J. Mark Lowe
Two hundred and thirteen years ago, (1811) an earthquake along the New Madrid fault created fear and turmoil throughout the South. Church pews were filled and calls of the end of the world were commonplace. The President was James Madison. He organized a large geographic survey to understand the extent of the earthquake damage. He was forced to face other issues very quickly with the War of 1812.
James Madison was President during these earthquakes. |
Let’s take a look at a
collection of scientific observations from an 1814 report.
The testimony of Colonel Samuel Hammong (6 Feb 1812) was to
the following effect. He confined himself strictly to what he knew from
personal observation. The first shock he witnessed was on the 15/16th of
December last (1811). A few seconds before the motion was felt, he and others
heard a considerable roaring or rumbling noise, resembling a blaze of fire
acted upon by wind. The motion of the frame of the house on which he stood was
tremulous. It began instantly after to rock pretty violently. This continued,
as he thought, about ten to twelve minutes. The vibrations of the chimney were,
perhaps, about three or four inches each way, and were in the direction of
southeast and northwest nearly. The noise which preceded the shock was from the
northwest. Its commencement was about two o'clock in the morning. One hour
after there was a second, which was light, and of very short duration. No
houses or chimneys were thrown down by either of those. The motion was very
much like the first, but of short duration. This injured several brick and
stone chimneys. Its duration between one and a half and two and a half minutes.
About sunrise the same morning there was a fourth shock. The vibrations of the
chimneys at twenty-five feet from the ground, were at least four inches each
way. The direction was the same as the first. The motion of the earth was very
perceptible. Cradles rocked, and the church bells rang. Several chimneys were
cracked to their bases, and some were broken off as low as the stem or funnel.
In this last shock, the water in the river Mississippi was thrown into
commotion, bubbling like boiling water; and, in a few minutes, the whole
atmosphere was filled with smoke or fog, so that a boat could not be seen
within twenty paces from the water's edge; and the houses were so shrouded as
not to be seen fifty feet; this smoke continued all the forepart of that day.
In passing along upon his journey, he found the effects had
been pretty uniform, and their occurrence and duration nearly the same, as far
as Carthage, in the state of Tennessee. There were one or more shocks every
twenty-four hours, from the first-mentioned one, until the night of January 1,
1812. Then, at about half after three in the morning, being at Carthage, he
felt a more severe shock. It threw bricks from a chimney which had been
previously broken by the first shock; he found, on inquiry, that the motion was
considerably greatest near the large water courses. The courthouse at Carthage
is a large brick edifice, and was cracked to its foundation, and considerably
damaged. Several chimneys had been cast down, by the shock of the 16th of
December. Everywhere it was stated to him by those who witnessed the motions,
that they were from the south of west, to the opposite point, or vice versa. In
the county of Christian, (Kentucky) a fine and fresh spring was observe to run
very muddy for several hours. On examining it, after the mud had settled, he
found it to be so strongly impregnated with sulphur; so much so that it was
spoiled for domestic uses; indeed it had been converted to one of the strongest
brimstone springs he ever saw.
I add another respectable communication, from Mr. Joseph
Ficklin of Russellville, (Kentucky) who thus describes the earthquakes, in a
letter dated 5 Feb 1812: The shocks continue. The accounts that you will see in
the Nashville and Lexington papers may be confided in. I have conversed with
several persons from New Madrid, all of whom confirm the above. The bottom of
the Mississippi river, two under miles west of this place, was cracked in some
places fifteen feet in width, and cast up warm water sufficient to inundate the
settlement from one to two feet. In this situation, the poor inhabitants sought
for the highest ground, where some remained for seventeen days, looking for the
earth to swallow them up.
Source: A Detailed Narrative Of The Earthquakes, US
Geological Services, 1814.
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