The citizens of Gotham probably don't spend a lot of time worrying about earthquakes. And why should they? The last time even a magnitude 5 quake -- a moderate shake, like the one that struck south of Los Angeles last month -- was 1884.
But new research from seismologists at Columbia University's Lamont-Doherty Earth Observatory should put the New York metro area on notice: the network of faults beneath New Yorkers' feet has the potential to break off a magnitude 6 or 7 quake. From the LDEO press release:
Based on the lengths of the faults, the detected tremors, and
calculations of how stresses build in the crust, the researchers say
that magnitude 6 quakes, or even 7—respectively 10 and 100 times bigger
than magnitude 5--are quite possible on the active faults they
describe. They calculate that magnitude 6 quakes take place in the area
about every 670 years, and sevens, every 3,400 years. The corresponding
probabilities of occurrence in any 50-year period would be 7% and 1.5%.
After less specific hints of these possibilities appeared in previous
research, a 2003 analysis by The New York City Area Consortium for
Earthquake Loss Mitigation put the cost of quakes this size in the
metro New York area at $39 billion to $197 billion.
Come again? Was that $197 billion dollars? Depending on how you tally up economic impact, Hurricane Katrina cost somewhere between $81 billion and $150 billion. Pretty steep, but then that's the bill for the total destruction of a major city in America.
So it should come as little surprise that flattening New York -- as unprepared for an earthquake as New Orleans was for Katrina, maybe even more so -- would be even more expensive. Lamont's Leonardo Seeber put it best:
"We need to step backward from the simple old model, where you worry about one large, obvious fault, like they do in California," said coauthor Seeber. "The problem
here comes from many subtle faults. We now see there is earthquake
activity on them. Each one is small, but when you add them up, they are
probably more dangerous than we thought. We need to take a very close
look." Seeber says that because the faults are mostly invisible at the
surface and move infrequently, a big quake could easily hit one not yet
identified. "The probability is not zero, and the damage could be
great," he said. "It could be like something out of a Greek myth."
Seeber's comment is a little unnerving. As you'll see in the image at right, the group's data from the last
34 years shows a bunch of smallish earthquakes clustered in a Northeast/Southwest trending line north of the city called the Ramapo Seismic Zone.
Incidentally, that line runs within about 2 miles of the Indian Point nuclear power plants. Last fall the Lamont researchers sent their still-unpublished data to the New York attorney general, warning that a powerful quake could seriously damage the plants.
But Seeber's saying that fault may be the least of our worries. A number of poorly-understood faults lie in a series of parallel lines to the south and east of the big fault. Nobody knows much about how big they are, or when they were last active. One of these, the ominously-named 125th Street fault in upper Manhattan may have been the site of a magnitude 5 or so temblor that shook the island.
Back then the area was largely uninhabited. When the next one hits, millions of New Yorkers are going to have really bad days.
Images: CA Dept. of Conservation, Columbia University via EurekAlert
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