The discovery of Encke's comet, which had a period of only 3 1/3d years, was

speedily followed, in 1826, by that of another, Biela's comet, whose period

of revolution is 6 3/4th years, and which is likewise planetary, having its

aphelion beyond the orbit of Jupiter, but within that of Saturn. It has a

fainter light than Encke's comet, and, like the latter, its motion is

direct, while Halley's comet moves in a course opposite to that pursued by

the planets. Biela's comet presents the first certain example of the orbit

of a comet intersecting that of the Earth. This position, with reference to

our planet, may therefore be productive of danger, if we can associate an

idea of danger with so extraordinary a natural phenomenon, whose history

presents no parallel, and the results of which we are consequently unable

correctly to estimate. Small masses endowed with enormous velocity may

certainly exercise a considerable power; but Laplace has shown that the mass

of the comet of 1770 is probably not equal to 1/5000th that of the Earth, or

about 1/2000th that of the Moon.*

[footnote] *Laplace, 'Expos. du Syst. du Monde', p. 216, 237.

We must not confound the passage of Biela's comet through the Earth's orbit

with its proximity to, or collision with our globe. When this passage took

place, on the 29th of October, 1832, it required a full month before the

Earth would reach the point of intersection of the two orbits. These two

comets of short periods of revolution also intersect each other, and it has

been justly observed,* that amid the many perturbations experienced by such

small bodies from the largr planets, there is a 'possibility' -- supposing a

meeting of these comets to occur in October -- that the inhabitants of the

Earth may witness the extraordinary spectacle of an encounter between two

cosmical bodies, and possibly of their reciprocal penetration and

amalgamation, or of their destruction by means of exhausting emanations.

[footnote] *Littrow, 'Beschreibende Astron.', 1835, s. 274. On the inner

comet recently discovered by M. Faye, at the Observatory of Paris, and whose

eccentricity is 0.551, its distance at its perihelion 1.690, and its

distance at its aphelion 5.832, see Schumacher, 'Astron. Nachr.', 1844, No.

495. Regarding the supposed identity of the comet of 1766 with the third

comet of 1819, see 'Astr. Nachr.', 1833, No. 239; and on the identity of the

comet of 1743 and the fourth comet of 1819, see No. 237 or the last

mentioned work.

Events of this nature, resulting either from deflection occasioned by

disturbing masses or primevally intersecting orbits, must have been of

frequent occurrence in the course of millions of years in the immeasurable

regions of ethereal space; but they must be regarded as isolated

occurrences, exercising no more general or alternative effects on cosmical

relations than the breaking forth or extinction of a volcano within the

limited sphere of our Earth.

A third interior comet, having likewise a short period of revolution was

discovered by Faye on the 22d of November, 1843, at the Observatory at

Paris. Its elliptic path, which approaches much more nearly to a circle

than that of any other known comet, is included within the orbits of Mars

and Saturn. This comet, therefore, which, according to Goldschmidt, passes

beyond the orbit of Jupiter, is one of the few whose perihelia are beyond

Mars. Its period of revolution is 7 29/100 years, and it is not improbable

that the form of its present orbit may be owing to its great approximation

to Jupiter at the close of the year 1839.

If we consider the comets in their inclosed elliptic orbits as members of

our solar system, and with respect to the length of their major axes, the

amount of their eccentricity, and their periods of revolution, we shall

probably find that the three planetary comets of Encke, Biela, and Faye are

most nearly approached in these respects, first, by the comet discovered in

1766 by Messier, and which is regarded by Clausen as identical with the

third comet of 1819; and next, by the fourth comet of the last-mentioned

year, discovered by Blaupain, but considered by Clausen as identical with

that of the year 1743, and whose orbit appears, like that of Lexell's comet,

to have suffered great variations from the proximity and attraction of

Jupiter. The two last-named comets would likewise seem to have a period of

revolution not exceeding five or six years, and their aphelia are in the

vicinity of Jupiter's orbit. Among the comets that have a period of

revolution of from seventy to

p 109

seventy-six years, the first in point of importance with respect to

theoretical and physical astronomy is Halley's comet, whose last appearance,

in 1835, was much less brilliant than was to be expected from preceding

ones; next we would notice Olbers's comet, discovered on the 6th of March,

1815; and, lastly, the comet discovered by Pons in the year 1812, and whose

elliptic orbit has been determined by Encke. The two latter comets were

invisible to the naked eye. We now know with certainty of nine returns of

Halley's large comet, it having recently been proved by Laugier's

calculations*, that in the Chinese table of comets, first made known to us

by Edward Biot, the comet of 1378 is identical with Halley's; its periods of

revolution have varied in the interval between 1378 and 1835 from 74.91 to

77.58 years, the mean being 76.1.

