This map shows shock wave attenuation across the central United States. Blue areas indicate regions through which shock waves travel fastest, and red areas indicate regions in which the waves are absorbed.
Credit: Andrea Gellegos, Nishath Ranasinghe, James Ni, and Eric Sandvol
New seismic maps of the central and eastern United States may help improve earthquake hazard assessments by identifying regions where seismic shock waves can travel the fastest and farthest from earthquake epicenters, according to a recent report.
When an earthquake strikes, the shock waves it generates pulse through the Earth's crust, traveling as far as 2,500 miles (4,000 kilometers) laterally before dissipating. The distance and force with which a shock wave travels depends on a variety of factors, including the strength of the earthquake and the composition of the surrounding crust (the uppermost layer of the planet). For example, shock waves may only travel several hundred miles through warm, tectonically active regions of the crust but may travel much farther in colder, inactive regions. [The 10 Biggest Earthquakes in History]
"Cold rock is very stable and solid, and waves like to travel through stable things," said Andrea Gallegos, a graduate student at New Mexico State University. "Hot things have a lot of random motion, and that slows down wave propagation."
Gallegos has worked with colleagues to analyze seismic data and create maps that illustrate seismic attenuation — the loss of intensity as shock waves get absorbed by the crust — across the central and eastern United States, in hopes of helping to improve seismic risk assessments within those regions.
The maps show that the most vulnerable regions surround the New Madrid Seismic Zone in New Madrid, Mo., where a series of damaging earthquakes occurred in 1811 and 1812.
Other areas with crustal conditions that allow shock waves to quickly pass through without dissipating much include central Georgia, Tennessee and Michigan. Texas, Louisiana and Alabama, on the other hand, appear less vulnerable.
"If you're in Louisiana and you get an earthquake from Oklahoma, that wave is probably going to die out within a couple of hundred kilometers, because the sediment is going to cause the wave to die out quickly," Gallegos told Live Science. "But if you go to Iowa or the Midwest, you are going to see that wave last for closer to 1,000 kilometers [about 600 miles]."
While the central and eastern United States may not experience earthquakes as frequently as the western United States does, those regions are not immune to temblors. An active fault zone in South Carolina resulted in a magnitude-4.1 earthquake on Feb. 15, and another active fault zone in Ottawa, Canada, poses a threat to states in the northeastern part of the United States. Other fault zones are scattered throughout the interior of the country and, in some ways, pose larger risks than the West Coast fault zones because communities in the eastern part of the country are generally less prepared for these threats, Gallegos said.
The team now plans to expand their methods to create a map that spans the entire country. Ultimately, they hope to share their data with seismic hazard teams at the U.S. Geological Survey or elsewhere to help update seismic hazard maps.
The study findings were detailed last month in the journal Earth and Planetary Science Letters.