The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
But, besides these phenomenal undulations, this mighty incident at
Krakatoa has taught us other lessons on the constitution of our
atmosphere. We previously knew little, or I might almost say nothing, as
to the conditions prevailing above the height of ten miles overhead. We
were almost altogether ignorant of what the wind might be at an altitude
of, let us say, twenty miles. It was Krakatoa which first gave us a
little information which was greatly wanted. How could we learn what
winds were blowing at a height four times as great as the loftiest
mountain on the earth, and twice as great as the loftiest altitude to
which a balloon has ever soared? We could neither see these winds nor
feel them. How, then, could we learn whether they really existed? No
doubt a straw will show the way the wind blows, but there are no straws
up there. There was nothing to render the winds perceptible until
Krakatoa came to our aid. Krakatoa drove into those winds prodigious
quantities of dust. Hundreds of cubic miles of air were thus deprived of
that invisibility which they had hitherto maintained. They were thus
compelled to disclose those movements about which, neither before nor
since, have we had any opportunity of learning.
With eyes full of astonishment men watched those vast volumes of
Krakatoa dust start on a tremendous journey. Westward the dust of
Krakatoa took its way. Of course, everyone knows the so-called
tradewinds on our earth’s surface, which blow steadily in fixed
directions, and which are of such service to the mariner. But there is
yet another constant wind. We cannot call it a trade-wind, for it never
has rendered, and never will render, any service to navigation. It was
first disclosed by Krakatoa. Before the occurrence of that eruption no
one had the slightest suspicion that far up aloft, twenty miles over our
heads, a mighty tempest is incessantly hurrying with a speed much
greater than that of the awful hurricane which once laid so large a part
of Calcutta on the ground, and slew so many of its inhabitants.
Fortunately for humanity, this new trade-wind does not come within less
than twenty miles of the earth’s surface. We are thus preserved from the
fearful destruction that its unintermittent blasts would produce, blasts
against which no tree could stand, and which would, in ten minutes, do
as much damage to a city as would the most violent earthquake. When this
great wind had become charged with the dust of Krakatoa, then, for the
first and, I may add, for the only time, it stood revealed to human
vision. Then it was seen that this wind circled round the earth in the
vicinity of the Equator, and completed its circuit in about thirteen
days.
Public-domain text, read in full here on John Shaqi.
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