A 4.7-magnitude earthquake that researchers described as the largest in Arkansas in 35 years was recorded late Sunday night near Greenbrier. It was the latest in a swarm of quakes that has bedeviled the region since early last fall, according to The New York Times. There were no reports of major damage, though some residents spoke of dislodged screen doors and cracked ceilings. Damage or not, some said this was the longest and scariest quake yet, the newspaper reports.
This earthquake swarm in Arkansas should serve as a reminder of the seismic risks facing properties in surrounding states, including Illinois, Indiana, Kentucky, Missouri and Tennessee to name a few. So what can residents living in these areas do to become better prepared? Learning from the recent quakes in New Zealand is a good place to start.
SmartPlanet.com's recent interview wtih Thomas O’Rourke, an engineering professor at Cornell University, focused on the earthquake in New Zealand last month that killed dozens of people and toppled buildings in Christchurch. O'Rourke says this event has implications for future disasters in the United States.
O’Rourke, who lived and worked in Christchurch, explained why an earthquake with a moderate intensity level caused such destruction — and what lessons we should take away from the disaster.
Here is an excerpt from the interview. Read the full report at SmartPlanet.com.
SmartPlanet.com: Since this was a moderate earthquake, how do you explain the level of damage?
O'Rourke: The New Zealanders are among some of the best seismic engineers in the world. They have one of the oldest codes. It’s certainly as old as the code in the United States for earthquakes. They also have a very up-to-date approach to structural design, disaster preparedness, understanding the effects of earthquakes on their built infrastructure and undertaking measures to ensure as good a performance as possible from their lifeline networks, such as transportation, water supply, electric power, telecommunications. They had a 7.1 magnitude earthquake on Sept. 4, 2010. The epicenter of this earthquake was located about 12 to 15 kilometers to the west of Christchurch. It’s very close and they did sustain significant levels of acceleration and other types of ground motion and they had massive liquefaction during that event. Yet not a single person died.
That reflects more than luck. It reflects many of the codes they had in place for their more modern buildings and the steps they’d taken to ensure that there would be a reliable response from their infrastructure.
The second event [in New Zealand] is really extraordinary in the fact that it was a rupture that occurred underneath the port of Lyttelton and a little north of Lyttelton, very close to the business district of Christchurch. It generated some significant dynamic movements or strong ground motions and it had a very significant impact on the built environment.
The central business district of Christchurch has a lot of unreinforced masonry structures. Many, if not the grand majority, of the unreinforced masonry structures have either collapsed or sustained serious damage.
The type of motion we’re seeing from this small magnitude earthquake, because of its proximity to the central business district, is very similar to the ground shaking one might [see] in earthquakes in the United States. [This is in places] where the infrastructure and ground behavior has certain very similar characteristics to what we see in Christchurch. In 1812, there were three earthquakes in the Mississippi River area. There is historical evidence for soil liquefaction. If you want a good likeness to what would happen if we had a severe earthquake in the New Madrid zone, all you’d have to do is look at the central business district of Christchurch.
We have even a greater concentration of unreinforced masonry structures in places like Memphis and St. Louis that would be vulnerable to this type of event. We know that recent sediments from the Mississippi River are very similar to those of sediments in New Zealand. So when you look at the massive liquefaction in Christchurch, you don’t have to have a lot of imagination to understand what would actually happen in a large and severe Midwestern earthquake.