Brorsen's Comet.
-
-On the 26th of February, 1846, Mr. Brorsen, of Kiel, discovered a faint
-comet, the mean distance and period of which are almost identical with
-those of De Vico's. This comet was not observed during the perihelion
-passage of 1851, on account of its unfavorable position with respect to
-the sun. It has, however, been subsequently detected.
-
-
-VII. D'Arrest's Comet.
-
-Dr. D'Arrest discovered a comet on the 27th of June, 1851, which was
-soon found to move in an elliptic orbit, with a period of about 6-1/2
-years. It entirely escaped observation, both in Europe and America,
-during its perihelion passage in 1857. It was observed, however, at the
-Cape of Good Hope. Its invisibility in 1864 was due to its unfavorable
-position. At its return in 1870, it was first seen on the 31st of
-August, by Dr. Winnecke, of Carlsruhe.
-
-
-VIII. Tuttle's Comet.
-
-A faint telescopic comet was discovered at the Observatory of Harvard
-College, on the evening of January 4, 1858, by Mr. H. P. Tuttle. The
-same body was independently found one week later by Dr. Bruhns, of
-Berlin. From observations made at Cambridge, Massachusetts, and Ann
-Arbor, Michigan, its elements were soon computed by different
-astronomers; the result in each case coinciding so closely with the
-elements of the second comet of 1790, as to place its identity wholly
-beyond doubt. Its period is nearly 13 years and 8 months. It had
-returned, therefore, without detection, in the years 1803, 1817, 1831,
-and 1844. On its approach to perihelion in 1871, it was first detected
-by M. Borelly, of Marseilles.
-
-
-IX. Winnecke's Comet.
-
-The second comet of 1858 was discovered on the 8th of March, by Dr.
-Winnecke, of Bonn. This proved to be identical with the third comet of
-1819, whose period was computed by Encke to be about 5-1/2 years. It had
-therefore returned unperceived no less than six times between 1819 and
-1858. At its return in 1863 it again escaped detection. The perihelion
-passage of 1869 was made on the 30th of June. The comet was seen as
-early as April 13, and, after passing the sun, as late as October 11.
-"Schoenfeld states that in part of April and May it appeared to have not
-one, but several, centres of condensation, and Vogel says that, in the
-beginning of June, it had a much greater resemblance to a star-cluster
-than to a nebula." This phenomenon, it may be remarked, bore a striking
-resemblance to the appearances observed in the comets of 389, 1618, and
-1661.
-
-
-X. Tempel's Comet.
-
-On the 19th of December, 1865, M. Tempel, of Marseilles, discovered a
-small comet, which continued visible four weeks, passing its perihelion
-January 11, 1866. Dr. Oppolzer, of Vienna, after a careful determination
-of its elements, announced the interesting fact that its orbit very
-nearly intersects those of the earth and Uranus; the perihelion being
-situated immediately within the former, and the aphelion a short
-distance exterior to the latter. The period, according to the same
-astronomer, is 33 years and 65 days. The identity of this comet with
-that of 1366 was suggested by Professor H. A. Newton soon after its
-appearance,--a suggestion which subsequent research has strongly
-corroborated. It is also highly probable that the comet observed in
-China, September 29, 1133, was a former return of the same body. In 1366
-it was conspicuous to the naked eye, while in 1866 it was wholly
-invisible without a telescope,--a fact indicative of its gradual
-dissolution. The connection of this comet with the meteors of November
-14 will be elsewhere considered.
-
-
-XI. The Second Comet of 1867.
-
-Another comet of short period was discovered by M. Tempel on the 3d of
-April, 1867. Its orbit is the least eccentric of all known comets: the
-perihelion being exterior to the orbit of Mars; the aphelion interior to
-that of Jupiter. Its motion is direct, and it completes a revolution in
-5 years and 8 months.
-
-
-
-
-CHAPTER III.
-
-COMETS WHOSE ELEMENTS INDICATE PERIODICITY, BUT WHOSE RETURNS HAVE NOT
-BEEN RECOGNISED.
-
-
-I. The Group whose periods are nearly equal to that of Uranus.
-
-Since the commencement of the present century five comets have been
-discovered, which form, with Halley's, an interesting and remarkable
-group. The first of these was detected by Pons, on the 20th of July,
-1812; the second by Olbers, on the 6th of March, 1815; the third by De
-Vico, on the 28th of February, 1846; the fourth by Brorsen, on the 20th
-of July, 1847; and the last by Westphal, on the 27th of June, 1852. The
-periods of these bodies are all nearly equal, ranging from 68 to 76
-years; their eccentricities are not greatly different; the motions of
-all, except that of Halley's, are direct; and the distances of their
-aphelia are somewhat greater than Neptune's distance from the sun. Of
-this group, the comets of 1812 and 1846 seem worthy of special notice.
-The former became visible to the naked eye shortly after its discovery,
-and each continued visible about ten weeks. Their elements are as
-follows:
-
- Perihelion Passage. 1812, Sept. 1846, Mar.
- 15_d._ 7_h._ 5_d._ 12_h._
- Long. of Perih'n. 92 deg. 51' 90 deg. 31'
- Long. of A. Node. 253 deg. 33' 77 deg. 37'
- Incl. 73 deg. 57' 85 deg. 6'
- Peri'n Dist. 0.7771 0.6637
- Eccentricity. 0.94454 0.96224
- Period. 70.68_y_ 73.715
- Direction. D D
- Computer. Encke. Peirce.
-
-The wonderful similarity of these elements, except in the longitude of
-the ascending node, is at once apparent. It will also be noticed that
-the longitude of the _descending_ node of the latter is very nearly
-coincident with that of the _ascending_ node of the former. These
-remarkable coincidences are presented to the eye in the following
-diagram, where the dotted ellipse represents the orbit of the comet of
-1812, and the continuous curve that of the comet of 1846.
-
-[Illustration: Fig. 3.]
-
-It is infinitely improbable that these coincidences should be
-accidental; they point undoubtedly to a common origin of the two bodies.
-
-According to the theory now generally accepted, comets enter the solar
-system _ab extra_, move in parabolas or hyperbolas around the sun, and,
-if undisturbed by the planets, pass off beyond the limits of the sun's
-attraction, to be seen no more. If in their motion, however, they
-approach very near any of the larger planets, their direction is changed
-by planetary perturbation,--their orbits being sometimes transformed
-into ellipses. The new orbits of such bodies would pass very nearly
-through the points at which their greatest perturbation occurred; and
-accordingly we find that the aphelia of a large proportion of the
-periodic comets are near the orbits of the major planets. "I admit,"
-says M. Hoek, "that the orbits of comets are by nature parabolas or
-hyperbolas, and that in the cases when elliptical orbits are met with,
-these are occasioned by planetary attractions, or derive their character
-from the uncertainty of our observations. To allow the contrary would be
-to admit some comets as permanent members of our planetary system, to
-which they ought to have belonged since its origin, and so to assert the
-simultaneous birth of that system and of these comets. As for me, I
-attribute to these a primitive wandering character. Traveling through
-space, they move from one star to another in order to leave it again,
-provided they do not meet any obstacle that may force them to remain in
-its vicinity. Such an obstacle was Jupiter, in the neighborhood of our
-sun, for the comets of Lexell and Brorsen, and probably for the greater
-part of periodical comets; the other part of which may be indebted for
-their elliptical orbits to the attractions of Saturn and the remaining
-planets.
-
-"Generally, then, comets come to us from some star or other. The
-attraction of our sun modifies their orbit, as had been done already by
-each star through whose sphere of attraction they had passed. We can put
-the question if they come as single bodies or united in systems."
-
-The conclusion of this astronomer's interesting discussion is that--
-
-"_There are systems of comets in space that are broken up by the
-attraction of our sun, and whose members attain, as isolated bodies, the
-vicinity of the earth during a course of several years._"[6]
-
- [6] Monthly Notices of the R. A. S., vol. xxv., p. 243.
-
-In the researches here referred to, it is shown by Professor Hoek that
-the comets of 1860 III., 1863 I., and 1863 IV. formed a group in space
-previous to their entrance into our system. The same fact has also been
-demonstrated in regard to other comets which need not here be specified.
-Now, the comets of 1812 and 1846 IV. have their aphelia near the orbit
-of Neptune, and hence the original parabolas in which they moved were
-probably transformed into ellipses by the perturbations of that planet.
-Before entering the solar domain, they were doubtless members of a
-cometary system. Passing Neptune near the same time, and at some
-distance from each other, their different relative positions with regard
-to the disturbing body may account for the slight differences in the
-elements of their orbits.
-
-
-_Comets of the Jovian Group._
-
-Besides the eight comets enumerated in Chapter II. whose aphelia are in
-the vicinity of Jupiter's orbit, five others have been observed which
-belong apparently to the same cluster. These are the comets of 1585,
-1743 I., 1766 II., 1783, and 1819 IV. "The fact that these comets have
-not been re-observed on their successive returns through perihelion may
-be explained either by the difficulty of observing them, owing to their
-unfavorable positions, and to the circumstances of observers not
-expecting their reappearance, their periodic character not being then
-suspected, or because they may have been thrown by the disturbing action
-of the larger planets into orbits such as to keep them continually out
-of the range of view of terrestrial observers."[7]
-
- [7] Dr. Lardner.
-
-Lexell's comet of 1770 is the most remarkable instance known of the
-change produced in the orbits of these bodies by planetary attraction.
-This comet passed so near Jupiter in 1779 that the attraction of the
-latter was 200 times greater than that of the sun. The consequence was
-that the comet, whose mean distance corresponded to a period of 5-1/2
-years, was thrown into an orbit so entirely different that it has never
-since been visible.
-
-
-PETERS' COMET.
-
-A telescopic comet was discovered by Dr. Peters on the 26th of June,
-1846, which continued to be observed till the 21st of July. Its period,
-according to the discoverer, is about 13 years, and its aphelion, like
-that of Tuttle's comet, is in the vicinity of Saturn's orbit. It was
-expected to return in 1859, and again in 1872, but each time escaped
-detection, owing probably to the fact that its position was unfavorable
-for observation.
-
-
-STEPHAN'S COMET (1867 I.).
-
-In January, 1867, M. Stephan, of Marseilles, discovered a new comet, the
-elements of which, after two months' observations, were computed by Mr.
-G. M. Searle, of Cambridge, Massachusetts. The perihelion of this body
-is near the orbit of Mars; its aphelion near that of Uranus,--the least
-distance of the orbits being about 2,000,000 miles. The present form of
-the cometary path is doubtless due to the disturbing action of Uranus.
-The comet completes its revolution in 33.62 years; consequently (as has
-been pointed out by Mr. J. R. Hind) five of its periods are almost
-exactly equal to two periods of Uranus. The next approximate appulse of
-the two bodies will occur in 1985, when the form of the comet's orbit
-may be sensibly modified.
-
-
-ELLIPTIC COMETS WHOSE APHELIA ARE AT A MUCH GREATER DISTANCE THAN
-NEPTUNE'S ORBIT.
