Scientists find potential catalyst for earthquakes on U.S. East Coast
Posted on September 16, 2013 by The Extinction Protocol
September 16, 2013 – BOSTON – A plume of hot material rising from deep within the earth scarred the underside of the North American tectonic plate as it drifted westward millions of years ago, suggests research published today in Nature Geoscience. The residual heat still affects seismic waves travelling through the continent, even though the mantle plume is now under the Atlantic Ocean. When such mantle plumes occur beneath thin oceanic crust, they often punch through and create volcanoes — the Hawaiian Islands are a prime example. But older, colder and thicker continental crust is not so easily breached, says Risheng Chu, a geophysicist at the Institute of Geodesy and Geophysics in Wuhan, China. The only signs on land of ancient hotspot paths typically are kimberlites — volcanic and sometimes diamond-bearing rocks that mark the site of an ancient, deep-seated eruption. But Chu and his colleagues inferred the path of a hotspot beneath eastern North America using a different sort of evidence — the speed of seismic waves, which travel more slowly in warmer rock. The data were gathered by dozens of seismometers in the USArray network, most of them along a stretch from Louisiana to Wisconsin, during the magnitude-5.6 quake that jolted central Virginia on 23 August 2011. Their analysis indicates that seismic waves travelling west from the earthquake’s source in Virginia towards Missouri arrived at seismometers later and with lower intensity than expected. Such vibration-damping behavior suggests the presence of a broad lane of warm rocks running east to west, about 200 kilometers beneath Kentucky — a depth that roughly coincides with the lower surface of the tectonic plate. Seismic waves travelling north and south of this lane arrived on time or slightly ahead of schedule.
Seismometers northeast of the Virginia quake’s epicentre also detected slow, stifled seismic waves, suggesting another hotspot track in that direction as well. The researchers suggest that the continent moving over the hotspot cut a path that swooped east-southeast from central Missouri (90 million years ago) to eastern Kentucky (some 70 million years ago), arced northeastward to Massachusetts (60 million to 50 million years ago) and then swerved eastward and moved offshore. A kimberlite deposit in eastern Kentucky, dated to about 75 million years ago, bolsters the notion that a hotspot lay below the region during that time, Chu and his colleagues contend. The evidence supporting the purported hotspot’s path is interesting but circumstantial, says Randel Cox, a geologist at the University of Memphis in Tennessee. “I’m still trying to keep an open mind about this [idea], but there are alternate explanations” for the seismic slowdown beneath Kentucky and the Virginia–Massachusetts corridor, he notes. For instance, seismic vibrations in the region could be scattered by features deep within or below Earth’s crust, such as a ‘crumple zone’ of rocks where one tectonic plate collided with another. Regardless, he adds, researchers need more data, from more than one earthquake, to produce a thorough subterranean map of the eastern United States. -Nature
Is there a blow torch under North America that causes rare, but deadly, earthquakes? Some geologists think they might have found the buried track of just such a hotspot from Missouri to Virginia. A team of Chinese and American scientists think they have found the track of a hotspot hidden in the very old, thick crust of Eastern United States, based on seismic data from the 2011 Virginia 5.6-magnitude earthquake. That event essentially lit up the structure of the crust in that part of North America for the USArray seismic network to see. The seismic anomaly, as it is called, cuts through the New Madrid rift system, which is responsible for some of the most powerful earthquakes in North American history. It also crosses a 75-million-year-old diamond-bearing formation in Kentucky. –Discovery
Hotspot Scorched Midwest, Leaving Legacy of Earthquakes, Rare RocksBy Becky Oskin, Staff Writer | September 15, 2013 01:00pm ET
A seismic speed trap that stretches from Missouri to Virginia suggests a hotspot scorched the Midwest during the Mesozoic Era, a new study finds.
Hotspots are scalding plumes of hot rock rising toward Earth’s surface from the mantle, the layer that sits under Earth’s crust. Though tectonic plates constantly shift, hotspots are homebodies, stuck in pretty much the same spot for their entire lives, scientists think…
Slow and low
The massive array of more than 500 seismometers, instruments that measure earthquake waves, spied an unusually slow zone beneath North America during the 2011 Virginia earthquake. This seismic “low-velocity” lane cuts west to east from Missouri to Virginia, then jogs north to Massachusetts and continues offshore. The corridor is 25 miles (40 kilometers) thick, and lies 75 miles to 100 miles (120 to 160 km) below the surface, said Risheng Chu, lead study author and a geophysicist with the Institute of Geodesy and Geophysics at the Chinese Academy of Sciences in Beijing. The zone also appears in other earthquakes, Chu said in an email interview.
…East Coast flow
Chu and his colleagues believe the hot spot now sits under the flat, featureless Sohm Plain, north of a chain of unrelated volcanic islands called the New England Seamounts. (In fact, the seamounts formed about 110 to 80 million years ago over the Great Meteor mantle plume). They hope to confirm their suspicions with the mobile seismometer network, which shifted east of the Appalachians this year, Helmberger said.
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