Wabash Valley Seismic Zone
The Wabash Valley Seismic Zone (also known as the Wabash Valley Fault System or Zone) is a tectonic region located in the Midwest of the United States, centered on the valley of the Lower Wabash River, along the state line between southeastern Illinois and southwestern Indiana.
The Wabash Valley Seismic Zone consists largely of vertically oriented ("normal") faults deeply buried under layers of sediment. Although the tectonics of the region are still not fully understood and are the subject of ongoing research, these faults are thought by some to be associated with a branch of the New Madrid aulacogen, an old rift zone where the lithosphere actively began to pull apart at perhaps two separate times in the distant past. Present-day GPS measurements show that the region deforms at about 1-2 mm/yr with compression along the Wabash Valley Fault Zone, and extension in SW Indiana [Hamburger et al., 2002; Galgana and Hamburger, 2010]. The crust in the area has been weakened by the numerous faults, which remain active sites for continuing seismic activity as the motion of the North American Plate exerts both compressional and tensional forces.
According to the United States Geological Survey, lesser earthquakes occur relatively frequently, but those at a magnitude of less than 3.5 or so are usually not felt. Ones strong enough to feel usually happen once or twice a year, and those large enough to cause moderate damage have occurred every decade or so. Quakes in this region can be felt in a much wider range than those in other zones such as California.
The concern of seismologists Douglas Wiens and Michael E. Wysession of Washington University in St. Louis, is that the New Madrid Fault may be becoming less active, while activity on the Wabash Fault could be increasing. Wiens states: "I think everyone's interested in the Wabash Valley Fault because a lot of the attention has been on the New Madrid Fault, but the Wabash Valley Fault could be the more dangerous one, at least for St. Louis and Illinois." "The strongest earthquakes in the last few years have come from the Wabash Valley Fault, which needs more investigation."
"Numerical modeling indicates that stress transfer following the 1811-1812 New Madrid earthquakes may be loading faults in the Wabash Zone." 
Notable modern earthquakes in this zone include:
- June 18, 2002, magnitude 4.6
- The earthquake was located close to Evansville, Indiana, with an epicenter between Darmstadt and Cynthiana in Posey County. There was minor damage associated with the earthquake. 
- April 18, 2008, magnitude 5.4
Main article: 2008 Illinois earthquakeThe initial magnitude 5.4 quake was followed by a 4.6 aftershock six hours later, followed by a 4.0 aftershock 3 days later. Its epicenter was located about 41 miles (66 km) NNW of Evansville, Indiana, near the communities of West Salem, Mount Carmel, and Bellmont. The quake was felt as far away as Kansas City, Atlanta, and Canada. Some minor damage was reported near the epicenter.
- Hill, John R. "Seismicity of the Lower Wabash Valley: Fact Sheet". Central United States Earthquake Consortium. Archived from the original on 2008-04-22. Retrieved 2008-04-18.
- Tony Fitzpatrick. "Earthquake in Illinois could portend an emerging threat". Washington University in St. Louis. Retrieved 2008-04-24.
- "Magnitude 5.2 - ILLINOIS". United States Geological Survey. 2008-04-18. Archived from the original on 2008-04-21. Retrieved 2008-04-18.
- Len Wells. "Geologist predicts next big quake spot". Evansville Courier and Press. Retrieved 2011-02-14.
- "USGS Fact Sheet 131-02: Earthquake Hazard in the Heart of the Homeland". United States Geological Survey. Retrieved 2008-04-18.