-
-In October, 1097, a comet was seen both in Europe and China, which was
-noted for the fact of its having two distinct tails, making with each
-other an angle of about 40 deg. From a discussion of the Chinese
-observations (which extended through a longer period than the European),
-Laugier concluded that this body is identical with the third comet of
-1840, which was discovered by Galle on the 6th of March. If, therefore,
-it has made no intermediate return without being observed, it must have
-a period of about 743 years. It is also highly probable, from the
-similarity of elements, that the comet which passed its perihelion on
-the 5th of June, 1845, was a reappearance of the comet of 1596,--the
-period of revolution being 249 years. The elements of the great comet of
-1843 are somewhat uncertain. There is a probability, however, of the
-identity of this body with the comet of 1668. This would make the period
-175 years. The third comet of 1862 is especially interesting from its
-connection with the August meteors. Its period, according to Dr.
-Oppolzer, is 121-1/2 years.
-
-
-THE GREAT COMET OF 1858
-
-was one of the most remarkable in the nineteenth century. It was
-discovered on the 2d of June, by Donati, of Florence, and first became
-visible to the naked eye about the last of August. The comet attained
-its greatest brilliancy about the 10th of October, when its distance
-from the earth was 50,000,000 miles. The length of its tail somewhat
-exceeded this distance. If, therefore, the comet had been at that time
-directly between the sun and the earth, the latter must have been
-enveloped for a number of hours in the cometic matter.
-
-The observations of this comet during a period of five months enabled
-astronomers to determine the elements of its orbit within small limits
-of error. It completes a revolution, according to Newcomb, in 1854
-years, in an orbit somewhat more eccentric than that of Halley's comet.
-It will not return before the 38th century, and will only reach its
-aphelion about the year 2800. Its motion per second when nearest the sun
-is 36 miles; when most remote, only 234 yards.
-
-
-
-
-CHAPTER IV.
-
-OTHER REMARKABLE COMETS.
-
-
-It remains to describe some of the most remarkable comets of which we
-have any record, but of which we have no means of determining with
-certainty whether they move in ellipses, parabolas, or hyperbolas.
-
-In the year 466 B.C., a large comet appeared simultaneously with the
-famous fall of meteoric stones near AEgospotamos. The former was supposed
-by the ancients to have had some agency in producing the latter
-phenomenon. Another of extraordinary magnitude appeared in the year 373
-B.C. This comet was so bright as to throw shadows, and its tail extended
-one-third of the distance from the horizon to the zenith. The years 156,
-136, 130, and 48, before our era, were also signalized by the appearance
-of very large comets. The apparent magnitude of the first of these is
-said to have equaled that of the sun itself; while its light was
-sufficient to diminish sensibly the darkness of the night. The second is
-said to have filled a fourth part of the celestial hemisphere. The comet
-of 130 B.C., sometimes called the comet of Mithridates, because of its
-appearance about the time of his birth, is said to have rivaled the sun
-in splendor.
-
-In A.D. 178 a large comet was visible during a period of nearly three
-months. Its nucleus had a remarkably red or fiery appearance, and the
-greatest length of its tail exceeded 60 deg. The most brilliant comets of
-the sixth century were probably those of 531 and 582. The train of the
-latter, as seen in the west soon after sunset, presented the appearance
-of a distant conflagration.
-
-Great comets appeared in the years 975, 1264, and 1556. Of these, the
-comet of 1264 had the greatest apparent magnitude. It was first seen
-early in July, and attained its greatest brilliancy in the latter part
-of August, when its tail was 100 deg. in length. It disappeared on the 3d of
-October, about the time of the death of Pope Urban IV., of which event
-the comet, in consequence of this coincidence, was considered the
-precursor. These comets, on account of the similarity of their elements,
-were believed by many astronomers to be the same, and to have a period
-of about 300 years. In the case of identity, however, another
-reappearance should have occurred soon after the middle of the
-nineteenth century. As no such return was observed, we may conclude that
-the comets were not the same, and that their periods are wholly unknown.
-
-The comet discovered on the 10th of November, 1618, was one of the
-largest in modern times; its tail having attained the extraordinary
-length of 104 deg. The comet of 1652, so carefully observed by Hevelius,
-almost equaled the moon in apparent magnitude. It shone, however, with a
-lurid, dismal light. The tail of the comet of 1680 was 90 deg. in length.
-This body is also remarkable for its near approach to the sun; its least
-distance from the solar surface having been only 147,000 miles. It will
-always be especially memorable, however, for having furnished Newton the
-data by means of which he first showed that comets in their orbital
-motions are governed by the same principle that regulates the planetary
-revolutions.
-
-Of all the comets which appeared during the eighteenth century, that
-which passed its perihelion on the 7th of October, 1769, had the
-greatest apparent magnitude. It was discovered by Messier on the 8th of
-August, and continued to be observed till the 1st of December. On the
-11th of September the length of its tail was 97 deg. The comet discovered
-on the 26th of March, 1811, is in some respects the most remarkable on
-record. It was observed during a period of 16 months and 22 days,--the
-longest period of visibility known. On account of its situation with
-respect to the earth, the apparent length of its tail was much less than
-that of some other comets; its true length, however, was at one time
-120,000,000 miles; and Sir William Herschel found that on the 12th of
-October the greatest circular section of the tail was 15,000,000 miles
-in diameter. The same astronomer found the diameter of the head of the
-comet to be 127,000 miles, and that of the envelope at least 643,000. As
-a general thing, the length of a comet-train increases very rapidly as
-the body approaches the sun. But the perihelion distance of the comet of
-1811 was considerably greater than the distance of the earth from the
-sun; while its nearest approach to the earth was 110,000,000 miles. Its
-true magnitude, therefore, has probably not been surpassed by any other
-observed; and had its perihelion been very near the sun, it must have
-exhibited an appearance of terrific grandeur. This comet has an elliptic
-orbit, and its period, according to Argelander, is 3065 years.
-
-The great comet of 1861 was discovered on the 13th of May, by Mr. John
-Tebbut, Jr., of New South Wales. In this country, as well as in Europe,
-it was first generally observed on the evening of June 30,--19 days
-after its perihelion passage. Sir John Herschel, who observed it in
-Kent, England, remarks that it far exceeded in brilliancy any comets he
-had ever seen, not excepting those of 1811 and 1858. According to Father
-Secchi, of the Collegio Romano, the length of its tail was 118 deg. This,
-with a single exception,[8] is the greatest on record. The computed
-orbit is elliptical; the period, 419 years.
-
- [8] The tail of the first comet of 1865 (observed in the
- Southern Hemisphere) attained the unprecedented length
- of 150 deg.--_M. N. R. A. S._, vol. xxv., p. 220.
-
-
-
-
-CHAPTER V.
-
-THE POSITION AND ARRANGEMENT OF COMETARY ORBITS.
-
-
-The cosmical masses from which comets are derived seem to traverse in
-great numbers the interstellar spaces. In consequence of the sun's
-progressive motion, these nebulous bodies are sometimes drawn toward the
-centre of our system. If, in this approach, they are not disturbed by
-any of the large planets, they again recede in parabolas or hyperbolas.
-When, however, as must sometimes be the case, they pass near Jupiter,
-Saturn, Uranus, or Neptune, their orbits may be transformed into
-elongated ellipses. The periodicity of many comets may thus be accounted
-for.
-
-In the present chapter it is proposed to consider the probable
-consequences of the sun's motion through regions of space in which
-cometary matter is widely diffused; to compare our theoretical
-deductions with observed phenomena; and thus refer to their physical
-cause a variety of facts which have hitherto received no satisfactory
-explanation.[9]
-
- [9] This chapter is the substance of a paper read before the American
- Philosophical Society, November 19, 1869.
-
-1. As comets, at least in many instances, owe their periodicity to the
-disturbing action of the major planets, and as this planetary influence
-is sometimes sufficient, especially in the case of Jupiter and Saturn,
-to change the _direction_ of cometary motion, the great majority of
-periodic comets should move in the same direction with the planets. Now,
-of the comets known to be elliptical, 70 per cent. _have direct motion_.
-In this respect, therefore, theory and observation are in striking
-harmony.
-
-2. When the relative positions of a comet and the disturbing planet are
-such as to give the transformed orbit of the former a small perihelion
-distance, the comet must return to the point at which it received its
-greatest perturbation; in other words, to the orbit of the planet. The
-aphelia of the comets of short period ought therefore to be found, for
-the most part, _in the vicinity of the orbits of the major planets_.
-This, as already shown in Chapters II. and III., is strikingly the case.
-The actual distances of these aphelia, however, as compared with the
-respective distances of Jupiter, Saturn, Uranus and Neptune, are
-presented at one view in the following tables:
-
-
-=I.= COMETS WHOSE APHELION DISTANCES ARE NEARLY EQUAL TO 5.20, THE
-RADIUS OF JUPITER'S ORBIT.
-
- Comets. Aph. Dist.
-
- 1. Encke's 4.09
- 2. 1819 IV 4.81
- 3. De Vico's 5.02
- 4. Pigott's (1783) 5.28
- 5. 1867 II 5.29
- 6. 1743 I 5.32
- 7. 1766 II 5.47
- 8. 1819 III 5.55
- 9. Brorsen's 5.64
- 10. D'Arrest's 5.75
- 11. Faye's 5.93
- 12. Bicla's 6.19
-
-
-=II.= COMETS WHOSE APHELION DISTANCES ARE NEARLY EQUAL TO 9.54, THE
-RADIUS OF SATURN'S ORBIT.
-
- Comets. Aph. Dist.
-
- 1. Peters' (1846 VI.) 9.45
- 2. Tuttle's (1858 I.) 10.42
-
-
-=III.= COMETS WHOSE APHELION DISTANCES ARE NEARLY EQUAL TO 19.18, THE
-RADIUS OF URANUS'S ORBIT.
-
- Comets. Aph. Dist.
-
- 1. 1867 I 19.28
- 2. November meteors 19.65
- 3. 1866 I 19.92
-
-
-=IV.= COMETS WHOSE APHELION DISTANCES ARE NEARLY EQUAL TO 30.04, THE
-RADIUS OF NEPTUNE'S ORBIT.
-
- Comets. Aph. Dist.
-
- 1. Westphal's (1852 IV.) 31.97
- 2. Pons' (1812) 33.41
- 3. Olbers' (1815) 34.05
- 4. De Vico's (1846 IV.) 34.35
- 5. Brorsen's (1847 V.) 35.07
- 6. Halley's[10] 35.37
-
- [10] Halley's comet _in aphelio_ is too remote from the plane of
- the ecliptic to be much disturbed by Neptune. Has the original
- position of the orbit been changed by Jupiter's influence?
-
-The coincidences here pointed out (some of which have been noticed by
-others) appear, then, to be necessary consequences of the motion of the
-solar system through spaces occupied by meteoric nebulae. Hence the
-observed facts receive an obvious explanation.
-
-In regard to comets of long period we have only to remark that, for
-anything we know to the contrary, there may be causes of perturbation
-far exterior to the orbit of Neptune.
