Earthquake
A late New York Evening
Post contains a letter from William L. Pierce, a
gentleman of respectability, who was on a tour from east
ward to New Orleans, which gives a more particular and
satisfactory account of the Earthquake and its effects on
the Mississippi than any yet published. The letter,
being very long, we can only insert such parts as are most
interesting. At the time of the first shocks
(Dec.16) the boat in which he was a passenger had landed
on the left bank of the Mississippi, about 116 miles from
the mouth of the Ohio. After stating the alarm,
occasioned by the violence of the shocks which occurred in
the night, he says -- Edit Lib. Hall.
At the dawn of day I went on shore to examine the
effects of the shocks; the earth about 20 feet from
the water’s edge was deeply cracked, but no visible
injury of moment had been sustained; fearing,
however, to remain longer where we were, it was
thought most advisable to leave our landing as
expeditiously as possible; this was immediately
done—at a few rods distance from the shore, we
experienced a fifth shock more severe than either of
the preceding.
I had expected this from the lowering appearances
of the weather; it was indeed most providential that
we started, for such was the strength of the last
shock that the bank to which we were (but a few
moments since) attached, was rent and fell into the
river, whilst the trees rushed from the forests,
precipitating themselves into the water with force
sufficient to have dashed us into a thousand atoms.
It was now light and we had an opportunity
of beholding in full extent all the horrors of our
situation. During the four first shocks,
tremendous and uninterrupted explosions, resembling a
discharge of artillery, was heard from the opposite
shore, at that time I imputed them to the falling of the
river banks.—this fifth shock explained the real cause.
Wherever the earthquake ran, there was a volcanic
discharge of combustible matter to great heights, an
incessant rumbling was heard below and the bed of the
river was excessively [agitated,] whilst the water
assumed a turbid [and] boiling appearance—near our boat
a spout [of] confined air breaking its way through the
[waters] burst forth, and with a loud report discharged
mud, sticks, etc. from the river’s [bed] at least 30
feet above the surface. Then it appeared to rise
to the very heavens. Large [trees] which had lain
for ages at the bottom of the river were shot up in
thousands of instances, some with their roots uppermost
and their [tops] planted; others were hurled into the
air; [many] again were only loosened and floated [upon]
the surface. Never was a scene more [replete] with
terrific threatenings of death; with [the] most lively
sense of this awful crisis, we contemplated in mute
astonishment a scene which completely beggars
description, and of which the most glowing imagination
is inadequate to form a picture. Here the earth,
[riven and] torn with furious convulsions, opened in
[large] trenches, whose deep jaws were instantaneously
closed; there through a thousand vents [sulphureous]
streams gushed from its very [bowels,] leaving vast and
almost unfathomable [caverns.] Every where nature
itself seemed [teetering] on the verge of
dissolution. [Encompassed] with the most alarming
dangers the [manly?] presence of mind and heroic
fortitude [of] the men were all that saved them.
It was [a] struggle for existence itself, and the [meed
to be?] purchased was our lives.
During the day there was very little
intermission, a continued series of shocks, attended
with innumerable explosions, like the [rolling?] of
thunder: the bed of the river was [incessantly]
disturbed, and the water boiled severely in every
part: I consider ourselves as [having] been in
the greatest danger from the [numerous] instances of
boiling directly under [the] boat; fortunately for us,
however, they [were] not attended with eruptions. - -
One of the [gouts?] which we had seen rising under the
boat [would?] inevitably have sunk it, and probably
have blown it into a thousand fragments; our [sides?]
were constantly assailed with the crushing [?] timber,
the banks were instantaneously [pushed?] down, and
fell with all their growth [into?] the water. It
was no less astonishing than [alarming?] to
behold the oldest trees of the [forest] whose firm
roots had withstood a thousand [storms] and weathered
the sternest tempests, [quivering?] and shaking with
the violence of the [shocks,] whilst their heads were
whipped [together?] with a quick and rapid
motion: many [were] torn from their native soil,
and hurled [with] tremendous force into the river; one
of [these] whose huge trunk (at least three feet in
[diameter]) had been much shattered, was thrown
[more?] than a hundred yards from the bank, [where] it
is planted in the bed of river, there [to stand?] a
terror to future navigators.
[Anxious] to obtain landing, and dreading the [?]
banks, we made for an island which [evinced?] sensible
marks of the earthquake; [there?] we fastened to some
willows, at the [extremity] of the sunken piece of
land, and [continued?] two days, hoping that this
scene of [horrors] wasnow over - - still, however, the
shocks [continued] though not with the like frequency
[as before.]
