New Madrid Earthquakes
This is a compilation from various sources, all referenced at the bottom of the page.
The new Madrid Earthquake caused wide spread damage, extending north to Saint Louis, eastward though Kentucky to present day West Virginia and south and westward into Arkansas. The tremors were felt as far east as Philadeplphis, where it is reported that church bells ran. For days before the first quake, animals fled the areas that would be effected. Passenger pigeons, in great flocks flew southward, deer and other animals attempted to swim the Ohio River. there would be a total of five earthquakes of 8.0 magnitude or higher from December 16, 1811 through February 7, 1812.
Right picture: Trees with double sets of roots. Elevated trees left by scooping out of sand by overflowing Mississippi waters south end of Reelfoot Lake. The surface is now about at its original level and the original tree trunk can be seen continuing down to the level of the ground. later the tree was buried by sand to a depth of 5 fett and new roots formed. Still later the sand was removed. New Madrid earthquake. Lake County, Tennessee. 1904.
*"The area of strong shaking associated with these shocks is two to three times larger than that of the 1964 Alaska earthquake and 10 times larger than that of the 1906 San Francisco earthquake."
*"The first earthquake caused only slight damage to man-made structures, mainly because of the sparse population in the epicentral area. The extent of the area that experienced damaging earth motion is estimated to be 600,000 square kilometers. However, shaking strong enough to alarm the general population occurred over an area of 2.5 million square kilometers."
*At the onset of the earthquake the ground rose
and fell - bending the trees until their branches intertwined and
opening deep cracks in the ground. Landslides swept down the
steeper bluffs and hillslides; large areas of land were uplifted;
and still larger areas sank and were covered with water that
emerged through fissures or craterlets. Huge waves on the
Mississippi River overwhelmed many boats and washed others high
on the shore. High banks caved and collapsed into the river; sand
bars and points of islands gave way; whole islands disappeared.
Surface rupturing did not occur, however. The region most
seriously affected was characterized by raised or sunken lands,
fissures, sinks, sand blows, and large landslides that covered an
area of 78,000 - 129,000 square kilometers, extending from Cairo,
Illinois, to Memphis, Tennessee, and from Crowleys Ridge to
Chickasaw Bluffs, Tennessee.
Although the motion during the first shock was violent at New Madrid, Missouri, it was not as heavy and destructive as that caused by two aftershocks about 6 hours later. Only one life was lost in falling buildings at New Madrid, but chimneys were toppled and log cabins were thrown down as far distant as Cincinnati, Ohio; St. Louis, Missouri; and in many places in Kentucky, Missouri, and Tennessee.
*A notable area of subsidence is Reelfoot Lake in Tennessee, just east of Tiptonville dome. Subsidence there ranged from 1.5 to 6 meters, although larger amounts were reported. It may be that the lake was enlarged by compaction, upwarping, and subsidence occurring simultaneously during the New Madrid earthquakes.
Other areas subsided by as much as 5 meters, although 1.5 to 2.5 meters was more common. Lake St. Francis, in eastern Arkansas, which was formed by subsidence, is 64 kilometers long by 1 kilometer wide. Coal and sand were ejected from fissures in the swamp land adjacent to the St. Francis River, and the water level is reported to have risen there by 8 to 9 meters.
Large waves were generated on the Mississippi River by fissures opening and closing below the surface. Local uplifts of the ground and water waves moving upstream gave the illusion that the river was flowing upstream. Ponds of water also were agitated noticeably."
*The third principal shock of the 1811-1812 sequence was January 23, 1812-The first earthquake of this series on December 16, 1811, was located in northeast Arkansas. 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. Using the December 16 earthquake as a standard, however, a comparison between it and the shock on January 23 indicates that the intensities were about equal at similar locations. The meizoseismal area was characterized by general ground warping, ejections, fissuring, severe landslides, and caving of stream banks.
*The fourth and largest earthquake of the 1811-1812 series of quakes: 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 modern city of Memphis, Tennessee, is built on a high bluff overlooking the Mississippi River. During the New Madrid earthquakes of 1811-12, many landslides occurred along the river. The most devastating effects of the shocks, however, were on the Mississippi itself, where river traffic and commerce were disrupted and boatmen were killed.
The central Mississippi Valley is the most
earthquake-prone region of the United States east of the Rocky
Mountains. Crosses show the locations of the many earthquakes
recorded in the New Madrid seismic zone since 1974.
The great earthquakes of 1811-12 were not freak events. In recent decades, earth scientists have collected evidence that strong earthquakes in the central Mississippi Valley have occurred repeatedly in the geologic past. Small earthquakes happen in the region frequently.
*Photos from the Earth Science Photographs from the U.S. Geological Survey Library, by Joseph K. McGregor and Carl Abston, U.S. Geological Survey Digital Data Series DDS-21, 1995.
*Abridged from Seismicity of the United States, 1568-1989 (Revised), by Carl W. Stover and Jerry L. Coffman, U.S. Geological Survey Professional Paper 1527, United States Government Printing Office, Washington: 1993.
USGS-authored or produced data and information are in the public domain.