-
-3. From what we observe in regard to the _larger_ bodies of the
-universe--a clustering tendency being everywhere apparent,--it seems
-highly improbable that cometic matter should be uniformly distributed in
-the sidereal spaces. We would expect, on the contrary, to find it
-collected in groups or clusters. This view is also in remarkable harmony
-with the facts of observation. In 150 years, from 1600 to 1750, 16
-comets were visible to the naked eye; of which 8 appeared in the 25
-years from 1664 to 1689. Again, during 60 years, from 1750 to 1810, only
-5 comets were visible to the naked eye, while in the next 50 years there
-were double that number. The probable cause of such variations is
-sufficiently obvious. As the sun in its progressive motion approaches a
-cometary group, the latter is drawn toward the centre of our system; the
-nearer members with greater velocity than the more remote. Those of the
-same cluster would enter the solar domain at periods not very distant
-from each other; the forms of their orbits depending upon their original
-relative positions with reference to the sun's course, and also on
-planetary perturbations. It is evident also that the passage of the
-solar system through a region of space comparatively destitute of
-cometic clusters would be indicated by a corresponding paucity of
-comets.
-
-4. The line of apsides of a large proportion of comets will be
-approximately coincident with the solar orbit. The point towards which
-the sun is moving is in longitude about 260 deg. The quadrants bisected by
-this point and that directly opposite extend from 215 deg. to 305 deg., and from
-35 deg. to 125 deg. The number of cometary perihelia found in these quadrants
-up to July, 1868 (periodic comets being counted but once) was 159, or
-62 per cent.; in the other two quadrants, 98, or 38 per cent.
-
-This tendency of the perihelia to crowd together in two opposite regions
-has been noticed by different writers.
-
-5. Comets whose positions before entering our system were very remote
-from the solar orbit must have _overtaken_ the sun in its progressive
-motion; hence their perihelia must fall, for the most part, in the
-vicinity of the point towards which the sun is moving; and they must in
-general have very small perihelion distances. Now, what are the observed
-facts in regard to the longitudes of the perihelia of the comets which
-have approached within the least distance of the sun's surface? But
-three have had a perihelion distance less than 0.01. _All_ these, it
-will be seen by the following table, have their perihelia in close
-proximity to the point referred to:
-
-
-=I.= COMETS WHOSE PERIHELION DISTANCES ARE LESS THAN 0.01.
-
- Perihelion Passage. Per. Dist. Long. of Per.
-
- 1. 1668, Feb. 28_d._ 13_h._ 0.0047 277 deg. 2'
- 2. 1680, Dec. 17 23 0.0062 262 49
- 3. 1843, Feb. 27 9 0.0055 278 39
-
-In Table II. all but the last have their perihelia in the same quadrant.
-
-
-=II.= COMETS WHOSE PERIHELION DISTANCES ARE GREATER THAN 0.01 AND LESS
-THAN 0.05.
-
- Perihelion Passage. Per. Dist. Long. of Per.
-
- 1. 1689, Nov 29_d._ 4_h._ 0.0189 269 deg. 41'
- 2. 1816, March 1 8 0.0485 267 35
- 3. 1826, Nov 18 9 0.0268 315 31
- 4. 1847, March 30 6 0.0425 276 2
- 5. 1865, Jan 14 7 0.0260. 141 15
-
-The perihelion of the first comet in Table III. is remote from the
-direction of the sun's motion; that of the second is distant but 14 deg.,
-and of the third 21 deg.
-
-
-=III.= COMETS WHOSE PERIHELION DISTANCES ARE GREATER THAN 0.05 AND LESS
-THAN 0.1.
-
- Perihelion Passage. Per. Dist. Long. of Per.
-
- 1. 1593, July 18_d._ 13_h._ 0.0891 176 deg. 19'
- 2. 1780, Sept. 30 22 0.0963 246 35
- 3. 1821, March 21 12 0.0918 239 29
-
-With greater perihelion distances the tendency of the perihelia to crowd
-together round the point indicated is less distinctly marked.
-
-6. Few comets of small perihelion distance should have their perihelia
-in the vicinity of longitude 80 deg., the point opposite that towards which
-the sun is moving. Accordingly we find, by examining a table of cometary
-elements, that with a perihelion distance less than 0.1 there is not a
-single perihelion between 35 deg. and 125 deg.; between 0.1 and 0.2 but 3; and
-between 0.2 and 0.3 only 1.
-
-
-
-
-CHAPTER VI.
-
-THE DISINTEGRATION OF COMETS.
-
-
-The _fact_ that in several instances meteoric streams move in orbits
-identical with those of certain comets was first established by the
-researches of Signor Schiaparelli. The _theory_, however, of an intimate
-relationship between comets and meteors was advocated by the writer as
-long since as 1861,[11]--several years previous to the publication of
-Schiaparelli's memoirs. In the essay here referred to it was
-maintained--
-
- [11] Danville Quarterly Review, December, 1861.
-
-1. That meteors and meteoric rings "are the _debris_ of ancient but now
-disintegrated comets whose matter has become distributed around their
-orbits."
-
-2. That the separation of Biela's comet as it approached the sun in
-December, 1845, was but one in a series of similar processes which would
-probably continue until the individual fragments would become invisible.
-
-3. That certain luminous meteors have entered the solar system from the
-interstellar spaces.[12]
-
- [12] Others, it was supposed, might have originated within the
- system,--a view which the writer has not wholly abandoned.
-
-4. That the orbits of some meteors and periodic comets have been
-transformed into ellipses by planetary perturbation; and
-
-5. That numerous facts--some observed in ancient and some in modern
-times--have been decidedly indicative of cometary disintegration.
-
-What was thus proposed as theory has been since confirmed as undoubted
-facts. When the hypothesis was originally advanced, the data required
-for its mathematical demonstration were entirely wanting. The evidence,
-however, by which it was sustained was sufficient to give it a high
-degree of probability.
-
-The existence of a divellent force by which comets near their perihelia
-have been separated into parts is clearly shown by the following facts.
-Whether this force, as suggested by Schiaparelli, is simply the unequal
-attraction of the sun on different parts of the nebulous mass, or
-whether, in accordance with the views of other astronomers, it is to be
-regarded as a cosmical force of repulsion, is a question left for future
-discussion.
-
-
-HISTORICAL FACTS.
-
-1. Seneca informs us that Ephoras, a Greek writer of the fourth century
-before Christ had recorded the singular fact of a comet's separation
-into two distinct parts.[13] This statement was deemed incredible by the
-Roman philosopher, inasmuch as the occurrence was then without a
-parallel. More recent observations of similar phenomena leave no room to
-question the historian's veracity.
-
- [13] "Quaest. Nat.," lib. vii., cap. xvi.
-
-2. The head of the great comet of A.D. 389, according to the writers of
-that period, was "composed of several small stars." (Hind's "Comets," p.
-103.)
-
-3. On June 27, A.D. 416, two comets appeared in the constellation
-Hercules, and pursued nearly the same apparent path. Probably at a
-former epoch the pair had constituted a single comet.[14]
-
- [14] Chambers' "Descr. Astr.," p. 374.
-
-4. On August 4, 813, "a comet was seen which resembled two moons joined
-together." They subsequently separated, the fragments assuming different
-forms.[15]
-
- [15] Ibid., p. 383.
-
-5. The Chinese annals record the appearance of three comets--one large
-and two smaller ones--at the same time, in the year 896 of our era.
-"They traveled together for three days. The little ones disappeared
-first, and then the large one."[16] The bodies were probably fragments
-of a large comet which, on approaching the sun, had been separated into
-parts a short time previous to the date of their discovery.
-
- [16] Ibid., p. 388.
-
-6. _The third comet of 1618._--The great comet of 1618 exhibited decided
-symptoms of disintegration. When first observed (on November 30), its
-appearance was that of a lucid and nearly spherical mass. On the eighth
-day the process of division was distinctly noticed, and on the 20th of
-December it resembled a cluster of small stars.[17]
-
- [17] Hevelius, "Cometographia," p. 341. See also Grant's "Hist.
- of Phys. Astr.," p. 302.
-
-7. _The comet of 1661._--The elements of the comets of 1532 and 1661
-have a remarkable resemblance, and previous to the year 1790
-astronomers regarded the bodies as identical. The similarity of the
-elements is seen at a glance in the following table:
-
- Comet of 1532. Comet of 1661.
-
- Longitude of perihelion 111 deg. 48' 115 deg. 16'
- Longitude of ascending node 87 23 81 54
- Inclination 32 36 33 1
- Perihelion distance 0.5192 0.4427
- Motion Direct. Direct.
-
-The elements of the former are by Olbers; those of the latter by
-Mechain. The return of the comet about 1790, though generally expected,
-was looked for in vain. As a possible explanation of this fact, it is
-interesting to recur to an almost forgotten statement of Hevelius. This
-astronomer observed in the comet of 1661 an apparent breaking up of the
-body into separate fragments.[18] The case may be analogous to that of
-Biela's comet.
-
- [18] "Cometographia," p. 417.
-
-8. The identity of the comets of 1866 and 1366, first suggested by
-Professor H. A. Newton, is now unquestioned. The existence then of a
-meteoric swarm, moving in the same track, is not the only evidence of
-the original comet's partial dissolution. The comet of 1866 was
-invisible to the naked eye; that of 1366, seen under nearly similar
-circumstances, was a conspicuous object. The statement of the Chinese
-historian that "it appeared nearly as large as a tow measure,"[19]
-though somewhat indefinite, certainly justifies the conclusion that its
-magnitude has greatly diminished during the last 500 years. The meteors
-moving in the same orbit are doubtless the products of this gradual
-separation.
-
- [19] Williams' "Chinese Observations of Comets," p. 73.
-
-9. The repartition of Biela's comet in 1845, as well as the
-non-appearance of the two fragments in 1865 and 1872,[20] were referred
-to in a previous chapter.
-
- [20] One of the parts was seen at Madras, India, on the mornings of
- December 2 and 3, 1872.
-
-The comet of Halley, if we may credit the descriptions given by ancient
-writers, has been decreasing in brilliancy from age to age. The same is
-true in regard to several others believed to be periodic. The comet of
-A.D. 1097 had a tail 50 deg. long. At its return, in March, 1840, the length
-of its tail was only 5 deg. The third comet of 1790 and the first of 1825
-are supposed, from the similarity of their elements, to be identical.
-Each perihelion passage occurred in May, yet the tail at the former
-appearance was 4 deg. in length, at the latter but 2-1/2 deg. Other instances
-might be specified of this apparent gradual dissolution. It would seem,
-indeed, extremely improbable that the particles driven off from comets
-in their approach to the sun, forming tails extending millions of miles
-from the principal mass, should again be collected around the same
-nuclei.
-
-The fact, then, that meteors move in the same orbits with comets is but
-a consequence of that disruptive process so clearly indicated by the
-phenomena described. In this view of the subject, comets--even such as
-move in elliptic orbits--are not to be regarded as permanent members of
-the solar system. Their _debris_ becomes gradually scattered around the
-orbit. Some parts of the nebulous ring will be more disturbed than
-others by planetary perturbation. Portions of such streams as nearly
-intersect the earth's path sometimes penetrate the atmosphere. Their
-rapid motion renders them luminous. If very minute, they are burnt up or
-dissipated without leaving any solid deposit; we then have the phenomena
-of _shooting-stars_. When, however, as is sometimes the case, they
-contain a considerable quantity of solid matter, they reach the earth's
-surface as _meteoric stones_.