[footnote] *Laugier, in the 'Comptes Rendus des Seances de l'Academie',

1843, t. xvi., p. 1006.

A host of other comets may be contrasted with the cosmical bodies of which

we have spoken, requiring several thousand years to perform their orbits,

which it is difficult to determine with any degree of certainty. The

beautiful comet of 1811 requires, according to Argelander, a period of 3065

years for its revolution, and the colossal one of 1680 as much as 8800

years, according to Encke's calculation. These bodies respectively recede,

therefore, 21 and 44 times further than Uranus from the Sun, that is to say,

33,600 and 70,400 millions of miles. At this enormous distance the

attractive force of the Sun is still manifested; but while the velocity of

the comet of 1680 at its perihelion is 212 miles in a second, that is,

thirteen times greater than that of the Earth, it scarcely moves ten feet in

the second when at its aphelion. This velocity is only three times greater

than that of water in our most sluggish European rivers, and equal only to

half that which I have observed in the Cassiquiare, a branch of the Orinoco.

It is highly probable that, among the innumerable host of uncalculated or

undiscovered comets, there are many whose major axes greatly exceed that of

the comet of 1680. In order to form some idea by numbers, I do not say of

the sphere of attraction, but of the distance in space of a fixed star, or

other sun, from the aphelion of the comet of 1680 (the furthest receding

cosmical body with which we are acquainted in our solar system), it must be

remembered that, according to the most recent determinations of parallaxes,

the nearest fixed star is full 250 times further removed from our sun than

the comet in its aphelion. The comet's distance is only 44

p 110

times that of Uranus, while 'a' Centauri is 11,000 and 61 Cygni 31,000 times

that of Uranus, according to Bessel's determinations.

Having considered the greatest distances of comets from the central body, it

now remains for us to notice instances of the greatest proximity hitherto

measured. Lexell and Burckhardt's comet of 1770, so celebrated on account

of the disturbances it experienced from Jupiter, has approached the Earth

within a smaller distance than any other comet. On the 28th of June, 1770,

its distance from the Earth was ony six times than of the Moon. The same

comet passed twice, viz., in 1769 and 1779, through the system of Jupiter's

four satellites without producing the slightest notable change in the

well-known orbits of these bodies. The great comet of 1680 approached at

its perihelion eight or nine times nearer to the surface of the Sun than

Lexell's comet did to that of our Earth, being on the 17th of December a

sixth part of the Sun's diameter, or seven tenths of the distance of the

Moon from that luminary. Perihelia occurring beyond the orbit of Mars can

seldom be observed by the inhabitants of the Earth, owing to the faintness

of the light of distant comets; and among those already calculated the comet

of 1729 is the only one which has its perihelion between the orbits of

Pallas and Jupiter; it was even observed beyond the latter.

