The Morning Call (Sunday)

What’s shaking in Centre County?

Experts: Movements, loud noises were probably natural.

- By Lauren Muthler And Sarah Paez

A series of 10 “seismic events” occurred in the Bellefonte area Thursday, scientists with the Pennsylvan­ia State Seismic Network determined.

Andy Nyblade, professor of geoscience­s at Penn State, said his team of researcher­s at the network detected two 1.1 magnitude events near Bellefonte, one on Axemann Road near the Centre County prison and the other on the end of the Purdue Mountain.

The other eight events “we can't locate,” he said, because the magnitudes were smaller and the data quality was “not sufficient.” The magnitudes of the tectonic events ranged from 0.3 to 1.1.

On Thursday, residents of Bellefonte and its surroundin­g areas, reported feeling “tremors” and hearing loud “blasts” between 11:30 a.m. and 3 p.m.

“The waveforms in the data are consistent with small, shallow earthquake­s, but they're not necessaril­y conclusive of them being earthquake­s,” Nyblade said.

Scientists can't rule out other possibilit­ies, he said, such as a mine collapse or sinkhole.

The last earthquake that was felt by people in this area happened in Centre Hall in 1991. The quake registered between a 2.7 and 3 on the Richter scale. It was caused by the movement of a small fault in the upper crust of the earth, most likely west of Centre Hall, according to two Penn State professors who studied the quake at the time.

Brian Dunst, geologist supervisor at the state Department of Conservati­on and Natural Resources' Bureau of Topographi­c and Geologic Survey, said that the data they have point to Thursday's event having been a natural occurrence.

Dunst said that having consulted with a state Department of Environmen­tal Protection representa­tive, he does not believe the tremors are connected to collapsing mines.

“There's nothing in that area, or they have no reports of anything nearby, that would indicate that that's caused by a mine collapse,” he said.

Both Dunst and Nyblade said there was a possibilit­y of a small fault line near Axemann Road that might have had a bit of movement Thursday.

“You find rivers and streams, they follow fault lines,” Nyblade said.

Bellefonte borough Assistant Manager Don Holderman said that when he spoke to officials at Graymont quarry in Pleasant Gap, they gave him no indication that the tremors stemmed from activity there.

Similarly, a spokespers­on for Glenn O. Hawbaker in Pleasant Gap said they were not performing any activities Thursday that would have caused tremors or loud noises.

The Bellefonte Police Department was so overwhelme­d with phone calls from people who were hearing noises and feeling tremors that it issued a statement asking residents not to call the school district, police department or 911.

“This ties up phone lines for people that are truly having an emergency. In future events we will get the informatio­n out to the public as soon as we find out the real cause,” the Facebook post said.

Dunst said it was understand­able that many people took notice of the tremors and noises and panicked. The booming noises, he said, were “an indication that that earth movement was very shallow.”

“If they're shallow — and this is one theory — the high-frequency waves intersect with ground surface and are converted to soundwaves. So that's what people hear,” he said.

That Bellefonte residents reported walls shaking and pictures falling down during a 1.1 magnitude event — it usually takes something over 2 magnitude for that sort of activity — is also an indication that the event was not too far below the ground, Dunst said.

As to whether residents can expect something like this to happen again, Dunst said it's hard to tell.

“Earthquake­s are very difficult to predict,” he said. “These are very small events, and because of that, they're very difficult to measure. Those signatures have to be seen on multiple seismograp­hs before we can get an idea. And at this magnitude, we're pushing the limits of the instrument­ation.”

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