WEAVERVILLE, NC — A magnitude 2.0 earthquake struck near Asheville this morning, marking the second earthquake in 24 hours to hit the western North Carolina mountains, though officials say the tremor was too weak to cause any damage.
Second Tremor in a Day Strikes the Mountains
The latest earthquake, recorded by the USGS, occurred at 7:57 a.m. on August 23 near Weaverville, located just north of Asheville, with a recorded depth of 2.2 miles below the surface. The quake’s epicenter was pinpointed at coordinates 35°43’05.4″N, 82°28’33.0″W, placing it in the mountainous terrain northeast of downtown Asheville.
This marks the second recorded earthquake in the area within a single 24-hour window, a notable occurrence for a region that experiences seismic activity far less frequently than more active fault zones elsewhere in the country.
Weak Magnitude Unlikely to Cause Damage
At magnitude 2.0, the earthquake falls well below the threshold typically associated with structural damage, though officials noted some residents in the immediate area may have felt light shaking. Earthquakes of this magnitude are generally only noticeable to people who are stationary indoors or particularly sensitive to ground vibration, and rarely cause any disruption to daily activity.
Mapping of the two recent events shows both centered in the same general area of the Blue Ridge Mountains, with one located near Weaverville and another slightly farther southwest near Waynesville, both within a short distance of the Pisgah National Forest.
Western North Carolina Sees Occasional Seismic Activity
While not a hotspot for major seismic activity, the western North Carolina mountains do experience periodic minor earthquakes tied to ancient geological fault structures beneath the Appalachian range. Communities including Asheville, Hendersonville, and Fletcher sit within the broader region where such minor tremors have occasionally been recorded in recent years…