The Boy Travellers in the Far East, Part Third: Adventures of Two Youths in a Journey to Ceylon and India; With Descriptions of Borneo, the Philippine Islands and BurmahKnox, Thomas Wallace
General
The Boy Travellers in the Far East, Part Third: Adventures of Two Youths in a Journey to Ceylon and India; With Descriptions of Borneo, the Philippine Islands and Burmah
Knox, Thomas Wallace
East Indies -- Description and travel -- Juvenile literature
"A shooting-star!" Frank exclaimed.
"Or perhaps a meteor," Fred responded.
"Either way you like," said the Doctor, "as both names are used for the
phenomenon. It also has the name of 'falling-star,' as the path is
generally downward, or apparently so."
Frank asked what a shooting-star, meteor, or falling-star was composed
of, and what was the reason of its appearance.
"That is a question more easily asked than answered," the Doctor
replied. "Scientific men in all parts of the world have devoted a great
deal of time and attention to the subject, but they are not, as yet,
satisfactorily informed as to the character of the meteor."
"Don't they fall on the earth sometimes?" Fred inquired. "I have read
of aerolites that came from the air to the earth, and were composed of
solid matter. Are not these aerolites parts of shooting-stars?"
"Circumstantial evidence favors the theory that some of the aerolites
come from falling-stars; but, at the same time, no solid matter has
reached the earth that can be directly traced to one. The amount of
solid matter in an ordinary shooting-star is so small that it is thought
to be consumed in its passage through the air, where its great velocity
causes it to be heated to a very high degree; whenever anything has
fallen from the sky to the earth, and been found at the time of its
fall, it is always intensely hot."
"How far off was that meteor we just saw?" said Frank.
"Fifty or sixty miles, I presume," the Doctor answered. "It has been
determined that shooting-stars begin to be visible at distances varying
from forty to one hundred and twenty miles, and disappear at from thirty
to eighty miles. During the time we saw it, it moved about ninety miles;
it was in sight three or four seconds, and its velocity was, therefore,
not far from thirty miles a second; a pretty fast rate of travelling."
"Ever so much faster than a cannon-ball," Fred remarked. "No wonder it
gets heated so that it is consumed."
"But you didn't tell us about the aerolites, and what they are made of,"
Frank protested.
"Nor about the circumstantial evidence in favor of their coming from the
shooting-stars," added Fred.
"Several instances may be given," Doctor Bronson replied; "but the
following from Professor Loomis will be sufficient to illustrate the
theory:
"On the morning of December 14th, 1807, a meteor of great brilliancy was
seen moving in the atmosphere over the town of Weston, in Connecticut.
Its apparent diameter was about half that of the full-moon; when it
disappeared several persons heard a sound resembling the discharge of a
cannon, followed by smaller reports like a fire of musketry. Soon after
the explosions a man heard a sound like the falling of a heavy body, and
upon examination he discovered that a stone had fallen upon a rock near
his house and was dashed into fragments, which were quite hot when
picked up. When put together they were found to weigh about twenty
pounds.
Public-domain text, read in full here on John Shaqi.
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