-
-
-
-
-II.
-
-METEORS.
-
-
-
-
-CHAPTER VII.
-
-METEORIC STONES.
-
-
-Although numerous instances of the fall of aerolites had been recorded,
-some of them apparently well authenticated, the occurrence long appeared
-too marvelous and improbable to gain credence with scientific men. Such
-a shower of rocky fragments occurred, however, on the 26th of April,
-1803, at L'Aigle, in France, as forever to dissipate all doubt on the
-subject. Similar displays since that time have been frequently
-witnessed;--indeed scarcely a year passes without the fall of meteoric
-stones in some part of the earth, either singly or in clusters. It would
-not comport with the design of the present treatise to give an extended
-list of these phenomena. The following account, however, includes the
-most important instances in which the fall of meteoric stones has been
-actually observed:
-
-(1.) 1478 B.C.--According to the celebrated Parian chronicle, an
-aerolite, or _thunder-stone_, as it was called, fell in the island of
-Crete, about 1478 years before the Christian era. This is undoubtedly
-the most ancient stone-fall on record. Meteoric masses have been
-_found_, however, the fall of which _probably_ occurred at an epoch
-still more ancient.
-
-(2.) 1200 B.C.--A number of stones, which were anciently preserved in
-Orchomenos, a town of Boeotia, were said to have fallen from heaven
-about twelve centuries before our era.
-
-(3.) 1168 B.C.--A mass of iron, as we learn from the Parian chronicle,
-was seen to descend upon Mount Ida, in Crete.
-
-(4.) 654 B.C.--According to Livy, a number of meteoric stones fell on
-the Alban Hill, near Rome, about the year 654 B.C.
-
-(5.) 616 B.C., _January_ 14.--It is related in the Chinese annals that
-on the 14th of January, 616 B.C., a meteoric stone-fall broke several
-chariots and killed ten men.
-
-(6.) 466 B.C.--A mass of rock, described as "of the size of two
-millstones," fell at AEgospotamos, in Thrace. An attempt to rediscover
-this meteoric mass, so celebrated in antiquity, was recently made, but
-without success. Notwithstanding this failure, Humboldt expressed the
-hope that, as such a body would be difficult to destroy, it may yet be
-found, "since the region in which it fell is now become so easy of
-access to European travelers."
-
-(7.) 465 B.C.--The famous stone called the "Mother of the Gods," and
-which is described or alluded to by many ancient writers, was said to
-have fallen from the skies. The poet Pindar was seated on a hill at the
-time of its descent, and the meteorite struck the earth near his feet.
-The stone, as it fell, was _encircled by fire_. "It is said to have been
-of moderate dimensions, of a black hue, of an irregular, angular shape,
-and of a metallic aspect. An oracle had predicted that the Romans would
-continue to increase in prosperity if they were put in possession of
-this precious deposit; and Publius Scipio Nasico was accordingly deputed
-to Attalus, King of Pergamus, to obtain and receive the sacred idol,
-whose worship was instituted at Rome 204 years before the Christian
-era."--_Edinburgh Encyclopedia._
-
-(8.) A.D. 921.--An immense aerolite fell into the river (a branch of the
-Tiber) at Narni, in Italy. It projected three or four feet above the
-surface of the water.
-
-(9.) 1492, _November_ 7.--An aerolite, weighing 276 pounds, fell at
-Ensisheim, in Alsace, penetrating the earth to the depth of three feet.
-This stone, or the greater part of it, may still be seen at Ensisheim.
-
-(10.) 1511, _September_ 14.--At noon an almost total darkening of the
-heavens occurred at Crema. "During this midnight gloom," says a writer
-of that period, "unheard-of thunders, mingled with awful lightnings,
-resounded through the heavens.... On the plain of Crema, where never
-before was seen a stone the size of an egg, there fell pieces of rock of
-enormous dimensions and of immense weight. It is said that ten of these
-were found, weighing 100 pounds each." A monk was struck dead at Crema
-by one of these rocky fragments. This terrific display is said to have
-lasted two hours, and 1200 aerolites were subsequently found.
-
-(11.) 1637, _November_ 29.--A stone, weighing 54 pounds, fell on Mount
-Vaison, in Provence.
-
-(12.) 1650, _March_ 30.--A Franciscan monk was killed at Milan by the
-fall of a meteoric stone.
-
-(13.) 1674.--Two Swedish sailors were killed on shipboard by the fall of
-an aerolite.
-
-(14.) 1751, _May_ 26.--Two meteoric masses, consisting almost wholly of
-iron, fell near Agram, the capital of Croatia. The larger fragment,
-which weighs 72 pounds, is now in Vienna.
-
-(15.) 1790, _July_ 24.--Between 9 and 10 o'clock at night a very large
-meteor was seen near Bordeaux, France. Over Barbotan a loud explosion
-was heard, which was followed by a shower of meteoric stones of various
-magnitudes.
-
-(16.) 1794, _July_.--A fall of about a dozen aerolites occurred at
-Sienna, Tuscany.
-
-(17.) 1795, _December_ 13.--A large meteoric stone fell near Wold
-Cottage, in Yorkshire, England. "Several persons heard the report of an
-explosion in the air, followed by a hissing sound; and afterward felt a
-shock, as if a heavy body had fallen to the ground at a little distance
-from them. One of these, a plowman, saw a huge stone falling toward the
-earth, eight or nine yards from the place where he stood. It threw up
-the mould on every side; and after penetrating through the soil, lodged
-some inches deep in solid chalk-rock. Upon being raised, the stone was
-found to weigh 56 pounds. It fell in the afternoon of a mild, but hazy
-day, during which there was no thunder or lightning; and the noise of
-the explosion was heard through a considerable district."--_Milner's
-Gallery of Nature_, p. 134.
-
-(18.) 1796, _February_ 19.--A stone of 10 pounds' weight fell in
-Portugal.
-
-(19.) 1803, _April_ 26.--This remarkable shower was referred to on a
-previous page. At 1 o'clock P.M., the heavens being almost cloudless, a
-tremendous noise, like that of thunder, was heard, and at the same time
-an immense fire-ball was seen moving with great rapidity through the
-atmosphere. This was followed by a violent explosion, which lasted
-several minutes, and which was heard not only at L'Aigle, but in every
-direction around it to the distance of 70 miles. Immediately after, a
-great number of meteoric stones fell to the earth, generally penetrating
-to some distance beneath the surface. Nearly 3000 of these fragments
-were found and collected, the largest weighing about 17 pounds. The
-occurrence very naturally excited great attention. M. Biot, under the
-authority of the government, repaired to the place, collected the
-various facts in regard to the phenomenon, took the testimony of
-witnesses, etc., and finally embraced the results of his investigations
-in an elaborate memoir.
-
-(20.) 1807, _December_ 14.--A large meteor exploded over Weston,
-Connecticut. The height, direction, velocity and magnitude of this body
-were discussed by Dr. Bowditch in a memoir communicated to the American
-Academy of Arts and Sciences in 1815. The appearance of the meteor
-occurred about 6h. 15m. A.M.,--just after daybreak. Its apparent
-diameter was half that of the full moon; its time of flight, about 30
-seconds. Within less than a minute from the time of its disappearance
-three distinct reports, like those of artillery, were heard over an area
-several miles in diameter. Each explosion was followed by the fall of
-meteoric stones. Unlike most aerolites, these bodies when first found
-were so soft as to be easily pulverized between the fingers. On
-exposure to the air, however, they gradually hardened. The weight of the
-largest fragment was 35 pounds.
-
-(21.) 1859, _November_ 15.--Between 9 and 10 o'clock in the morning an
-extraordinary meteor was seen in several of the New England States, New
-York, New Jersey, the District of Columbia, and Virginia. The apparent
-diameter of the head was nearly equal to that of the sun, and it had a
-train, notwithstanding the bright sunshine, several degrees in length.
-Its disappearance on the coast of the Atlantic was followed by a series
-of the most terrific explosions. It is believed to have descended into
-the water, probably into Delaware Bay. A highly interesting account of
-this meteor, by Professor Loomis, may be found in the _American Journal
-of Science and Arts_ for January, 1860.
-
-(22.) 1860, _May_ 1.--About 20 minutes before 1 o'clock, P.M., a shower
-of meteoric stones fell in the southwest corner of Guernsey county,
-Ohio. Full accounts of the phenomena are given in _Silliman's Journal_
-for July, 1860, and January and July, 1861, by Professors E. B. Andrews,
-E. W. Evans, J. L. Smith, and D. W. Johnson. From these interesting
-papers we learn that the course of the meteor was about 40 deg. west of
-north. Its visible track was over Washington and Noble counties, and the
-prolongation of its projection, on the earth's surface, passes directly
-through New Concord, in the southeast corner of Muskingum county. The
-meteor when first seen was about 40 miles from the earth's surface. The
-sky, at the time, was for the most part covered with clouds over
-northwestern Ohio, so that if any portion of the meteoric mass
-continued on its course it was invisible. The velocity of the meteor, in
-relation to the earth's surface, was from three to four miles per
-second; and hence its absolute velocity in the solar system must have
-been somewhat greater than that of the earth.
-
-"At New Concord,[21] Muskingum county, where the meteoric stones fell,
-and in the immediate neighborhood, there were many distinct and loud
-reports heard. At New Concord there was first heard in the sky, a little
-southeast of the zenith, a loud detonation, which was compared to that
-of a cannon fired at the distance of half a mile. After an interval of
-ten seconds, another similar report. After two or three seconds another,
-and so on with diminishing intervals. Twenty-three distinct detonations
-were heard, after which the sounds became blended together and were
-compared to the rattling fire of an awkward squad of soldiers, and by
-others to the roar of a railway train. These sounds, with their
-reverberations, are thought to have continued for two minutes. The last
-sounds seemed to come from a point in the southeast 45 deg. below the
-zenith. The result of this cannonading was the falling of a large number
-of stony meteorites upon an area of about 10 miles long by 3 wide. The
-sky was cloudy, but some of the stones were seen first as 'black
-specks', then as 'black birds', and finally falling to the ground. A few
-were picked up within 20 or 30 minutes. The warmest was no warmer than
-if it had lain on the ground exposed to the sun's rays. They penetrated
-the earth from two to three feet. The largest stone, which weighed 103
-pounds, struck the earth at the foot of a large oak-tree, and, after
-cutting off two roots, one five inches in diameter, and grazing a third
-root, it descended two feet ten inches into hard clay. This stone was
-found resting under a root that was not cut off. This would seemingly
-imply that it entered the earth obliquely."
-
- [21] New Concord is close to the Guernsey county line. Nearly all
- the stones fell in Guernsey.
-
-Over thirty of the stones which fell were discovered, while doubtless
-many, especially of the smaller, being deeply buried beneath the soil,
-entirely escaped observation. The weight of the largest ten was 418
-pounds.
