WebThe 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. Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present.. The fall line marks the geologic boundary of hard metamorphosed terrain—the product of … WebJan 1, 1992 · The Hollister fault zone outcrops in southeastern Virginia and in northeastern North Carolina and is an important constituent of the eastern Piedmont fault system. The Hollister fault zone is a steeply westward dipping, north-south trending D[sub 3] ductile mylonite zone that has an average width of less than 1/2 km. It is a dextral strike-slip ...
(PDF) Eastern Piedmont fault system: Speculations on its extent
WebThree subparallel zones constitute the northeast-trending Inner Piedmont belt in South Carolina and northeastern Georgia. The Inner Piedmont core defines the axis and consists of an assemblage of sillimanite-grade rocks, including mica schist, biotite gneiss, granitoid gneiss, and minor amphibolite. The core is bounded by two flanks of kyanite ... WebJan 1, 1977 · The EPFS comprises multiple geophysically inferred faults (prominent elongate magnetic anomalies related to ductile deformation during the Paleozoic) … northern finance association
Earthquakes: Why are they happening in South Carolina? - WRDW
http://people.uncw.edu/lamaskint/GEO%20501%20FALL%202415/Blake%20et%20al%202412%20GSA%20Field%20Guide%20NC.pdf WebJul 1, 2024 · The Elgin and Lugoff area lie on top of an ancient fault line called the Eastern Piedmont Fault System. It is unlikely that this fault zone will produce a larger earthquake. WebDownload scientific diagram Revised intensity map of the January 1, 1913, Union County earthquake with intensity contours in the Modified MercalAeromagnetic image of South Carolina and Georgia. northern film studios