A recent study, authored by geologists from the University of Rochester and College of New Jersey, focuses on a block of dense, mafic volcanic rock beneath the bend. The scientists argued that this underground mass forced the mountain chain to shift as it formed hundreds of millions of years ago. As the North American and African plates collided, the North American plate began to fold and thrust upward. However, the mass of volcanic rock became a barrier and forced the mountains to push up around it.
Geologists have known about this mass for some time, but after analyzing new seismic and gravitational data, they concluded that the expanse of volcanic rocks was about 450 kilometers (286 miles) by 100 kilometers (124 miles). “What we didn’t understand was the size of the structure or its implications for mountain-building processes,” said Cynthia Ebinger, one of the study authors.
The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite captured this view of the bend on November 17, 2012. Other physiographic regions are also visible. A portion of the Appalachian Plateau lies to the north of the mountains. The Appalachian Piedmont, a low-elevation plateau in the foothills, lies to the east and transitions into the Atlantic Coastal Plain.
References
- Benoit, M. et al (2014, April 28) Orogenic bending around a rigid Proterozoic magmatic rift beneath the Central Appalachian Mountains. Earth and Planetary Science Letters, 402 (15), 197-208.
- Commonwealth of Pennsylvania Physiographic Provinces of Pennsylvania. Accessed September 17, 2014.
- Geomorphology from Space (1986) Folded Appalachians Accessed September 17, 2014.
- Maryland Geologic Survey Physiographic Map of Maryland. Accessed September 17, 2014.
- University of Rochester (2014, July 18) Bend in Appalachian mountain chain finally explained. Accessed September 17, 2014.
NASA image courtesy Jeff Schmaltz, LANCE MODIS Rapid Response Team at NASA GSFC. Caption by Adam Voiland.
- Instrument(s):
- Aqua - MODIS- NASA
