8. Upon this statement itself, it is only needful to remark, that the

rising of the pillars in the North-east, or to the East of North,

rather than to the North-west, or West of North, almost at the same

time with their first appearance in the North, is not, perhaps,

even as seen between the Lena and Yenesei, so uniformly the case as

M. Gmelin may have been led to believe; and that, at all events,

as above described, the progress of the late display, observed in

London, was, first from North to West, and afterward from West to

East; the North being always the centre, or always light, while the

West and East were changed. The covering of the whole sky, and the

splendour of the scene produced, have been the subject of previous

remark; and the observation, “that the streams (previously called

pillars) are then seen meeting together in the zenith,” entirely

corroborates what the present writer has said of the nature of the

lights seen skimming across the zenith, and across each other, and

the deduction which he has thence made, that the luminous appearances

in the zenith are the summits of those very pillars of which the

bases are on or below the horizon. The clear and calm weather which,

on the shores of the Icy Sea, commonly follows the appearance of

the Aurora is, in some degree, in concord with the phenomena of its

recent appearance in London; where, without any material change

in the temperature, a succession of clear, calm, and bright days

supervened, within a day or two of the Aurora. As to the hissing,

crackling, or rushing noise, which is said to accompany the Aurora

in the more northern regions, and which has sometimes been compared

to that of the furling and [p415] unfurling of flags, there is

nothing difficult, (knowing what we do of the noise of winds and of

thunder,) in admitting its probability, unless what may arise from

the consideration, that the noise might, or might not, be expected

to be heard, where-ever the phenomenon is to be seen. But the most

striking and important truth, communicated in the foregoing account,

is that which we cannot but rigorously infer from the collective

testimony of two very distinct descriptions, which is afforded in two

of the concluding sentences. It consists in that real _infrequency_,

as well in the Northern, as in the Southern Hemisphere, of the

appearance of the Aurora; an _infrequency_ the knowledge of which is

so essential to the true history of the phenomenon, and therefore

to its true philosophy, and consequently to much of the history and

philosophy of nature at large;—an _infrequency_ which the present

writer has given notice of above, as a proposition for which, in

dissent from all received authorities, he will contend; and upon the

opposite account of which matter, in the general account quoted,

he has already requested the reader to suspend his judgment. It is

obvious that, as a natural phenomenon, an Aurora Borealis, which,

though _constantly_ experienced in the more Northerly regions, is but

rarely observed in the more Southern; that is, an Aurora Borealis

which, though familiar to the Samoiede, the Laplander, and even

the Shetlander, is an extraordinary, and a terrific, or at least a

marvellous event, to the Italian, the Frenchman, and even to the

Englishman; it is obvious, that such an Aurora Borealis, _constant_

in its occurrence a little further to the Northward, and almost

the solitary spectacle of a generation a little further to the

South, is, as a natural phenomenon, a very different thing from an

Aurora Borealis which, though far enough to the South, sufficiently

frequent in comparatively trivial magnitudes and lustre, is seen,

either in the South or in the North, in its greatness, and in its

splendour, but yet rarely, and with, perhaps, almost equal rareness;

it is obvious that, as natural phenomena, and not less so as sights

connected by mankind with their own fortunes, the two things now

described are exceedingly unlike as matter of history, and equally so

as matter of philosophy. If we are simply to record the occurrence,

it is one thing to speak of a phenomenon [p416] which, in the South,

is seen only at long intervals, while it is a “constant attendant”

