---------- | Calaveras Fault | North Central South | 54a 54b 54c 54d | 123 km76 miles | | 10% (+8%) || (+17%) || 54% (+32%) |- ---------- |San Jacinto Fault Zone | San Bernardino San Jacinto Valley Stepovers Anza Clark Coyote Creek Borrego Superstition Mtn | 125a 125b 125c 125d 125e 125f 125g | 309 km192 miles | 1918 San Jacinto earthquake | 0% (−14%) || (23%) || 35% (−20%) |- ---------- |Garlock Fault | East Central West | 69a 69b 69c | 254 km158 miles | | 0% (−3%) || (+2%) || 37% (+24%) |- ---------- |Elsinore Fault Zone | Whittier Glen Ivy Stepovers Temecula Julian Coyote Mountains | 126a 126b 126c 126d 126e 126f 126g | 249 km217 miles | 1910 Elsinore earthquake | 1% (−4%)|| (−6%) || 17% (−8%) |- ---------- |} Notes. 1. Adapted from Table 6 in . Values are aggregated from the fault sections comprising each fault. Some sections have higher individual probabilities; see Table 4 in . "M" is moment magnitude (p. 512). 2. These are the six faults for which UCERF2 had enough data to do stress-renewal modeling. The Hayward fault zone and Rodgers Creek fault are treated as a single fault; the San Andreas fault is treated as two sections. 3. UCEF3 fault sections, with links to "participation" maps for each section (outlined in black), showing the rate (in color) that section participates in ruptures with other sections. Participation maps for all fault sections available at http://pubs.usgs.gov/of/2013/1165/data/UCERF3_SupplementalFiles/UCERF3.3/Model/FaultParticipation/ Some faults have had sections added or split since UCERF2. 4. USGS Quaternary Fault and Fold Database fault numbers, with links to summary reports. QFFDB maps are no longer available. 5. Lengths from UCERF-2, Table 4; may vary from QFFDB values. 6. Min. and Max. probabilities correspond to the least and most likely alternatives in the logic tree; the Mean is a weighted average. 7. Slip-rates not included due to variation across sections and deformation models. See figure C21 (below) for an illustration. Methodology California earthquakes result from the Pacific Plate, heading approximately northwest, sliding past the North American continent. This requires accommodation of 34 to 48 millimeters (about one and a half inches) of slippage per year, with some of that taken up in portions of the Basin and Range Province to the east of California. This slippage is accommodated by ruptures (earthquakes) and aseismic creep on the various faults, with the