CHAPTER IV.

We now propose to furnish a brief sketch of the life of Sir John

Frederick William Herschel, the only son of Sir William, and not less

illustrious as a man of science.

He was born at Slough, in the year 1792. Evincing considerable talents

at a very early age, he received a careful private education under Mr.

Rogers, a Scottish mathematician of distinguished merit; and afterwards

was sent to St. John's College, Cambridge, always famous as a nursery of

mathematical and scientific prodigies! Here he pursued his studies with

remarkable success, suffering no obstacles to daunt him, and wasting no

opportunities of improvement. His fellow-collegians regarded him as one

who would add to the high repute of the college, and rejoiced at the

brilliant ease with which he passed every examination. In 1813 he took

his degree of B.A., and consummated a long series of successes by

becoming "senior wrangler," and "Smith's prizeman;" these being the two

highest distinctions to which a Cambridge scholar can attain.

In the same year, when he was hardly twenty-one, he published a work

entitled, "A Collection of Examples of the Application of the Calculus

to Finite Differences." To our young readers such a title will convey no

meaning; and we refer to it here only to illustrate the industry and

careful thought of the young student, which had rendered possible such a

result.

Returning to Slough, he continued his studies in mathematics, chemistry,

and natural philosophy, and in various publications exhibited that

faculty of observation and analyzation, that intelligence and

scrupulousness in collecting facts, and that boldness in deducing new

inferences from them, which were characteristic of his illustrious

father. The subjects he took up were so abstruse, that we could not hope

to make our readers understand what he accomplished, or how far he

excelled his predecessors in his grasp and comprehension of them. For

instance: if we tell them that in 1820 he wrote a paper "On the Theory

and Summation of Series;" communicated to the Cambridge Philosophical

Society his discovery that the two kinds of rotatory polarization in

rock crystal were related to the plagihedral faces of that mineral; and

issued an able treatise "On Certain Remarkable Instances of Deviation

from Newton's Tints in the Polarized Tints of Uniaxal Crystals,"--they

will gain no very distinct idea of the significance or value of these

researches. Again: it will not be very intelligible to them to be

informed that, in 1822, he communicated to the Royal Society of

Edinburgh a paper "On the Absorption of Light by Coloured Media", in

which he enunciated a new method of measuring the dispersion of

transparent bodies by stopping the green, yellow, and most refrangible

red rays, and thus rendering visible the rays situated rigorously at the

end of the spectrum. But they will understand that these results could

have been attained only by the most assiduous industry and the most

unflinching perseverance. And it is on account of this industry and

this perseverance that we recommend Herschel as an example to our

readers. They may not make the same progress in science, or achieve the

same reputation. It is not necessary they should. Humble work is not

less honourable, if it be done conscientiously, and with a sincere

desire to do the best that it is in our power to do.

An interesting feature in the younger Herschel's character was his

loving care for his father's fame. He was ever most anxious that the

full measure of his services to science should be recognized and

appreciated. Thus, in 1823, he writes to his aunt:--

"I have been long threatening to send you a long letter, but

have always been prevented by circumstances and want of leisure

from executing my intention. The truth is, I have been so much

occupied with astronomy of late, that I have had little time

for anything else--the reduction of those double stars, and the

necessity it has put me under of looking over the journals,

reviews, &c, for information on what has already been done, and

in many cases of re-casting up my father's measures, swallows

up a great deal of time and labour. But I have the satisfaction

of being able to state that our results in most instances

confirm and establish my father's views in a remarkable manner.

These inquiries have taken me off the republication of his

printed papers for the present.

"I think I shall be adding more to his fame by pursuing and

verifying his observations than by reprinting them. But I have

by no means abandoned the idea. Meanwhile, I am not sorry to

hear they are about to be translated into German.... I hope

this season to commence a series of observations with the

twenty-foot reflector, which is now in fine order. The

forty-foot is no longer capable of being used, but I shall

suffer it to stand as a monument."

* * * * *

In reference to this famous telescope, we may digress to state that its

remains have been carefully preserved.

The metal tube of the instrument, carrying at one end the recently

cleaned mirror of four feet ten inches in diameter, has been placed

horizontally in the meridian line, on solid piles of masonry, in the

midst of the circle where the apparatus used in manoeuvring it was

formerly placed. On the 1st of January 1840, Sir John Herschel, his

wife, their seven children, and some old family servants, assembled at

Slough. Exactly at noon the party walked several times in procession

round the instrument; they then entered the gigantic tube, seated

themselves on benches previously prepared, and chanted a requiem with

English words composed by Sir John Herschel himself. Then issuing from

the tube, they ranged themselves around it, while its opening was

hermetically sealed.

* * * * *

In March 1821, the younger Herschel, in conjunction with Sir James

South, undertook a series of observations on the distances and positions

of three hundred and eighty double and triple stars, by means of two

splendid achromatic telescopes of five and seven focal length. These

were continued during 1822 and 1823, and have proved of great service to

astronomers.

