New Madrid Earthquake
Based on maps in W. Atkinson, 1989, The Next New Madrid Earthquake, Southern Illinois University Press
Hartford is about 155 miles from New Madrid, MO, as the crow flies. Near enough to be shaken hard in 1811 and 1812 (magnitude 5 or 6 on the map above). I’m certain these earthquakes and aftershocks were frightening to our ancestors, and probably resulted in injury and property damage.
The three earthquakes occurred in 1811 and 1812 near New Madrid, MO. They are among the Great earthquakes of known history, affecting the topography more than any other earthquake on the North American continent. Judging from their effects, they were of a magnitude of 8.0 or higher on the Richter Scale. They were felt over the entire United States outside of the Pacific coast. Large areas sank into the earth, new lakes were formed, the course of the Mississippi River was changed, and forests were destroyed over an area of 150,000 acres. Many houses at New Madrid were thrown down. "Houses, gardens, and fields were swallowed up" one source notes. But fatalities and damage were low, because the area was sparsely settled then.
The probability for an earthquake of magnitude 6.0 or greater is significant in the near future, with a 50% chance by the year 2000 and a 90% chance by the year 2040. A quake with a magnitude equal to that of the 1811- 1812 quakes could result in great loss of life and property damage in the billions of dollars. Scientists believe we could be overdue for a large earthquake and through research and public awareness may be able to prevent such losses.
EYEWITNESS ACCOUNTS OF THE NEW MADRID EARTHQUAKE
(1) The following letter was found in a book entitled, "Lorenzo Dow's Journal," Published by Joshua Martin, printed by John B. Wolff, 1849, on pages 344 - 346. This was written by Eliza Bryan, a resident of New Madrid, MO.
New Madrid, Territory of Missouri, March 22, 1816
In compliance with your request, I will now give you a history, as full in detail as the limits of the letter will permit, of the late awful visitation of Providence in this place and vicinity.
On the 16th of December, 1811, about two o'clock, A.M., we were visited by a violent shock of an earthquake, accompanied by a very awful noise resembling loud but distant thunder, but more hoarse and vibrating, which was followed in a few minutes by the complete saturation of the atmosphere, with sulphurious vapor, causing total darkness. The screams of the affrighted inhabitants running to and fro, not knowing where to go, or what to do - the cries of the fowls and beasts of every species - the cracking of trees falling, and the roaring of the Mississippi - the current of which was retrogade for a few minutes, owing as is supposed, to an irruption in its bed -- formed a scene truly horrible.
From that time until about sunrise, a number of lighter shocks occurred; at which time one still more violent than the first took place, with the same accompaniments as the first, and the terror which had been excited in everyone, and indeed in all animal nature, was now, if possible doubled. The inhabitants fled in every direction to the country, supposing (if it can be admitted that their minds can be exercised at all) that there was less danger at a distance from, than near to the river. In one person, a female, the alarm was so great that she fainted, and could not be recovered.
There were several shocks of a day, but lighter than those already mentioned until the 23d of January, 1812, when one occurred as violent as the severest of the former ones, accompanied by the same phenomena as the former. From this time until the 4th of February the earth was in continual agitation, visibly waving as a gentle sea. On that day there was another shock, nearly as hard as the proceeding ones. Next day four such, and on the 7th about 4 o'clock A.M., a concussion took place so much more violent than those that had proceeded it, that it was dominated the hard shock. The awful darkness of the atmosphere, which was formerly saturated with sulphurious vapor, and the violence of the tempestuous thundering noise that accompanied it, together with all of the other phenomena mentioned as attending the former ones, formed a scene, the description of which would require the most sublimely fanciful imagination.
At first the Mississippi seemed to recede from its banks, and its waters gathering up like a mountain, leaving for the moment many boats, which were here on their way to New Orleans, on bare sand, in which time the poor sailors made their escape from them. It then rising fifteen to twenty feet perpendicularly, and expanding, as it were, at the same moment, the banks were overflowed with the retrogade current, rapid as a torrent - the boats which before had been left on the sand were now torn from their moorings, and suddenly driven up a little creek, at the mouth of which they laid, to the distance in some instances, of nearly a quarter of a mile. The river falling immediately, as rapid as it had risen, receded in its banks again with such violence, that it took with it whole groves of young cotton-wood trees, which ledged its borders. They were broken off which such regularity, in some instances, that persons who had not witnessed the fact, would be difficultly persuaded, that is has not been the work of art. A great many fish were left on the banks, being unable to keep pace with the water. The river was literally covered with the wrecks of boats, and 'tis said that one was wrecked in which there was a lady and six children, all of whom were lost.
In all the hard shocks mentioned, the earth was horribly torn to pieces - the surface of hundreds of acres, was, from time to time, covered over, in various depths, by the sand which issued from the fissures, which were made in great numbers all over this country, some of which closed up immediately after they had vomited forth their sand and water, which it must be remarked, was the matter generally thrown up. In some places, however, there was a substance somewhat resembling coal, or impure stone coal, thrown up with the sand. It is impossible to say what the depths of the fissures or irregular breaks were; we have reason to believe that some of them are very deep.
The site of this town was evidently settled down at least fifteen feet, and not more than a half a mile below the town there does not appear to be any alteration on the bank of the river, but back from the river a small distance, the numerous large ponds or lakes, as they are called, which covered a great part of the country were nearly dried up. The beds of some of them are elevated above their former banks several feet, producing an alteration of ten, fifteen to twenty feet, from their original state. And lately it has been discovered that a lake was formed on the opposite side of the Mississippi, in the Indian country, upwards of one hundred miles in length, and from one to six miles in width, of the depth of ten to fifty feet. It has communication with the river at both ends, and it is conjectured that it will not be many years before the principal part, if not the whole of the Mississippi, will pass that way.
We were constrained by the fear of our houses falling to live twelve or eighteen months, after the first shocks, in little light camps made of boards; but we gradually became callous, and returned to our houses again. Most of those who fled from the country in the time of the hard shocks have since returned home. We have, since the commencement in 1811, and still continue to feel, slight shocks occasionally. It is seldom indeed that we are more than a week without feeling one, and sometimes three of four in a day. There were two this winter past much harder than we had felt them for two years before; but since then they appear to be lighter than they have ever been, and we begin to hope that ere long they will entirely cease.
I have now, sir, finished my promised description of the earthquake - imperfect it is true, but just as it occurred to my memory; many of, and most of the truly awful scenes, having occurred three or four years ago. They of course are not related with that precision which would entitle it to the character of a full and accurate picture. But such as it is, it is given with pleasure - in the full confidence that it is given to a friend. And now, sir, wishing you all good, I must bid you adieu.
