A 3.9 magnitude earthquake struck 30 miles SE of Charlottesville Virginia.
Magnitude 3.9 VIRGINIA
2003 May 05 16:32:32 UTC
Preliminary Earthquake Report
U.S. Geological Survey, National Earthquake Information Center
World Data Center for Seismology, Denver
Date-Time Monday, May 05, 2003 at 16:32:32 (UTC) - Coordinated Universal Time
Monday, May 05, 2003 at 12:32:32 PM local time at epicenter
Time of Earthquake in other Time Zones
Location 37.75N 78.07W
Depth 5.0 kilometers
Reference 45 km (30 miles) SE of Charlottesville, Virginia
60 km (35 miles) NNE of Farmville, Virginia
60 km (35 miles) WNW of RICHMOND, Virginia
80 km (50 miles) SW of Fredericksburg, Virginia
Location Quality Error estimate: horizontal +/- 15.3 km; depth fixed by location program
Parameters Nst=11, Nph=11, Dmin=78.9 km, Rmss=0.61 sec, Erho=15.3 km, Erzz=0 km, Gp=192.5 degrees
Source USGS NEIC
EARTHQUAKES IN THE CENTRAL VIRGINIA SEISMIC ZONE
Since at least 1774, people in central Virginia have felt small earthquakes and suffered damage from infrequent larger ones. The largest damaging
earthquake in the seismic zone occurred in 1875 (magnitude 4.8). Smaller earthquakes that cause little or no damage are felt each year or two.
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
out to 40 km (25 mi).
Earthquakes everywhere occur on faults within bedrock, usually several 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.
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.
Earthquakes can trigger other earthquakes. The most common triggered earthquakes are the familiar aftershocks that occur in the vicinity of the fault
that ruptured. Additionally, small, distant earthquakes (~1000 km) have been triggered following extremely large earthquakes.
There are no examples of earthquake triggering between events as small and as distant from each other as the recent events in Arkansas, Alabama, and
Virginia. Therefor, the close spacing in time of these events is believed to be purely random.