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  2. Ramapo Fault - Wikipedia

    en.wikipedia.org/wiki/Ramapo_Fault

    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.

  3. Brevard Fault - Wikipedia

    en.wikipedia.org/wiki/Brevard_Fault

    The Brevard Fault Zone is a 700-km [1] long and several km-wide thrust fault that extends from the North Carolina-Virginia border, runs through the north metro Atlanta area, and ends near Montgomery, Alabama. It is an important Paleozoic era feature in the uplift of the Appalachian Mountains. [2]

  4. Northern Appalachians seismic zone - Wikipedia

    en.wikipedia.org/wiki/Northern_Appalachians...

    The Northern Appalachians seismic zone is an active seismic zone in the Appalachian Mountains of eastern North America, extending from New Brunswick southwards into New England and Boston. [1] Both the seismic zone and the resultant Appalachian Mountains were created by the collision of two tectonic plates about 440–480 million years ago ...

  5. Eastern Tennessee seismic zone - Wikipedia

    en.wikipedia.org/wiki/Eastern_Tennessee_seismic_zone

    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 ...

  6. Geology of the Appalachians - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Appalachians

    As Pangea rifted apart a new passive tectonic margin was born, and the forces that created the Appalachian, Ouachita, and Marathon Mountains were stilled. Weathering and erosion prevailed, and the mountains began to wear away. [10] By the end of the Mesozoic, the Appalachian Mountains had been eroded to an almost-flat plain. [10]

  7. Geology of Georgia (U.S. state) - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Georgia_(U.S...

    The Appalachian foreland of Georgia, which lies in the northwest corner of the state, is separated from metamorphic rocks of the western Blue Ridge by the Talladega-Cartersville-Great Smoky fault. The oldest rocks of the foreland include Cambrian-Ordovician stratigraphy of the Chilhowee Group , Shady Dolomite , Rome Formation , Conasauga Group ...

  8. What is the Almanor Fault Zone? Geologist explains region ...

    www.aol.com/news/almanor-fault-zone-geologist...

    A map by the California Geological Survey shows faults near the Lake Almanor area in Plumas County, where a magnitude 5.5 earthquake struck Thursday, May 11, 2023, followed by a magnitude 5.2 ...

  9. Ramapo Mountains - Wikipedia

    en.wikipedia.org/wiki/Ramapo_Mountains

    The Ramapo Mountains are a forested chain of the Appalachian Mountains in northeastern New Jersey and southeastern New York, in the United States. They range in height from 900 to 1,200 feet (270 to 370 m) in New Jersey, and 900 to 1,400 feet (270 to 430 m) in New York.