Curiosities of Science, Past and Present: A Book for Old and YoungTimbs, John
Science
Curiosities of Science, Past and Present: A Book for Old and Young
Timbs, John
Science
In conformity with the Copernican view of our system, we must learn to
look upon the sun as the comparatively motionless centre about which
the earth performs an annual elliptic orbit of the dimensions and
excentricity, and with a velocity, regulated according to a certain
assigned law; the sun occupying one of the foci of the ellipse, and
from that station quietly disseminating on all sides its light and
heat; while the earth travelling round it, and presenting itself
differently to it at different times of the year and day, passes
through the varieties of day and night, summer and winter, which we
enjoy.--_Sir John Herschel’s Outlines of Astronomy._
Laplace has shown that the length of the day has not varied the
hundredth part of a second since the observations of Hipparchus, 2000
years ago.
STABILITY OF THE OCEAN.
In submitting this question to analysis, Laplace found that the
_equilibrium of the ocean is stable if its density is less than
the mean density of the earth_, and that its equilibrium cannot be
subverted unless these two densities are equal, or that of the earth
less than that of its waters. The experiments on the attraction of
Schehallien and Mont Cenis, and those made by Cavendish, Reich, and
Baily, with balls of lead, demonstrate that the mean density of the
earth is at least _five_ times that of water, and hence the stability
of the ocean is placed beyond a doubt. As the seas, therefore, have at
one time covered continents which are now raised above their level,
we must seek for some other cause of it than any want of stability in
the equilibrium of the ocean. How beautifully does this conclusion
illustrate the language of Scripture, “Hitherto shalt thou come, but no
further”! (_Job_ xxxviii. 11.)
COMPRESSION OF BODIES.
Sir John Leslie observes, that _air compressed_ into the fiftieth
part of its volume has its elasticity fifty times augmented: if it
continued to contract at that rate, it would, from its own incumbent
weight, acquire the density of water at the depth of thirty-four
miles. But water itself would have its density doubled at the depth
of ninety-three miles, and would attain the density of quicksilver at
the depth of 362 miles. In descending, therefore, towards the centre,
through nearly 4000 miles, the condensation of ordinary substances
would surpass the utmost powers of conception. Dr. Young says, that
steel would be compressed into one-fourth, and stone into one-eighth,
of its bulk at the earth’s centre.--_Mrs. Somerville._
THE WORLD IN A NUTSHELL.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account