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| | Geotimes - March 2007 - New Madrid fault dying? |
 | | The earthquakes changed the Mississippi River’s course, opened deep fissures, destroyed forests and lakes, and produced intense ground-shaking that liquefied the soil, turning the land to the consistency of jelly across an area of 10,000 square kilometers. |
 | | Such intraplate earthquakes are still poorly understood, and what caused the 19th century temblors, and how much longer they might remain a hazard in the region, remains hotly debated (see Geotimes online, Web Extra, May 28, 2004). |
 | | Some studies have suggested that the reason the New Madrid earthquakes occurred is that the seismic zone is significantly hotter, and therefore is structurally weaker, than its surroundings — creating a zone of weakness where stresses building up in the plate become concentrated in the upper crust by the hot lower crust and mantle. |
| www.geotimes.org /mar07/article.html?id=nn_newmadrid.html (842 words) |
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