Intraplate Earthquakes
An intraplate earthquake occurs within the interior of a tectonic plate rather than at its boundary.
Over geological time, tectonic forces create zones of weakness within plates, including ancient faults and rift zones, which can later become sites of intraplate earthquakes.
One example is the 2011 Virginia earthquake, which occurred in the Central Virginia Seismic Zone. This quake happened along the Spotsylvania fault, an ancient fault line in the middle of the North American plate.
This region was once part of an active plate boundary during the formation of Pangaea hundreds of millions of years ago. These tectonic processes contributed to the uplift of the Appalachian Mountains.
The Washington Monument, Washington National Cathedral, and other historic structures in Washington, D.C., sustained damage in the Virginia earthquake and required extensive repairs.
Another area prone to intraplate earthquakes is the New Madrid Seismic Zone, located in the central U.S. This region experienced the massive 1812 New Madrid earthquake, which had a magnitude of 7.5 and even altered the course of the Mississippi River.
An intraplate earthquake occurs within the interior of a tectonic plate rather than at its boundary.
Over geological time, tectonic forces create zones of weakness within plates, including ancient faults and rift zones, which can later become sites of intraplate earthquakes.
One example is the 2011 Virginia earthquake, which occurred in the Central Virginia Seismic Zone. This quake happened along the Spotsylvania fault, an ancient fault line in the middle of the North American plate.
This region was once part of an active plate boundary during the formation of Pangaea hundreds of millions of years ago. These tectonic processes contributed to the uplift of the Appalachian Mountains.
The Washington Monument, Washington National Cathedral, and other historic structures in Washington, D.C., sustained damage in the Virginia earthquake and required extensive repairs.
Another area prone to intraplate earthquakes is the New Madrid Seismic Zone, located in the central U.S. This region experienced the massive 1812 New Madrid earthquake, which had a magnitude of 7.5 and even altered the course of the Mississippi River.
An intraplate earthquake occurs within the interior of a tectonic plate rather than at its boundary.
Over geological time, tectonic forces create zones of weakness within plates, including ancient faults and rift zones, which can later become sites of intraplate earthquakes.
One example is the 2011 Virginia earthquake, which occurred in the Central Virginia Seismic Zone. This quake happened along the Spotsylvania fault, an ancient fault line in the middle of the North American plate.
This region was once part of an active plate boundary during the formation of Pangaea hundreds of millions of years ago. These tectonic processes contributed to the uplift of the Appalachian Mountains.
The Washington Monument, Washington National Cathedral, and other historic structures in Washington, D.C., sustained damage in the Virginia earthquake and required extensive repairs.
Another area prone to intraplate earthquakes is the New Madrid Seismic Zone, located in the central U.S. This region experienced the massive 1812 New Madrid earthquake, which had a magnitude of 7.5 and even altered the course of the Mississippi River.
View the full transcript and gain access to JoVE Core videos