The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
stars and their positions would be recorded in their millions; but, said
the philosopher to whom I have referred, though you might accomplish all
this, and much more in the same direction, yet there is a well-marked
limit to your possible achievements; you can, he said, never expect to
discover the actual chemical elements of which the heavenly bodies are
composed. Nobody could dispute the reasonableness of this statement at
the time he made it; indeed, it seemed to be a necessary deduction from
our knowledge of the arts of chemistry, as those arts were understood
before the middle of the last century.
In the prosecution of his researches by the older method, the chemist
could no doubt discover the different elements of which the body was
formed. That is to say, his art enabled him to accomplish this task,
provided one very essential and fundamental condition could be complied
with. However accomplished the chemist of fifty years ago might have
been, he would assuredly have thought that he was being mocked if asked
to determine the composition of a body which was 93,000,000 miles away
from him. The very idea of forming an analysis under such conditions
would have been scouted as preposterous. He would naturally ask that a
specimen of the body should be delivered into his hands, a specimen
which he could take into his laboratory, pulverise in his mortars, place
in his test-tubes, treat with his re-agents, or examine with his
blowpipe. Only by such methods was it then thought possible to obtain an
analysis and discover the elements from which any given substance was
formed.
For in the early part of this century the splendid method of spectrum
analysis, that method which has revealed to us so many of the secrets of
Nature, had not yet come into being. When that memorable event took
place it was at once perceived that the spectroscope required no actual
contact with the object to be tested, but only asked to receive some of
the rays of light which that object dispersed when sufficiently heated.
It was obvious that this new method must be capable of an enormously
enlarged application. The flame producing the vapour might be at one end
of the room, while the spectroscope testing the elements in that vapour
might be at the other end. This new and beautiful optical instrument
could analyse an object at a distance of a hundred feet. But if
applicable at a distance of a hundred feet, why not at a hundred yards,
or a hundred miles, or a hundred million miles? Why might the method not
be used if the source of light were as far as the sun, or as far as a
star, or even as far as the remotest nebula, whose faint gleam on the
sky is all that the mightiest telescope can show.
Public-domain text, read in full here on John Shaqi.
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