Dozens of Earthquakes Rattle Southern California as Ground Continues to Shift
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Southern California was shaken by a swarm of earthquakes this week, as at least 40 seismic events struck the region around Holtville in Imperial County over a span of roughly 24 hours. According to the U.S. Geological Survey (USGS), the earthquakes began early Wednesday morning and continued into Thursday, with the strongest registering a magnitude of 4.4.
The first quake was recorded near Holtville at approximately 1:40 a.m. PT on Wednesday. Since then, residents across Southern California reported feeling repeated tremors, with shaking also detected as far away as Arizona and northern Mexico. Hundreds of people submitted shaking reports to the USGS as the swarm unfolded.
The earthquakes ranged in magnitude from 1.1 to 4.4. While many of the smaller quakes were too weak to be felt, those above magnitude 2.5 were noticeable to residents and, in some cases, caused light shaking indoors. Experts note that earthquakes below 2.5 are rarely felt, while those between 2.5 and 5.4 can be felt and may cause minor damage.
Holtville, a small city of about 6,500 residents located roughly 130 miles east of San Diego, sits within one of California’s most active seismic regions. The area lies in the Salton Trough, a geologically young rift valley where the Earth’s crust is slowly pulling apart. This stretching of the crust creates frequent small- to moderate-sized earthquakes, often occurring in clusters known as swarms.
The Salton Trough is part of the larger Baja California Rift Zone, which connects the San Andreas Fault system in the north with spreading centers in the Gulf of California to the south. The region contains a dense network of fault lines, including the Imperial Fault, which are closely linked to the San Andreas system.
Geologists explain that earthquake swarms occur when stress is released across multiple faults rather than along a single fracture. As tectonic plates continue to shift—specifically, as the Pacific Plate moves northwest relative to the North American Plate—the crust in this region thins and fractures, producing repeated seismic activity over hours, days, or even weeks.
While swarms like this are typically not dangerous on their own, scientists caution that they reflect ongoing tectonic stress in a region capable of generating much larger earthquakes. The Imperial Valley has experienced significant seismic events in the past, including a magnitude 6.9 earthquake in 1940 and a magnitude 6.4 quake in 1979, both of which caused widespread damage and led to advances in earthquake engineering and monitoring.
Seismologists continue to monitor the area closely, noting that while most swarms subside without escalation, the interconnected nature of Southern California’s fault systems means the region remains vulnerable to larger earthquakes in the future.
For now, the shaking serves as another reminder of California’s dynamic geology and the powerful forces continually reshaping the landscape beneath residents’ feet.
Source: DailyMail



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