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 220-kilometre (140 mi) 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.[1] The fault zone has been associated with the Eastern Tennessee seismic zone.[2]
References
[edit]- ^ Steltenpohl, Mark G.; Zeitz, Isidore; Horton, J. Wright Jr.; Daniels, David L. (January 27, 2010). "New York–Alabama lineament: A buried right-slip fault bordering the Appalachians and mid-continent North America". Geology. 38 (6): 571–574. doi:10.1130/G30978.1.
- ^ O'Hanlon, Larry (May 28, 2010). "San Andreas-like fault found in eastern U.S." Retrieved August 24, 2011.