[On] Wednesday in the afternoon I visited [every] part
of the island where we lay, it was [extensive?] and
partially covered with willow. [The] earthquake
had rent the ground in large [?] numerous gaps; vast
quantities of burnt [wood?] in every stage of
alteration, from its [primitive?] nature to stove coal
had been spread [over] the ground to very considerable
distances; [frightful?] and hideous caverns yawned on
every [?], and the earth's bowels appeared to have the
tremendous force of the shocks which [?] thus riven
the surface. I was gratified [?] seeing several
places where those spouts [which] had so much
attracted our wonder and admiration had arisen, they
were generally on the beach, and have left large
circular holes in the sand formed much like a
funnel. For a great distance around the orfice
vast quantities of coal have been scattered, many
pieces weighing from 15 to 20 lbs, were discharged 160
measured paces. These holes were of
various dimensions, oen of them I observed most
particularly, it was 16 feet in perpendicular depth
and 63 feet in circumference at the mouth.
On Thursday morning the 19th, we loosed our cables,
with hearts filled with fervent gratitude to
Providence, whose protection had supported us through
the perils to which we had been exposed.
As we descended the river every thing was a
scene of ruin and devastation, where, a short time
since, the Mississippi rolled its waters in a calm and
placid current, now, subterranean forests have been
ushered into existence and raise their heads hard and
black as ebony, above the surface of the water, whose
power has been so wonderfully increased that our
strength and skill are equally baffled. Our boat
was borne down by an irresistable impulse, and
fortunately escaped uninjured. We passed
thousands of acres of land which had been cleft from
the main shore and tumbled intot he water, leaving
their growth waving above the surface. In many
places, single trees & whole brakes of cane had
slipped into the river. A single instance
of this kind peculiarly attracted my observation; a
large sycamore had slipped from its station on the
bank and had so admirably preserved its
equilibrium that it has een left standing erect in
thew ater, immersed about ten feet, and has every
appearance of having originally grown there.
The obstructions in the river, which have always been
quite numerous, are now so considerably encreased as
to demand the utmost prudence and caution from
subsequent navigators, indeed I am very apprehensive
that it will be almost impassablei n flood water, for
until such time, it will be impossible to say where
the currents will hereafter run, what portion (if any)
of the present embarrassments will be destroyed, and
what new sand bars, &c. may yet be caused by this
portentous phenomenon. Many poor fellows are
undoubtedly wrecked or buried under the ruin of the
banks. Of the loss of four boats I am certain.
It is almost impossible to trace at present the exact
course of this earthquake or where the greatest
injuries have happened. From numerous inquiries
however, which I have made of persons above and below
us at the time of the first shock, I am induced to
believe, that we were very nearly in the height of it;
the ruin immediately in the vicinity of the river, is
most extensive on the right side in descending.
For the first two days the veins appeared to run a due
course from W. to E. afterwards they became more
variable, and generally took a N.W. direction.
A little below Bayou River, 130 miles from mouth of
Ohio, and 13 miles from the spot where we lay, the
ruin begins intensive and general.
At Long Beach, 146 miles, there is one continued
forest of roots and trees which have been ejected from
the bed of the river.
At and near Fleur Island, 174 miles, the destruction
has been very great, and the impediments in the river
much increased.
At the Devils Race Ground, 193 miles, an immense
number of very large trees have been thrown up, and
the river is nearly impassable. The Devil’s
Elbow, 214 miles, is in the same predicament, below
this, the ruin is much less, and, indeed, no material
traces of the earthquake are discoverable.
It is a circumstance well worthy of
remark, that during the late convulsions the current of
the river was almost instantaneously and rapidly
increased. In times of the highest floods it rates at
from 4 to 5 knots per hour. The water is now low,
and when we stopped on the 16th inst. at half after 4
P.M. we had then run from that morning 52 miles rating
at 6 knots generally. This current was increased
for two days, and then fell to its usual force. It
is also singular that the water has fallen with
astonishing rapidity. The most probable and easy
solution of this fact, which presented itself to my
mind, was, that the strength of the Mississippi current
was greater than the tributary streams could support.
It is a singular, but well authenticated
fact, that in several places on the Mississippi, where
the shocks were most severe, the earth was rent (as it
were) by two distinct processes. By one it burst
asunder, and instantaneously closed, leaving no traces
whatever of the shock; by the other it was rent, and an
electric flash ran along the surface, tearing the earth
to pieces in its progress. These last were
generally attended with an explosion and streams of
matter, in a liquid state, gushed from the gaps which
were left open when the shocks subsided, and were, in
many instances of an immense depth.
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