New York–Alabama Lineament
The New York–Alabama Lineament is a magnetic anomaly in the geology of eastern North America running from Alabama to New York. The lineament is defined by discontinuities in aeromagnetic measurements indicating an approximately  displacement of buried geologic structures along this line. The displacement is attributed to the presence of a deeply buried strike-slip fault, possibly dating to the general time of the Grenville orogeny. The lineament was first described in 1978. The fault zone has been associated with the Eastern Tennessee Seismic Zone. References

Geology of Alabama
Geology of Tennessee
Geology of West Virginia
Geology of Pennsylvania
Geology of New York (state)
Magnetic anomalies
Seismic faults of the United States