in the North; and another thing to speak of that which, whether

in the South or in the North, is equally rare, and equally out of

the “constant” course of nature. If we are to write the history of

nature, it is one thing to relate, that such phenomena, or rather

others, infinitely more splendid, more terrific, or more marvellous,

than that which was witnessed in London, in the month of September

in this year, or in the same month some three-and-twenty years ago,

or else some six-and-thirty, and, to judge by experience, is not

to be looked for, in the same city, during twenty or thirty years

again;—it is one thing to relate that, in the Shetland Islands,

such a spectacle is a “constant attendant of clear evenings,” and

another thing to relate, that though, perhaps, on clear evenings,

in the Shetland Islands, some small displays of the Aurora are

not unfrequently perceived, yet, that such an exhibition as has

recently been witnessed in London, and still more, such as, more

effulgent, and more extended, and more vigorous, and even coloured

by the atmosphere into the terrific;—that those exhibitions, in

short, of which our naturalists and men of science would persuade

us, that, while beheld nightly by those of the North, they are known

to us by very faint examples alone;—those exhibitions,—that those

extraordinary examples of the brightness and vigour of the Aurora—are

as rare, or almost as rare, not only in the Shetland Islands, but

in Iceland, and on the shores of the Icy Sea, as in the streets of

London themselves! It is obvious, too, that if we are to speak of

this phenomenon philosophically, if we are to attempt to explain its

origin and use,—its source in the natural elements, and its office in

the natural economy; here, too, the solving of this question of the

_frequency_ or _infrequency_, the _constancy_ or the _inconstancy_,

of these mighty exhibitions, even in the North, and under the Pole

itself, is matter of foremost importance. And what is the testimony,

upon these heads, which is borne by the accounts collected by Gmelin?

Is the Northern Light of the German naturalist, the apparently

constant attendant of clear evenings, even in the countries between

the Lena and the Yenesei? Is the spectacle, and the atmospherical

hurley, which seems to rush over the [p417] hunting-grounds of

the hunters and their dogs, and which frightens the very dogs, and

pins them to the ground till it is passed, or has seemed to pass;

is this the “constant attendant of clear evenings,” or, is it a

prodigy so uncommon as to defy familiarity? But, if this evidence is

insufficient, let us look to what is said of its influence, in these

countries, on the subsequent state of the atmosphere. So far from the

Aurora being an attendant or follower of clear evenings, it seems

that clear evenings follow the Aurora! It is said, that after its

occurrence, clear and calm weather is customary to follow; and, here,

the expression itself is implicative of the rarity of the occurrence.

If it were constant, how should this result come to be noticed;

and, indeed, if the Aurora Borealis were the constant attendant of

each twenty-four hours, and if clear weather were usually in the

train of the Aurora Borealis, how could it ordinarily happen, that

there should be any thing else than clear weather, in the countries

visited by the Aurora, or any foul weather for the Aurora to dispel?

Yet, such is the established prejudice concerning this supposed

frequency of the more powerful displays of the Aurora in the climates

further to the North than our own, that a writer, quoting the very

statement above, absolutely prefaces it with the remark, that

Gmelin, in pointed terms, speaks of the Aurora as “frequent,” as

well as “very loud,” “in the North-eastern parts of Siberia[125]!” A

simple perusal, in the meantime, is sufficient to show, that Gmelin

says nothing affirmative as to its _frequency_; while a slight

consideration of the facts which he adduces must satisfy us, as no

doubt they satisfied Gmelin himself, that the occurrence, even in

Siberia, is actually _infrequent_!

* * * * *

XI. In reference, however, as well to the image presented above, of

“a vast tent expanded in the heavens, glittering with gold, rubies,

and sapphires;” as also to many less ambitious and figurative

descriptions of the spectacle of the Aurora Borealis, (not excepting

that indicted by himself,) the author is anxious to suggest a caution

against the too exaggerated conception of the realities intended.

Words, [p418] upon such occasions, are rarely more than imperfect

pictures, presenting but feeble likenesses, and either deficient or

excessive in the amount of beauty, or of the reverse, of whatever

kind, which they attempt to copy from their originals; and the

inconvenience is seriously great, whenever the object portrayed is

wholly strange to the mind before which it is placed. The imperfect

power, both of words and written characters, to convey precise, and

sometimes even tolerable ideas, of the objects, either sensible or

abstract, which they are intended to represent, and the superior

intelligibility so often belonging to diagrams or figures, or other

resources of the art of drawing, (the primitive, and, for so many

purposes, the most instructive mode of writing[126],) would have

led the present writer, had time permitted, to endeavour, as often

as possible, to elucidate by such means the several parts of the

foregoing observations; but which means, at last, and in reference to

the actual phenomena of the Aurora, would necessarily fail to convey

the due, and yet no more than the due impression, to such as are

wholly without its ocular acquaintance. We are little aware how much,

upon ordinary occasions, our understanding of words heard or read is

assisted by our previous knowledge of the sensible objects, or of

the acquired notions, to which they refer; and the examples would be

endless, of the sensible objects preposterously misconceived, as well

as the propositions made false or ridiculous, through the frequent

inadequacy of words to communicate truths entirely new [p419] to the

disciple. Even the history of opinions concerning the Aurora Borealis

itself, might be cited upon this very point.

