4/30/2023 0 Comments Kentucky earth quake![]() ![]() New Madrid dwindled to insignificance and decay the people trembling in their miserable hovels at the distant and melancholy rumbling of the approaching shocks. The Great Prarie settlement, one of the most flourishing before on the west bank of the Mississippi, was much diminished. The Little Prarie settlement was broken up. One account of this phenomena stated that the Pemiscot Bayou "blew up for a distance of nearly fifty miles."Īfter the earthquake moderated in violence, the country exhibited a melancholy aspect of chasms, of sand covering the earth, of trees thrown down, or lying at an angle of forty-five degrees, or split in the middle. In addition, the earthquakes liquefied subsurface sediment over a large area and at great distances resulting in ground fissuring and violent venting of water and sediment. One such uplift related to faulting near New Madrid, Missouri, temporarily forced the Mississippi River to flow backwards. ![]() They caused bank failures along the Mississippi River, landslides along Chickasaw Bluffs in Kentucky and Tennessee, and uplift and subsidence of large tracts of land in the Mississippi River floodplain. In the New Madrid region, the earthquakes dramatically affected the landscape. Louis, Missouri, and were felt as far away as Hartford, Connecticut, Charleston, South Carolina, and New Orleans, Louisiana. The three largest 1811-1812 earthquakes destroyed several settlements along the Mississippi River, caused minor structural damage as far away as Cincinnati, Ohio, and St. In the winter of 18, the New Madrid seismic zone generated a sequence of earthquakes that lasted for several months and included three very large earthquakes estimated to be between magnitude 7 and 8. It shows 20 localities where geologists have found and published their findings on faults or evidence of large earthquakes (from sand blows see image to the right). Other relatively young faults, which are not necessarily associated with recent earthquakes, or the main seismicity trend in the New Madrid region, are shown in this map. A map of earthquakes epicenters, however, reflects faulting at depth and shows that the earthquakes define several branches of the New Madrid seismic zone in northeastern Arkansas, southwestern Kentucky, southeastern Missouri, and northwestern Tennessee. The faults that produce earthquakes are not easy to see at the surface in the New Madrid region because they are eroded by river processes and deeply buried by river sediment. Since 1974, seismometers, instruments that measure ground shaking, have recorded thousands of small to moderate earthquakes. Until 2014, when the dramatic increase in earthquake rates gave Oklahoma the number one ranking in the conterminous U.S., the most seismically active area east of the Rocky Mountains was in the Mississippi Valley area known as the New Madrid seismic zone. But earthquakes also happen in the eastern and central U.S. When people think of earthquakes in the United States, they tend to think of the west coast. Earthquakes with magnitudes equal to or larger than 2.5 are shown by the yellow dots. New Madrid Seismic Zone - Quaternary Fault Localities. ![]()
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