Are shifts in Earth's crust causing New Orleans to sink?
By Peter N. Spotts | Staff writer of The Christian Science Monitor
Hurricane Katrina's devastating strike on New Orleans last fall highlighted shortcomings in the city's levee system. It also focused attention another long-term problem: The city and the region around it are sinking.
New research suggests, however, that at least for nearby Michoud, La., the dominant driver pulling the region under may not be among the usual suspects: oil extraction, pumping groundwater to the surface, or diverting the Mississippi for navigation.
Instead, the King of Slump may be a deep fault that cuts across southeastern Louisiana and under Michoud. During the 1970s, the fault appears to have contributed from 50 to 73 percent of the subsidence in this section of Orleans parish, depending on the time period measured. If sustained over a century, that would equate to as much as a six-foot sea-level rise, independent of any increase tied to global warming.
"Something dynamic is going on down there," says Roy Dokka, who heads the Center for GeoInformatics at Louisiana State University in Baton Rouge, La. "It doesn't occur everywhere," but it certainly appears to be affecting Orleans parish, he adds.
If these results hold up, they would imply that to build new levees properly, engineers will have to take into account the effects of further slumping along the fault - data hard to come by because the fault is so deep and difficult to study. The work is controversial. It builds on a study Dr. Dokka and Kurt Shinkle of the National Oceanic and Atmospheric Administration's National Geodetic Survey (NGS) completed in 2004 for NOAA. That study drew on some 2,700 measuring points around southern Louisiana to measure subsidence rates. It yielded far higher sinking rates than other scientists had calculated.
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http://www.csmonitor.com/2006/0331/p02s01-sten.html