1. Magnitude 5.8 - VIRGINIA 2011 August 23 17:51:03 UTC Department of Geology and Planetary Science, University of Pittsburgh Seismic records from the University of Pittsburgh Seismograph included

2. 3 component

4. Magnitude 5.8 Magnitude5.9 Date-Time Tuesday, August 23, 2011 at 17:51:03 UTC Tuesday, August 23, 2011 at 01:51:03 PM at epicenter Location37.975°N, 77.969°W Depth1 km (~0.6 mile) (poorly constrained) RegionVIRGINIA Distances 45 km (27 miles) E of Charlottesville, Virginia 55 km (34 miles) SW of Fredericksburg, Virginia 64 km (39 miles) NW of RICHMOND, Virginia 82 km (50 miles) NNE of Farmville, Virginia Location Uncertainty horizontal +/- 10.9 km (6.8 miles); depth +/- 7.4 km (4.6 miles) Parameters NST=390, Nph=390, Dmin=57.9 km, Rmss=1.17 sec, Gp= 47°, M-type=regional moment magnitude (Mw), Version=6 Source Magnitude: USGS NEIC (WDCS-D) Location: USGS NEIC (WDCS-D) Event IDusc0005ild Magnitude5.8 Date-Time Tuesday, August 23, 2011 at 17:51:04 UTC Tuesday, August 23, 2011 at 01:51:04 PM at epicenter Time of Earthquake in other Time Zones Location37.936°N, 77.933°W Depth6 km (3.7 miles) RegionVIRGINIA Distances 8 km (5 miles) SSW (195°) from Mineral, VA 11 km (7 miles) SSE (148°) from Louisa, VA 29 km (18 miles) NE (45°) from Columbia, VA 61 km (38 miles) NW (317°) from Richmond, VA 135 km (84 miles) SW (217°) from Washington, DC Location Uncertainty horizontal +/- 2.3 km (1.4 miles); depth +/- 3.1 km (1.9 miles) Parameters NST= 22, Nph= 23, Dmin=50 km, Rmss=0.44 sec, Gp= 79°, M-type=centroid moment magnitude (Mw), Version=B Source Southeast U.S. Seismic Network Event IDse082311a Initial EstimateSix hours after earthquake

5. Virginia earthquake history 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 (magnitude 4.8) in the seismic zone occurred in 1875. 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 as far away as 40 km (25 mi). FAULTS 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. 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.

6. Thrust mechanism is estimated for this earthquake by quake.usgs.gov

8. Immediately following earthquake 6 hours after earthquake

10. Peak acceleration and Peak Velocity

11. Plate tectonic motion: The cause of earthquakes

12. Some details Approximate energy release, 7.6 kt (kilotons) Number of 5.0 to 5.9 earthquakes (globally), approximately 800 per year. Approximate North America Plate motion 16.2 mm/yr to the West in our region. ModelLatitudeLongitude Speed mm/yr Azimuth (cw from N) N Vel. mm/yr E Vel. mm/yr Plate (referenc e) GSRM v1.2 40° 26' 26" N 40.44055 6° 79° 59' 49" W - 79.99694 4° 14.93272.36°0.61-14.91NA(NNR)

13. Richter Scale

17. Variation of earthquake shaking with increased distance from the epicenter From: Geotechnical Earthquake Engineering By Ikuo Towhata

18. Variation of earthquake shaking with increased distance from the epicenter From: Geotechnical Earthquake Engineering By Ikuo Towhata