Since scientific knowledge, although frequently blended with vague and

superficial views, has been more extensively diffused through wider circles

of social life, apprehensions of the possible evils threatened by comets

have acquired more weight as their direction has become more definite. The

certainty that there are within the known planetary orbits comets which

revisit our regions of space at short intervals -- that great disturbances

have been produced by Jupiter and Saturn in their orbits, by which such as

were apparently harmless have been converted into dangerous bodies -- the

intersection of the Earth's orbit by Biela's comet -- the cosmical vapor,

which, acting as a resisting and impeding medium, tends to contract all

orbits -- the individual difference of comets, which would seem to indicate

considerable decreasing gradations in the quantity of the mass of the

nucleus, are all considerations more than equivalent, both as to number and

variety, to the vague fears entertained in early ages of the general

conflagration of the world by 'flaming swords', and stars with 'fiery

streaming hair'. As the consolatory considerations which may be derived

from the calculus of probabilities address themselves to reason and to

p 111

meditative understanding only, and not to the imagination or to a desponding

condition of mind, modern science has been accused, and not entirely without

reason, of not attempting to allay apprehensions which it has been the very

means of exciting. It is an inherent attribute of the human mind to

experience fear, and not hope or joy, at the aspect of that which is

unexpected and extraordinary.*

[footnote] *Fries, 'Vorlesungen uber die Sternkunde', 1833, s. 262-267

(Lectures on the Science of Astronomy). An infelicitously chosen instance

of the good omen of a comet may be found in Seneca, 'Nat. Quest.', vii., 17

and 21. The philosopher thus writes of the comet: "Quem nos Neronis

principatu latissimo vidimus et qui cometis detraxit infamiam."

The strange form of a large comet, its faint nebulous light, and its sudden

appearance in the vault of heaven, have in all regions been almost

invariably regarded by the people at large as some new and formidable agent

inimical to the existing state of things. The sudden occurrence and short

duration of the phenomenon lead to the belief of some equally rapid

reflection of its agency in terrestrial matters, whose varied nature renders

it easy to find events that may be regarded as the fulfillment of the evil

foretold by the appearance of these mysterious cosmical bodies. In our own

day, however, the public mind has taken another and more cheerful, although

singular, turn with regard to comets; and in the German vineyards in the

beautiful valleys of the Rhine and Moselle, a belief has arisen, ascribing

to these once ill-omened bodies a beneficial influence on the ripening of

the vine. The evidence yielded by experience, of which there is no lack in

these days, when comets may so frequently be observed, has not been able to

shake the common belief in the meteorological myth of the existence of

wandering stars capable of radiating heat.

This material taken from pages 111- 147

COSMOS: A Sketch of the Physical Description of the Universe, Vol. 1

by Alexander von Humboldt

Translated by E C Otte

from the 1858 Harper & Brothers edition of Cosmos, volume 1

--------------------------------------------------

From comets I would pass to the consideration of a far more enigmatical

class of agglomerated matter -- the smallest of all asteroids, to which we

apply the name 'aërolites', or 'meteoric stones',* when they reach our

atmosphere in a fragmentary condition.

[footnote] * (Much valuable information may be obtained regarding the

origin and composition of aërolites or meteoric stones in Memoirs on the

subject, by Baumbeer and other writers, in the numbers of Poggendorf's

'Annalen', from 1845 to the present time.) -- Tr.

If I should seem to dwell on the specific enumeration of these bodies, and

of comets, longer than the general nature of this work might warrant, I have

not done so undesignedly. The diversity existing in the individual

characteristics of comets has already been noticed. The imperfect knowledge

we possess of their physical character renders it

p 112

diifficult in a work like the present, to give the proper degree of

circumstantiality to the phenomena, which, although of frequent recurrence,

have been observed with such various degrees of accuracy, or to separate the

necessary from the accidental. It is only with respect to measurements and

computations that the astronomy of comets has made any marked advancement,

and, consequently, a scientific consideration of these bodies must be

limited to a specification of the differences of physiognomy and

conformation in the nucleus and tail, the instances of great approximation

to other cosmical bodies, and of the extremes in the length of their orbits

and in their periods of revolution. A faithful delineation of these

phenomena, as well as of those which we proceed to consider, can only be

given by sketching individual features with the animated circumstantiality

of reality.

Shooting stars, fire-balls, and meteoric stones are, with great probability,

regarded as small bodies moving with planetary velocity, and revolving in

obedience to the laws of general gravity in conic sections round the Sun.

