At some epoch in the past, probably at least one thousand million

years ago, our own sun may have undergone some cataclysmic change

and this may, conceivably, have been brought about by disturbances

within the sun itself. Elements may have been so formed and

distributed within the interior of the sun that friction and internal

instability resulted and in time produced an upheaval of solar

elements with initial velocities so great that, possibly, through

electrical repulsion and light-pressure, portions of the ejected

streams were permanently detached from the sun and became the nuclei

of future planets. In some such way, it is conceivable, our own

planet Earth and the other members of our solar system may have been

brought into existence in the dim and distant past--many hundred

million years ago.

XIX

JUPITER AND HIS NINE MOONS

Jupiter shines by reflected sunlight with a brilliancy that usually

exceeds that of the brightest of the stars, Sirius. When seen during

the midnight hours the remarkable unflickering brightness of this

largest and most distinguished member of the solar system at once

serves to set it apart from the scintillating stars far beyond.

There is but one planet, Venus, that always surpasses Jupiter in

brilliancy, though Mars on the occasions of its close approaches

to the earth may equal or slightly surpass Jupiter in brightness.

As Venus never departs more than forty-eight degrees from the sun,

and so is never seen in the midnight hours, Jupiter usually shines

without a rival when visible at midnight. To one who has observed the

two planets together the silvery radiance and surpassing brilliancy

of Venus, due not to its size, but to its comparative nearness to

the earth, at once serves to distinguish it from the golden glow of

Jupiter.

Even the smallest telescopes of two- or three-inch aperture will show

the four historic moons of Jupiter which were the first celestial

objects to be discovered when Galileo turned his crude telescope to

the heavens in the year 1610.

The fact that these tiny points of light were actually revolving

around the great planet was soon detected by the famous astronomer

and we can imagine with what breathless interest he observed these

satellites of another world whose discovery dealt such a severe blow

to the old Ptolemaic theory that the earth was the center of the

universe. It was not until the great telescopes of modern times were

invented that the five additional moons of Jupiter were discovered.

The four satellites first observed by Galileo were fancifully named

Io, Europa, Ganymede and Callisto, in the order of their positions

outward from the planet, but these names are rarely used now, the

satellites being designated for convenience I, II, III and IV,

respectively. The first of the new satellites to be discovered was

Satellite V, which is the nearest to Jupiter of all the nine moons.

It is an extremely small body, not more than one hundred miles in

diameter, and to discover this tiny body as it skirted rapidly around

the great planet within sixty-seven thousand miles of its surface,

nearly lost in the glaring rays, was a difficult feat even for an

experienced observer. It was accomplished, however, by Prof. E.

