The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
In 1883 Krakatoa suddenly sprang into notoriety. Insignificant though it
had hitherto seemed, the little island was soon to compel by its tones
of thunder the whole world to pay it instant attention. It was to become
the scene of a volcanic outbreak so appalling that it is destined to be
remembered throughout the ages. In the spring of that year there were
symptoms that the volcanic powers in Krakatoa were once more about to
awake from the slumber that had endured for many generations. Notable
warnings were given. Earthquakes were felt, and deep rumblings proceeded
from the earth, showing that some disturbance was in preparation, and
that the old volcano was again to burst forth after its long period of
rest. At first the eruption did not threaten to be of any serious type;
in fact, the good people of Batavia, so far from being terrified at what
was in progress in Krakatoa, thought the display was such an attraction
that they chartered a steamer and went forth for a pleasant picnic to
the island. Many of us, I am sure, would have been delighted to have
been able to join the party who were to witness so interesting a
spectacle. With cautious steps the more venturesome of the excursion
party clambered up the sides of the volcano, guided by the sounds which
were issuing from its summit. There they beheld a vast column of steam
pouring forth with terrific noise from a profound opening about thirty
yards in width.
As the summer of this dread year advanced the vigour of Krakatoa
steadily increased, the noises became more and more vehement; these were
presently audible on shores ten miles distant, and then twenty miles
distant; and still those noises waxed louder and louder, until the great
thunders of the volcano, now so rapidly developing, astonished the
inhabitants that dwelt over an area at least as large as Great Britain.
And there were other symptoms of the approaching catastrophe. With each
successive convulsion a quantity of fine dust was projected aloft into
the clouds. The wind could not carry this dust away as rapidly as it was
hurled upwards by Krakatoa, and accordingly the atmosphere became
heavily charged with suspended particles. A pall of darkness thus hung
over the adjoining seas and islands. Such was the thickness and the
density of these atmospheric volumes of Krakatoa dust that, for a
hundred miles around, the darkness of midnight prevailed at midday. Then
the awful tragedy of Krakatoa took place. Many thousands of the
unfortunate inhabitants of the adjacent shores of Sumatra and Java were
destined never to behold the sun again. They were presently swept away
to destruction in an invasion of the shore by the tremendous waves with
which the seas surrounding Krakatoa were agitated.
Public-domain text, read in full here on John Shaqi.
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