Magnitude 3.9 earthquake near Meter and Stillmore, did you feel it?

At approximately 4:00 AM this morning, an earthquake occurred near Metter and Stillmore, more specifically 7 km east of Stillmore. According to the USGS, the volume was 3.9 megawatts (amount of moment).

The Charleston National Weather Service tweeted that people reported feeling “shake” in Savannah, Bluffton and Statesboro, and as far away as Columbia, Augusta, Warner Robins and Atlanta. Did you feel it? If so, you can fill out the report form about your experience here.

USGS 06182022 stillmore earthquake meter USGS 06182022 stillmore earthquake meter USGS

Earthquake information from USGS:

Earthquakes east of the Rockies, although less frequent than in the west, are usually felt over a much wider area than earthquakes of similar size in the west. East of the Rocky Mountains, an earthquake can be felt in an area ten times larger than a similar earthquake on the West Coast.

Most earthquakes in North America east of the Rocky Mountains occur as a fault within the rock, usually miles deep. However, a few earthquakes east of the Rocky Mountains have been linked to particular geological faults, unlike the situation at plate boundaries such as the San Andreas fault system in California, where scientists can use geological evidence to determine which fault has resulted in a major fault. An earthquake that is likely to produce major earthquakes in the future. Scientists who study earthquakes in eastern and central North America often operate from the hypothesis that modern earthquakes occur as a result of slipping on pre-existing faults that formed in earlier geologic ages and reactivated under current stress conditions. However, bedrock in eastern North America is riddled with faults that were active in earlier geological eras, and few of these faults are known to have been active in the current geological age. In most areas east of the Rockies, the potential for future harmful earthquakes is currently estimated by the frequencies and magnitudes of machine-recorded earthquakes or earthquakes documented in historical records.

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