The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
Gradually the development of the volcanic energy proceeded, and
gradually the terror of the inhabitants of the surrounding coasts rose
to a climax. July had ended before the manifestations of Krakatoa had
attained their full violence. As the days of August passed by the spasms
of Krakatoa waxed more and more vehement. By the middle of that month
the panic was widespread, for the supreme catastrophe was at hand.
[Illustration: Fig. 26.—SHOWING COASTS INVADED BY THE GREAT SEA-WAVES
FROM KRAKATOA.
(_From the Royal Society’s Reports._)]
On the night of Sunday, August 26th, 1883, the blackness of the
dust-clouds, now much thicker than ever in the Straits of Sunda and
adjacent parts of Sumatra and Java, was only occasionally illumined by
lurid flashes from the volcano. The Krakatoan thunders were on the point
of attaining their complete development. At the town of Batavia, a
hundred miles distant, there was no quiet that night. The houses
trembled with the subterranean violence, and the windows rattled as if
heavy artillery were being discharged in the streets. And still these
efforts seemed to be only rehearsing for the supreme display. By ten
o’clock on the morning of Monday, August 27th, 1883, the rehearsals were
over and the performance began. An overture, consisting of two or three
introductory explosions, was succeeded by a frightful convulsion which
tore away a large part of the island of Krakatoa and scattered it to the
winds of heaven. In that final effort all records of previous explosions
on this earth were completely broken.
This supreme effort it was which produced the mightiest noise that, so
far as we can ascertain, has ever been heard on this globe. It must have
been indeed a loud noise which could travel from Krakatoa to Batavia and
preserve its vehemence over so great a distance; but we should form a
very inadequate conception of the energy of the eruption of Krakatoa if
we thought that its sounds were heard by those merely a hundred miles
off. This would be little indeed compared with what is recorded, on
testimony which it is impossible to doubt.
[Illustration: THE EARLY STAGE OF THE ERUPTION OF KRAKATOA.
(_From a Photograph taken on May 27th, 1883._)]
Westward from Krakatoa stretches the wide expanse of the Indian Ocean.
On the opposite side from the Straits of Sunda lies the island of
Rodriguez, the distance from Krakatoa being almost three thousand miles.
It has been proved by evidence which cannot be doubted that the booming
of the great volcano attracted the attention of an intelligent
coastguard on Rodriguez, who carefully noted the character of the sounds
and the time of their occurrence. He had heard them just four hours
after the actual explosion, for this is the time the sound occupied on
its journey.
We shall better realise the extraordinary vehemence of this tremendous
noise if we imagine a similar event to take place in localities more
known to most of us than are the far Eastern seas.
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.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account