The ordinary and natural resource, in such circumstances, is

comparison; but even comparison has been the source of great and

endless errors of description. Of the degree of resemblance proposed

between the known and the unknown, there is no common measure for

the minds of the hearer and the listener, and the point or points

of comparison intended by the first must often be mistaken by the

second; or, if reference is made to a similitude under one aspect,

the imagination conceives a resemblance also under another: thus,

if it is said, that an unknown animal is as _large_ as a horse,

the idea of the _figure_ also of a horse, is apt to be attached. A

modern English work of science premises, upon the subject of the

Aurora Borealis, that its appearance is so well known as to render

description needless. It is true that the work referred to is

printed in the Northern part of the island, where the phenomenon is

doubtless more familiar than in the Southern; but, in the foregoing

pages themselves, it has, perhaps, been demonstrated as probably

certain, that if it is any where sufficiently known to render

description trite for the common eye, it has at least never hitherto

been described with sufficient precision for the aid of speculative

research. To attempt to explain its _cause_, and to relate its

entire history, its _appearance_ must first be either observed or

described with accuracy; and we have seen, above, that some of the

most scientific reasonings which have hitherto been offered as to

the former, are wholly inapplicable to the true peculiarities of the

latter.

Considered simply as a visual object, and as a meteor differing

from all others, and especially from all other luminous meteors,

in this, that its duration extends to hours, if not to days and

months; the only resemblance, perhaps, that can be suggested, is to

that description of lightning which is called _heat-lightning_, the

frequent companion of our summer-evenings. But, here, the similitude

is inexpressibly feeble; since heat-lightning has nothing, either of

the splendour, the volume, or the beauty of the Aurora; and since

the light of the latter, however mobile, varied, and, from time to

time, increased and diminished in itself, is yet, as to general

effect, continuous and [p420] steady. There remains, then, but to

compare the phenomenon of the Aurora with the rising or the setting

Sun. In both of these latter, as in the Aurora, the light is in

the horizon, and that light is shot upward, perpendicularly, or

obliquely, toward the zenith or toward the right and left; and both

of these, like the Aurora, are more or less constantly attended with

a variety of colouring, similar in hue if not in depth, and always

beautiful, and often gorgeous. With the _Sun_, and with the beams

of the Sun, ancient description, in point of fact, has confounded

the _Aurora Borealis_, to the degree, perhaps, of giving origin to

some of the ancient and poetical descriptions of the Sun, utterly

inappropriate and inexplicable as understood of that day-star, but

easily recognised in the Aurora; yet the dissimilitudes, at last, are

numerous and great! Of the essential difference of figure, both as to

the _beams_ of the Sun, and the _beams_ of the Aurora, in severalty,

and of the inevitable difference of indication of which, as to their

nature, mention has been already made; and also as to the general

or collective figure of the beams of the Aurora, as contrasted with

that of the rising, or of the setting Sun. The next point is the

homogeneity of colour in the beams of the Sun, however the apparent

colour may vary, as it is seen to do, from horizontal stratum to

horizontal stratum, from the horizon to the zenith, according to the

varied density of the medium between the light and the eye of the

spectator. The light, upon the other hand, of the beams of the Aurora

is heterogeneously coloured in itself, and is so displayed; and

not, therefore, varied as the beams ascend from horizontal stratum

to horizontal stratum, or as crossing all the beams together, but

found in each particular beam itself, and attending its direction,

whether vertical or inclined, and whether rectilinear or curved.

Waiving, then, any comparison in detail, between the phenomena of

the Aurora, and the phenomena of the rising or of the setting Sun,

but admitting that, to a certain degree, all are alike vast in

dimensions, splendid in light, rich in colour, and durable upon the

eye; there is still nothing else to be subjoined, than that, at least

with reference to vastness of dimension and magnitude of the volume

of light; to the quantity of light diffused; and to the richness and

gorgeousness of [p421] the attendant colouring; there can be little

risk, in the assertion that, vast, and splendid, and beautiful, and

rich, and gorgeous, as, when seen in the most favourable situation,

and under the most favourable circumstances, the Aurora may be, it

is, at last, but insignificant, when compared, for those features,

to the vastness, the splendour, the beauty, the richness, and the

gorgeousness, more or less, from day to day, displayed in the rising

or the setting of the Sun; and, that for chaster beauty, and even for

amount of light diffused, it is not even to be likened to the silver

Moon! As a substitute, too, for either, or for both, the Aurora, in

the regions of cold and night, may justly demand the admiration and

the blessing of mankind; and, in regions cold and inclement, its

rarity, not unaccompanied by beauty, by grandeur, and sometimes even

by the terrible in appearance, may well invite the gaze and fix the

attention of beholders; but, considered along with the light of the

luminaries of heaven, its claims reduce themselves in quality, though

certainly not in degree, to a level with those of an artificial

lustre; and we almost repeat, in reference to the light of the

Aurora, as compared with that of the Sun, or even of the Moon, what

the poet has said in reference to the lights of our chambers:—

“Who but rather turns

To heaven’s broad beam his unconstrained eye,

Than to the glimmering of a waxen flame?”