Your humble servant,
There is one circumstance which I think worthy of remark. This country was formerly subject to very hard thunder; but for more than twelve months before the commencement of the earthquake there was none at all, and but very little since, a great part of which resembles subterraneous thunder. The shocks still continue, but are growing more light, and less frequent. -E.B
(2) The following was written by John Bradbury on December 15, 1811:
On December 15, 1811, John Bradbury, a Scottish naturalist, was headed down the Mississippi River with a party of boatmen. They were tied up for the night just upstream from the Chicksaw Bluffs (the future Memphis) and Bradbury was fast asleep when "a most tremendous noise" panicked the group. "All nature seemed running into chaos," he later wrote, "as wild fowl fled, trees snapped and river banks tumbled into the water." Bradbury recorded twenty-seven shocks.
After the first December rumbling, jolts continued. One Louisville observer recorded 1,874 separate quakes between December and March. During this time the epicenter moved closer to New Madrid, and on February 7 the residents deserted what once had bid fair to become the metropolis of the middle Mississippi River. The houses had fallen, and possibly even the land on which the town stood had sunk by March.
Because so few persons were in the area of greatest damage and most of those who were there were illiterate, only a few firsthand account provide detailed information. Stories and legends grew apace, however, for the earthquake was felt all over North America, and reinforced the evangelical religious notion that the end of the world was at hand. Henry Schoolcraft, who took to poetry to record the quake wrote: "the rivers they boiled like a pot over coals, And mortals fell prostrate, and prayed for their souls."
Actually, the 1811-1812 earthquake was merely a continuation in a series which included rumblings in 1699, 1776, 1779, 1792, 1795, and 1804. These predecessor quakes were quite possibly even stronger; and some of the changes later credited to the New Madrid Quake probably came earlier. In time, the quake was credited with causing the Mississippi River to flow backward, with creating the "Sunk Lands" in the Saint Francis River Valley, in raising Crowley's Ridge, and creating Reelfoot Lake in Tennessee.
If another quake of the magnitude of the New Madrid Quake of 1811 should hit the region, it would be the worst natural disaster in American history. Especially vulnerable are buildings of brick and concrete. Almost all of downtown Memphis would fall. The highways and interstate systems would be shattered and bridges destroyed. Massive gas line ruptures would threaten life and property. If the Mississippi River were already near flood stage, the destruction of levees could result in the flooding of perhaps a quarter of the state (of Arkansas). Overall the loss of life could run into the hundreds of thousands.
Despite its prominence as one of the great recorded natural events in American history, the New Madrid Earthquake had very little impact on the history of the region. Although minor tremors were felt off and on, and some timid folks, especially in the 1890's decided to move elsewhere, the earthquake remained irrelevant to life until Iben Browning, a business consultant with some scientific pretensions, announced that another quake was due on December 3, 1990.
Despite numerous scientific attacks on Browning's methodology, the public became truly alarmed. Local communities took disaster relief seriously and sales of earthquake policies soared. Many residents stockpiled water, flashlight batteries, plastic bags, and toilet paper. Timid folk even left the state (of Arkansas). Days prior to the supposed event, every motel room near New Madrid was taken up by news persons ready to cover the projected disaster.
December 3, 1990, passed with nary a tremor and the quake became the Great Non-Event of 1990. Nevertheless, the publicity did have a positive effect as few area residents could claim to be unaware of eastern Arkansas' natural heritage.
Michael Bruce Dougan, Arkansas Odyssey: The Saga of Arkansas from Prehistoric Times to Present (c) 1994 Rose Publishing Company, Inc., Little Rock, Arkansas.
(3) This following account of the New Madrid Earthquake was recorded by George Heinrich Crist, residing at the time in the north-central Kentucky county of Nelson, near the present location of Louisville. It was submitted by Floyd Creasey - 4th tier great-grandchild to author, now a Texas resident.
16 December 1811
"There was a great shaking of the earth this morning. Tables and chairs turned over and knocked around - all of us knocked out of bed. The roar I thught would leave us deaf if we lived. It was not a storm. when you could hear, all you cold hear was screams from people and animals. It was the worst thing that I have ever wittnesed. It was still dark and you could not see nothng. I thought the shaking and the loud roaring sound would never stop. You could not hold onto nothing neither man or woman was strong enough - the shaking would knock you lose like knocking hicror nuts out of a tree. I don't know how we lived through it. None of us was killed - we was all banged up and some of us knocked out for awile and blood was every where. When it got day break you could see the damage done all around. We still had our home it was some damage. Some people that the home was not built to strong did not. We will have to hunt our animals. Every body is scared to death. we still do not know if anybody was killed. I made my mind to one thing. If this earth quake or what ever it was did not happen in the Territory of Indiana then me and my family is moving to Pigeon Roost as soon as I can get things together.”
23 January 1812
"What are we gonna do? You cannot fight it cause you do not know how. It is not something that you can see. In a storm you can see the sky and it shows dark clouds and you know that you might get strong winds but this you can not see anything but a house that just lays in a pile on the ground - not scattered around and trees that just falls over with the roots still on it. The earth quake or what ever it is come again today. It was as bad or worse than the one in December. We lost our Amandy Jane in this one - a log fell on her. We will bury her upon the hill under a clump of trees where Besys Ma and Pa is buried. A lot of people thinks that the devil has come here. Some thinks that this is the beginning of the world coming to a end.”
8 Febuary 1812
"If we do not get away from here the ground is going to eat us alive. We had another one of them earth quakes yesterdy and today the ground still shakes at times. We are all about to go crazy - from pain and fright. We can not do anything until we can find our animals or get some more. We have not found enough to pull he wagons.”
20 March 1812
"I do not know if our minds have got bad or what. But everybody says it. I swear you can still feel the ground move and shake some. We still have not found enough animals to pull the wagons and you can not find any to buy or trade.”
14 April 1813
"We lived to make it to Pigeon Roost. We did not lose any lives but we had aplenty troubles. As much as I love my place in Kentucy - I never want to go back. From December to April no man - woman or animal if they could talk would dare to believe what we lived through. From what people say it was not that bad here - They felt the ground move and shake but it did not destroy cabins and trees like it did in Kentucky. I guess that things was as bad here but at least they could see the enemy. on 3 September 1812 the Shawnees that William thought was friendly went crazy and them savages killed twenty four people...."
