Earthquakes – and large ones at that – threaten to shake residents and buildings of the central and eastern United States, a reality that scientists, emergency responders and others hope to drive home during the bicentennial of the 1811 and 1812 New Madrid earthquakes. Scientific presentations and discussions about these historic events and recent major earthquakes conclude today at the annual Seismological Society of America Meeting in Memphis.
During 1811-12, the central Mississippi River Valley was violently shaken by a series of three earthquakes above a magnitude 7, and up to 200 aftershocks between magnitude 4 and 7.
A similar risk exists today in the New Madrid seismic zone, which threatens Alabama, Arkansas, Illinois, Indiana, Kentucky, Mississippi, Missouri and Tennessee. Recent projections by the U.S. Geological Survey place the likelihood of a magnitude 6 or higher earthquake at about 25-50 percent over the next few decades, whereas a magnitude 7 or higher has a 10 percent chance of occurring.
With large cities like Memphis, St. Louis, and Nashville well within range of a large-scale New Madrid earthquake, understanding the science of earthquakes and the area’s geologic history helps communities prepare for earthquake hazards and prevent them from becoming catastrophes.
“If we build good buildings, there’s no reason any building should collapse; there’s no reason any person should die in an earthquake,” said Dr. Michael Blanpied, associate coordinator of the USGS Earthquake Hazards Program. He and other scientists from around the globe are discussing this hazard as well as recent seismic events that have occurred, including the Japanese and New Zealand earthquakes. The meeting concludes on Friday.
Blanpied emphasized that residents outside of the west coast need to realize that earthquakes can affect them too. In fact, earthquakes in the central and eastern U.S. can have far greater effects than their western equivalents. Western rock is fairly young, which means it absorbs a lot of the shaking caused by earthquakes. Thus, western earthquakes result in intense shaking close to the epicenter, but fade quickly the farther they travel.
Not so in the central and eastern United States.
“Here, the rocks are old, and really ring like a bell when an earthquake strikes,” Blanpied explains. The result—large earthquakes in the central and eastern states can travel nearly half the distance of the continental United States. The February 1812 New Madrid earthquake was felt as far east as North and South Carolina, some 750 miles away from the epicenter in New Madrid, in what would become the state of Missouri.
The source of these earthquakes was the Reelfoot fault, part of a 120-mile-long New Madrid seismic zone. This seismic zone is a system of faults that lies well within the North American tectonic plate, as opposed to the more familiar faults that mark the boundaries between plates.
For more information on the earthquake science of the New Madrid seismic zone, please listen to a Corecast interview with Mike Blanpied, available here. More information about New Madrid earthquakes can be found online.
Additional information about the history and events related to the New Madrid Bicentennial may be found at the New Madrid Bicentennial website and Central U.S. Great Shakeout website. A recent USGS publication about residents being prepared can be found at Putting Down Roots.
Links and contacts within this release are valid at the time of publication.