Marysville Appeal-Democrat

Rare magnitude 4.8 earthquake rattles New Jersey, New York Occasional earthquake­s occur on faults formed when the Appalachia­n Mountains were created or when North America first drifted away from Africa and Europe about 200 million years ago ...

- By Rong-gong Lin II, Jenny Jarvie and Laura King Los Angeles Times

NEW YORK — A rare magnitude 4.8 earthquake rattled New Jersey on Friday, shaking buildings in Manhattan and sending tremors across the Northeast United States, a region unfamiliar with much seismic activity.

The U.S. Geological Survey said the quake was felt across New

York, Connecticu­t and Pennsylvan­ia. It struck about 40 miles southwest of Manhattan at 10:23 a.m. Eastern time. Its epicenter was less than 1 mile northwest of the unincorpor­ated community of Oldwick, New Jersey.

Weak shaking was felt from Washington, D.C., to Maine, including in Boston, Philadelph­ia and Albany, New York.

There were no immediate reports of damage or injuries, but in New York City, people reported feeling buildings sway. Then, at 11:02 a.m., they received a beeping emergency alert on their phones urging them to stay indoors and call 911 if injured.

At busy intersecti­ons, people’s cellphones shrieked as a series of the same alerts warned of aftershock­s.

In midtown Manhattan, convenienc­e store proprietor Arun Kumar, 50, said he thought the rattling was a heavy truck passing nearby.

“But it felt a little weird, a little different, you know?” he said.

Maria Marta, 75, who was visiting from Buenos Aires, said she barely felt a tremor. But she lived in the city in the 1980s and experience­d an earthquake then.

“It’s New York, you know?” she said Friday. “Anything can happen.”

The Federal Aviation Administra­tion initially warned that the quake could disrupt air traffic facilities in New York, New Jersey, Philadelph­ia and Baltimore. Three hours after the quake, Newark Liberty Internatio­nal Airport’s “air train” service, which carries passengers between the airport train station and the terminals, remained suspended for inspection­s.

President Joe Biden said Friday from the White House that he had spoken with New Jersey Gov. Phil Murphy.

“He thinks everything is under control,” Biden said of Murphy. “He’s not too concerned.”

The USGS said there was “a low likelihood of casualties and damage” from the quake.

According to the agency, strong shaking was felt at the epicenter, as defined by the Modified Mercalli Intensity Scale. That’s enough to be felt by everyone, but cause only slight damage.

A large part of the Midatlanti­c and Northeast felt weak shaking, according to people who filed reports to the USGS’ “Did You Feel It?” tracking service. Weak shaking is defined as being felt quite noticeably by people indoors, especially on the upper floors of a building, and may rock standing motor vehicles slightly.

Earthquake­s are less frequent and powerful in the eastern United States than in the West. Over the last half-century, more than 400 quakes of magnitude 3.5 or greater have been recorded across eastern North America, according to the USGS.

Shaking from a single quake in the eastern U.S. can be felt much farther away than an equivalent­ly powerful magnitude quake in California.

Leslie Sonder, an associate professor of earth sciences at Dartmouth specializi­ng in geodynamic­s, said the eastern U.S. typically experience­s small and moderate earthquake­s — and far less frequently than the West — because the nearest plate boundary is way off in the middle of the Atlantic Ocean.

Occasional earthquake­s occur on faults formed when the Appalachia­n

Mountains were created or when North America first drifted away from Africa and Europe about 200 million years ago, Sonder said.

“Because the rocks are old — basically nothing’s happened to them for 200 million years — they’ve cooled off and so they transmit seismic waves more efficientl­y than in the West, where the rocks are hotter,” Sonder said. “So that’s why they’re felt more widely in the East.”

In 2011, a magnitude 5.8 earthquake struck near Mineral, Virginia, about 300 miles from Friday’s temblor.

That quake — which produced more than 32 times more energy than Friday’s — resulted in severe shaking at the epicenter and caused more than $200 million in damage, including to historic structures such as the Washington Monument, the Washington National Cathedral and the Smithsonia­n Institutio­n Building.

More recently, a magnitude 5.1 earthquake occurred in 2020 near Sparta, North Carolina, rattling northweste­rn North Carolina and southweste­rn Virginia.

Other historic damaging quakes in the eastern

U.S. include one off Cape Ann, Massachuse­tts, in 1755, estimated to be a magnitude 5.9, which resulted in damage to the Boston waterfront; an estimated magnitude 4.5 quake near Petersburg, Virginia, in 1774, which shoved homes from their foundation­s and was felt by Thomas Jefferson; and an estimated magnitude 7 quake near Charleston, South Carolina, in 1886 that killed 60 people, according to the USGS.

While California is the focus of national attention for its outsized seismic risk, a report issued by the USGS last year noted that the eastern U.S. faces risk too.

Calculatin­g an “annualized” earthquake loss to average out the projected cost of earthquake damage on a yearly basis, the USGS found that the Memphis area faces an annual earthquake loss of $131 million a year, and the

New York City region $49 million a year.

In any given year, New York City has a low probabilit­y of a damaging earthquake, but any quake could still cause significan­t damage because of the city’s density and age of its buildings, according to the city’s emergency management agency. A large number of older brick buildings have not been retrofitte­d, putting them especially at risk.

Benjamin Fernando, a postdoctor­al fellow with the Department of Earth and Planetary Sciences at Johns Hopkins University who studies seismology, said the New Jersey quake was probably on the Ramapo fault, a 700-million-year-old fault that runs through that state and hasn’t produced a quake of this size in quite some time.

“For people here in the Northeast, who are not used to events like this, it really calls people’s attention,” Fernando said. “But in California, people certainly wouldn’t get excited at all.”

Sally Taylor, a 77-yearold artist, said she felt the vibrations Friday morning in her apartment in Manhattan’s west 30s. When she wasn’t sure what the shaking was, relatives visiting her from the

San Francisco Bay Area said: “Nope, that was an earthquake.

”And that was nothing!” they added.

Sonder, the Dartmouth professor, said Friday’s quake was small, just starting to get into moderate size.

“This was significan­t in the social sense, because people felt it and they’re curious about it,” Sonder said. “But in a geological sense, it’s very generic. It’s maybe slightly bigger than a lot of the earthquake­s in the East Coast. But it’s still no big deal geological­ly.”

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