A minor earthquake rattled parts of the New York City metropolitan area and New Jersey late Saturday night, according to the U.S. Geological Survey (USGS). The 3.0 magnitude quake, centered northeast of Hasbrouck Heights, New Jersey, in Bergen County, struck approximately 10 kilometers below the surface.
Earthquake Details
While the earthquake was relatively small, reports of brief shaking surfaced across the region. Social media quickly filled with accounts of residents feeling the tremor. One homeowner's security camera captured the moment a family reacted with confusion as the quake hit, jumping up and searching for the cause of the shaking.
WABC-TV reporter Darla Miles described the sensation as feeling like a car had hit her house. She reported a loud boom and shaking, prompting her and her family to inspect their home for damage. Neighbors also emerged from their homes, sharing similar experiences and concerns.
No Major Damage Reported
Fortunately, initial reports indicate no major damage or injuries as a result of the earthquake. However, communities continued to inspect homes and buildings late into the night.
Seismologist's Perspective
Roberto Masis, a seismologist at Rutgers University, suggests that the recent earthquake activity is likely not a cause for significant concern. While two earthquakes occurred in the New Jersey area in less than two weeks (a 1.6 magnitude quake struck Morris County 12 days prior), Masis believes it is more of a reminder that earthquakes do occur in the region.
The New Jersey area typically experiences felt earthquakes every two to three years. While the Ramapo Fault is known to have caused a recent quake, the specific fault responsible for Saturday's event remains unknown, highlighting the ongoing discoveries of new fault lines in the region.
East Coast Earthquakes: Rare but Real
Earthquakes large enough to be felt are uncommon in the eastern U.S., but smaller earthquakes with magnitudes of 2.5 or lower are quite common. This recent event serves as a reminder that even in areas not typically associated with major seismic activity, the earth beneath our feet can still move.