Having pursued with much zeal the study of optics, and experimented

largely and carefully on the double refraction and polarization of

light, he compiled a treatise on the subject for the "Encyclopaedia

Metropolitana" It has been translated into French by M. Quetelet; and

both foreign and English men of science have been accustomed to regard

it as indicating a new point of departure in the important branch of

science to which it is devoted.

Astronomy, however, became for him, as for his father, the great

pursuit of his laborious life; and having constructed telescopes of

singular magnitude and power, he entered upon a study of the Sidereal

World. In 1825 he commenced a careful re-examination of the numerous

nebulae and starry clusters which had been discovered by his father, and

described in the "Philosophical Transactions," fixing their positions

and investigating their aspects. He devoted eight years to this _magnum

opus_, completing it in 1832. The catalogue which he then contributed to

the "Philosophical Transactions" includes 2306 nebulae and

star-clusters, of which 525 were discovered by himself. While engaged in

this difficult task, Herschel discovered between three and four thousand

double stars, which he described in the Memoirs of the Astronomical

Society. His observations were made with an excellent Newtonian

telescope, twenty feet in focal length, and eighteen and a half inches

in aperture; and having obtained, to use his own expression, "a

sufficient mastery over the instrument," the idea occurred to him of

making it available for a survey of the southern heavens. Accordingly,

he left England on the 13th of November 1833, and arrived at Cape Town

on the 16th of January 1834. Five days later he wrote to his aunt as

follows:--

"Here we are safely lauded and comfortably housed at the far

end of Africa; and having secured the landing and final storage

of all the telescopes and other matters, as far as I can see,

without the slightest injury, I lose no time in reporting to

you our good success _so far_. M----[1] and the children are,

thank God, quite well; though, for fear you should think her

too good a sailor, I ought to add that she continued sea-sick,

at intervals, during the whole passage. We were nine weeks and

two days at sea, during which period we experienced only one

day of contrary wind. We had a brisk breeze 'right aft' all the

way from the Bay of Biscay (which we never entered) to the

'calm latitudes;' that is to say, to the space about five or

six degrees broad near the equator, where the trade-winds

cease, and where it is no unusual thing for a ship to lie

becalmed for a month or six weeks, frying under a vertical sun.

Such, however, was not our fate. We were detained only three or

four days by the calms usual in that zone, but never _quite_

still, or driven out of our course; and immediately on crossing

'the line' got a good breeze (the south-east trade-wind), which

carried us round Trinidad; then exchanged it for a north-west

wind, which, with the exception of one day's squall from the

south-east, carried us straight into Table Bay. On the night of

the 14th we were told to prepare to see the Table Mountain.

Next morning (_N.B._, we had not seen land before since leaving

England), at dawn, the welcome word land' was heard; and there

stood this magnificent hill, with all its attendant

mountain-range down to the farthest point of South Africa, full

in view, with a clear blue ghost-like outline; and that night

we cast anchor within the Bay. Next morning early we landed,

under escort of Dr. Stewart, M----'s brother, and you may

imagine the meeting. We took up our quarters at a most

comfortable lodging-house (Miss Robe's), and I proceeded,

without loss of time, to unship the instruments. This was no

trifling operation, as they filled (with the rest of our

luggage) fifteen large boats; and, owing to the difficulty of

getting them up from the hold of the ship, required several

days to complete the landing. During the whole time (and indeed

up to this moment) not a single south-east gale, the summer

torment of this harbour, has occurred. This is a thing almost

unheard of here, and has indeed been most fortunate, since

otherwise it is not at all unlikely that some of the boats,

laden as they were to the water's edge, might have been lost,

and the whole business crippled.

[Footnote 1: Herschel married a Miss Stewart in February 1826.]

"For the last two or three days we have been looking at houses,

and have all but agreed for one--a most beautiful place within

four or five miles out of town, called 'The Grove.' In point of

situation it is a perfect paradise, in rich and magnificent

mountain-scenery, and sheltered from all winds, even the fierce

south-easter, by thick surrounding woods. I must reserve for my

next all description of the gorgeous display of flowers which

adorns this splendid country, as well as of the astonishing

brilliancy of the constellations, which the calm, clear nights

show off to great advantage."

Mr. Herschel settled at Feldhausen, about 142 feet above the sea, and in

long. 22° 46' 9".11 E., and lat. 33° 58' 26".59 S. Here he entered upon

his great series of observations of the southern heavens, which he

continued with unwearied ardour for a period of four years. The results

were afterwards published, at the cost of the Duke of Northumberland, in

a work entitled "Results of Astronomical Observations made in

1834-35-36-37-38, at the Cape of Good Hope." In this superb work, which

placed its author on an equality with the most brilliant and illustrious

astronomers, he defined and described 4015 of the nebulae and

star-groups in the southern hemisphere, and 2995 of the double stars;

besides entering into a variety of valuable particulars relative to

Halley's comet, the solar spots, the satellites of Saturn, and the

measurement of the apparent magnitude of stars.