E. Barnard with the great Lick refractor in 1892. Satellite V is

hopelessly beyond the reach of any but the greatest telescopes, as

are also the four satellites discovered since that date. In fact,

most of these tiny moons are observed photographically. Satellites VI

and VII were discovered photographically in 1905. They are both about

seven million miles from the planet and their paths loop through

one another; they are, moreover, highly inclined to each other at

an angle of nearly thirty degrees. When nearest together they are

separated by a distance of two million miles. Two more extremely

small bodies, known as Satellites VIII and IX, have been discovered

since then, one at Greenwich, England, in 1908, the other at the Lick

Observatory in 1914. These excessively faint bodies are the most

remote satellites of Jupiter and they are of particular interest

because they travel around the planet in a retrograde direction, or

from east to west, which is _opposite_ to the direction of revolution

prevailing in the solar system. The ninth and most distant satellite

of Saturn also retrogrades, or revolves in a clockwise rather than

a counter-clockwise direction around the planet. One explanation

given for this peculiarity of the outermost satellites of Jupiter

and Saturn is that this backward revolution around the planet is

more stable when the satellites are at great distances from the

primary, and the gravitational control that the planet exerts is

therefore weak. The moons of the planets are, of course, subject

to the attraction of the sun as well as to the attraction of the

controlling planet, and the greater the distance of the satellite

from the planet the stronger the pull exerted by the sun and the

weaker the bonds that bind the moon to the planet. Beyond a certain

limit it would be impossible for the planet to hold the satellite

against the sun's greater attraction and the satellite would leave

the planet to revolve directly around the sun, thereby becoming a

planet. It appears that as this danger limit is neared it is safer

for the satellite to "back" around the planet than to follow the

usual "west to east" direction of revolution. The eighth satellite

of Jupiter is more than fourteen million and the ninth more than

fifteen million miles from the parent planet and they require about

two years and three years, respectively, to complete one trip around

Jupiter. When we consider that Satellite V darts around the planet

in less than twelve hours at a distance of only sixty-seven thousand

miles from its surface we realise what tremendous differences exist

in the distances and periods of revolution of the nine moons. There

is also great disparity in the sizes of the various moons. The five

moons discovered in modern times are all excessively faint and

extremely small. The diameter of the largest of these, Satellite

V, is less than one hundred miles. On the other hand, the four

historic moons of Jupiter are of planetary dimensions. The smallest,

Satellite II, is slightly larger than our own moon, while the

largest, Satellite III, has a diameter, according to measurements

made with the 40-inch Yerkes refractor in 1916, of three thousand

nine hundred and eight miles, which is only four hundred miles less

than the diameter of Mars. The periods of revolution of these four

satellites range from one day and eighteen hours for the nearest,

which is about two hundred and sixty-one thousand miles from the

center of Jupiter, to sixteen days and sixteen and one-half hours for

the most distant, which is more than one million one hundred and

sixty thousand miles from the planet. These four moons are so near

to the great planet that they are continually dipping into his huge

shadow and experiencing an eclipse of the sun which, owing to the

nearness and great size of Jupiter, lasts for two or three hours. At

times of eclipse the moon suddenly disappears from the observer's

view, though it may be considerably to one side of the planet. Its

reappearance later on is just as sudden, or it may pass out of the

shadow while hidden from us behind the disk of the planet, in which

case its reappearance is invisible from the earth. The occultations

of the satellites, or, in other words, their disappearance behind

the planet's disk, are also interesting phenomena to observe, as

are their "transits" across the disk of the planet as the satellite

passes in front of it. Not only the satellite itself but its shadow

as well can be seen, a small black dot passing over the surface of

Jupiter. The satellite is totally eclipsing the sun for this small

dark portion of the planet's disk. Two satellites and their shadows

are frequently seen crossing the face of the planet at the same

time. It is possible to observe all the phenomena of the satellite's

transits and shadows, eclipses and occultations with very small

telescopes. From observations of the eclipses of Jupiter's satellites

the important discovery of the finite velocity of light was first

made as far back as the year 1675.

Faint surface markings have been made out at certain times on the

largest of the four satellites, Satellite III, and also on Satellite

I. Observations of the markings on the former seem to indicate that

it always keeps the same face turned toward Jupiter as does our own

moon toward the earth.

There are also reasons for believing that the equatorial regions of

Satellite I are light colored and the polar regions dark. There is

the possibility that forms of life may exist on these satellites of

Jupiter, though they are more likely barren, lifeless worlds, such as

Mercury and the moon. Their great distance from the earth, never less

than three hundred and sixty-eight million miles, makes observations

of their surface markings very difficult.

How beautiful beyond description must the heavens appear as viewed

from the satellites of Jupiter! Viewed from the distance of Io, or

Satellite I, the mighty planet Jupiter presents a spectacle such

as the eye of man has never been privileged to behold. The huge

flattened globe, ninety thousand miles in equatorial diameter, equal

in mass to _three hundred planets such as our own_ and in volume to

nearly _fourteen hundred_, fills a space in the heavens nearly twenty

degrees in extent as viewed from this satellite. Fifteen hundred of

our own full moons would hardly fill the same space. Whirling on its

axis with frightful speed in a period of less than ten hours, the

huge ball glides rapidly but majestically onward through the sky. A

far distant sun shrunk to but one-fifth the diameter of the full moon

throws light and shade across the rapidly changing surface of the

planet, rich in the reds, browns and yellows and all the gorgeous

shades and tints of its dense, seething, gaseous envelope. The phases

of the moon on a greatly enlarged scale rapidly succeed each other

on Jupiter as it is viewed from the satellite in all positions with

reference to the sun. The cause of the belts of Jupiter, that lie

parallel to the planet's equator and are constantly changing in

number, width and shade, as well as the nature of all the peculiar

splashes of color and intensely white flecks that come and go in

the dense atmosphere of the planet would not be such a mystery to

us were it possible to view the great planet from the distance of

Satellite I, which is about as far from the surface of Jupiter as

the moon is from the earth. It is uncertain whether the planet is

entirely gaseous throughout or has a central core of solid or liquid

matter. Its density is only one and one-quarter times that of water

and slightly less than that of the sun, showing that it is composed

largely, if not entirely, of matter in a gaseous state. Jupiter is a

world as different from our own as it is possible to imagine. There

is no visible surface crust and there are no permanent markings.

Different spots on the planet's disk give different periods of

rotation showing that it is atmospheric phenomena that we observe.

All is constant flux and change on Jupiter. Dense vapors arise

from a highly heated interior and spread out into belts parallel

to the equator in the direction of the planet's rotation. From its

nearest satellite all the interesting changes of color and form that

constantly take place in the atmosphere of this great globe could be

observed in great detail. The high percentage of light and heat that

Jupiter reflects from the sun to its nearer satellites makes it a

secondary sun to them of tremendous size though feeble strength.

