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This event has been reviewed by a seismologist.
Wednesday, April 11, 2012 at 04:39:12 UTC
Wednesday, April 11, 2012 at 12:39:12 AM at epicenter
Time of Earthquake in other Time Zones
19.4 km (12.1 miles)
10 km (6 miles) E (85°) from Eagleton Village, TN
10 km (6 miles) ESE (116°) from Rockford, TN
10 km (6 miles) SW (215°) from Seymour, TN
22 km (14 miles) SSE (154°) from Knoxville, TN
232 km (144 miles) NNE (13°) from Atlanta, GA
horizontal +/- 0.4 km (0.2 miles); depth +/- 0.8 km (0.5 miles)
NST= 18, Nph= 24, Dmin=16 km, Rmss=0.14 sec, Gp= 86°,
M-type=duration magnitude (Md), Version=B
Southeast U.S. Seismic Network
Earthquake rumbles Maryville night (Maryville is the town directly next to Seymour)
MARYVILLE, Tenn. (WVLT) -- The ground rumbled early Wednesday morning and the U.S. Geological Survey called it 2.3 magnitude earthquake.
The earthquake hit a few miles northeast of Maryville close to the Pea Ridge Rd. and Temple Rd. intersection around 12:40 a.m. Wednesday, according to coordinates provided by the U.S. Geological Survey.
No damage was caused by the earthquake, but the rumble was felt for miles.
EARTHQUAKES IN THE EASTERN TENNESSEE SEISMIC ZONE
The Eastern Tennessee seismic zone extends across Tennessee and northwestern Georgia into northeastern Alabama. It is one of the most active earthquake areas in the Southeast. Although the zone is not known to have had a large earthquake, a few earthquakes in the zone have caused slight damage. The largest known (magnitude 4.6) occurred on April 29, 2003, near Fort Payne, Alabama. Earthquakes too small to cause damage are felt about once a year. Earthquakes too small to be felt are abundant in the seismic zone, and seismographs have recorded hundreds of them in recent decades.
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).
Earthquakes everywhere occur on faults within bedrock, usually miles deep. Most of eastern Tennessee's bedrock originated several hundred million years ago, as the Appalachian Mountains were formed.
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 Eastern Tennessee seismic zone is far from the nearest plate boundaries, which are in the center of the Atlantic Ocean and in the Caribbean Sea. The Eastern Tennessee 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 Eastern Tennessee 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.
When my area got hit by golf ball sized hail 10 years ago, my car was totaled. It looked terrible. I was at a soccer tournament and there were many cars there that took as much damage as mine. We all sat inside a building and watched our cars take a beating. It was a nightmare lol. I got a check from my insurance company and kept the money and left the dents on my car.
Originally posted by Evan_Dood
Edit to add: I could probably go outside right now and count how many cars have hail damage, and it'd easily be in the double digits!