The Moon, in the meantime, inferior as she is to the Sun, has

been “blessed,” from age to age, for her “useful light;” and the

“useful light” of the Aurora, also, has its claims to “blessing.” It

co-operates with the Sun, the Moon, and with other agents of nature,

to make, not merely the Polar regions of the earth, but the entire

globe of the earth, fruitful, at once, and habitable[127]! [p422]

* * * * *

XII. In a succeeding paper, the author may possibly submit to the

consideration of his reader, the particular and novel hypotheses

which he has allowed himself to form, as to the _substance_,

_causes_, and _effects_ of the Aurora; hypotheses partly dependent

upon those _facts in its natural history_, which, above, have been

almost the exclusive objects of attention. At present, the leading

particulars of the _natural history_ of the phenomenon, which it has

been attempted either to bring or to fix in view, are these:

1. That the Aurora is a phenomenon observed both in the Northern and

Southern Hemispheres.

2. That, in either hemisphere, it is observed in the general

direction of the corresponding _pole of the earth_.

3. That, in the Northern Hemisphere, on the shores of the Icy Sea, or

at the furthest distance north, its situation is still observed to be

the northward.

4. That, in the Southern Hemisphere, it has been observed to the east

of the South Pole, and in the Northern, to the east and west of the

North Pole.

5. That, upon the late occasion, the place of its columns, during the

exhibition, was observed to change from the west of north to the east

of north; but, so as always to have the north for the apparent centre

of its strength.

6. That, in the Arctic regions, the appearance of the Aurora is said

to be usually followed by clear and calm weather.

7. That the appearance of the Aurora Borealis is no wise peculiar

to the winter solstice, but has been observed in each of the eight

months of September, October, November, December, January, February,

March, and April, and may be regarded, therefore, as coincident

with the Arctic winter; and that the appearance of an Aurora in the

Southern Hemisphere, in the month of February, or beginning of the

Antarctic winter, as observed during the voyage of Captain Cook, in

the year 1773, is [p423] consistent with the persuasion, that the

Aurora _Australis_, in its turn, is a phenomenon of the Austral or

Antarctic winter.

8. That _considerable_ or powerful displays of the Aurora are

infrequent, even in the extreme Polar regions; and that it is _very

considerable_ or powerful displays alone, which make themselves

visible in the lower latitudes, north or south of the equator.

9. That no appearance belongs to the Aurora itself, but that of its

coruscations, columns, spears, or streamers; and that all colours,

therefore, or coloured figures, not belonging to the coruscations,

but coincident in their appearance, are to be regarded only as

reflections or refractions of light, derived from the coruscations by

the clouds which happen to cover the sky.

10. That the colours, or coloured light, proper to the Aurora, or

seen in the columns or coruscations themselves, are varied from

column or coruscation to column or coruscation, and severally

continued in the direction, and throughout the length or height, of

each.

11. That, in the late example, the columns or coruscations situate

in the due north, or apparent centre or focus of the phenomenon,

exhibited a light at least comparatively white; and that the

variation, from white to colour, had an apparent relation to the

comparative remoteness of each column or coruscation from the column

or coruscation in the central north.

12. That the direction or position of the columns or coruscations of

the Aurora, are so far from being uniformly convergent toward the

zenith, or uniformly vertical, or from the horizon to the zenith,

that, in the late example, they _did not converge_ toward the zenith,

but, contrariwise, _diverged_ from it; spreading themselves like the

sticks of a fan, or like stalks in a flower-basket.

13. That the columns or coruscations of the Aurora are not uniformly

rectilinear in their figure; but that, in the late example, those

on the north-eastward were curved outwardly, or “bent sideways,” as

described in the appearance of the columns or coruscations of an

Aurora seen in the Southern Atlantic, during the voyage of Captain

Cook, in the year 1773. [p424]

FOOTNOTES:

[120] Literary Gazette, Sept. 29, 1827.