-
-(23.) 1860, _July_ 14.--About 2 o'clock P.M. on the 14th of July, 1860,
-a shower of aerolites fell at Dhurmsala, in India. The fall was attended
-by a tremendous detonation, which greatly terrified the inhabitants of
-the district. The natives, supposing the stones to have been thrown by
-some of their deities from the summit of the Himalayas, carried off many
-fragments to be kept as objects of religious veneration. Lord Canning
-and Mr. J. R. Saunders succeeded, however, in obtaining numerous
-specimens, which they forwarded to the British Museum and several
-European cabinets. They are earthy aerolites, of a specific gravity
-somewhat greater than that of granite.
-
-(24.) 1864, _May_ 14.--Early in the evening a very large and brilliant
-meteor was seen in France, from Paris to the Spanish border. At
-Montauban and in the vicinity loud explosions were heard, which were
-followed by showers of meteoric stones near the villages of Orgueil and
-Nohic. The principal facts in regard to the meteor are the following:
-
- Elevation when first seen, over 55 miles
- " at the time of its explosion 20 "
- Inclination of its path to the horizon 20 deg. or 25 deg.
- Velocity per second, about 20 miles,
- or equal to that of the earth's orbital motion.
-
-"This example," says Professor Newton, "affords the strongest proof that
-the detonating and stone-producing meteors are phenomena not essentially
-unlike."
-
-(25.) 1868, _January_ 30.--It is obviously a matter of much importance
-that the composition and general characteristics of aerolites, together
-with the phenomena attending their fall, should be carefully noted; as
-such facts have a direct bearing on the theory of their origin. In this
-regard the memoirs of Professors J. G. Galle, of Breslau, and G. vom
-Rath, of Bonn, on a meteoric fall which occurred at Pultusk, Poland, on
-the 30th of January, 1868, have more than ordinary interest. These
-memoirs establish the fact that the aerolites of the Pultusk shower
-_entered our atmosphere_ as a swarm or cluster of distinct meteoric
-masses. It is shown, moreover, by Dr. Galle that this meteor-group had a
-proper motion when it entered the solar system of at least from 4-1/2 to
-7 miles per second.
-
-The foregoing list contains but a small proportion of the meteoric
-stones whose fall has been actually observed. But, besides these, other
-masses have been found so closely similar in structure to aerolites
-whose descent has been witnessed, as to leave no doubt in regard to
-their origin. One of these is a mass of iron and nickel, weighing 1680
-pounds, found by the traveler Pallas, in 1749, at Abakansk, in Siberia.
-This immense aerolite may be seen in the Imperial Museum at St.
-Petersburg. On the plain of Otumpa, in Buenos Ayres, is a meteoric mass
-7-1/2 feet in length, partly buried in the ground. Its estimated weight
-is about 16 tons. A specimen of this stone, weighing 1400 pounds, has
-been removed and deposited in one of the rooms of the British Museum. A
-similar block, of meteoric origin, weighing more than six tons, was
-discovered some years since in the province of Bahia, in Brazil.
-
-
-GENERAL REMARKS.
-
-1. A Committee on Luminous Meteors was appointed several years since by
-the British Association for the Advancement of Science. This committee,
-consisting at present of James Glaisher, F.R.S., Robert P. Greg, F.R.S.,
-Alexander S. Herschel, F.R.A.S., and Charles Brooke, F.R.S., report from
-year to year not only their own observations on aerolites, fire-balls,
-and falling stars, but also such facts bearing upon the subject as can
-be derived from other sources. An analysis of these reports justifies
-the conclusion that meteoric stone-falls, like star-showers, occur with
-greater frequency than usual on or about particular days. These epochs,
-established with more or less certainty, are the following:
-
- (_a._) January 4th.
- (_b._) " 16th.
- (_c._) " 29th.
- (_d._) February 10th.
- (_e._) " 15th--18th.
- (_f._) March 6th.
- (_g._) " 12th.
- (_h._) April 1st.
- (_i._) " 10th--14th.
- (_j._) May 8th--9th.
- (_k._) " 13th--14th.
- (_l._) " 17th--19th.
- (_m._) June 3d.
- (_n._) " 9th.
- (_o._) " 12th.
- (_p._) " 16th.
- (_q._) July 3d--4th.
- (_r._) " 14th--17th.
- (_s._) August 5th--7th.
- (_t._) " 11th.
- (_u._) September 4th--10th.
- (_v._) October 13th.
- (_w._) November 5th.
- (_x._) " 12th--13th.
- (_y._) " 27th--30th.
- (_z._) December 5th.
- (_z'._) " 8th--14th.
- (_z''._) " 27th.
-
-2. It is worthy of remark that no new elements have been found in
-meteoric stones. Humboldt, in his "Cosmos," called attention to this
-interesting fact. "I would ask," he remarks, "why the elementary
-substances that compose one group of cosmical bodies, or one planetary
-system, may not in a great measure be identical? Why should we not adopt
-this view, since we may conjecture that those planetary bodies, like all
-the larger or smaller agglomerated masses revolving round the sun, have
-been thrown off from the once far more expanded solar atmosphere, and
-have been formed from vaporous rings describing their orbits round the
-central body?"
-
-3. But while aerolites contain no elements but such as are found in the
-earth's crust, the manner in which these elements are combined and
-arranged is so peculiar that a skillful mineralogist will readily
-distinguish them from terrestrial substances.
-
-4. Of the eighteen or nineteen elements hitherto observed in meteoric
-stones, iron is found in the greatest abundance. The specific gravities
-vary from 1.94 to 7.901: the former being that of the stone of Alais;
-the latter that of the meteorite of Wayne county, Ohio, described by
-Professor J. L. Smith in _Silliman's Journal_ for November, 1864, p.
-385.
-
-5. The average number of aerolitic falls in a year was estimated by
-Schreibers at 700. Baron Reichenbach, however, after a discussion of the
-data at hand, makes the number much larger. He regards the probable
-annual average for the entire surface of the earth as not less than
-4500. This would give twelve daily falls. They are of every variety as
-to magnitude, from a weight of less than a single ounce to over fifteen
-tons. The baron even suspects the meteoric origin of large masses of
-dolerite which all former geologists had considered native to our
-planet.
-
-6. An analysis of any extensive table of meteorites and fire-balls
-proves that a greater number of aerolitic falls have been observed
-during the months of June and July, when the earth is near its aphelion,
-than in December and January, when near its perihelion. It is found,
-however, that the reverse is true in regard to bolides, or fire-balls.
-These facts are susceptible of an obvious explanation. The fall of
-meteoric stones would be more likely to escape observation by night than
-by day, on account of the relatively small number of observers. But the
-days are shortest when the earth is in perihelion, and longest when in
-aphelion; the ratio of their lengths being nearly equal to that of the
-corresponding numbers of aerolitic falls. On the other hand, it is
-obvious that fire-balls, unless very large, would not be visible during
-the day. The _observed_ number will therefore be greatest when the
-nights are longest; that is, when the earth is near its perihelion.
-This, it will be found, is precisely in accordance with observation.
-
-
-
-
-CHAPTER VIII.
-
-SHOOTING-STARS.--METEORS OF NOVEMBER 14.
-
-
-Although shooting-stars have doubtless been observed in all ages of the
-world, it is only within the last half century that they have attracted
-the special attention of scientific men. A few efforts had been made to
-determine the height of such meteors, but the first general interest in
-the subject was excited by the brilliant meteoric display of November
-13, 1833. This shower of fire can never be forgotten by those who
-witnessed it. The meteors were observed from the West Indies to British
-America, and from 60 deg. to 100 deg. west longitude from Greenwich. As early as
-10 o'clock on the evening of the 12th shooting-stars were observed with
-unusual frequency; their motions being generally westward. Soon after
-midnight their numbers became so extraordinary as to attract the
-attention of all who happened to be in the open air. The meteors,
-however, became more and more numerous till 4, or half past 4, o'clock;
-and the fall did not entirely cease till ten minutes before sunrise.
-From 2 to 6 o'clock the numbers were so great as to defy all efforts at
-counting them; while their brilliancy was such that persons sleeping in
-rooms with uncurtained windows were aroused by their light. The meteors
-varied in apparent magnitude from the smallest visible points to
-fire-balls equaling the moon in diameter. Occasionally one of the larger
-class would separate into several parts, and in some instances a
-luminous train remained visible for three or four minutes. No sound
-whatever accompanied the display. It was noticed by many observers that
-all the meteors diverged from a point near the star _Gamma Leonis_; in
-other words, their paths if traced backward would intersect each other
-at a particular locality in the constellation Leo. In some parts of the
-country the inhabitants were completely terror-stricken by the
-magnificence of the display. In the afternoon of the day on which the
-shower occurred the writer met with an illiterate farmer who, after
-describing the phenomena as witnessed by himself, remarked that "the
-stars continued to fall till none were left," and added, "I am anxious
-to see how the heavens will appear this evening; I believe we shall see
-no more stars." A gentleman of South Carolina described the effect on
-the negroes of his plantation as follows:--"I was suddenly awakened by
-the most distressing cries that ever fell on my ears. Shrieks of horror
-and cries for mercy I could hear from most of the negroes of the three
-plantations, amounting in all to about 600 or 800. While earnestly
-listening for the cause I heard a faint voice near the door, calling my
-name. I arose, and, taking my sword, stood at the door. At this moment I
-heard the same voice still beseeching me to arise, and saying, 'O my
-God, the world is on fire!' I then opened the door, and it is difficult
-to say which excited me the most,--the awfulness of the scene, or the
-distressed cries of the negroes. Upwards of a hundred lay prostrate on
-the ground,--some speechless, and some with the bitterest cries, but
-with their hands raised, imploring God to save the world and them. The
-scene was truly awful; for never did rain fall much thicker than the
-meteors fell towards the earth; east, west, north, and south, it was the
-same."
-
-At the time of this wonderful meteoric display Captain Hammond, of the
-ship _Restitution_, had just arrived at Salem, Massachusetts, where he
-observed the phenomenon from midnight till daylight. He recollected with
-astonishment that precisely one year before, viz., on the 13th of
-November, 1832, he had observed a similar appearance (although the
-meteors were less numerous) at Mocha, in Arabia. It was found, moreover,
-as a further and most remarkable coincidence, that an extraordinary fall
-of meteors had been witnessed on the 12th of November, 1799. This was
-seen and described by Andrew Ellicott, Esq., who was then at sea near
-Cape Florida. It was also observed by Humboldt and Bonpland, in Cumana,
-South America. Baron Humboldt's description of the shower is as
-follows:--"From half after two, the most extraordinary luminous meteors
-were seen toward the east. Thousands of bolides and falling stars
-succeeded each other during four hours. They filled a space in the sky
-extending from the true east 30 deg. toward the north and south. In an
-amplitude of 60 deg. the meteors were seen to rise above the horizon at
-E.N.E. and at E., describe arcs more or less extended, and fall toward
-the south, after having followed the direction of the meridian. Some of
-them attained a height of 40 deg., and all exceeded 25 deg. or 30 deg. Mr. Bonpland
-relates, that from the beginning of the phenomenon there was not a space
-in the firmament equal in extent to three diameters of the moon, that
-was not filled at every instant with bolides and falling stars. The
-Guaiqueries in the Indian suburb came out and asserted that the firework
-had begun at one o'clock. The phenomenon ceased by degrees after four
-o'clock, and the bolides and falling stars became less frequent; but we
-still distinguished some toward the northeast a quarter of an hour after
-sunrise."
