Scattered clouds
Scattered clouds
86 °F
July 23, 2014
River Reporter Facebook pageTRR TwitterRSS Search Login
news

Did you feel the earthquake? What about fracking?

By Fritz Mayer
August 31, 2011

The 5.8 magnitude earthquake that struck Virginia on August 23 wreaked a bit of damage nearby: the tip of the Washington Monument was cracked. But its vibrations were felt as far away as Detroit and Canada. That’s according to information from the U.S. Geological Survey’s feature called “Did you feel it?” located at http://earthquake.usgs.gov/earthquakes/dyfi/events/se/082311a/us/index.html.

Here in the Upper Delaware Valley, a lot of people felt it, and others didn’t. At 93 Erie Ave, in the building that houses The River Reporter, three staffers felt a slight bit of movement, but several others did not. An upstairs tenant indicated that the movement set her rocking chair in motion.

Rowena Lohman, an earthquake scientist with Cornell University, said that whether or not a person felt the earthquake is related to what they were doing at the time. She said, “I felt it, and ’m about 300 miles away [in Ithaca], but that’s in part because my window faces southward, and I was sitting at my office quietly at the time basically looking toward the earthquake, and I felt ‘boom, boom,’ and other people in my building didn’t feel it. People on the ground floor often don’t feel it as much as people higher up. We had people on the 11th floor of this building on campus who actually felt the building swaying, so they really felt it.”

Lohman said that when such large earthquakes occur on the East Coast, it’s not unusual to have them felt across a much larger expanse of land than earthquakes on the West Coast of comparable size. She said the earth’s crust in California is much younger and hotter, therefore “it absorbs energy much better; it’s mushy in a way,” whereas on the East Coast the crust is “much older; it’s cold, so when you hit it with something like an earthquake, it rings like a bell.”

She added that in the east, judging not only by modern seismic readings but also historical records of such things as where church steeples fell, there had been five or six earthquakes of this size over the past couple of centuries.