When these masses meet the Earth in their course, and are attracted by it,

they enter within the limits of our atmosphere in a luminous condition, and

frequently let fall more or less strongly heated stony fragments, covered

with a shining black crust. When we enter into a careful investigation of

the facts observed at those epochs when showers of shooting stars fell

periodically in Cumana in 1799, and in North America during the years 1833

and 1834, we shall find that 'fire-balls' can not be considered separately

from shooting stars. Both these phenomena are frequently not only

simultaneous and blended together, but they likewise are often found to

merge into one another, the one phenomenon gradually assuming the character

of the other alike with respect to the size of their disks, the emanation of

sparks, and the velocities of their motion. Although exploding smoking

luminous fire-balls are sometimes seen, even in the brightness of tropical

daylight,* equaling in size the apparent

p 113

diameter of the Moon, innumerable quantities of shooting stars have, on the

other hand, been observed to fall in forms of such extremely small

dimensions that they appear only as moving points or 'phosphorescent

lines.'**

[footnote] *A friend of mine, much accustomed to exact trigonometrical

measurements, was in the year 1788 at Popayan, a city which is 2 degrees 26'

north latitude, lying at an elevation of 5583 feet above the level of the

sea, and at noon, when the sun was shining brightly in a cloudless sky, saw

his room lighted up by a fire-ball. He had his back to the window at the

time, and on turning round, perceived that great part of the path traversed

by the fire-ball was still illuminated by the brightest radiance. Different

nations have had the most various terms to express these phenomena: The

Germans use the word 'Sternschnuppe', literally 'star snuff' -- an

expression well suited to the physical views of the vulgar in former times,

according to which, the lights in the firmament were said to undergo a

process of 'snuffing' or cleaning; and other nations generally adopt a term

expressive of a 'shot' or 'fall' of stars, as the Swedish 'stjernifall', the

Italian 'stella cadente', and the English 'star shoot.' In the woody

district of the Orinoco, on the dreary banks of the Cassiquiare, I heard the

natives in the Mission of Vasiva use terms still more inelegant than the

German 'star snuff.' ('Relation Historique du Voy. aux Régions Equinox.',

t. ii., p. 513.) These same tribes term the pearly drops of dew which cover

the beautiful leaves of the heliconia 'star spit.' In the Lithuanian

mythology, the imagination of the people has embodied its ideas of the

nature and signification of falling stars under nobler and more graceful

symbols. The Parcæ, 'Werpeja', weave in heaven for the new-born child its

thread of fate, attaching each separate thread to a star. When death

approaches the person, the thread is rent, and the star wanes and sinks to

the earth. Jacob Grimm, 'Deutsche Mythologie', 1843, s. 685.

[footnote] ** According to the testimony of Professor Denison Olmsted, of

Yale College, New Haven, Connecticut. (See Poggend., 'Annalen der Physik',

bd. xxx., s. 194.) Kepler, who excluded fire-balls and shooting stars from

the domain of astronomy, because they were, according to his views, "meteors

arising from the exhalations of the earth, and blending with the higher

ether," expresses himself, however, generally with much caution. He says:

"Stellæ cadentes sunt materia viscida inflammata. Earum aliquæ inter

cadendum absumuntur, aliquæ verè in terram cadunt, pondere suo tractæ.

Nec est dissimile vero, quasdam conglobatas esse ex materia fæculentâ, in

ipsam auram ætheream immixta: exque aëtheris regione, tractu rectilineo,

per aërem trajicere, ceu minutos competas, occultâ causa motus

utrorumque." -- Kepler, 'Epit. Astron. Copernicanæ', t. i., p. 80.

It still remains undertermined whether the many luminous bodies that shoot

across the sky may not vary in their nature. On my return from the

equinoctial zones, I was impressed with an idea that in the torrid regions

of the tropics I had more frequently than in our colder latitudes seen

shooting stars fall as if from a height of twelve or fifteen thousand feet;

that they were of brighter colors, and left a more brilliant line of light

in their track; but this impression was no doubt owing to the greater

transparency of the tropical atmosphere*, which enables the eye to penetrate

further into distance.

