Earthquake on the east coast

I was having a meeting at work when all of a sudden the floor started to shake.  Of course of all people nervous nelly Kurt was in my office.  It felt like it went on for 15 seconds.  My co worker said that's construction but I knew it wasn't a shake that bad and off & on.  We knew it was a earthquake.  When do we get earthquakes on the east coast, not usual so I was nervous.  We are located on the 21st floor in New York city so people thought it was terrorism.  I took my stuff and ran down the stairs outside where I just assumed I would be safe but Riviera was the only office outside.  If the building went down I was going to be in it.  I text Josh right away that I loved him and was almost in tears.  Maybe it's a 9-11 thing I just get so nervous anything can happen.  Of course the phone lines were backed up so I couldn't talk to anyone.  My sister text me as well as my mother. It was confirmed on facebook that it was a earthquake that started in Virgina.  It was amazing that so many states miles away felt this tremor.  That was one scary experience.  Luckily Debbie and the girls didn't feel it because I think if you experience something like that it's really scary.

Below is the article from that day.


Magnitude 5.8 - VIRGINIA


2011 August 23 17:51:04 UTC

DetailsSummaryMapsScientific & TechnicalAdditional InfoEarthquake DetailsThis event has been reviewed by a seismologist.Magnitude 5.8

Date-Time Tuesday, August 23, 2011 at 17:51:04 UTCTuesday, August 23, 2011 at 01:51:04 PM at epicenter Time of Earthquake in other Time Zones

Location 37.936°N, 77.933°W

Depth 6 km (3.7 miles)

Region VIRGINIA

Distances 8 km (5 miles) SSW (195°) from Mineral, VA11 km (7 miles) SSE (148°) from Louisa, VA29 km (18 miles) NE (45°) from Columbia, VA61 km (38 miles) NW (317°) from Richmond, VA135 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 ID se082311a

Did you feel it? Report shaking and damage at your location. You can also view a map displaying accumulated data from your report and others.

Earthquake Summary

Earthquake Summary Poster



Felt Reports

Widespread damage occurred from central Virginia to southern Maryland including the Washington D.C. area. Minor damage reported in parts of Delaware, southeastern Pennsylvania and southern New Jersey. Felt (VII) at Boston, Bumpass, Kent Store, Louisa, Mineral, Rhoadsville and Summerduck. Felt strongly in much of central Virginia and southern Maryland. Felt throughout the eastern US from central Georgia to central Maine and west to Detroit, Michigan and Chicago, Illinois. Felt in many parts of southeastern Canada from Montreal to Windsor.



Tectonic Summary

The Virginia earthquake of 2011 August 23 occurred as reverse faulting on a north or northeast-striking plane within a previously recognized seismic zone, the "Central Virginia Seismic Zone." The Central Virginia Seismic Zone has produced small and moderate earthquakes since at least the 18th century. The previous largest historical shock from the Central Virginia Seismic Zone occurred in 1875. The 1875 shock occurred before the invention of effective seismographs, but the felt area of the shock suggests that it had a magnitude of about 4.8. The 1875 earthquake shook bricks from chimneys, broke plaster and windows, and overturned furniture at several locations. A magnitude 4.5 earthquake on 2003, December 9, also produced minor damage.



Previous seismicity in the Central Virginia Seismic Zone has not been causally associated with mapped geologic faults. Previous, smaller, instrumentally recorded earthquakes from the Central Virginia Seismic Zone have had shallow focal depths (average depth about 8 km). They have had diverse focal mechanisms and have occurred over an area with length and width of about 120 km, rather than being aligned in a pattern that might suggest that they occurred on a single causative fault. Individual earthquakes within the Central Virginia Seismic Zone occur as the result of slip on faults that are much smaller than the overall dimensions of the zone. The dimensions of the individual fault that produced the 2011 August 23 earthquake will not be known until longer-term studies are done, but other earthquakes of similar magnitude typically involve slippage along fault segments that are 5 - 15 km long.



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).