(Transactions of the Literary and Philosophical Society of NY, vol. 1, pp. 281-307)
Samuel L. Mitchill, Representative in Congress
Transcription and notes, Susan E. Hough, U.S. Geological Survey, Pasadena (May, 2000).
[Read before the Society on the 14th of April, and the 12th of May, 1814]
“The beautiful comet which travelled through the northern celestial hemisphere during 1811, had offered itself plainly to view until the approach of the following year. Its elements, as calculated by Nathaniel Bowditch, Esq. and his learned associates, have already been placed before the public eye. The tremendous storm from the northeast, near the end of December, 1811, began to leeward, near Cape Hatteras, and swept the American coast to the banks of Newfoundland, doing great damage to navigation, and exhibiting some curious facts in the history of the atmosphere. The particulars of this furious and memorable tempest have been collected by myself; and are in readiness to be offered to the society at the first convenient time.
My present intention is to read to you the information I have gathered on another occurrence of those portentous days. I mean the phenomena of the earthquakes, which terrified the country about the same period, and which continued a long time afterwards.
On the morning of Monday, the 16th of December, 1811, several shocks of earthquakes were felt at the city of Washington. The first of these happened at three o'clock; and in some houses was considerable enough to shake the doors and windows, and wake persons from their sleep. There were successive tremors. Tassels of curtains were seen to move; and pitchers of washing-stands were heard to rattle upon their basins. The sound was very distinguishable, and was believed by many to pass from southwest to northeast. The alarm was so great in some families, that searches were made from room to room, to discover the robbers who were imagined to have broken into the houses. A second shock, though lighter, was experienced about six o'clock, and a third about eight.
A gentleman standing in his chamber at his desk and writing, in the third story of a brick house, upon the Capitol Hill, suddenly perceived his body to be in motion, vibrating backward and forward, and producing dizziness. Not suspecting the moment that the uncomfortable sensation was caused by an earthquake, he examined his desk to know whether it stood firm. Finding that it did, he dropped his pen; and turning his eyes upward, discerned that the looking-glass, and other things hanging near him, were in a similar motion.
Another person was near a table placed beneath a mirror. Feeling a giddiness come upon him, he seized the table for support. The general agitation of the chamber and house ceased in about a minute; but the looking-glass, which was suspended in the usual manner, continued to swing for some seconds longer. These observations, made by Messrs. Bigelow and Mosely, may serve as specimens of a multitude of phenomena of those kinds.
The atmosphere seemed to forebode some unusual occurrence. One of my most correct and respectable friends, declared in conversation, and stated to me in writing, that he made an observation of the sky about ten o'clock that night. It was quite calm. There was not a breath of wind stirring. The air was perfectly clear and free from clouds. Nevertheless, it was uncommonly dark, and the stars which appeared in every part through the gloom, were lurid and dim, and afforded little light.
In Richmond the signs of an earthquake were witnessed by many persons. At three o'clock on the same morning, (the 16th of December,) there were said to be three successive shocks; another about six; and a third about eight. Several people were impressed with a belief that thieves had entered their dwellings; and in one of the most elevated mansions, the bells were set a ringing in both the upper and lower rooms. The noise and concussion were supposed by some to proceed from east to west.
It was stated at Norfolk that two very distinct shocks were felt in that town and in Portsmouth; to wit, at three and eight o'clock in the morning of the 16th. Some clocks were reported to have stopped; the doors rattled; and articles hanging from the ceilings of shops and houses, swung to and fro, although a perfect calm prevailed.
At Raleigh (N.C.) several slight earthquakes were felt on the morning of the 16th December. The first happened between two and three o'clock, and was distinctly perceived by all who were awake at the time. Two others were reported to have occurred between that time and seven o'clock, but were not plainly observed, except by some members of the legislature, who were in the state-house, and were considerably alarmed at the shaking of the building.
From Georgetown, (S.C.) it was told, that several shocks had been experienced between the hours of three and eight, on the morning of the 16th. The inhabitants were much alarmed. The shocks were so considerable, that the parade-ground of the fort was said to have settled from one to two inches below its former level. A tub of water, standing upon a table in the barracks, was reported to have been overset by the jarring of the building. Another severe shock was felt two days afterwards, at noon.
At Columbia, (S.C.) the inhabitants were alarmed by repeated shocks. The first took place at half after two in the morning of Monday, which was represented as shaking the houses as if rocked by the waves of the sea. It was followed, after the cessation of a minute, by three slighter ones. At eight o'clock two others took place, and at ten, some slight ones. The South Carolina college appeared to rock from its foundation, and a part of its plaster fell; which so alarmed the students, that they left the chambers without their clothes. It seemed as if all the buildings would be leveled. The dogs barked; fowls made a racket; and many persons ran about with lights, not knowing where to go, so great was their terror. During the first agitation, it was observed, that the air felt as if impregnated with a vapour, which lasted for some time.
On Tuesday, at a quarter after twelve, another smart shock was experienced. At Laurens and Newbury, in the interior districts, it was so violent as to crack and start several chimnies.
At Charleston (S.C.) the sensation was of considerable strength. One account stated; that on the morning of the 16th, at a few minutes before three o'clock, a severe shock of an earthquake was felt. Its duration conjectured to have been between two and three minutes. For an hour previous, though the air was perfectly calm, and several stars visible, there was, at intervals of about five minutes, a rumbling noise like that of distant thunder; which increased in violence of sound just before the shock was felt. The vibrations of St. Philip's steeple caused the clock bell to ring about ten seconds. Two other shocks were felt afterwards, one a little before eight, and the other about a quarter of an hour after. Both these were slighter and shorter than the first. Many of the family clocks were stopped by the concussions. In many wells the water was considerably agitated. From another source it was related that Charleston was shaken by an earthquake severely, at the time before specified. This was preceded by a noise resembling the blowing of a smith's bellows. The agitation of the earth was such that the bells in the church steeples rang to a degree indicative of an alarm for fire. The houses were so much moved that many persons were induced to rise from their beds. The clocks generally stopped. Another slight shock was experienced about fifteen minutes after; and yet another at eight o'clock. This last one produced a considerable rattling among glass, china, and other furniture. A looking-glass hanging against a west wall was observed to vibrate two or three inches from north to south.
The ingenious writer of the meteorological observations for Charleston during December, 1811, has noticed these occurrences in a manner too interesting to be omitted. According to his remarks, there were seven shocks during the month, having a vibratory motion from east to west. In many persons the motion produced nausea. All the shocks, except the last, were preceded by noises resembling the rattling of a carriage over a pavement. There had been less thunder during the preceding season than usual. The days of thunder amount annually to about sixty; but this year there were no more than thirty-eight. The beautiful comet was visible in the northwest during the whole month.
