Scientists may have found another cause of a series of devastating earthquakes that struck the Midwest nearly 200 years ago and have confused geologists ever since.
The results suggest the region, still seismically active today, is going to keep shaking for a long time.
The New Madrid Earthquake, the largest earthquake ever recorded in the continental U.S., struck on Feb, 7, 1812 and had an estimated 8.0 magnitude, strong enough to cause the nearby Mississippi River to temporarily flow backward.
It was preceded by two, possibly three large quakes over the previous months — one or two on Dec. 16, 1811 and another on Jan. 23, 1812.
The epicenter for all the temblors was near the town of New Madrid in what is now southeastern Missouri, near the Kentucky and Tennessee state lines. The town was partly destroyed, and hundreds of aftershocks followed for several years.
A similar event today in the region — about equidistant from St. Louis, Memphis and Nashville — would be devastating, seismologists and engineers agree.
More to come
The seismic zone generates about 200 tiny quakes annually, but it also let loose a magnitude 4.1 quake in February 2005 and a magnitude 4.0 quake in June 2005.
The U.S. Geological Survey says there is a 9-in-10 chance of a magnitude 6 or 7 temblor occurring in this area within the next 50 years.
These mid-continent temblors have long fascinated seismologists because of they occur not at the edges, but in the center of tectonic plates, such as the North American Plate that underlies the continent.
One team of seismologists had thought that high-density pillow lavas in the lower crust beneath the New Madrid region could have pulled the crust downward and thereby generated surface stresses that triggered the quakes.
Now, Allessandro Forte of the Université du Québec à Montréal and his colleagues have arrived at a more dramatic mechanism — an ancient, giant slab of Earth called the Farallon slab that started its descent under the West Coast 70 million years ago.
It may now be causing mayhem and deep mantle flow 360 miles beneath the Mississippi Valley, where it effectively pulls the crust down an entire kilometer (.62 miles).
"This remarkable localization of flow in the mantle below New Madrid, originating so deep below the surface, was completely unrecognized prior to our work," Forte told LiveScience.
Slabs like this that sink oceanic crust are called subduction zones, and those adjacent to Japan produce intense and damaging seismic activity.
"We have discovered an analogous subduction zone, deep inside the Earth below the central Mississippi River Valley," Forte said.
Forte and his colleagues at the University of Toronto and the University of Texas based their findings on high-resolution seismic tomography images that were used to predict the topography and viscous flow of the mantle under and around North America.
They used the model to focus on the New Madrid seismic zone and propose that the descending slab and associated mantle flow directly below the New Madrid seismic zone strains the overlying crust, causing seismic ruptures.
The results were published in a recent issue of Geophysical Research Letters.
The Farallon plate will continue to descend into the deep mantle and thus to cause mantle downwelling in the New Madrid region for a long time.
"[This] suggests that the seismic risk in the New Madrid region will not fade with time," Forte said.
The weakened crust under the New Madrid region was there long before the Farallon slab began its journey.
The underlying fault system is the result of a "failed rift" created by the opening of the ocean that later became the Atlantic Ocean 650 to 600 million years ago, Forte said.
That activity also caused rifts in the St. Lawrence, Saguenay and Ottawa river valleys in Canada, where there is similar mid-continental quaking, he said.
Another set of faults far from the boundaries of the North American Plate are associated with the Keweenawan Rift, a 1,240-mile-long rift in the area surrounding Lake Superior.
Copyright © 2007 Imaginova Corp. All Rights Reserved. This material may not be published, broadcast, rewritten or redistributed.