-
-This wonderful correspondence of dates excited a very lively interest
-throughout the scientific world. It was inferred that a recurrence of
-the phenomenon might be expected, and accordingly arrangements were made
-for systematic observations on the 12th, 13th, and 14th of November. The
-periodicity of the shower was thus, in a very short time, placed wholly
-beyond question. The facts in regard to the phenomena of November 13,
-1833, were collected and discussed by Olmsted, Twining, and other
-astronomers. The inquiry, however, very naturally arose whether any
-trace of the same meteoric group could be found in ancient times. To
-determine this question many old historical records were ransacked by
-the indefatigable scientist, Edward C. Herrick, in our own country, and
-by Arago, Quetelet, and others, in Europe. These examinations led to the
-discovery of ten undoubted returns of the November shower previous to
-that of 1799. The descriptions of these former meteoric falls are given
-by Professor H. A. Newton in the _American Journal of Science_, for May,
-1864. They occurred in the years 902, 931, 934, 1002, 1101, 1202, 1366,
-1533, 1602, and 1698. Historians represent the meteors of A.D. 902 as
-innumerable, and as moving like rain in all directions. The exhibition
-of 1202 was scarcely less magnificent. "On the last day of Muharrem,"
-says a writer of that period, "stars shot hither and thither in the
-heavens, eastward and westward, and flew against one another like a
-scattering swarm of locusts, to the right and left; this phenomenon
-lasted until daybreak; people were thrown into consternation, and cried
-to God the Most High with confused clamor." The shower of 1366 is thus
-described in a Portuguese chronicle, quoted by Humboldt: "In the year
-1366, twenty-two days of the month of October being past, three months
-before the death of the king, Don Pedro (of Portugal), there was in the
-heavens a movement of stars such as men never before saw or heard of. At
-midnight, and for some time after, all the stars moved from the east to
-the west; and after being collected together, they began to move, some
-in one direction and others in another. And afterward they fell from the
-sky in such numbers, and so thickly together, that as they descended low
-in the air they seemed large and fiery, and the sky and the air seemed
-to be in flames, and even the earth appeared as if ready to take fire.
-That portion of the sky where there were no stars seemed to be divided
-into many parts, and this lasted for a long time."
-
-
-The Showers of 1866-9.
-
-The fact that all great displays of the November meteors have taken
-place at intervals of 33 or 34 years, or some multiple of that period,
-had led to a general expectation of a brilliant shower in 1866. In this
-country, however, the public curiosity was much disappointed.[22] The
-numbers seen were greater than on ordinary nights, but not such as would
-have attracted any special attention. The greatest number recorded at
-any one station was seen at New Haven by Professor Newton. On the night
-of the 12th 694 were counted in five hours and twenty minutes, and on
-the following night, 881 in five hours. A more brilliant display was,
-however, witnessed in Europe. Meteors began to appear in unusual
-frequency about 11 o'clock on the night of the 13th, and their numbers
-continued to increase with great rapidity for more than two hours; the
-maximum being reached a little after 1 o'clock. A writer in Edinburgh,
-Scotland, thus describes the phenomenon as observed at that
-city:--"Standing on the Calton Hill, and looking westward,--with the
-observatory shutting out the lights of Princes Street,--it was easy for
-the eye to delude the imagination into fancying some distant enemy
-bombarding Edinburgh Castle from long range; and the occasional
-cessation of the shower for a few seconds, only to break out again with
-more numerous and more brilliant drops of fire, served to countenance
-this fancy. Again, turning eastward, it was possible now and then to
-catch broken glimpses of the train of one of the meteors through the
-grim dark pillars of that ruin of most successful manufacture, the
-National Monument; and in fact from no point in or out of the city was
-it possible to watch the strange rain of stars, pervading as it did all
-points of the heavens, without pleased interest and a kindling of the
-imagination, and often a touch of deeper feeling that bordered on awe."
-At London about 1 o'clock a single observer counted 200 in two minutes.
-The whole number seen at Greenwich was 8485. The shower was also
-observed in different countries on the continent.
-
- [22] The first indication of the approaching shower was the appearance
- of meteors in unusual numbers at Malta, on the 13th of November,
- 1864. In 1865, as observed at Greenwich and other stations, they
- were still more numerous.
-
-In 1867 the display was generally observed throughout the United States.
-From the able and interesting reports of Commodore Sands and Professors
-Newcomb, Harkness, and Eastman, we derive the following facts in regard
-to the shower as seen at Washington, D. C.:
-
- Commencement 1_h._ 0_m._ A.M. Nov. 14.
- Maximum 4 20 " "
- End 5 0 " "
- Number of meteors per hour at maximum 3000
- Mean height on first appearance 75 miles.
- " " on disappearance 55 "
- Position of radiant, R. A. 151 deg., Decl. 22-1/2 deg.
-
-The shower of 1868 was in some respects quite remarkable, though the
-number of meteors was less than in 1866 or 1867. At New Haven the fall
-commenced about midnight, and from 2 o'clock till daybreak over 5000
-meteors were counted. The time of maximum could not be accurately
-determined, as no decrease in the numbers was observable till dawn. The
-display was also witnessed in England and in Cape Colony, South Africa.
-The times of maxima in these countries differed so materially as to
-indicate a decided stratification of the meteoric stream. The entire
-depth, moreover, where crossed by the earth in 1868, was much greater
-than at the part traversed either in 1866 or 1867.
-
-In 1869 the shower was observed at Port Said, Lower Egypt, by G. L.
-Tupman, Esq.; in Florida, U. S., by Commander William Gibson, U.S.N.;
-and at Santa Barbara, California, by Mr. G. Davidson and Mrs. E.
-Davidson. The first observed 112 meteors in 1h. 54m., from 2h. 30m. to
-4h. 24m., Alexandria mean time; the numbers during this interval being
-nearly equal, though slightly decreasing. Throughout the morning
-(November 14) the sky was only partly clear. The two observers at Santa
-Barbara saw 556 in 2h. 25m., ending at 3h. 43m. A.M. In Florida also the
-display was quite brilliant, though inferior to that of 1868. It should
-be remarked that the morning in many parts of the United States was
-cloudy. No considerable number of the meteors of this stream has been
-observed in any part of the world since 1869.
-
-
-DISCUSSION OF THE PHENOMENA.
-
-Since the memorable display of November 13, 1833, the phenomena of
-shooting-stars have been observed and discussed with a very lively
-interest. Among the first laborers in this department of research the
-names of Olmsted, Herrick, and Twining must ever hold a conspicuous
-place. The fact that the position of the radiant point did not change
-with the earth's rotation at once placed the cosmical origin of the
-meteors wholly beyond question. The theory of a ring of nebulous matter
-revolving round the sun in an elliptic orbit--a theory somewhat
-different from that proposed by Olmsted--was found to afford a simple
-and satisfactory explanation of the phenomena. This hypothesis of an
-eccentric stream of meteors intersecting the earth's orbit was adopted
-by Humboldt, Arago, and others, shortly after the occurrence of the
-meteoric shower of 1833.
-
-A few years previous to the display of 1866 it was shown by Professor
-Newton, of Yale College, that the distribution of meteoric matter around
-the ring or orbit is far from uniform; that the motion is retrograde;
-that the node of the orbit has an annual forward motion of 102''.6 with
-respect to the equinox, or of 52''.4 with respect to the fixed stars;
-that the periodic time must be limited to five accurately determined
-periods, viz.: 180.05 days, 185.54 days, 354.62 days, 376.5 days, or
-33.25 years; and that the inclination of the orbit to the ecliptic is
-about 17 deg. Professor Newton, for reasons assigned, regarded the third
-period named as the most probable. He remarked, however, that by
-computing the secular motion of the node for each periodic time, and
-comparing the result with the known precession, it was possible to
-determine which of the five periods is the correct one.
-
-For the application of this crucial test,--a problem of more than
-ordinary interest,--we are indebted to Professor J. C. Adams, of
-Cambridge, England. By an elegant analysis it was first shown that for
-either of the first four periods designated by Professor Newton, the
-annual motion of the node, resulting from planetary perturbation, would
-be considerably less than one half of the observed motion. It only
-remained, therefore, to examine whether the period of 33-1/4 years would
-give a motion of the node corresponding with observation. Professor
-Adams found that in this time the longitude of the node is increased 20'
-by the action of Jupiter, 7' by the action of Saturn, and 1' by that of
-Uranus. The effect of the other planets is scarcely perceptible. The
-_calculated_ motion in 33-1/4 years is therefore 28'. The _observed_
-motion in the same time, according to Professor Newton, as previously
-stated, is 29'. This remarkable accordance was at once accepted by
-astronomers as satisfactory evidence that the period is about 33.25
-years.
-
-Having determined the periodic time, the mean distance, or semi-axis
-major, is found by Kepler's third law to be 10.34. The aphelion is
-consequently situated at a comparatively short distance beyond the orbit
-of Uranus. The orbit is represented in Fig. 4.
-
-[Illustration: Fig. 4.]
-
-It was stated at the close of Chapter VI. that shooting-stars are the
-dissevered fragments of cometic matter, which, penetrating our
-atmosphere, are rendered luminous by the resistance so encountered. The
-discovery that comets and meteors are actually moving in the same orbits
-was first announced by Signor Schiaparelli in 1867. The coincidence of
-the orbits of Tempel's comet[23] as computed by Dr. Oppolzer, and the
-meteors of November 14 as determined by Schiaparelli, is too close to be
-regarded as merely accidental. These elements are as follows:
-
- Nov. Meteors. Tempel's Comet.
- Perihelion passage Nov. 10.092, 1866. Jan. 11.160, 1866.
- Passage of descending node Nov. 13.576,
- Longitude of perihelion 56 deg. 26' 60 deg. 28'
- Longitude of ascending node 231 deg. 28' 231 deg. 26'
- Inclination 17 deg. 44' 17 deg. 18'
- Perihelion distance 0.9873 0.9765
- Eccentricity 0.9046 0.9054
- Semi-major axis 10.3400 10.3240
- Periodic time 33.2500 _y._ 33.1760 _y._
- Motion Retrograde. Retrograde.
-
- [23] See page 30.
-
-The fact is thus obvious that the meteors of November 14 are the
-products of the comet's gradual dissolution. It has been stated that the
-comets of 1366 and 1866 are probably identical. The interval indicates a
-period of 33.283 years--greater by 39 days than that found by Oppolzer.
-With this value of the periodic time and the known secular variation of
-the node it is found that the comet and Uranus were in close proximity
-about the beginning of the year 547 B.C. It is therefore not improbable
-that the former was then thrown into its present orbit by the attraction
-of the latter. The celebrated Leverrier designated the year 126 of our
-era as the probable epoch of the comet's entrance into our system. This
-date, however, is incompatible with the period here adopted. It is
-worthy of remark, moreover, as bearing on this question, that the
-extension of the cluster in the tenth century, as indicated by the
-showers of 902, 931, and 934, was too great to have been effected in so
-short a period as 800 years.
