Geology: The Science of the Earth's Crust — John Stuart Mill — John Shaqi
Geology: The Science of the Earth's Crust
John Stuart Mill · en
Since the problem of the origin of the earth is an essential part of
the problem of the origin of the solar system, the following well-known
facts should be clearly in the mind of the reader. Eight planets,
including the earth, revolve in nearly circular paths around the
central sun, whose diameter is 866,000 miles. The radius of the solar
system is at least 2,800,000,000 miles, this being the distance of
the outermost known planet (Neptune) from the Sun. Neptune requires
164 years for a trip around the sun, while the earth, which averages
about 93,000,000 miles from the sun, makes its circuit once a year. The
planets all revolve around the sun in the same direction, and in nearly
the same plane. The sun and all eight planets rotate on their axes
in the same direction, the earth's rotation being accomplished every
twenty-four hours. Most of the planets have one or more smaller bodies
called satellites revolving about them, such as Earth, with its one
satellite (the moon), and Saturn, with its eight satellites, etc. It is
well known that this solar system is only a very small part of the vast
universe, as shown by the facts that no star is nearer the earth than
several trillion miles, and that some stars are so far away that light
traveling at the rate of 186,000 miles per second requires a thousand
years to reach the earth!
Toward the end of the eighteenth century the famous nebular or ring
hypothesis was set forth by the astronomer named Laplace. This assumes
an original very hot incandescent mass of gas spheroidal in shape and
greater in diameter than the present solar system. This mass rotated
in the direction of rotation of our sun and its planets. Loss of heat
by radiation caused the mass to shrink, and this in turn not only made
it rotate faster, but also caused the centrifugal force (i.e., the
force whose direction was from the center) in its equatorial portion
to gradually become stronger. Finally a time came when the force of
gravity (i.e., the force whose direction was toward the center) and the
centrifugal force became equal and a ring was left (not thrown) off,
while the rest of the mass of gas continued to shrink. After a time the
material of the ring collected to form the outermost planet. The other
planets were similarly formed from other rings which were left off as
contraction of the great mass of gas went on. The sun represents the
remainder of the great mass of rotating gas.