Background
Since at least 1774, people in central
Virginia have felt small earthquakes and suffered damage from infrequent
larger ones. The largest damaging earthquake (magnitude 5.9 with a Modified
Mercalli Intensity of VII) occured on August 23, 2011. The second largest
damaging earthquake (magnitude 4.8) in the seismic
zone occurred in 1875. Smaller earthquakes that cause little or no damage
are felt each year or two.
Huge "Felt Areas" of Eastern Earthquakes
Earthquakes in the central and eastern U.S., although less frequent than in
the western U.S., are typically felt over a much broader region. East of the
Rockies, an earthquake can be felt over an area as much as ten times larger
than a similar magnitude earthquake on the west coast. A magnitude 4.0
eastern U.S. earthquake typically can be felt at many places as far as 100
km (60 mi) from where it occurred, and it infrequently causes damage near
its source. A magnitude 5.5 eastern U.S. earthquake usually can be felt as
far as 500 km (300 mi) from where it occurred, and sometimes causes damage
as far away as 40 km (25 mi).
"Felt Area" of the August 23, 2011 Earthquake
A compilation of news reports from various sources indicates that the August 23, 2011 earthquake was felt in at least 22 states (New Jersey, New York,
Pennsylvania, Delaware, Maryland, Virginia, West Virginia, North Carolina, South
Carolina, Tennessee, Kentucky, Ohio, Massachusetts, Rhode Island, Connecticut,
Vermont, New Hampshire, Maine, Indiana, Georgia, Florida) plus The District of Colombia.
Virginia Bedrock History
Earthquakes everywhere occur on faults within bedrock, usually miles deep.
Most bedrock beneath central Virginia was assembled as continents collided
to form a supercontinent about 500-300 million years ago, raising the
Appalachian Mountains. Most of the rest of the bedrock formed when the
supercontinent rifted apart about 200 million years ago to form what are now
the northeastern U.S., the Atlantic Ocean, and Europe.
Virginia Earthquakes Occur on Subsurface Faults
At well-studied plate boundaries like the San Andreas fault system in
California, often scientists can determine the name of the specific fault
that is responsible for an earthquake. In contrast, east of the Rocky
Mountains this is rarely the case. The Central Virginia Seismic Zone is far
from the nearest plate boundaries, which are in the center of the Atlantic
Ocean and in the Caribbean Sea. The seismic zone is laced with known faults
but numerous smaller or deeply buried faults remain undetected. Even the
known faults are poorly located at earthquake depths. Accordingly, few, if
any, earthquakes in the seismic zone can be linked to named faults. It is
difficult to determine if a known fault is still active and could slip and
cause an earthquake. As in most other areas east of the Rockies, the best
guide to earthquake hazards in the seismic zone is the earthquakes
themselves.
Find it on Geology.com
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| Two distinct seismic zones are located in Virginia. The Central Virginia
Seismic Zone and the Giles County Seismic Zone. Both of these zones produce
recurrent small earthquakes at least every few years. Map by USGS, click map to enlarge. |
| Although occasional earthquakes occur in the Central Virginia Seismic Zone and the Giles County Seismic Zone
the earthquake hazard in these areas is much lower than in other parts of the
United States. Map by USGS, click map to enlarge. |
|
