How Often Does the New Madrid Fault Have Earthquakes?

By Anna Duncan

The New Madrid Fault, also known as the New Madrid Seismic Zone, is a region located in the central United States that is known for its frequent seismic activity. The fault stretches from Arkansas to Illinois and has been the site of some of the most powerful earthquakes in North American history.

While it may seem like earthquakes occur on a daily basis along the New Madrid Fault, this is actually not the case. In fact, seismic activity in the region can be quite sporadic, with periods of relative quiet interspersed with sudden bursts of activity.

How Often Does The New Madrid Fault Have Earthquakes?

The frequency of earthquakes along the New Madrid Fault can be difficult to predict. On average, there are about 200 small earthquakes (less than magnitude 2) each year in the region. However, larger earthquakes (magnitude 5 or higher) are much less common.

According to the United States Geological Survey (USGS), there have been three major earthquake sequences along the New Madrid Fault since European settlement of North America:

1811-1812 Earthquake Sequence

The most well-known earthquake sequence along the New Madrid Fault occurred in late 1811 and early 1812. This sequence included four mainshocks with magnitudes estimated to be between 7.0 and 8.0 on the Richter scale. These powerful earthquakes caused widespread damage throughout the central United States and were felt as far away as Canada.

1843 Earthquake

In 1843, an earthquake with an estimated magnitude of 6.0 struck near Marked Tree, Arkansas. While this earthquake was not as powerful as those in the 1811-1812 sequence, it still caused significant damage throughout eastern Arkansas.

1895 Earthquake

The last major earthquake to occur along the New Madrid Fault was a magnitude 6.6 earthquake that struck Charleston, Missouri in 1895. This earthquake caused significant damage throughout the region and was felt as far away as Chicago.

While these three major earthquake sequences are the most well-known events along the New Madrid Fault, there have been numerous smaller earthquakes throughout the region in recent history. In fact, there have been over 4,000 earthquakes with magnitudes of 2.0 or greater recorded in the region since 1974.

Why Does The New Madrid Fault Experience Earthquakes?

The New Madrid Fault is located in an area called a “failed rift.” This means that it is located along a boundary where two tectonic plates are pulling apart but have not yet formed a new ocean basin. As a result, the crust in this area is weaker than other areas and is more likely to experience seismic activity.

In addition to its location along a failed rift, the New Madrid Fault is also located near several major fault lines, including the Wabash Valley Seismic Zone and the Reelfoot Rift. These nearby faults can contribute to seismic activity along the New Madrid Fault.

Conclusion

While earthquakes along the New Madrid Fault can be infrequent, they can also be quite powerful and have the potential to cause significant damage throughout the central United States. While it’s impossible to predict when the next major earthquake will occur along this fault, scientists continue to study seismic activity in the region in order to better understand how earthquakes work and how we can mitigate their effects on society.