-
-With the period of 33.283 years it is easy to find that the comet will
-make a near approach to the earth about the 16th or 17th of November,
-1965, and to Uranus in 1983. At one of these epochs the cometary orbit
-will probably undergo considerable transformation.
-
-We have seen that the comet of 1866, and also the meteoroids following
-in its path, have their perihelion at the orbit of the earth, and their
-aphelion at the orbit of Uranus. Both planets, therefore, at each
-encounter with the current not only appropriate a portion of the
-meteoric matter, but entirely change the orbits of many meteoroids. In
-regard to the devastation produced by the earth in passing through the
-cluster, it is sufficient to state that, according to Weiss, the meteor
-orbits resulting from the disturbance will have all possible periods
-from 21 months to 390 years. It may be regarded, therefore, as evidence
-of the recent[24] introduction of this meteor-stream into the solar
-system that the comet of 1866, which constitutes a part of the cluster,
-has not been deflected from the meteoric orbit by either the earth or
-Uranus.
-
- [24] Recent in comparison with the origin of the August meteors,
- which constitute a continuous ring.
-
-
-
-
-CHAPTER IX.
-
-OTHER METEORIC STREAMS.
-
-
-_The Meteors of August 7-11._--Muschenbroek, in his "Introduction to
-Natural Philosophy," published in 1762, stated as the result of his own
-observations that shooting-stars are more abundant in August than in any
-other part of the year. The fact, however, that a maximum occurs on the
-9th or 10th of the month was first shown by Quetelet in 1835. Since that
-time the shower has been regularly observed both in Europe and America;
-the number of meteors at the maximum sometimes amounting to 160 per
-hour. Their tracks when produced backward intersect each other at a
-particular point in the constellation Perseus.
-
-Of the 315 meteoric displays given in Quetelet's catalogue, 63 belong to
-the August epoch. Their dates up to the commencement of the present
-century are as follows:
-
- 1. A.D. 811, July 25th.
- 2. 820, " 25th-30th.
- 3. 824, " 26th-28th.
- 4. 830, " 26th.
- 5. 833, " 27th.
- 6. 835, " 26th.
- 7. 841, " 25th-30th.
- 8. 924, " 27th-30th.
- 9. 925, " 27th-30th.
- 10. 926, " 27th-30th.
- 11. 933, " 25th-30th.
- 12. 1243, Aug. 2d.
- 13. 1451, " 7th.
- 14. 1709, " 8th.
- 15. 1779, " 9th-10th.
- 16. 1781, " 8th.
- 17. 1784, " 6th-9th.
- 18. 1789, " 10th.
- 19. 1798, " 9th.
- 20. 1799, " 9th-10th.
- 21. 1800, " 10th.
-
-As the earth is about five days in crossing the ring, its breadth in
-some parts cannot be less than 8,000,000 miles.
-
-In 1866 Professor Schiaparelli, on computing the orbit of this meteoric
-stream, noticed the remarkable agreement of its elements with those of
-Swift's or Tuttle's comet[25] (1862, III.), as computed by Dr. Oppolzer.
-These coincidences are exhibited in the following table:
-
- Meteors of Comet III.
- August 10. of 1862.
-
- Longitude of perihelion 343 deg. 38' 344 deg. 41'
- Ascending node 138 deg. 16' 137 deg. 27'
- Inclination 63 deg. 3' 66 deg. 25'
- Perihelion distance 0.9643 0.9626.
- Period 105 years (?) 121.5 years.
- Motion Retrograde. Retrograde.
-
- [25] Mr. Swift, of Marathon, N. Y., had two or three days priority
- in the discovery of this comet, but unfortunately delayed his
- announcement of the fact.
-
-It appears, therefore, that the third comet of 1862 is a part of the
-meteoric stream whose orbit is crossed by the earth on the 10th of
-August.
-
-The characteristics of different meteor-zones afford interesting
-indications in regard to their relative age, the magnitude and
-composition of their corpuscles, etc. Thus, if we compare the streams of
-August 10 and November 14, we shall find that the former probably
-entered our system at a comparatively remote epoch. We have seen that at
-each return to perihelion the meteoric cluster is extended over a
-greater arc of its orbit. Now, Tuttle's comet and the August meteors
-undoubtedly constituted a single group previous to their entering the
-solar domain. It is evident, however, from the annual return of the
-shower during the last 90 years, that the ring is at present nearly if
-not quite continuous. That the meteoric mass had completed many
-revolutions before the ninth century of our era is manifest from the
-frequent showers observed between the years 811 and 841. At the same
-time, the long interval of 83 years between the last observed display in
-the ninth century, and the first in the tenth, seems to indicate the
-existence of a wide chasm in the ring no more than a thousand years
-since.
-
-Neither the period of the meteors nor that of the comet can yet be
-regarded as accurately ascertained. The latter, however, in all
-probability, exceeds the former by several years. Now, at each passage
-of the earth through the elliptic stream, those meteoroids nearest the
-disturbing body must be thrown into orbits differing more or less from
-that of the primitive group. In like manner the near approach of the
-_comet_ to the earth at an ancient epoch may account for the lengthening
-of its periodic time.
-
-
-The Meteors of November 27.
-
-Professor Schiaparelli's brilliant discovery of the relation between
-comets and meteors may now be ranked with the established truths of
-astronomy. His hypothesis, however, in regard to the _origin_ of
-meteoric streams has not been generally accepted. Comets and meteors,
-according to his theory, are derived from cosmical clouds existing in
-great numbers in stellar space. These nebulae, in consequence of their
-own motion or that of the sun, are drawn towards the centre of our
-system. By the unequal influence of the sun's attraction on different
-parts, such clouds are transformed into currents of great length before
-reaching the limits of the planetary system. Shooting-stars, fire-balls,
-aerolites, and comets being all of the same nature, differing merely in
-size, sometimes fall towards the sun as parts of the same current.
-
-The views of Dr. Weiss, of Vienna, differ from those of Schiaparelli, in
-that he regards comets as the original bodies by whose disintegration
-meteor-streams are gradually formed.[26] "Cosmical clouds," he remarks,
-"undoubtedly appear in the universe, but only of such density that in
-most cases they possess sufficient coherence to withstand the
-destructive operation of the sun's attraction, not only up to the
-boundaries of our solar system, but even within it. Such cosmical clouds
-will always appear to us as comets when they pass near enough to the
-earth to become visible. Approaching the sun, the comet undergoes great
-physical changes, which finally affect the stability of its structure:
-it can no longer hold together: parts of it take independent orbits
-around the sun, having great resemblance to the orbit of the parent
-comet. With periodical comets, this process is repeated at each
-successive approach to the sun. Gradually the products of disintegration
-are distributed along the comet's orbit, and if the earth's orbit cuts
-this, the phenomenon of shooting-stars is produced."
-
- [26] _Astr. Nach._, Nos. 1710, 1711. For a fuller statement of
- Schiaparelli's theory, see Silliman's Journal for May, 1867.
-
-These views of the distinguished astronomer of Vienna are confirmed by
-the star-shower of November 27, 1872. That the orbits of the earth and
-Biela's comet intersect at the point passed by the former about the last
-of November, and that in 1845 the comet separated into two visible
-parts, has been stated in a previous chapter. The comet's non-appearance
-in December, 1865, and in September, 1872, was regarded by astronomers
-as presumptive evidence of its progressive dissolution. A meteoric
-shower, resulting from the earth's collision with the cometary _debris_,
-was accordingly expected about the 27th of November.
-
-The first indication of the approaching display appeared on the evening
-of November 24, when meteors in unusual numbers were observed by
-Professor Newton, at New Haven, Connecticut. On Wednesday evening, the
-27th, from the close of twilight till 8 o'clock, a decided shower of
-shooting-stars was noticed in various parts of the United States. At
-Greencastle, Indiana, Professor Joseph Tingley counted 110 meteors in 40
-minutes, and at Princeton, in the same State, Mr. D. Eckley Hunter
-counted 70 in 80 minutes. The numbers seen at New Haven were
-considerably greater. The fact that the display commenced before
-daylight had entirely closed seemed to indicate that only the
-termination of the shower had been observed in this country. Accordingly
-the display was soon found to have been witnessed from 60 deg. E. to 90 deg. W.
-of Greenwich, or through 150 deg. of longitude. In England the first bolide
-of the swarm was seen by M. M. Brinkley, at 3 o'clock, P.M., in full
-daylight. The meteors were most numerous in the southern part of the
-continent, particularly in Italy. At the Observatory of Breslau,
-according to M. Faye, 3000 were seen from 6h. 30m. to 7h. 50m. Dr. Heis
-reported that at Muenster 2500 per hour were counted by two observers. At
-Naples, Signor Gasparis observed two meteors per second. At Turin, M.
-Denza, Director of the Observatory, reported 33,400 in 6h. 30m.; many of
-various and delicate colors, and followed by long and brilliant trains.
-At some points the numbers were so great that an accurate enumeration
-was wholly impossible. In short, the display was decidedly the most
-brilliant that has occurred since that of November 13, 1833.
-
-But some of the most interesting circumstances in connection with the
-phenomena of November 27, 1872, remain to be detailed. Astronomers
-without exception regarded the display as due to the earth's passage
-through the _debris_ following in the path of Biela's comet. In
-accordance with this view Dr. Klinkerfues, of Gottingen, concluded that
-the comet itself, or rather its largest portion, ought to be found in
-the region of the heavens nearly opposite to that from which the
-meteoroids appeared to radiate.[27] As this point in the southern
-hemisphere could not be observed in Europe, he conceived the happy idea
-of detecting the fugitive _by means of the electric telegraph_. The
-following was accordingly dispatched to Mr. Pogson, Director of the
-Government Observatory at Madras, in Southern India: "_Biela touched
-earth on 27th; search near Theta Centauri_." The first two mornings
-after the receipt of this dispatch were cloudy at Madras. On the third,
-however, the cometary fragment was found, and its motion accurately
-measured. The observer described it as circular and rather bright, with
-no traces of a tail. But one fragment could be detected. On the next
-morning, December 3, the comet was again observed. Its diameter had
-sensibly increased; it had a bright nucleus, and still presented a
-circular aspect. A faint tail was also noticed, equal in length to
-one-fourth of the moon's apparent diameter. The following mornings being
-again cloudy, no further observations could be obtained. This cometary
-mass will be in close proximity to the earth about the last of November,
-1892. Another brilliant meteoric shower may therefore be expected at
-that epoch.
-
- [27] The radiant of the Biela meteors is near _Gamma Andromedae_.
-
-
-The Meteors of April 20.
-
-Meteoric showers have occurred about the 20th of April in the following
-years:
-
- B.C. 687
- 15
- A.D. 582
- 1093 }
- 1094 }
- 1095 }
- 1096 }
- 1122 }
- 1123 }
- 1803
-
-The probability that these meteors are derived from a ring which
-intersects the earth's orbit, was first suggested by Arago in 1836. A
-comparison of dates led Herrick to designate 27 years as the probable
-period of the cluster. In the _Astronomische Nachrichten_, No. 1632, Dr.
