1/3/2024 0 Comments Reflection lake san jacinto![]() All of these observations suggest that the San Jacinto stepover, which has been used as the primary basis for segmenting the northern San Jacinto fault zone, is being bypassed and that the fault zone may now be capable of larger earthquakes than previously expected. Address, Phone Number, and Hours for Reflection Lake RV Park, a RV Park, at Cottonwood Avenue, San Jacinto CA. ![]() Name Reflection Lake RV Park Address 3440 Cottonwood Avenue San Jacinto, California, 92582 Phone 95 Hours Open Daily 12:00 AM-11:59 PM. Finally, new paleoseismic data from the Mystic Lake site suggest that some late Holocene earthquakes may have jumped the stepover. Address, Phone Number, and Hours for Reflection Lake RV Park, a RV Park, at Cottonwood Avenue, San Jacinto CA. Seismicity observations suggest the presence of many faults within the stepover zone. Numerous tectono‐geomorphic features observed in satellite and Light Detection and Ranging Digital Elevation Model (LiDAR DEM) imagery are interpreted to delineate the location of the currently active faults, including a zone of faults that cut across the basin from the northern end of the Casa Loma fault to the Claremont fault. Previous seismic‐reflection data also suggest the presence of a young fault that cuts basin strata beneath the middle of Mystic Lake farther west of our study area. San Jacinto, CA, is notable for being home to many dairy farms and is. Multiple faults are inferred from the CPT data within a small sag at the northeast side of the stepover that cuts through younger stratigraphy to the west of the basin‐bounding fault near Mystic Lake. Learn about living in and moving to San Jacinto. Our new cone penetration test (CPT) and trench observations along the Claremont fault at Mystic Lake indicate that the main strand of the Claremont fault has jumped nearly a half kilometer westward into the San Jacinto releasing stepover during the late Quaternary. We investigate a releasing stepover between the Casa Loma and Claremont strands of the northern San Jacinto fault zone to evaluate the late Quaternary structural evolution of the fault zone, and to assess the likelihood of a rupture jumping across the stepover. ![]()
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