The inhabitants of Savannah were sensible of four earthquakes. The first was on the morning of the 16th December, between two and three o'clock. It was preceded by a flash of light, and a rattling noise, resembling that of a carriage passing over a paved road. It lasted about a minute. A second soon succeeded, but its duration was shorter. A third happened about eight o'clock; and a fourth about noon on the 17th. Persons who experienced the hardest shock, were made to totter, as if on shipboard. Its course was believed to be from southwest to northeast.
It was observed, by Dr. Macbride of Pineville, (S.C.) that the earthquake terrified the inhabitants exceedingly. It was accompanied by several appearances that countenances the theory of this phenomenon, which brings in the agency of the electric fluid. 1. The infrequency or absence of thunder storms; that is, they were much less frequent this year than usual, especially in the autumn. 2. Immediately before the earthquake, a red appearance of the clouds, which had much darkened the water for twenty-four hours immediately before the shock; and 3. The loudness of the thunder, and the number of the peals within twenty-four hours after the first shock, and but a few hours before the last, which was felt before he wrote. Such thunder was very unusual at that season.
At Natchez, the occurrences, as related by a careful observer, were as follow: Four shocks were felt on the morning of the 16th. The principal one was at tem minutes after two, A.M. There was no noise, except in a few situations. Several clocks were stopped. Articles, in some instances, fell from shelves. Plastered walls were sometimes cracked. The Mississippi was agitated as if the banks were falling in. The trees in the forests waved their tops. Many houses were shaken considerably. And things suspended on nails or pins swung backwards and forwards.
Information was forwarded from Tennessee, that the earth quaked so violently, as to throw down chimnies, in some places. Eighteen or twenty acres of land, adjacent to Piney river, suddenly fell down, and sunk so low, that the tops of the trees were on a level with the surrounding earth. Four other shocks were experienced on the 17th, and one or more continued daily until the 30th.
At Knoxville, the quaking of the earth on the 16th was represented to have lasted more than three minutes. The rattling of the windows and furniture of the houses were such as to awaken almost every family. This was about two in the morning. It was followed, in half an hour, by another, which continued half a minute. Between sunrise and breakfast, three others were felt, of only a few seconds in duration. At the end of the first and longest shock, there were, in a direction due north, two flashes of light, at the interval of about a minute, very much like distant lightning.
At Columbia, in Tennessee, between two and three o'clock on the morning of the 16th December, the inhabitants were suddenly alarmed by a violent agitation in the earth. It was accompanied by a peculiar sound, proceeding from southwest to northeast. Immediately after the shock had ceased, a very large volume of something like smoke was discovered to rise in the quarter whence the sound appeared to come; and pursuing nearly the same course, finally settled in the north, exhibiting the appearance of a black cloud. The shock was computed to have continued from ten to fifteen minutes.
At Louisville, (Ken.) near the falls of the Ohio, on Monday morning about three o'clock, a violent shock of an earthquake was felt. It was judged to have continued about three minutes. This was followed by three or four others of less violence. A number of houses suffered considerable damage; the chimnies having been so much cracked as to require repairs by the mason. On the evening previous to the shock, there was a gentle rain, such as we have in April; and the night was rather close and dark; but at the termination of the first shock, it was light enough to enable a pin to be seen.
By information from Jeffersonville, in the Indiana Territory, on the opposite side of the Ohio, it was understood that the shocks were reiterated, and the writer of the account I am now copying, declares that the table was in motion from the earthquake, while he was employing his pen to describe the phenomena. The day preceding was extremely dark and gloomy there, and warmth and smokiness distinguished the weather for some time after.
At Vincennes, the earthquake occurred about two o'clock on the morning of the 16th December. Other shocks of less violence followed it for several days. It was so severe that the inhabitants were greatly concerned for the safety of their houses.
At the Red Banks, one hundred and fifty miles below Louisville, it was stated in a letter to my friend, the hon. Anthony New, dated January 4, 1812, "that there had been from twenty to thirty shocks of earthquakes at that place. They begun on the morning of December 16, at about half after two o'clock. The first one, and another at sunrise the same morning, were most violent indeed. We had to flee from our houses. Several chimnies were thrown down, and many others so wrecked and cracked as to be very dangerous. The noise which accompanied the several shocks is said to have come from the west."
The town of St. Louis, in Louisiana, experienced a full proportion of the commotion. Mr. Riddick, being at St. Louis, near the Mississippi, observed to me, that the shocks were preceded by a remarkable calm. The atmosphere was of a dingy and lurid aspect, and gleams and flashes of light were frequently visible around the horizon, in different directions, generally ascending from the earth. Sometimes sounds were heard, like wind rustling through the trees, but not resembling thunder. The first earthquake was felt about a quarter of an hour after two in the morning of the 16th. It roused persons from their sleep, by the clatter of windows, doors, and furniture, in tremulous motion. There was a rumbling distant noise, resembling a number of carriages passing over a pavement. In a few seconds the motions and noises had considerably increased. The sky was obscured by a thick and hazy fog, without a breath of wind. The weather was moderate, with the mercury about eight degrees above the freezing point. At forty-seven minutes after two, a second shock was felt. At thirty-four minutes after three, a third came; which was as tremulous as the first, but not followed by so much noise. A little after daylight, there was a fourth; at eight, a fifth; and at half past eleven, a sixth; several persons felt, or imagined, others. They were of different lengths, from two minutes to a few seconds. No lives were lost; some chimnies were thrown down; and a few stone houses split. The morning was observed to be very hazy, and unusually warm for the season. The houses and fences seemed to be covered with a white frost; but on examination, this appearance was illusive. A vapour hovered over every thing, and shrouded the morning in awful gloom.
At Lebanon, in Ohio, the alarm was so great, that many persons forsook their houses. The vibration of the shocks seemed to be from east to west.
At Circleville on Monday morning between one and two o'clock, many of the inhabitants were considerably alarmed by a sudden and violent trembling of their houses, which was supposed to have proceeded from an earthquake. Many persons, affrighted, leaped out of bed. Another was felt at eight; but there was no explosion.
A letter from Kentucky to my friend, the hon. John Talliaferro, informed him that on the night between the 15th and 16th December, 1811, the shock of an earthquake was sensibly and alarmingly felt. The shakings continued, in greater or less degrees, through night and day, up to the 30th of the same month, when a more severe shock than any preceding one occurred. It overturned almost every brick or stone chimney in Henderson county, or the region thereof, situated on Green river, down to its confluence with the Ohio.
