Natural history -- Nicaragua; Nicaragua -- Description and travel
"The strangest fact about this eruption was, that the mountain did
not make use of its old crater. The original vent must have become
so jammed and consolidated, in the few years between 1785 and 1812,
that it could not be reopened even by a steam-force the vastness of
which may be guessed at from the vastness of the area which it had
shaken for two years. So when the eruption was over it was found
that the old crater-lake, incredible as it may seem, remained
undisturbed, as far as has been ascertained. But close to it, and
separated only by a knife-edge of rock some 700 feet in height, and
so narrow that, as I was assured by one who had seen it, it is
dangerous to crawl along it, a second crater, nearly as large as
the first, had been blasted out, the bottom of which, in like
manner, is now filled with water.
"The day after the explosion, 'Black Sunday,' gave a proof, but no
measure, of the enormous force which had been exerted. Eighty miles
to windward lies Barbados. All Saturday a heavy cannonading had
been heard to the eastward. The English and French fleets were
surely engaged. The soldiers were called out, the batteries manned,
but the cannonade died away, and all went to bed in wonder. On the
1st of May the clocks struck six; but the sun did not, as usual in
the tropics, answer to the call. The darkness was still intense,
and grew more intense as the morning wore on. A slow and silent
rain of impalpable dust was falling over the whole island.
"The trade-wind had fallen dead; the everlasting roar of the surf
was gone; and the only noise was the crashing of the branches
snapped by the weight of the clammy dust. About one o'clock the
veil began to lift, a lurid sunlight stared in from the horizon,
but all was black overhead. Gradually the dust-cloud drifted away;
the island saw the sun once more, and saw itself inches deep in
black, and in this case fertilising, dust.
"Those who will recollect that Barbados is eighty miles to windward
of St. Vincent, and that a strong breeze from east-north-east is
usually blowing from the former island to the latter, will be able
to imagine, not to measure, the force of an explosion which must
have blown the dust several miles into the air above the region of
the trade-wind. Whether into a totally calm stratum or into that
still higher one in which the heated south-west wind is hurrying
continually from the tropics toward the pole."* (* "At Last" by
Charles Kingsley volume 1 page 90.)
Public-domain text, read in full here on John Shaqi.
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