On his return to England (in 1838) the astronomer received a noble

welcome. Honours poured in upon him. The Gold Medal of the Astronomical

Society was conferred upon him for a second time. William IV. had

previously distinguished him with the Hanoverian order of K.H.; but, on

the coronation of Queen Victoria, he received a baronetcy; and in 1839

the University of Oxford made him a D.C.L.

Continuing his career of scientific industry, he issued, in 1849, his

important and very valuable treatise entitled "Outlines of Astronomy."

In 1845, he was appointed President of the British Association; and in

1848, of the Royal Astronomical Society. To his other honours was added

that of Chevalier of the Prussian order, "Pour la Mérite," founded by

Frederick the Great, and bestowed at all times with a discrimination

which renders it a deeply-coveted distinction. Of the academies and

leading scientific institutions of the Continent and the United States,

he was also an honorary or corresponding member.

Besides his works on meteorology and physical geography, he published,

in 1867, an admirable little volume--"Familiar Lectures on Scientific

Subjects." In this he showed that he could write with as much ease and

intelligibility for the general public as for the higher order of

scientific inquirers. His style in this valuable manual of information

has a charm of its own, and entices the reader into the consideration of

subjects apparently abstruse. He is earned on from page to page without

any great mental effort, and finds himself rapidly mastering

difficulties which he had been accustomed to regard as insuperable.

Let us take the first lecture on "Volcanoes and Earthquakes," and obtain

a glimpse of Herschel's mode of treatment. He refers to the greater and

more permanent agencies which affect the configuration of our planet.

Everywhere, he says, and along every coast-line, we see the sea warring

against the land, and overcoming it; wearing it and eating it down, and

battering it to pieces; grinding those pieces to powder; carrying that

powder away, and spreading it out over its own bottom, by the continued

effect of the tides and currents. What a scene of continual activity is

presented by the chalk-cliffs of Old England! How they are worn, and

broken up, and fantastically sculptured by the influence of winds and

waters! Precipices cut down to the sea-beach, constantly hammered by the

waves, and constantly crumbling; the beach itself made of the flints

outstanding after the softer chalk has been ground down and washed

away; themselves grinding one another under the same ceaseless

discipline--first rounded into pebbles, then worn into sand, and then

carried further and further down the slope, to be replaced by fresh ones

from the same source. Here the likeness of an old Gothic cathedral, with

lofty arch, and shapely pinnacle; there the similitude of a mass of

medieval fortifications, with crumbling battlements and shattered

towers!

The same thing, the same waste and wear, is going on everywhere, round

every coast. The rivers contribute their share to the great work of

change. Look at the sand-banks at the mouth of the Thames. What are

they, says Sir John Herschel, but the materials of our island carried

out to sea by the stream? The Ganges carries away from the soil of

India, and delivers into the sea, twice as much solid substance weekly

as is contained in the Great Pyramid of Egypt. The Irawaddy sweeps off

from Burmah sixty-two cubic feet of earth in every second of time, on an

average Sometimes vast amount of earthy materials is transferred from

one locality to another by river agency, as is the case in the deltas

of the Nile and the Mississippi.

These changes operate silently, continuously, and unperceived by the

ordinary observer; but Nature does not limit herself always and

everywhere to such peaceful agencies. At times, and in certain places,

she acts with startling abruptness and extraordinary violence. Let the

volcano and the earthquake attest the immensity of her power. Let the

earthquake tell how, within the memory of man, the whole coast-line of

Chili, for 100 miles about Valparaiso, with the mighty chain of the

Andes, was hoisted at one blow, and in a single night (November 19,

1822), from two to seven feet above its former level, leaving the beach

below the old low-water mark high and dry. One of the Andean peaks

upheaved on this occasion was the colossal mass of Aconcagua, which

overlooks Valparaiso, and measures nearly 24,000 feet in height. On the

same occasion, at least 10,000 square miles of country were estimated as

having been upheaved; and the upheaval was not confined to the land, but

extended far away to sea,--which was proved by the soundings off

Valparaiso and along the coast having been found considerably shallower

than they were before the shock.

In the year 1819, in an earthquake in India, in the district of Cutch,

bordering on the Indus, a tract of country more than fifty miles long

and sixteen miles broad was suddenly raised _ten feet_ above its former

level. The raised portion still stands up above the unraised, like a

long perpendicular rampart, known by the name of Ullah Bund, or God's

Wall.

* * * * *

With a similar fertility of illustration, Herschel sets before us the

phenomena of volcanic eruptions and their extraordinary effects.