The editor of the Western Spy, a newspaper printed at Cincinnati, in Ohio, after writing an intelligent account of the phenomena of the earthquake, gave a valuable summary from the gazettes of the occurrences in other places along the western waters.
By the intelligence from Detroit, from Judge James Witherall, it appears that Michigan was agitated by the same subterranean power. A small shock was felt at Detroit on the 17th December. The atmosphere was serene, but cold. Thirty miles northwest of that village is a lake about nine miles in circumference, of an oval form, and which is supposed to have communication under ground with Lake Sinclair. In the centre of this lake there is an island of perhaps three miles in circumference, inhabited only by Indians. They relate, that on the said 17th December the waters of the lake appeared to tremble, and boil like a great pot over a hot fire; and immediately a vast number of large tortoises rose to the surface, and swam rapidly to the shore, where they were taken for food. The testimony of Colonel Samuel Hammong, in a letter of the 6th February, 1812, which I received from him, was to the following effect. He confined himself strictly to what he know from personal observation. The first shock he witnessed was on the 15/16th of December last. He was then at Herculaneum in Louisiana. 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 chimnies 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 chimnies 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 severer 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 court-house at Carthage is a large brick edifice, and was cracked to its foundation, and considerably damaged. Several chimnies 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,) af fine and fresh spring was observe to run very muddy for several hours. On examining it, after the feculence 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 met with.
But considerable as these operations were, they were surpassed by others which took place along the river Mississippi; indeed, the strata underlying the bed of this stream appear to have been the principal seat of the commotion or, at least, the place where it was most considerable. The phenomena were described in the most fearful and alarming strains by several writers. Much exaggeration was interwoven with some of the narratives. Some, indeed, were tinctured with fable and burlesque. Among the various recitals it became exceedingly difficult to find out the true, or even the most probable, account. Five or six witnesses, who seem to have been wholly unknown to each other, agree in so many particulars, that their united evidence may be considered to approach as near to the truth as we can expect to arrive.
First, the writer of a letter from the Chickasaw Bluffs, dated December 21st, to his correspondent in Cincinnati, stated many particulars from his personal observation. The first shock happened at thirty minutes after two, on the morning of the 16th, and was followed by many more within a few days. The boat was acted upon by the water in such a manner as to induce a belief that she had grounded; but upon sounding, he could find no bottom. The current, at the place where he was at the time of the occurrence, (eighty-seven miles below the mouth of the Ohio,) acquired three times its former velocity, and the river rose six feet upon its former level; the trunks of trees, bedded in the bottom, suddenly rose in great numbers to the surface; the banks tumbled down at an alarming rate; and the land was rent by cracks and fissures.
Secondly, a writer from New Madrid, in a communication to a friend in Lexington, dated 16th December, describes a tremendous noise as rousing the family from their sleep, rocking the house, throwing down the chimney, and terrifying them so, that they passed the remainder of the morning, from two o'clock, when the shock was felt, in the open air. During the time of the shock, the heavens were very clear and serene; there being not a breath of air stirring; but in five minutes it became very dark; and a vapour which seemed to impregnate the atmosphere, had a disagreeable smell, and produced a difficulty of breathing. This darkness continued until nearly the break of day. During its continuance there were six more shocks. About half after six it cleared up. However, the danger was increased by another shock, which racked the houses violently, and threw down the chimneys. The darkness returned, and it was accompanied by loud noises, and a bounding motion up and down. Many persons were so alarmed that they formed encampments in the fields. The shocks were repeated from time to time, until the 28th, and then amounted to sixty-seven.
Accounts from Little Prairie stated that ponds had been converted to upland, and dry land to lakes; that the banks of the river had sunk and fallen in to great extent; that cracks had been formed in the earth; that water had gushed out; and that there was a strange and chaotic mixture of the elements. In some places, sand, mud, water, and stone-coal were reported to have been thrown up thirty yards high.
Thirdly; a more full and circumstantial history of those eruptions and commotions was drawn up by Mr. William Leigh Pierce, who, at the time of their occurrence, was passing down the Mississippi in a boat.
After having described the occurrences of the 16th, 17th, and 18th, up to the 19th, he wrote from the Big Prairie, under date of December 25th, to his acquaintance in New-York, a very circumstantial account, which was published in the journals of the time. His narrative abounds with facts showing the irresistible and ruinous effects of the commotion, which he thinks might have been considered as protracted to the surprising length of one hundred and seventy-eight hours.
Fourthly; to these I subjoin another respectable communication, from Mr. Joseph Ficklin of Russellville, (Ken.) who thus describes the earthquakes, in a letter dated February 5, 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. Indians who were two hundred and fifty miles beyond the Mississippi, and about five hundred miles west of this place, relate sights of horror, in the tumbling down of rocks, the fall of trees, and the lights of fire; which prove to my satisfaction that the cause of this alarm lies in the mountains or hills which are between the head of the Arkansas river, and the waters of the Missouri, not more than six hundred miles from this place, a little south of west. The shocks are much more severe one hundred and fifty miles west of this than they are here. Fortunately, there are no brick or stone houses near the seat of danger to destroy the people. The Indians cannot have suffered much in their tends and bark houses. But the United States will suffer in the sales of their public lands west of the Mississippi for an age. At least the present generation must be buried before the spirit of wandering, in that direction, revives; and may it not be an advantage that some power exists to fix a boundary for our fellow citizens; for my own part, I am pleased in viewing the benefits which my country will derive from this great shock. We had one last night."
Fifthly: there is further information contained in a letter from a gentlemen at the mouth of the Cumberland river to his friend in Woodford county, Kentucky, dated February 10, 1812: it was published in the newspapers of that state, and corroborates substantially the recitals of the other witnesses.
Sixthly; Daniel Bedinger, Esq. who was passing down the Mississippi, in a boat, at the very time, was a witness of the occurrences, near him; and he described them in his journal, dated at New-Orleans, January 15, 1812: He bears witness of the noises that attended the shocks; the froth that formed on the surface of the river from the bursting of air bubbles; and of the elevation of innumerable logs and trees from the bottom of the Mississippi. Cracks and rents in the earth and the falling of banks were frequent and terrible.
The earthquakes were not felt quite so strongly at or below New Orleans.
In all these shakings of the ground it is particularly to be observed, that there were but slight indications of them at Baltimore, or in any place to the eastward or northward. The evidence from Philadelphia and New York was of a dubious character; though some persons at the latter place, and at Newark, assured me they felt several small concussions. It seemed, however, as if the Maryland side of the Potomac and the ridge of the Alleghany, might almost be deemed the limits of their extension; the more considerable proofs of their power having been to the westward of the latter, and to the southward of the former, of those boundaries.
