Reading: Earthquake In Los Angeles: 4.1 temblor near Frazier Park linked to Pleito Fault

Earthquake In Los Angeles: 4.1 temblor near Frazier Park linked to Pleito Fault

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A magnitude 4.1 earthquake struck near Frazier Park early Sunday morning and scientists said preliminary analysis points to the Pleito Fault, not the San Andreas Fault or the Garlock Fault. The quake hit at 3:38 a.m., about 1 mile east-southeast of Frazier Park, at a depth of roughly 8 miles.

That matters because the shaking was felt in Southern California, and the fault call cuts against the online guess that this was some new jolt at the meeting point of the San Andreas and Garlock systems. Seismologists said the event did not appear to have occurred on either major fault, even though those two names often dominate any earthquake conversation in the region.

The Southern California Seismic Network said the Pleito Fault was the likelier source because the quake’s location fit a smaller structure west of Interstate 5 near Frazier Park better than the larger faults that sit nearby. The San Andreas Fault passes just southwest of Frazier Park, while the Garlock Fault lies farther to the east, so a location only about a mile east-southeast of town made the smaller fault a cleaner fit for the preliminary read.

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Several aftershocks followed, including a magnitude 3.2 quake later Sunday morning. Scientists said that kind of sequence is not unusual after a magnitude 4 earthquake, and smaller aftershocks can continue for days or even weeks after the first event. In other words, the ground may keep answering back even after the main jolt has passed.

The broader picture is less dramatic than the speculation that spread online. The Frazier Park area sits in a complicated fault network, and that complexity can make every sharp shake look like the start of something bigger. But the size of this quake, and the preliminary fault link, point instead to a relatively common earthquake in Southern California rather than a clear sign that the major neighboring faults were moving.

What comes next is the same thing seismologists watch after almost every moderate quake: whether the aftershocks stay small and fade with time. For now, the best reading is straightforward — the 4.1 quake near Frazier Park was real, it was felt, and it appears to have come from the Pleito Fault rather than the San Andreas Fault or the Garlock Fault.

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