The Prophecy is much more than seeing into the future. Schlesinger-Miller, and N.L. In the top figure, closed red circles indicate 1924-2006 epicenters and open black circles indicate locations of the larger earthquakes that occurred in 1737, 1783 and 1884. Please click on the PDF icon to access. Structural and stratigraphic development of the Newark extensional basin, eastern North America: Evidence for the growth of the basin and its bounding structures. For The Prophecy sees without the limits of time. The Ramapo fault system forms the northwestern boundary of the Newark Triassic basin in New York and adjacent northern New Jersey, and is commonly attributed to Mesozoic crustal fracturing. These observations, along with the remarkable longevity, suggest that this fault zone may be part of a fundamental crustal fracture system that was operative during formation of the Appalachian orogen.The ideas presented here require a degree of tectonic permanence not commonly reported in orogenic belts. Please check your email address / username and password and try again.
Nearby bigger faults in other states could also have their own earthquakes that could radiate shocks into New York through its faults. There is insufficient evidence to unequivocally demonstrate any strong correlation of earthquakes in the New York City area with specific faults or other geologic structures in this region. Armbruster, W.Y. Activity along this fracture system in pre-Middle Ordovician time as documented here suggests strongly that the northern end of the Reading Prong is not allochthonous in the sense proposed by Isachsen (1964).Department of Geology, City College of City University of New York, New York, New York 10031
It is responsible for several of the fault lines that run through New York City, including one under 125This 150 mile-long series of faults stretches under five states: Illinois, Missouri, Arkansas, Tennessee and Kentucky, and is responsible for four of the largest earthquakes in the history of the United States, which took place over three months from December 1811 and February 1812. tinued fault activity in the vicinity of the border fault (Ramapo fault) in New York and New Jerse~. Green lines indicate the trace of the Ramapo fault.As can be seen in the maps of earthquake activity in this region(shown in the figure), The NYC area is part of the geologically complex structure of the Northern Earthquake rates in the northeastern United States are about 50 to 200 times lower than in California, but The northeastern U.S. has many known faults, but virtually all of the known faults have not been active for perhaps 90 million years or more. 11:11 LLCSeismicity in the vicinity of New York City. 1). As in most other areas east of the Rocky Mountains, the best guide to earthquake hazard in the northeastern U.S. is probably the locations of past earthquakes themselves.The Ramapo Fault has been blamed for several past earthquakes, but the specific association of any significant earthquake with this fault has yet to be demonstrated.East of the Highlands is the Piedmont, specifically the To the east of the Newark Basin are varying geologic provinces. However, the detailed geology in the vicinity of this fault indicates an earlier, complex tectonic ancestry, perhaps dating from late Precambrian time. The Ramapo Fault, which runs through it, was responsible for a big earthquake in 1884, and Dr. Gates warns that a recurrence is overdue. The Ramapo fault system forms the northwestern boundary of the Newark Triassic basin in New York and adjacent northern New Jersey, and is commonly attributed to Mesozoic crustal fracturing. However, it wasn’t until the discovery of the Cascadia Fault in the 1960s th… Recent seismic activity along this fault system reported by Page and others (1968) suggests that the fault may still be active. Also, the locations of the known faults are not well determined at earthquake depths. Data are from the U.S. Geological Survey (Top, USGS) and the National Earthquake Information Center (Bottom, NEIC). In southeastern New York, from With initial activity in the Late Precambrian - Early Paleozoic age, specifically the Despite the rarity of strong East Coast earthquakes in the United States, there are some that do occur. The Ramapo Fault zone is a system of faults between the northern Appalachian Mountains and Piedmont areas to the east.
[contact-form to=’author@nypost.com’ subject=’NYPost.com Feedback’][contact-field label=’Name’ type=’name’ required=’1’/][contact-field label=’Email’ type=’email’ required=’1’/][contact-field label=’Comment’ type=’textarea’ required=’1’/][/contact-form]But while Americans are aware of the San Andreas fault and the seismic activity in California, which has wreaked havoc in San Francisco and Los Angeles, there are other, lesser-known fault lines in the United States that fly dangerously under the radar. For The Prophecy sees what is, what was, and what always shall be.
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