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Atlantis : the antediluvian world by Ignatius Donnelly
page 44 of 487 (09%)
fable. With the wider knowledge which scientific research has afforded
the modern world, we can affirm that such an event is not only possible,
but that the history of even the last two centuries has furnished us
with striking parallels for it. We now possess the record of numerous
islands lifted above the waters, and others sunk beneath the waves,
accompanied by storms and earthquakes similar to those which marked the
destruction of Atlantis.

In 1783 Iceland was visited by convulsions more tremendous than any
recorded in the modern annals of that country. About a month previous to
the eruption on the main-land a submarine volcano burst forth in the
sea, at a distance of thirty miles from the shore. It ejected so much
pumice that the sea was covered with it for a distance of 150 miles, and
ships were considerably impeded in their course. A new island was thrown
up, consisting of high cliffs, which was claimed by his Danish Majesty,
and named "Nyoe," or the New Island; but before a year had elapsed it
sunk beneath the sea, leaving a reef of rocks thirty fathoms under water.

The earthquake of 1783 in Iceland destroyed 9000 people out of a
population of 50,000; twenty villages were consumed by fire or inundated
by water, and a mass of lava thrown out "greater than the entire bulk of
Mont Blanc."

On the 8th of October, 1822, a great earthquake occurred on the island
of Java, near the mountain of Galung Gung. "A loud explosion was heard,
the earth shook, and immense columns of hot water and boiling mud, mixed
with burning brimstone, ashes, and lapilli, of the size of nuts, were
projected from the mountain like a water-spout, with such prodigious
violence that large quantities fell beyond the river Tandoi, which is
forty miles distant. . . . The first eruption lasted nearly five hours;
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