[121] “PENCELLS.—Pencills, or flagges for horsemen, must be a

yard and a halfe long.” Harleian MSS., cited in an interesting

and valuable essay on the “Banners used in the English army, from

the Conquest to the reign of Henry VIII.” By N. H. NICOLAS, Esq.,

F.S.A—_Retrospective Review_, Oct. 1, 1827.

“The Pensell, or Pennoncelle, was the diminutive of the Pennon,

being a long narrow flag.”—MEYRICK’S ANCIENT ARMOUR.

“STREAMER.—A Streamer shall stand in the toppe of a shippe, or in

the forecastle, and therein be put no armes, but a man’s conceit or

device, and may be of the lengthe of twenty, forty, or sixty yards;

and it is slit, as well as a guydhomme or standarde.”—HARLEIAN MSS.

An item, in a bill of parcels, charged to the Earl of Warwick, in

1437, consists of “a great Stremour for the Ship, of xl yerdis

lenghth, and viij yerdis in brede.”—BANNERS USED IN THE ENGLISH

ARMY, &c.

[122] Meteorological Journal, Literary Gazette, Sept. 29th.

[123] Literary Gazette, as above.

[124] _Encyclopædia Britannica_. Art. Aurora Borealis.

[125] Encyclopædia Britannica.

[126] The individual, social, and political importance of making

the _art of drawing_ a branch of general education, is a subject

which the author can never cease to urge upon the attention of his

fellow-countrymen, and of all the civilised world. It is more than

ten years since he first endeavoured to lead the public eye to its

regard. In England, and with a view to the subsistence of a large

and always increasing population, it is an EDUCATION IN THE ARTS

which is the great want; and the _art of drawing_, besides being

the assistant of all _knowledge_ whatever, is peculiarly so of all

other _arts_ than itself, or of all other works of the _hand_. A

recent Sermon, by the Lord Bishop of Bath and Wells, preached at

Wells, for the benefit of the Diocesan National Schools, bears ample

testimony to the deficiency, and even the dangers, to the poor not

less than to others, in all the present popular education; and, so

far, therefore, to the soundness of the author’s principles, and

to the fitness of his remedy. His own design, however, is not only

to remedy an evil arising from the present practice, but also to

produce an independent good; and, not merely to aid the poor, nor

merely to promote the political welfare of this kingdom, but to

increase the resources, physical and intellectual, of all classes,

and to promote the welfare of the whole world.

[127] The author has an opinion, that among the “agents of nature,”

for equalising the temperature of the surface of the globe, is to

be reckoned, not only the Northern and Southern Lights, but the

entire Ocean; and that this agency is the immediate object aimed at

in the existence of this last, as one body of water surrounding the

entire globe. His evidence consists in geographical, hydrographical,

meteorological, and physiological facts, as also in the apparent

reason of the case. He supposes, in consequence, a perpetual

circulation of the waters of the sea, longitudinally round the

globe, or from North to South, and from South to North again; and

the result of Captain Parry’s late attempt to reach the Arctic

Pole, as also some of the facts which have transpired respecting

Captain Franklin’s late land expedition, appear to confirm his

theory, according to which the physical use, or final cause, of

the existence of the Ocean has never previously been understood.

His theory affects the question of the North-west Passage, which

latter object he suspects to have never yet been pursued in the true

direction; even the discoveries of Captain Parry appearing to him to

have fallen short of ascertaining the communication with the Polar

Sea by the channel of Davis’s Strait.—Some introductory observations

upon this subject have been already made in an article in the New

Monthly Magazine for October, 1826, (vol. xvii. p. 371.)

_Proceedings of the Royal Society_.

The anniversary meeting of the Royal Society for the election of a

president, and other officers, was held as usual at Somerset House,

on Thursday, the 30th of November, being St. Andrew’s day.

Till within a few days of the election, it was generally understood

that the Rt. Hon. Robert Peel was a candidate for the chair; in

consequence, however, of that gentleman having declined, Davies

Gilbert, Esq., M.P., was put in nomination, and was almost

unanimously elected the President of the Royal Society.

The late secretaries, Messrs. Herschel and Children, having resigned

their respective offices, Dr. Roget and Captain Sabine were nominated

in their places, and were duly elected.

The Quarterly Journal of Science, Literature and the Arts, July-December, 1827 · 第 41 / 51 段