As seen from Satellite I the other three major moons of Jupiter

present all the phases of our own moon in rapid succession, due to

their constantly changing positions with reference to the sun. The

five small moons, discovered in modern times, are so minute that they

are simply star-like points of light even when viewed from the other

moons of Jupiter.

To keep track of the rapidly changing positions and various phases

of the moons of Jupiter as seen from any one of them, as well as

the rapid _apparent_ motion of the planet through the sky due to

the revolutions of the satellite around the planet, would be a

troublesome task for an astronomer stationed on one of these far

distant worlds. It would be a common sight to see in the sky at one

time the huge planet, the far-distant, shrunken sun, and one, two

or three moons. Seen from the moons of Jupiter the constellations

would appear as they do to us on earth, for such a slight change in

position as five hundred million miles, more or less, is trivial

when one is looking at the stars. Observations of the stars from the

nearest moon of Jupiter would be attended with great difficulties at

times, since reflected sunlight from a body nearly twenty degrees in

diameter would be extremely troublesome, especially were the phases

of the planets near that of the full moon. We know how the presence

of our own moon in the heavens at the full dims the brightness of

the stars so that only the brightest stars are seen. Even as viewed

from the fourth or most distant of the major satellites the planet

subtends an angle of nearly five degrees. Occultations of the stars

are many and frequent as the huge planet globe glides swiftly through

the heavens. Many a moonlight night appears almost as day owing to

the presence of the enormous, brilliantly reflecting ball of light

and at times two or three moons in addition. Only the brightest stars

could possibly be seen under such circumstances. When, however, the

small worlds pass into the shadow of the great mother planet and not

only the light of the sun but also the reflected light of Jupiter

disappears for many minutes, the stars shine forth in all their glory

there as here. At such times some of the larger moons would usually

be seen shining by the reflected light of the far distant sun. Saturn

also would be visible as a magnificent star, but beautiful Venus and

ruddy Mars would fail to appear. Tiny bodies, mere specks of light at

this distance, they would be lost to view in the glare of the sun.

XX

THE RINGS AND MOONS OF SATURN

Nearly everyone has felt at some time or other a strong desire to

gaze at some of the beauties and wonders of the heavens through

a telescope and the one object that all of us wish to see, if,

perchance, this desire is to be gratified is Saturn, whose unusual

ring system has, so far as we know, no counterpart in the sky.

All the planets in the solar system with the exception of the two

innermost, Mercury and Venus, are attended by satellites, but Saturn,

alone, has in addition to a family of nine moons, three distinct

rings of great dimensions which are composed of swarms of minute

particles revolving around the planet.

Why Saturn should be the only planet to possess such a system of

rings has never been explained in an entirely satisfactory manner.

There is an interesting law known as "Roche's Law," however, named

from its investigator, that states that no satellite of a planet can

exist intact with 2.44 times the radius of the planet. This limit is

spoken of as "Roche's Limit" and applying it to the planet Saturn we

find that the rings of Saturn fall within this limit. It does not

necessarily follow from this that the minute particles of which the

rings are composed are the shattered remains of one small satellite,

but rather that they are the material from which a satellite might

have been formed were it not so close to the planet. Within "Roche's

Limit" the mutual attraction of the various particles for each other

that would tend eventually to gather them into one body is overcome

by tidal forces that arise from such close proximity to the huge

planet. The stress and strain of such forces is so great that no

grouping of particles can take place. This explains, possibly, why

the rings continue to exist in their present condition. The total

quantity of matter in the rings is known to be very small, for

it does not disturb the motions of any of the nearer and smaller

satellites, though tiny Mimas, six hundred miles in diameter, is only

thirty-one thousand miles beyond the outer edge of the outer ring.

An interesting observation was made a few years ago of the passage

of the rings of the planet between us and a star. Though the light

of the star was diminished to one-fourth of its normal brightness

when the rings passed before it, at no time was its light entirely

eclipsed by any of the particles. It was computed that if the

diameters of any of the individual particles had amounted to as much

as three or four miles the star would have been temporarily eclipsed.

An upper limit for the size of the moonlets was thus obtained. The

average diameter of the particles is probably much less than three

miles.