On the 23d of January, the earthquakes were renewed, to greater extent than before, and in some places with increased violence.
One was felt at Washington, about nine A. M., and the witnesses of the concussion were very numerous. The phenomena very much resembled that of the 16th of December. A few recitals will answer all the purposes of information.
At Nottingham, in Maryland, the shock was alleged to have happened twenty minutes after nine, and to have lasted a minute. The writer of the account was sitting in a room with two other persons, occupied in reading, when it was asked by one of them what made the chamber shake so? This called the attention of them all to the movement, which they described as having the same effects as the rolling of a vessel on an agitated sea.
The inhabitants of Richmond (Va.) felt it severely at half after none. Like the former, it was more sensible on Shockoe and Richmond hills, than in the lower parts of the city. In some instances, books were nearly thrown from their shelves, and many persons at breakfast perceptibly left the tables.
At Cashockton, in the state of Ohio, on the morning of the 23d of January, at Georgetown, Louisville, Chilicothe, Paris, Washington, and Frankfort, the shocks excited a great share of attention.
At Charleston, (S.C.) on the same morning, to wit, of the 23d of January, at fifteen minutes after nine o'clock, the vibratory shock on an earthquake was felt more severely than on the former occasions. This was said to have been more extensive than the preceding ones, inasmuch as the newspapers stated that it was felt at New York.
Another was experienced in Kentucky, on the 30th of January. It was described in a letter from Louisville to Stephen Ormsby, Esq. as having proceeded from the west, about the same time of night with that of December 29. It was not near so violent. The relater was waked from sleep by a noise like that of a carriage, which was followed by a shake. About six minutes before the shock, the whole heavens appeared to be illuminated, and darkness immediately afterwards ensued. No damage was done.
These commotions were renewed in February, as appears by the intelligence from Michigan, written to me by Judge Witherall:
"The earthquakes continue to visit us. On the 3d instant, fourteen minutes past 4 P. M., a small shock was felt; the mercury low, but not quite in the ball; it had risen very considerably a few hours previous to the shock. On the 7th, at 4 P. M., the weather continuing moderate, the shock was strong, nearly equaling the one I previously mentioned to you, and continued about ninety seconds; on the same evening, at half past seven, another small shock; at fifty-five minutes past nine, the same evening, another small shock; at eleven, another, and at 2 A. M. of the 8th, one which seemed to produce a different motion; that is, like pounding up and down, instead of oscillating.
On the 7th of February several shocks occurred at Pittsburgh. These were most extensively felt, and by no means confined to that region. They began about four in the morning. Many persons were so much alarmed as to rise from their beds and run out of doors, screaming with affright. Flashes of light similar to those seen on the 16th of December were perceived toward the southwest. The last concussions were greater than any that had been experienced before. There was another shake between ten and eleven that night.
Being on horseback in Livingston County, Kentucky, Mr. Riddick, on the morning of the 8th of February, was sensible of the earthquake. His horse refused to proceed, and bracing himself on his legs, stood still. The atmosphere was remarkably luminous for some time prior to the shaking of the ground. There was no moonshine; and yet objects could be seen to a considerable distance. On this occasion the brightness was general and did not proceed from any point or spot in the heavens. It was broad and expanded, reaching from the zenith, on every side, toward the horizon. It exhibited no flashes, nor coruscations; but, as long as it lasted, was a diffused illumination of the atmosphere on all sides; but no noise was distinguished until the shaking of the earth began; then the usual rumbling sound was heard.
William W. Worsely, Esq. of Lexington, (Ken.) on the 29th of February, reported the particulars at large, and published them in the newspapers.
Thomas Crawford, jun. of Louisville, (Ken.) published an account of the terrestrial commotions in very emphatical terms at Russelville, (Kentucky.)
Mr. Mathias M. Speed wrote to his friend, Thomas Speed, Esq. of Bardstown, an account of the earthquake of February 7, and the following days, in a communication dated March 3, 1812. He states the appearance of frequent lights during the commotions, and that from one of the low islands in the Mississippi, where he was, sand, coal, and warm water were ejected from holes in the earth. Some of the coal was collected by Mr. Pierce, and transmitted to me. About the 1st of May, 1812, I made a few experiments upon it at the city of Washington. I found it to be very inflammable; it consumed with a bright and vivid blaze. A copious smoke was emitted from it, whose smell was not at all sulphureous, but bituminous in a high degree. Taken out of the fire in its ignited and burning state it did not immediately become extinct; but continued to burn until it was consumed. While blowed upon, instead of being deadened, it became brighter by the blast. The ashes formed during the combustion were of a whitish colour; and when put into water, imparted to it the quality of turning to a green the blue corolla of a phlox whose juice was subjected to its action. By this, and other tests, the alkalinity of the residue was fully ascertained.
The Hon. Israel Pickens of Buncombe county, (N. C.) received a letter from the Rev. John Carrigan, dated 28th of February, and containing the following information:
"During my travels lately to and from the state of Georgia, I made it a part of my business to obtain the most accurate accounts of the present shaking of the earth, from all parts. I have found that in all parts of the continent the motion of the earth has been the same, and its partiality remarked in the same neighborhoods. In this country, the first rocking (as it is generally called) was perceived on the 23d of December, a little before daylight. Since that time it has been observed almost every week through South Carolina and parts of Georgia. Several persons in those states have told me that they had felt it almost every day since. No damages have arisen, more than a few bricks shaken off some chimneys. There is no truth in the report in circulation respecting the fall of the Painted Rock, and other extraordinaries in Buncombe county. I gave my friend, Colonel Freeman, (in Georgia,) a call, who informed me that he had particularly noticed some tall poplars in his lane during the time of the second shock, rocking with equable motion from northeast to southwest, which I have found to be general. On the 7th and 16th instant the shaking has been general here. I do not consider it an earthquake proceeding form the usual causes."
"Captain Robert Alexander, of Lincoln, (N. C.) gave me a most alarming account of a phenomenon which was generally seen on the night of the 20th instant. Three large extraordinary fires, in the air, one appeared in an easterly direction, one in the north, and one in the south. Their continuance was several hours; their size as large as a house on fire; the motion of the blaze quite visible, but no sparks appeared."
