The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
All of our readers will recollect the Jamaica earthquake which
occurred comparatively recently. Port Kingston, in Jamaica, has had
its share of earthquake disasters. In the year 1692 Port Royal, the
then chief city, was destroyed, and in rebuilding it the Jamaicans
moved it across the harbour, because the old town site was largely
submerged beneath the sea. It was a recurrence of the settlement
of the ground which in part produced the earthquake of January
14th, 1907. There were slight shocks preceding the earthquake, and
subterranean rumblings. The chief damage was done before thirty-five
seconds had gone by, and of course the catastrophe was greater
because the shocks were felt in the neighbourhood of a city.
Considered by itself the earthquake was not of the order of "great"
earthquakes, but many of the effects were most curious. A statue of
Queen Victoria on a pedestal was partly turned round; a series of
steep terraces was formed by the side of the harbour; a small spring
was converted into a stream eight feet wide; and, as we all know,
very great destruction was inflicted on life and property. Soundings
which have since then been made in the harbour show that its depth
has greatly increased in some parts, in one instance by not less
than twenty-seven feet. The greatest depression occurred near Port
Royal (the old city), where a hundred yards or more of the ground was
submerged by water varying from eight to twenty-five feet in depth.
Proceeding northwards from the Antilles to North America, we come
to other famous areas of earthquake disturbance. In 1811 and 1812
there were earthquakes along the lower lands of the great Mississippi
River, which were felt throughout the whole of the eastern portion
of the United States and as far west as exploration had gone. At
New Madrid, which appears to have been near the centre of the
disturbance, "subterranean thunder" appears to have been heard
frequently for many years preceding the earthquake, though it had
ceased for nearly a year. About two o'clock in the morning of
December 16th, 1811, there came a severe shock accompanied by a noise
which was like near thunder, and a few minutes afterwards the air was
filled with sulphurous vapour. People thought that the end of the
world had come. Light shocks were felt till sunrise; and then one
more violent than the first occurred. But this was not the end. For
three months the shocks went on, and in that time no fewer than 1874
shocks were recorded, eight of them great ones. The shock of January
23rd, though as violent as any that preceded it, was surpassed by
the so-called "hard shock," which came at about four o'clock in the
afternoon of February 7th. It was accompanied by a discharge of
sulphurous vapour in the atmosphere, and an unusual darkness which
added greatly to the terror of the people.
[Illustration:
_Stereo Copyright, Underwood & U._ _London and New York_
A House destroyed by an Earthquake
Public-domain text, read in full here on John Shaqi.
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