The thickness of the ring system is not over fifty or one hundred

miles, but its total diameter is one hundred and seventy-two thousand

miles. There are, in all, three concentric rings. The faint inner

ring, known as the "crape" ring, is invisible in a telescope under

four inches in aperture. The width of this inner ring is eleven

thousand miles. Just beyond the crape ring is the chief, bright

ring, eighteen thousand miles in width. It shades gradually in

brightness from its juncture with the crape ring to its most luminous

portion at its outer edge, which is separated from the third or

outer ring by a gap two thousand two hundred miles in width, known

as Cassini's Division. The third or outer ring is eleven thousand

miles wide and is less bright than the central ring. The inner edge

of the inner ring is but six thousand miles above the surface of the

planet. On account of the curvature of the planet the ring system

is invisible from the north and south poles of Saturn. As in the

case of the satellites of a planet the inner particles of the rings

revolve around the planet more rapidly than the outer particles. The

innermost particles of the crape ring require but five hours for one

journey around Saturn while the outermost particles of the outer ring

require one hundred and thirty-seven hours, or nearly six days to

complete one revolution.

In addition to the gap in the rings known as Cassini's Division

several other fainter divisions exist. If a group of moonlets were

to revolve around the planet in the positions marked by these gaps

their periods of revolution would be commensurable with the periods

of several of the satellites of Saturn. As a result the attraction

exerted on such particles by these satellites would gradually disturb

their motion in such a way as to draw them away from these positions.

It is owing, therefore, to the attraction of the satellites of Saturn

for the moonlets that these gaps in the rings exist.

As a result of the disturbances produced in the motion of the

moonlets by the satellites of Saturn collisions are bound to occur

occasionally among the various particles. When two particles collide

the period of revolution of one or both of them is reduced and as a

result collisions tend to bring the moonlets gradually closer and

closer to the surface of the planet. The dusky inner ring, it is

believed, may consist largely of particles whose periods have been

continually shortened by collisions.

Saturn may, therefore, lose its ring system in the course of time

through its gradually being drawn down upon the planet by collisions

of the various particles until all of the material is finally swept

up by the planet. Such a change would probably require millions of

years, however, as collisions are probably, on the whole, infrequent.

It is possible that the ring system of Saturn may have been much more

extensive in the past than it is now and other members of our solar

system may have had such appendages in the far distant past.

The appearance of the rings of Saturn as viewed from our planet

changes periodically as a result of the revolution of the earth

and Saturn around the sun, which places them in constantly changing

positions with reference to each other. The rings lie in the plane of

Saturn's equator, which is inclined twenty-seven degrees to its orbit

and twenty-eight degrees to the Earth's orbit.

Since the position of the equator remains parallel to itself while

the planet is journeying around the sun it happens that half the time

the earth is elevated above the plane of the rings and the remainder

of the time it lies below the plane of the rings. Twice in the period

of Saturn's revolution around the sun, which occupies nearly thirty

years, the earth lies directly in the plane of the rings and at this

time the rings entirely disappear from view for a short time. Mid-way

between the two dates of disappearance the rings are tilted at their

widest angle with reference to the earth and they are then seen to

the best advantage. As the date of their disappearance approaches

they appear more and more like a line of light extending to either

side of the planet's equator. Even in the most powerful telescope

the rings entirely disappear from view for a few hours at the time

the earth lies exactly in the same plane. It is at this time that

the ball of the planet is best seen. Its flattening at the poles,

which is nearly ten per cent. of its equatorial diameter then gives

it a decidedly oval appearance. Ordinarily one of the hemispheres

of Saturn is partly or entirely concealed by the rings so that the

oblate form is not so noticeable. It was the change in the tilt and

visibility of the rings that so perplexed Galileo when he attempted

to make out the nature of these appendages of Saturn with his

crude telescope of insufficient magnifying power. So great was his

bewilderment when the rings finally disappeared that he cried out in

despair that Saturn must have swallowed his children, according to

the legend. He finally became so exasperated with the results of his

observations that he gave up observing the planet. The true nature of

these appendages of Saturn remained a mystery until Huygens solved

the problem in 1655, some time after the death of Galileo.

In addition to the rings, Saturn has nine satellites named, in the

order of their distance outward from the planet, Mimas, Enceladus,

Tethys, Dione, Rhea, Titan, Hyperion, Iapetus and Phoebe. The

last-mentioned satellite was discovered by W. H. Pickering in 1899.

It aroused great interest at the time because it was the first

satellite to be discovered with "retrograde" motion in its orbit. Two

satellites of Jupiter since discovered revolve in the same direction

around their primary.

The satellites of Saturn are approximate to those of Jupiter in

size and exactly equal them in number. The largest, Titan, is three

thousand miles in diameter and can be easily seen with the smallest

telescopes. With a four-inch telescope five of the satellites can

be readily found, though they are not as interesting to observe as

the satellites of Jupiter because they are far more distant from

the earth. The time they require to make one journey around Saturn

varies from nearly twenty-three hours for Mimas, the nearest, to

approximately five hundred and twenty-four days for Phoebe, the most

distant.

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