In a district of Mexico, between the two streams of the Cintimba and the

San Pedro, on the 28th of September 1789, a whole tract of ground, from

three to four miles in extent, surged up like a foam-bubble, or the

swell of a wave, to a height of upwards of 500 feet. Flames, lurid and

crackling, broke forth over a surface of more than half a square league;

and the earth, as if softened by heat, was seen to rise and sink like

the rolling tide. Vast chasms opened in the earth, into which the two

rivers poured their waters headlong; reappearing afterwards at no great

distance from a cluster of _hornitos_, or small volcanic cones, which

sprang out of the mighty mud-torrent that gradually covered the entire

plain. Wonderful and awful as were these phenomena, they were surpassed

by the sudden opening of a chasm which vomited forth fire, and red-hot

stones and ashes, until they accumulated in a range of six large

mountain masses,--one of which, now known as the volcano of Jorullo,

attains an altitude of 1690 feet above the ancient level.

In like manner Sir John proceeds to describe an eruption of Mount

Tomboro, in the island of Sumbawa, the influence of which was felt to a

distance of 1000 miles from its centre, in strange tremulous motions of

the earth, and in the clash and clang of loud explosions. He says that

he had seen it computed that the quantity of ashes and lava ejected in

the course of this tremendous eruption would have formed three mountains

of the size of Mont Blanc.

As to the nature of the forces which operate to produce this astounding

result, Herschel puts forward a theory of singular simplicity and

directness.

"The origin," he says, "of such an enormous power thus occasionally

exerting itself, will no doubt seem very marvellous--little short,

indeed, of miraculous intervention; but the mystery, after all, is not

quite so great as at first it seems. We are permitted to look a little

way into these great secrets of Nature; not far enough, indeed, to clear

up every difficulty, but quite enough to penetrate us with admiration of

that wonderful system of counterbalances and compensations, that

adjustment of causes and consequences, by which, throughout all nature,

evils are made to work their own cure, life to spring out of death, and

renovation to tread in the steps and efface the vestiges of decay." And

he finds the clew to the secret, the key of the whole matter, in the

earth's vast central heat. This it is which produces the convulsions

that change the terrestrial configuration, and fill the minds of men

with fear and awe. Conceive of "a sea of fire, on which we are all

floating, land and sea,"--a boiling, seething, incandescent reservoir in

the centre of our planet; and the solution of the problem will seem to

you not difficult. Such a sea would necessarily roll its liquid matter

to and fro; and the removal of ever so small a portion from one point to

another on the earth's surface would tend to disturb the equilibrium of

the floating mass; just as, when a ship is launched into the river, the

water it displaces is carried to the opposite bank with greater or less

violence, according to the amount of displacement.

It is impossible, adds Herschel, but that this increase of pressure in

some places and relief in others must be very unequal in their bearings.

So that at some point or another our planet's floating crust must be

brought into a state of strain, and if there be a weak or a soft part a

crack will at last take place. This is exactly what happened in the

earthquake which originated the Allah Bund, or God's Wall, in Cutch.

Volcanic eruptions are easily explicable on this principle,--the volcano

being simply a vent for the passage of heated and molten matter, which

the elevating pressure of the liquid below tends to eject. It is a

well-known fact that volcanoes and earthquake-centres are nearly all

situated on the borders or in the immediate neighbourhood of seas and

oceans; and the reason would seem to be, that at such positions the

accumulation of transported matter would necessarily attain its maximum,

to whatever cause it might be due. Then again, as Herschel points out,

the eruption of scorite and lava from the mouths of volcanoes, the

result of the upward movement of the fiery liquid below, compensates in

some degree for the downward transfer of material by detritus and

alluvial deposits. Hence it may be inferred that, on the whole, the

quantity of solid matter above the ocean-level probably remains nearly

always at the same amount.

* * * * *

It is with this ease and lucidity that Sir John deals with scientific

subjects of the greatest importance,--his genius resembling the

elephant's trunk, which can balance a straw or rend an oak. In private

life he displayed a simplicity of manner in harmony with the general

unassumingness of his character. In his books as in society, in society

as in his books, he was the same,--that is, free from all ostentation,

free from self-pride, free from the arrogance of superior knowledge, and

as ready to unbend himself to a child as to discourse with men of

science.

His career was a tranquil and a prosperous one, and, apart from the

record of his discoveries and his honours, presents nothing of interest.

He was peculiarly happy in his domestic relations; and in the wide

circle of friends attracted by the mingled charm of his intellect and

manners. A devout Christian, a man of generosity and culture, a

philosopher of great breadth of view and infinite patience of

research,--we can place few better or brighter examples before our

English youth than Sir John Herschel.

The Story of the Herschels, a Family of Astronomers Sir William Herschel, Sir John Herschel, Caroline Herschel · 第 4 / 5 章