[footnote] *'Relation Historique', t. i., p. 80, 213, 527. If in falling

stars, as in comets, we distinguish between the head or nucleus and the

tail, we shall find that the greater transparency of the atmosphere in

tropical climates is evinced in the greater length and brilliancy of the

tail which may be observed in those latitudes. The phenomenon is therefore

not necessarily more frequent there, because it is oftener seen and

continues longer visible. The influence exercised on shooting stars by the

character of the atmosphere is shown occasionally even in our temperate

zone, and at very small distances apart. Wartmann relates that on the

occasion of a November phenomenon at two places lying very near each other,

Geneva and Aux Planchettes, the number of the meteors counted were as 1 to

7. (Wartmann, 'Mém. sur les Etoiles filantes', p. 17.) The tail of a

shooting star (or its 'train'), on the subject of which Brandes has made so

many exact and delicate observations, is in no way to be ascribed to the

continuance of the impression produced by light on the retina. It sometimes

continues visible a whole minute, and in some rare instances longer than the

light of the nucleus of the shooting star; in which case the luminous track

remains motionless. (Gilb., 'Ann.', bd. xiv., s. 251.) This circumstance

further indicates the analogy between large shooting stars and fire-balls.

Admiral Krusenstern saw, in his voyage round the world, the train of a

fire-ball shine for an hour after the lluminous body itself had disappeared,

and scarcely move throughout the whole time. ('Reise', th. i., s. 58.) Sir

Alexander Burnes gives a charming description of the transparency of the

clear atmosphere of Bokhara, which was once so favorable to the pursuit of

astronomical observations. Bokhara is situated in 39 degrees 48' north

latitude, and at an elevation of 1280 feet above the level of the sea.

"There is a constant serenity in its atmosphere, and an admirable clearness

in the sky. At night, the stars have uncommon luster, and the Milky Way

shines gloriously in the firmament. There is also a never-ceasing display

of the most brilliant meteors, which dart like rockets in the sky; ten or

twelve of them are sometimes seen in an hour, assuming every color -- fiery

red, blue, pale, and faint. It is a noble country for astronomical science,

and great must have been the advantage enjoyed by the famed observatory of

Samarkand." (Burnes, 'Travels into Bokhara', vol. ii. (1834), p. 158.) A

mere traveler must not be reproached for calling ten or twelve shooting

stars in an hour "many," since it is only recently that we have learned,

from careful observations on this subject in Europe, that eight is the mean

number which may be seen in an hour in the field of vision of one individual

(Quetelet, 'Corresp. Mathém.', Novem., 1837, p. 447); this number is,

however, limited to five or six by that diligent observer, Olbers. (Schum.,

'Jahrb.', 1838, s. 325.)

p 114

Sir Alexander Burnes likewise extols as a consequence of the purity of the

atmosphere in Bokhara the enchanting and constantly-recurring spectacle of

variously-colored shooting stars.

The connection of meteoric stones with the grander phenomenon of fire-balls

-- the former being known to be projected from the latter with such force as

to penetrate from ten to fifteen feet into the earth -- has been proved,

among many other instances, in the falls of azzzuerolites at Barbotan, in

the Department des Landes (24th July, 1790), at Siena (16th June, 1794), at

Weston, in Connecticut, U. S. (14th December, 1807), and at Juvenas in the

Department of Ardèche (14th June, 1821). Meteoric stones are in some

instances thrown from dark clouds suddenly formed in a clear sky, and fall

with a noise resembling thunder. Whole districts have thus occasionally

been covered with thousands of fragmentary masses, of uniform character but

unequal magnitudes, that

p 115

have been hurled from one of these moving clouds. In less frequent cases,

as in that which occurred on the 16th of September, 1843, at Kleinwenden,

near Mühilhausen, a large aërolite fell with a thundering crash while the

sky was clear and cloudless. The intimate affinity between fire-balls and

shooting stars is further proved by the fact that fire-balls, from which

meteoric stones have been thrown have occasionally been found, as at Angers,

on the 9th of June, 1822, having a diameter scarcely equal to that of the

small fire-works called Roman candles.

The formative power, and the nature of the physical and chemical processes

involved in these phenomena are questions all equally shrouded in mystery,

and we are as yet ignorant whether the particles composing the dense mass of

meteoric stones are originally, as in comets, separated from one another

when they become luminous to our sight, or whether in the case of smaller

shooting stars, any compace substance actually falls, or, finally, whether a

meteor is composed only of a smoke-like dust, containing iron and nickel;

while we are wholly ignorant of what takes place within the dark cloud from

which a noise like thunder is often heard for many minutes before the stones

fall.*

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