"Another phenomenon appeared on the 22d of November, of which I was a spectator. About 2 o'clock P. M. a meteor took fire in the air, attended with a fulminating noise, and bore a southeast direction; and however unaccountable, it is a fact, that about the same instant, a whitish substance, resembling a duck in size and shape, detached itself, and descended with a swift motion, from the cloud of smoke that was formed, and was beheld at my house, and fifteen miles due north of it, and twenty-three miles west of it, at the same instant."
"Whether these things are ominous or not, one thing is certain, this is a time of extraordinaries."
To these curious notices, I add the communication from New-Orleans, of William Shaler, Esq. dated March 23d, 1812.
"Knowing the interest you take in all natural events, I do myself the pleasure to communicate to you the following simple account of the late earthquake, as I received it from the patron of a Kentucky boat lately arrived here. On the 7th of last February, at 3 A. M., being moored to the bank of the Mississippi, about thirteen miles above New Madrid, he was awakened by a tremendous roaring noise, felt his vessel violently shaken, and observed the trees over the bank falling in every direction, and agitated like reeds on a windy day, and many sparks of fire emitted from the earth. He immediately cut his cable and put off into the middle of the river, where he soon found the current changed, and the boat hurried up, for about the space of a minute, with the velocity of the swiftest horse; he was obliged to hold his hand to his head to keep his hat on. On the current's running its natural course, which it did gradually, he continued to proceed down the river, and at about daylight he came to a most terrific fall, which, he thinks, was at least six feet perpendicular, extending across the river, and about half a mile wide. The whirls and ripplings of this rapid were such that the vessel was altogether unmanageable, and destruction seemed inevitable; some of the former he thinks were, at least, thirty feet deep, and seemed to be formed by the water's being violently sucked into some chasm in the river's bottom. He and his men were constantly employed in pumping and bailing, by which, and the aid of Providence, he says, he got safe through! As soon as he was able to look round, he observed whole forests on each bank fall prostrate, to use his own comparison, like soldiers grounding their arms at the word of command. On his arrival at New-Madrid he found that place a complete wreck, sunk about twelve feet below its level, and entirely deserted; its inhabitants, with those of the adjacent country, who had fled there for refuge, were encamped in its neighbourhood: he represents their cries as truly distressing. A large barge loaded with five hundred barrels of flour, and other articles, was split from end to end, and turned upside down at the bank. Of nearly thirty loaded boats only this and one more escaped destruction; the water ran twelve feet perpendicular, and threw many of them a great many rods on shore; several lives were lost among the boatmen. Another fall was formed about eight miles below the town, similar to the one above, the roaring of which he could distinctly hear at New-Madrid. He waited five days for the fall to wear away; during that time the earth was constantly trembling, at intervals of about five minutes. He observed many fissures in the earth below the town, five or six feet wide, extending in length out of sight, and one side several feet lower than the other. On the fifth day he passed the lower fall which had worn away to a practicable rapid. He felt a succession of shocks of earthquake until he came down to Flam Island. He spoke of many physical changes in the river, particularly a great multiplication of sawyers, but he does not describe them with sufficient accuracy to enable me to give you an account of them."
"I have also seen several persons who passed New-Madrid on the 20th of February; they report that the earth still continues to tremble there, at that time. The falls had worn away to smooth rapids."
"With very great respect and esteem I am, Dear Sir, your very humble servant,"
"The Hon. Samuel L. Mitchill
The information contained in a description, forward to William Duane, Esq. by one of his correspondents at St. Genevieve, in Louisiana, shows the state of opinion in the mind of the sensible writer, there, about the 1st of April, 1812, on the subjects of the earthquakes at New Madrid, and the surrounding region. This may be found on the pages of his Aurora.
Dr. Robertson, the enterprising traveler to the sources of the Arkansas River, by order of the government, in 1806, witnessed the phenomenona of these earthquakes, very particularly at St. Genevieve, where he resided during their occurrence. He travelled with me from Washington to Fredericktown, on the 3d of July, 1812, and parted with me at that place on the morning of the 4th, he journeying to the westward by the way of Hagerstown, and I proceeding southwestwardly to Harper's Ferry, and its vicinity. This gentleman, among other matters, declared to me, that the had kept a record or memorandum of the shocks of these earthquakes, until they exceeded five hundred , and then ceased to note them any more, because he became weary of the task.
The commotions, however, did not end here. They were renewed from time to time. My correspondent, Peter H. Cole, wrote me, in a letter dated at Clarksville, in Montgomery county, Tennessee, under date of December 15, 1812, as follows: "The earthquakes continue to visit us. We had a tolerably severe one on the morning of the 14th instant. The 16th instant will make one year since they commenced. They have destroyed a number of chimneys in this state, and terrified many of the inhabitants."
So, on the 24th of November, 1812, a shock was again felt in the morning, near Russellville, in Kentucky.
The same gentleman afterwards, in a communication from the same place, of January 26, 1813, furnished additional facts, "In the month of September," he stated, "I visited a spring of about the distance of fourteen miles from my residence. It was situated on the bank of a creek that issued forth strong sulphureous water. The smell was evident to a considerable distance. It received its sulphureous impregnation from a very heavy earthquake that occurred in January. Before that event it was a limestone water. On that occasion a new limestone spring broke out about twenty feet above the original spring; and to this day, the respective fountains pour forth their calcarious and sulphureous waters, in distinct currents. Some springs ceased to run for some time; and others ran muddy several hours after the earth had been convulsed. The earthquakes appeared to affect very sensibly both the body and mind of human beings. In some instances, where individuals had been deprived of their usual sleep, through fear of being engulfed in the earth, their stomachs were troubled with nausea, and sometimes even vomiting. Others complained of debility, tremor, and pain in the knees and legs. The shocks seemed to produce effects resembling those of electricity. We have had a very wet spring, summer, and autumn, with a loaded atmosphere; and I have no doubt much impregnated with sulphureous particles. Sickness was much more prevalent last winter, spring, summer, and fall, than ever was known in this country; and, no doubt, the state of the atmosphere was the principal cause."
Nor had those subterranean tumults ceased at the close of 1813. For two shocks were felt at Russellville, on the 5th of December, one at ten o'clock in the morning, and the other four in the afternoon.
They were repeated in the Illinois Territory about the same time. Stanley Griswold, Esq. gave an account of them in a short narrative of December 18th. This was printed in the gazettes of the time. They were particularly severe at the salt works belonging to the United States; and but moderate at a short distance off. In the 16th volume of the Medical Repository, P. 304, there are other sensible observations of the same ingenious gentleman.
