This web site may reference real estate listing(s) held by a brokerage firm other than the broker and/or agent who owns this web site. Property information referenced on this web site comes from the Internet Data Exchange (IDX) program of the MLS. Any dissemination of this information is in violation of copyright laws and is strictly prohibited. The data contained herein is copyrighted by CRMLS, CLAW, I-Tech, ROWMLS, GPSMLS, SDMLS, VCRDS/PFAR, Idyllwild Association of Realtors, Ojai Valley Board of REALTORS and/or AVMLS is protected by all applicable copyright laws. Information being provided is for the visitor’s personal, noncommercial use and may not be used for any purpose other than to identify prospective properties visitor may be interested in purchasing. ![]() Listing Courtesy of Eva Raleigh, Broker, Eva Raleigh, DRE #01826907īased on information from one of the following Multiple Listing Services: CRMLS, CLAW, I-Tech, ROWMLS, GPSMLS, SDMLS, VCRDS/PFAR, Idyllwild Association of Realtors, Ojai Valley Board of REALTORS and/or AVMLS. Photos may be virtually staged or digitally enhanced and may not reflect actual property conditions. They identified signs of three earthquake events in the past 2,000 years, based on radiocarbon and pollen dating.No guarantee, warranty or representation of any kind is made regarding the completeness or accuracy of descriptions or measurements (including square footage measurements and property condition), such should be independently verified, and Compass expressly disclaims any liability in connection therewith. ![]() To get evidence of potential shared earthquakes, Rodríguez Padilla and colleagues hand-dug a trench 15 meters long and 1.5-3 meters deep into the Lytle Creek Ridge Fault. The Lytle Creek Ridge Fault does not itself do any work during these shared earthquakes, just acting as a passive marker, Rodríguez Padilla said. This fault would slip only when there is an earthquake shared across the two bigger faults. "However, prior to our study, there was no direct physical evidence that these joint ruptures, or shared earthquakes, do in fact occur," Rodríguez Padilla said.īetween the south end of the San Andreas Fault and the northern end of the San Jacinto lies a small fault, the Lytle Creek Ridge Fault. But researchers previously have shown that it's theoretically possible for an earthquake to transfer from one fault to another where they come close together at Cajon Pass, north of Los Angeles, she said. ![]() "Typically, we think earthquakes will remain confined to a single fault, especially for "mature" faults such as the San Andreas and the San Jacinto, which are well-established, geometrically simple plate boundary faults," Rodríguez Padilla said. However, each of these faults on their own can generate a large-magnitude (7.5 or above) earthquake, said Alba Rodríguez Padilla, a graduate student at UC Davis and first author on the paper. Large earthquakes involving multiple faults increase the threat of strong ground shaking.
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