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The Ramapo Fault zone is a system of faults between the northern Appalachian Mountains and Piedmont areas to the east. [1] Spanning more than 185 miles (298 km) in New York , New Jersey , and Pennsylvania , it is perhaps the best known fault zone in the Mid-Atlantic region, and some small earthquakes have been known to occur in its vicinity.
The Atlantic Seaboard Fall Line, or Fall Zone, is a 900-mile (1,400 km) escarpment where the Piedmont and Atlantic coastal plain meet in the eastern United States. [2] Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present.
East Anatolian Fault ~700: ... Utah, United States: Normal fault: Active: 2020 Salt Lake City (M5.7) Wellington Fault >100: North Island, New Zealand: Dextral strike ...
The Atlantic Seaboard Fall Line, or Fall Zone, is a 1,400-kilometre (900-mile) escarpment where the Piedmont and Atlantic Coastal Plain meet in the eastern United States. [3] Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present.
The Cascadia subduction zone is a 960 km (600 mi) fault at a convergent plate boundary, about 100–200 km (70–100 mi) off the Pacific coast, that stretches from northern Vancouver Island in Canada to Northern California in the United States
However, buried under several states to the south-southwest of Michigan lies the New Madrid fault line, extending 120 miles from southeast Missouri into northeastern Arkansas. But in the event of ...
What are the fault lines under New York and New Jersey? ... Is the Northeast’s infrastructure built to sustain earthquakes? “There are earthquake building codes throughout the United States ...
The Eastern Tennessee seismic zone (ETSZ), also known as the East Tennessee seismic zone and the Southern Appalachian seismic zone, is a geographic band stretching from northeastern Alabama to southwestern Virginia that is subject to frequent small earthquakes. The ETSZ is one of the most active earthquake zones in the eastern United States. [1 ...