Nature readers : $b Sea-side and way-side. No. 4 — John Shaqi
Nature readers : $b Sea-side and way-side. No. 4Wright, Julia McNair
Science
Nature readers : $b Sea-side and way-side. No. 4
Wright, Julia McNair
Nature study -- Juvenile literature; Readers
Before we consider the orbs which compose our own solar system, their
motions and relationships, which we shall do in another chapter, let
us consider for a little the theory of the origin of systems, taking
our own for a sample of the rest. Tennyson the poet, puts the story of
system-building thus:--
“This world was once a fluid haze of light
Till toward the centre set the starry tides,
And eddied into suns that wheeling cast
The planets.”
We saw in a previous lesson that our world was once a vast ball
of fiery vapor. The great astronomer Laplace, after many years of
study, published a theory about system-making, called the “Nebular
Hypothesis,” which, as simply as we can put it, is this: First, there
is a great cloud of glowing vapor, the various particles of which
are by the law of gravitation drawn toward a single centre. As the
particles press equally to the centre from all sides, it is evident
that the first result will be a ball of constantly increasing solidity.
This nebulous mass possesses also a motion of rotation, or turning over
on its own axis. As the ball grows smaller and more dense, it will spin
round faster and faster.
The gaseous matter of the sphere having become fluid or partly fluid,
the ball still whirls on, and we must now notice a second motion,
called centrifugal or tangental, which has become more apparent as the
rotation increases in velocity. While by the force of gravity all atoms
seek the centre, by this centrifugal force atoms are driven from the
centre. This tangental motion is familiarly seen in the case of mud
on a wheel-tire, the mud being flung off from the wheel by a motion
created by rotation. So from the spinning globe a ring of matter will
be detached and fly off into space.
If this ring were equally hard and thick in all its parts, and exactly
poised about the globe from which it sprung, it might keep the ring
shape. But in nearly all cases the ring when flung off would be
irregular, and would consequently break up. As it broke, the largest
fragments, keeping the wheeling motion and made spherical by gravity,
would draw into themselves the smaller near fragments. Then, after a
while, following the example of the globe from which they spun off,
these new globes would cast off rings of matter which would contract
and harden into globes, and become their satellites or attendants, as
they, held by the force of gravity, remain attendants upon the first
great globe.
Public-domain text, read in full here on John Shaqi.
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