And on the 29th of December Mr. Hempstead, the delegate in congress from the Missouri Territory, moved for the consideration of a proposition relative to an additional judge in that quarter. He said he has been instructed by the legislature of the territory to bring the measure forward. The settlement of Arkansas, for which the new judge was asked, was situated two hundred miles from New-Madrid, where the courts were then held, and since the late earthquakes, the road had become so nearly impassable, that a circuit of three hundred miles was required to go from one place to the other. So great a distance from the seat of justice, obviously amounted, in many cases, to a denial of the benefits of the judiciary, and called loudly upon the legislature for a remedy.
After this minute, reiterated, and, perhaps, tedious detail of facts, it will be rational to attempt some deductions. When I engaged the task of collecting the evidence on these curious and interesting phenomena, I was in expectation that physical occurrences so immediately before our eyes and under our feet, would have qualified me to form something like a tolerable theory of earthquakes. I must own, however, that after all the information I have collected, I have not been enabled to offer a solution, by any means satisfactory to myself. But, although materials may yet be wanting for a perfect theory, it is a matter of some consolation to have assembled into one body, the phenomena of the most memorable earthquakes that ever agitated these parts of North America, and to have made a record of them for my sagacious and fortunate successors.
1. The trembling of the earth was felt from the Atlantic Ocean to the regions far beyond the Mississippi. The accounts given by the Indians uniformly stated that the shocks had been very frequent and violent, to a great distance up the Arkansas. They appear to have been felt very little to the north of the Potomac, and east of the Alleghany.
2. Though the commotions were of great extent, it was not possible to assign a priority to any place. Though the earthquakes were not equally violent or extensive, yet in those of the widest diffusion or circuit, there was no method of tracing a succession; on the contrary, the shocks in the most distant situations were synchronous, or nearly so.
3. Air was produced below, and extricated into the atmosphere.
4. This, when it passed through water, produced bubbles and froth, and after their extrication, formed visible vapour, obscuring the atmosphere.
5. Hot water was ejected with considerable force.
6. Coal or carbonated wood was thrown up in a similar manner, and about the same time.
7. Light, in some cases, was extricated, and from the circumstances of its appearance, may be considered, not as an accidental coincidence of the earthquake, but as a natural and necessary accompaniment. But, in most places, there was no luminous appearance.
8. Sounds were sometimes heard, but by no means uniformly or steadily. In very many cases there was no noise at all.
9. The gas (3. and 4.) the hot water (5.) and the coal (6.) lead conclusively to the existence of subterranean fire; and the light (7.) and sound (8.) induce the same belief.
10. But, after all, it is not very evident what kindles the flame beneath; by what means it is supported by air, and kept from extinction by water; how deep it lies; how it convulses the superincumbent strata, and communicates its tremors instantaneously, for several hundred miles. Nor am I able to explain to my satisfaction, why a certain part of the bed of the Mississippi was its focus; nor why it happened during the winter season.
I console myself, however, that the history which I have written will give valuable information to the curious on these subjects, and assist some more happy inquirer into nature, to deduce a full and adequate theory of earthquakes.
Let me, nevertheless, before I lay down my pen, request the reader to consider this paper as a sequel to the history of the earthquakes in New-England, as has it been written by the learned and ingenious Samuel Williams, LL. D. and published in the transactions of the American Academy of Arts and Sciences at Boston.
Permit me also to observe, that contemporaneous earthquakes have agitated other regions of the globe. Terrible commotions were experienced among the Azores in 1808 and 1811; and in Venezuela and St. Vincents in 1812. I have collected the facts into distinct histories, which I intend at convenient times to offer to this society.
The favourers of the several hypotheses invented to explain the awful phenomena of earthquakes, may all find arguments to support them, in the preceding recitals. The mechanical reasoner will find the great strat of the earth falling in some places, rising in others, and agitated everywhere. The chemical expositor will discover evidence enough of subterranean fire in the coal, hot water, vapour, and air bubbles which were ejected and extricated. The electrical philosopher will deduce from the lights, the noises, and the velocity of their motions, conclusions favourable to the origin of earthquakes from electron, that subtle and universal agent. Even the believer of the conversion of metallic potassium, by rapid inflammation, into common potash in the deep recesses of the earth, will find in the salt-petrous sandstone of the western states, a better argument than any I am acquainted with, to countenance the alkaline system of earthquakes. And yet, these various expositions, plausible, in some respects, as each of them is, are deficient in that general character and universal application which ought to pervade scientific researches.”
The following is from the US government web site earthquakes.usgs.gov
1811, December 16, 08:15 UTC Northeast Arkansas - the first main shock - 2:15 am local time - Magnitude ~7.7
This powerful earthquake was felt widely over the entire eastern United States. People were awakened by the shaking in New York City, Washington, D.C., and Charleston, South Carolina. Perceptible ground shaking was in the range of one to three minutes depending upon the observers location. The ground motions were described as most alarming and frightening in places like Nashville, Tennessee, and Louisville, Kentucky. Reports also describe houses and other structures being severely shaken with many chimneys knocked down. In the epicentral area the ground surface was described as in great convulsion with sand and water ejected tens of feet into the air (liquefaction).
1811, December 16, 13:15 UTC Northeast Arkansas - the "Dawn" Aftershock - 7:15 am local time - Magnitude ~7.0
A large event felt on the East Coast that is sometimes regarded as the fourth principal earthquake of the 1811-1812 sequence. The event is described as "severe" at New Bourbon, Missouri, and was described by boatman John Bradbury, who was moored to a small island south of New Madrid, as "terrible, but not equal to the first". Hough believes that this large aftershock occurred around dawn in the New Madrid region near the surface projection of the Reelfoot fault.
The second principal shock of the 1811-1812 sequence. It is difficult to assign intensities to the principal shocks that occurred after 1811 because many of the published accounts describe the cumulative effects of all the earthquakes and because the Ohio River was iced over, so there was little river traffic and fewer human observers. Using the December 16 earthquake as a standard, however, there is a general consensus that this earthquake was the smallest of the three principals. The meizoseismal area was characterized by general ground warping, ejections, fissuring, severe landslides, and caving of stream banks.
The third principal earthquake of the 1811-1812 series. Several destructive shocks occurred on February 7, the last of which equaled or surpassed the magnitude of any previous event. The town of New Madrid was destroyed. At St. Louis, many houses were damaged severely and their chimneys were thrown down. The meizoseismal area was characterized by general ground warping, ejections, fissuring, severe landslides, and caving of stream banks.
The following map is from the Central United States Earthquake Consortium, a partnership of Alabama, Arkansas, Illinois, Indiana, Kentucky, Mississippi, Missouri, and Tennessee that was formed to plan and coordinate activities related to earthquake research and planning.