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In top figure, closed red circles show 1924–2006 epicenters. Open black circles show larger earthquakes of 1737, 1783 and 1884. Green lines are the Ramapo fault. Seismicity of the New York City area is relatively low. [1] New York is less seismically active than California because it is far from any plate boundaries.
A damaging earthquake affecting New York City in 1884 was incorrectly argued to be caused by the Ramapo fault, likely because it is the most prominent mapped fault in the greater New York City area. At the present, the relationship between faults and earthquakes in the New York City area is understood to be more complex than any simple ...
A newly found fault line with a rare slanted angle shows why an earthquake rattled New York City in April harder than its epicenter in New Jersey — and may be a bigger seismic activity threat ...
The Dyckman Street Fault is a seismologically active fault in New York City which runs parallel along the southern border of Inwood Hill Park, crossing the Harlem River and into Morris Heights. [1] As recently as 1989, activity of this fault caused a magnitude 2 earthquake. [2] [3] [4]
A view of New York City after a 4.8 magnitude earthquake shook parts of New York and New Jersey. (Fatih Aktas/Anadolu via Getty Images) ... What are the fault lines under New York and New Jersey?
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These actually lie both east and west of Cameron's Line because it makes a sharp U-turn, heading south from Manhattan into Staten Island and hooking back north into Hudson County, New Jersey. Indeed, near New York City the term "line" becomes less applicable and its position is subject to much debate, because the boundary has been warped and ...
The New York State Thruway has a rock cut at Batavia which clearly shows the fault and is a popular point for geology class field trips. [5] The fault, which runs from Attica, New York northward to Lake Ontario, is still active and periodically causes minor earthquakes in the area.