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garlock fault creeping

People survey the earthquake damage to roads in the Ridgecrest area. The following day, the town of Hollister got a magnitude-4.7 quake. Wendy Bohon, a geologist at the Incorporated Research Institutions for Seismology, told Business Insider that these recent earthquakes are "nothing to be overly concerned about," though. California has experienced a small spate of seismic activity in recent weeks, which has coincided with the 30th anniversary of the magnitude-6.9 Loma Prieta earthquake that damaged the Bay Bridge in 1989. "Creep is our friend," he said. [2], A study published in October 2019 in the journal Science indicated that a part of the Garlock fault slipped after being triggered by the series of earthquakes in the Ridgecrest area which occurred in July 2019. The Garlock Fault, which runs 185 miles from the San Andreas Fault to Death Valley, has not moved much over the past 500 years, the study said. Scientists expect to experience this "Big One" in their lifetimes - though they're not sure where or when. "Earthquakes, both large and small, are part of life in California," Bohon said. But satellite imagery is so precise that it can measure the movement. © ScienceAlert Pty Ltd. All rights reserved. While most of the fault is locked, certain segments[which?] Advertisement The fault is capable of producing a magnitude 8 earthquake, though it’s currently moving at a slow, continuous pace – a process known as “creeping”. Both earthquakes and creep occur when tectonic plates side slide past each other along a fault. [5] It is thought to have been triggered by the Landers earthquake, just two weeks earlier. Instead, the Garlock fault underwent postseismic creep and exhibited a sizeable earthquake swarm. The fault is capable of producing a magnitude 8 earthquake, though it's currently moving at a slow, continuous pace - a process known as "creeping". Even if the earthquakes were to trigger more creeping, that wouldn't necessarily spell disaster. "It's up to all of us to be prepared.". "We don't understand the physics of the process.". Research has pinned the interval between significant ruptures on the Garlock as being anywhere between 200 and 3,000 years, depending on the segment of the fault. Recent aftershocks have headed southeast toward the Garlock fault, a lesser-known fault capable of … The Garlock is not considered to be a particularly active fault, seldom producing any shaking detectable by humans, although it has been known to generate sympathetic seismic events when triggered by other earthquakes and in one instance by the removal of ground water. The Garlock fault is just creeping at a slow pace, without any shaking going on. But thus far, the Garlock Fault hasn’t otherwise budged. An analysis of a large series of earthquakes that rocked Southern California earlier this summer shows that a major fault line quiet for 500 years is now slowly slipping. So when researchers detected strange seismic activity along a major California fault line this week, it prompted a familiar question: Is the Big One coming? "This was the first time that we'd seen this happen.". [4] The most recent notable event in the Garlock Fault Zone was a magnitude 5.7 near the town of Mojave on July 11, 1992. Creep on the Garlock Fault following the Ridgecrest earthquakes was shallow, occurring from the surface to around 300 feet below ground. The discovery marks the first observation, through modern recording tools, of the fault’s “creep,” which is the slow movement of a fault. Why it matters: The fault is capable of producing an 8.0 magnitude earthquake, but it has never previously produced a strong quake or creep. The Garlock Fault has not produced large earthquakes since instrument-keeping began—at least a century—but is considered … The Garlock Fault runs from a junction with the San Andreas Fault in the Antelope Valley, eastward to a junction with the Death Valley Fault Zone in the eastern Mojave Desert. This article was originally published by Business Insider. [6][7][8], Learn how and when to remove this template message, series of earthquakes in the Ridgecrest area, "Seismicity of the Garlock fault, California", "Scientists: Movement Detected Along California Fault That Could Cause an 8-Magnitude Earthquake", "The Big One could trigger series of large earthquakes, study finds", "Unprecedented Movement on Mojave Desert Fault Capable of Magnitude 8.0 Earthquake: Caltech Study", "Unprecedented movement detected on California earthquake fault capable of 8.0 temblor", "Hierarchical interlocked orthogonal faulting in the 2019 Ridgecrest earthquake sequence", Southern California Earthquake Data Center: Faults in Southern California, Rescue Lineament-Bear Mountains fault zone, https://en.wikipedia.org/w/index.php?title=Garlock_Fault&oldid=980078844, Natural history of Kern County, California, Natural history of Los Angeles County, California, Natural history of San Bernardino County, California, Articles needing additional references from August 2020, All articles needing additional references, All articles with specifically marked weasel-worded phrases, Articles with specifically marked weasel-worded phrases from November 2016, Creative Commons Attribution-ShareAlike License, This page was last edited on 24 September 2020, at 13:40. As detailed in the journal Science, the tremors from the earthquake sequence triggered a chain reaction of slips and shocks along the Garlock Fault. The dynamic details of the rupture process during the mainshock are largely unknown, as is the amount of stress needed to bring the Garlock fault to failure. On Thursday, scientists released a study warning that the Garlock fault, which runs through the Mojave Desert in southern California, has been moving for the first time on record. Stretching for 250 kilometers (160 mi), it is the second-longest fault in California, and one of the most prominent geological features in the southern part of the state. In many cases, Allen said, creep reduces the strain on fault lines. "We know that faults talk to one another," Richard Allen, the director of the Seismological Laboratory at the University of California, Berkeley, told Business Insider. In the modern historical record, the 160-mile-long Garlock fault on the northern edge of the Mojave Desert has never been observed to produce either a strong earthquake or even to creep… The bulging of the Garlock fault line in California can be seen from space and it's moving in ways never seen before, raising the question for Californians if it raises the risk of "The Big One." At least one fsection of the fault has shown movement by creep in recent years. [3] Reports in the Los Angeles Times indicated that a magnitude 8 earthquake along the Garlock fault would have the potential for grave disaster. It is named after the historic mining town of Garlock, founded in 1894 by Eugene Garlock and now a ghost town. The northeast- to east-striking Garlock fault of southern California is a major strike-slip fault with a left-lateral displacement of at least 48 to 64 km. In fact, the Hollister earthquake occurred near "the creeping section" of the San Andreas Fault, she added. "The two Ridgecrest earthquakes were fairly large-magnitude earthquakes and they're fairly close to the Garlock fault, so the change that they caused in the stress fields would obviously have an impact.". While most of the fault is locked, certain segments have been shown to move by aseismic creep, which is motion without resulting earthquakes. Aftershocks of the magnitude 7.1 earthquake near Ridgecrest have been creeping into areas close to two major earthquake faults, sparking concern. which is motion without resulting earthquakes.. Relatively few communities lie directly along the Garlock, as it is primarily situated in the desert, with Frazier Park, Tehachapi, Mojave, and Johannesburg being the closest to it. The Garlock Fault is believed to have developed to accommodate the strain between the extensional tectonics of the Great Basin crust and the right lateral strike-slip faulting of the Mojave Desert crust.[1]. 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