-Weiss called attention to the fact that the orbit of the first comet of
-1861 very nearly intersects that of the earth, in longitude 210 deg.--the
-point passed by the latter at the epoch of the April meteoric shower. A
-relation between the meteors and the comet, indicating an approximate
-equality of periods, was thus suggested as probable. But the comet,
-according to Oppolzer, does not complete a revolution in less than 415
-years. If, therefore, the meteoric period is nearly the same, the known
-dates of star-showers indicate a diffusion of meteoroids around one half
-of the orbit previous to the display of the year 15 B.C. No subsequent
-perturbation, then, of a particular _part_ could sensibly effect the
-general orbit of the stream. The infrequency of the display renders,
-therefore, the hypothesis of a long period extremely improbable.
-
-The entire interval between 687 B.C. and A.D. 1803 is 2490 years, or 92
-periods of 27.0652 years; and the known dates are all satisfied by the
-following scheme:
-
- B.C. 687 to B.C. 15 .. 672 years = 25 periods of 26.8800 _y._ each.
- 15 to A.D. 582 .. 597 " = 22 " 27.1363 "
- A.D. 582 to 1095 .. 513 " = 19 " 27.0000 "
- 1095 to 1122 .. 27 " = 1 " 27.0000 "
- 1122 to 1803 .. 681 " = 25 " 27.2400 "
-
-With a period of 27 years, the perihelion being interior to the earth's
-orbit, the aphelion distance of the meteors would be very nearly equal
-to the distance of Uranus. The next shower, if the assumed period be
-correct, ought to occur about 1884. It is worthy of remark that near the
-time of the last (hypothetical) return Mr. Du Chaillu witnessed the
-meteors of this epoch, in considerable numbers, in the interior of
-Africa.
-
-
-The Meteors of December 12.
-
-Meteoric showers have occurred about the 12th of December in the
-following years:
-
-1. A.D. 901. "The whole hemisphere was filled with those meteors called
-falling-stars from midnight till morning, to the great surprise of the
-beholders in Egypt."
-
-2. In 930 a remarkable shower of falling stars was observed in China.
-
-3. Extraordinary meteoric phenomena were observed at Zurich at the same
-epoch in 1571.
-
-4. On the night of the 11th and 12th of December, 1833, a great number
-of shooting-stars were seen at Parma. At the maximum as many as ten
-were visible at the same time.
-
-5. (Doubtful.) 1861, 1862, and 1863. Maximum probably in 1862. The
-meteors at this return were far from being comparable in numbers with
-the ancient displays. The shower, however, was distinctly observed.
-R. P. Greg, Esq., of Manchester, England, says the period of December
-12, 1862, was "exceedingly well defined."
-
-These dates indicate a period of about 29-1/8 years. Thus:
-
- 901 to 930 1 period of 29.000 years.
- 930 to 1571 22 periods of 29.136 "
- 1571 to 1833 9 periods of 29.111 "
- 1833 to 1862 1 period of 29.000 "
-
-
-Meteors of October 16-20.
-
-Meteoric showers were observed from the 16th to the 20th of October in
-the years 288, 1436, 1439, 1743, and 1798. These dates render it
-somewhat probable that the period is about 27-1/2 years. Thus:
-
- A.D. 288 to 1439 42 periods of 27.405 years each.
- 1439 to 1743 11 " 27.636 " "
- 1743 to 1798 2 " 27.500 " "
-
-If these periods are correct, it is a remarkable coincidence that the
-aphelion distances of the meteoric rings of April 20, October 18,
-November 14, and December 12, as well as those of the comets 1866 I.,
-and 1867 I., are all nearly equal to the mean distance of Uranus.
-
-
-The Meteors of April 30, May 1.
-
-Professor Schiaparelli, in his list of meteoric showers whose radiant
-points are derived from observations made in Italy during the years
-1868, 1869, and 1870, describes one as occurring on April 30 and May 1;
-the radiant being in the Northern Crown. The same shower has also been
-recognized by R. P. Greg, F.R.S., of Manchester, England. This
-meteor-stream, it is now proposed to show, is probably derived from one
-much more conspicuous in ancient times.
-
-In Quetelet's "Physique du Globe" we find meteoric displays of the
-following dates. In each case the corresponding day for 1870 is also
-given,[28] in order to exhibit the close agreement of the epochs:
-
- 1. A.D. 401, April 9th; corresponding to April 29th, for 1870.
- 2. 538, " 6th; " April 25th, "
- 3. 839, " 17th; " May 1st, "
- 4. 927, " 17th; " April 30th, "
- 5. 934, " 18th; " May 1st, "
- 6. 1009, " 16th; " April 28th, "
-
- [28] Making proper allowance for the precession of the equinoxes.
-
-The epochs of 927 and 934 suggest as probable the short period of 7
-years. It is found accordingly that the entire interval of 608
-years--from 401 to 1009--is equal to 89 mean periods of 6.8315 years
-each. With this approximate value the six dates are all represented as
-follows:
-
- From A.D. 401 to A.D. 538, 20 periods of 6.85 years.
- 538 to 839, 44 " 6.84 "
- 839 to 927, 13 " 6.77 "
- 927 to 934, 1 " 7.00 "
- 934 to 1009, 11 " 6.82 "
-
-This period nearly corresponds to those of several comets whose aphelion
-distances are somewhat greater than the mean distance of Jupiter. So
-long as the cluster occupied but a small arc of the orbit the displays
-would evidently be separated by considerable intervals. The comparative
-paucity of meteors in modern times may be explained by the fact that the
-ring has been subject to frequent perturbations by Jupiter.
-
-
-Groups in which the Meteoroids are sparsely scattered.
-
-By the labors of Heis, Greg, Herschel, Schiaparelli, and others, the
-radiants of more than fifty sparsely strewn meteor-systems have been
-determined. Of these the following, which are well defined, seem worthy
-of special study:
-
- DATE. POSITION OF RADIANT.
- R. A. N. Decl.
- January 1-4 234 deg. 51 deg.
- January 18 232 deg. 36 deg.
- April 25 142 deg. 53 deg.
-
-The orbits and periods, except in the few cases previously considered,
-are entirely unknown. Some of the observed clusters are probably the
-_debris_ of ancient comets whose aphelia were in the vicinity of
-Jupiter's orbit.
-
-
-
-
-CHAPTER X.
-
-THE ORIGIN OF COMETS AND METEORS.
-
-
-The fact that comets and meteors, or at least a large proportion of such
-bodies, have entered the solar system from stellar space, is now
-admitted by all astronomers. The question, however, in regard to the
-origin and nature of these cosmical clouds still remains undecided. The
-theory that they consist of matter expelled with great velocity from the
-fixed stars appears to harmonize the greatest number of facts, and is
-accordingly entitled to respectful consideration. The evidence by which
-it is sustained may be briefly stated as follows:
-
-1. The observations of Zollner, Respighi, and others, have indicated the
-operation of stupendous eruptive forces beneath the solar surface. The
-rose-colored prominences, which Janssen and Lockyer have shown to be
-masses of incandescent hydrogen, are regarded by Professor Respighi as
-phenomena of eruption. "They are the seat of movements of which no
-terrestrial phenomenon can afford any idea; masses of matter, the volume
-of which is many hundred times greater than that of the earth,
-completely changing their position and form in the space of a few
-minutes." The nature of this eruptive force is not understood. We may
-assume, however, that it was in active operation long before the sun
-had contracted to its present dimensions.
-
-2. With an initial velocity of projection equal to 380 miles per second,
-the matter thrown off from the sun would be carried beyond the limits of
-the solar system, never to return. With velocities somewhat less, it
-would be transported to distances corresponding to those of the aphelia
-of the periodic comets.
-
-3. On the 7th of September, 1871, Professor Young, of Dartmouth
-College,[29] witnessed an extraordinary explosion on the sun's surface.
-The observer, with his telescope, followed the expelled matter to an
-elevation of over 200,000 miles. The mean velocity between the altitudes
-of 100,000 and 200,000 miles was 166 miles per second. This rate of
-motion _in vacuo_ would indicate an initial velocity of about 260 miles
-per second. But the sun is surrounded by an extensive atmosphere, whose
-resistance must have greatly retarded the velocity of the outrush before
-reaching the height of 100,000 miles. The original velocity of these
-hydrogen clouds was therefore sufficient, in all probability, to have
-carried them, if unresisted, beyond the solar domain. Solid or dense
-matter propelled with equal force would doubtless have been driven off
-never to return.[30]
-
- [29] Boston Journal of Chemistry, November, 1871.
-
- [30] See Mr. Proctor's interesting discussion of this subject in
- the Monthly Notices of the R.A.S., vol. xxxii.
-
-4. This eruptive force, whatever be its nature, is probably common to
-the sun and the so-called fixed stars. If so, the dispersed fragments
-of ejected matter ought to be found in the spaces intervening between
-sidereal systems. Accordingly, the phenomena of comets and meteors have
-demonstrated the existence of such matter, widely diffused, in the
-portions of space through which the solar system is moving.
-
-5. According to Mr. Sorby the microscopic structure of the aerolites he
-has examined points evidently to the fact that they have been at one
-time in a state of fusion from intense heat,--a fact in striking harmony
-with this theory of their origin.
-
-6. The velocity with which some meteoric bodies have entered the
-atmosphere has been greater than that which would have been acquired by
-simply falling toward the sun from any distance, however great. On the
-theory of their sidereal origin, this excess of velocity has been
-dependent on the primitive force of expulsion. The shower of aerolites
-which fell at Pultusk, Poland, on the 30th of January, 1868,[31] is not
-only a remarkable illustration of the fact here stated, but also of
-another which may be accounted for by the same theory, viz.: that
-meteoric bodies sometimes enter the solar system in groups or clusters.
-
- [31] See Chapter VII.
-
-7. A striking argument in favor of this theory may be derived from the
-researches of the late Professor Graham, considered in connection with
-those of Dr. Huggins and other eminent spectroscopists. Professor Graham
-found large quantities of hydrogen confined in the pores or cavities of
-certain meteoric masses. Now, the spectroscope has shown that the sun's
-rose-colored prominences consist of immense volumes of incandescent
-hydrogen; that the same element exists in great abundance in many of the
-fixed stars, and even in certain nebulae; and that the star in the
-Northern Crown, whose sudden outburst in 1866 so astonished the
-scientific world, afforded decided indications of its presence.
-
-
-THE END.
-
-
-
-
-_BY THE AUTHOR OF THIS VOLUME._
-
-
- METEORIC ASTRONOMY:
- A TREATISE ON
- SHOOTING STARS, FIRE BALLS,
- AND AEROLITES.
-
- BY DANIEL KIRKWOOD, LL.D.
-
- 12mo. Extra Cloth. $1.50.
-
-
- For sale by Booksellers generally, or will be sent by mail,
- postpaid, on receipt of the price by
-
- J. B. LIPPINCOTT & CO., Publishers,
- _715 and 717 Market St., Philadelphia_.
-
-
-
-
-Transcriber's Note: Obvious errors in spelling and punctuation have been
-corrected. Footnotes have been renumbered and moved from the page end to
-the end of the paragraph. Images have been moved from the
-middle of a paragraph to the closest paragraph break.
-
-
-
-
-
-
-End of the Project Gutenberg EBook of Comets and Meteors, by Daniel Kirkwood
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