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U.S. Geological Survey Final Technical Report

Award No. G12AP20066 Recipient: University of at Santa Barbara

Mapping the 3D Geometry of Active Faults in

Craig Nicholson1, Andreas Plesch2, John Shaw2 & Egill Hauksson3 1Marine Science Institute, UC Santa Barbara 2Department of Earth & Planetary Sciences, Harvard University 3Seismological Laboratory, California Institute of Technology

Principal Investigator: Craig Nicholson Marine Science Institute, University of California MC 6150, Santa Barbara, CA 93106-6150 phone: 805-893-8384; fax: 805-893-8062; email: [email protected]

01 April 2012 - 31 March 2013

Research supported by the U.S. Geological Survey (USGS), Department of the Interior, under USGS Award No. G12AP20066. The views and conclusions contained in this document are those of the authors, and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government.

1

Mapping the 3D Geometry of Active Faults in Southern California

Abstract Accurate assessment of the seismic hazard in southern California requires an accurate and complete description of the active faults in three dimensions. Dynamic rupture behavior, realistic rupture scenarios, segmentation, and the accurate prediction of fault interactions and strong ground motion all strongly depend on the location, sense of slip, and 3D geometry of these active fault surfaces. Comprehensive and improved catalogs of relocated for southern California are now available for detailed analysis. These catalogs comprise over 500,000 revised hypocenters, and nearly 200,000 well-determined earthquake focal mechanisms since 1981. These extensive catalogs need to be carefully examined and analyzed, not only for the accuracy and resolution of the earthquake hypocenters, but also for kinematic consistency of the spatial pattern of fault slip and the orientation of 3D fault surfaces at seismogenic depths. The system in southern California has a high probability of generating a major damaging earthquake. How big, when and where such an event will occur appears to depend on subtle, second-order variations in stress, strength and fault geometry, such as fault bends, offsets, changes in fault dip, or other fault discontinuities that seem to control fault segmentation and rupture behavior. As demonstrated by recent large earthquakes, rupture along major through-going faults in southern California can be quite complex, and strongly affected by both local fault geometry and the interaction with adjacent secondary structures, such as sub-parallel fault strands, left-lateral conjugate cross faults, tear faults, and low-angle basal detachments. Identification of these features, especially at seismogenic depths, often depends on careful kinematic analysis of the earthquake hypocenters and focal mechanisms in both space and time. For this project and in close collaboration with other members of the SCEC Community Model Development Team, detailed analysis of well-determined earthquake locations and focal mechanism slip planes was used to define the geometry of active subsurface faults and to create improved, more accurate, updated digital 3D fault surface models for the SCEC Community Fault Model (CFM). Newly revised 3D models for several major fault zones, including sections of the San Andreas from Parkfield to the , San Jacinto, Elsinore-, Agua Tibia-Earthquake Valley, Garlock, Imperial-Brawley, Landers-Joshua Tree, San Gabriel, Oak Ridge-Northridge and the San Fernando/Sierra Madre faults, as well as for several major intervening cross faults, were developed. Special attention and more detailed studies were conducted in areas of particularly complex fault geometry. This included the San Gorgonio Pass region along the San Andreas fault zone, and the Laguna Salada and adjacent Sierra Cucapah region highlighted by the 2010 M7.2 El Mayor- Cucapah sequence. These new models allow for more non-planar, multi-stranded 3D fault geometry, including changes in dip and dip direction along strike and down dip, based on the changing patterns of earthquake hypocenter and focal-mechanism nodal plane alignments, rather than projecting faults to depth assuming a constant (often vertical) dip and dip direction, as was the case for many of the previous preliminary fault models in CFM. In addition, the CFM database was reorganized with a new hierarchical name and numbering system that allows CFM to properly organize, name and number the increasing variety and complexity of modeled, multi-stranded principal slip surfaces and associated secondary faults. These new CFM fault surfaces describe a more complex pattern of interacting fault sets at depth accommodating crustal deformation in southern California, and have already provided the basis for improved dynamic rupture models, variable fault slip rate models, and correlations with associated regional topography along major active faults of the San Andreas fault system. 2

Introduction Accurate assessment of the earthquake hazards in southern California requires accurate and complete 3D fault maps. Many aspects of seismic hazard evaluation, including understanding earthquake rupture and geodetic strain, developing credible earthquake rupture scenarios, modeling geodetic and geologic fault slip rates, or predicting strong ground motion, are all strongly dependent on accurately resolving the 3D geometry of active faults at seismogenic depths [Herbert and Cooke, 2012; Lindsey et al., 2012, Oglesby and Mai, 2012; Shi et al., 2012]. In southern California, these structures can be quite complex and include both relatively high-angle strike-slip and oblique-slip faults—many of which intersect and are mapped at the surface, as well as low-to-moderate-angle faults, some of which are blind and are difficult to identify. The 1994 M6.7 Northridge earthquake was on one such blind fault and produced over $40 billion in damage. Because of this, both the Southern California Earthquake Center (SCEC) and US Geological Survey NEHRP have consistently targeted the identification and mapping in 3D of active faults in southern California as a primary research objective. The purpose of this project was to provide just such improved, more detailed, updated digital 3D fault representations of major faults in southern California for input into the online SCEC Community Fault Model (CFM) and USGS Quaternary Fault Database (Qfault). Recently, a considerable effort has been focused on developing improved catalogs of earthquake hypocenters and focal mechanism solutions for southern California (e.g., Fig.1) [e.g., Lin et al., 2007; Hauksson et al., 2012; Yang et al., 2012]. These catalogs comprise over 500,000 relocated hypocenters and nearly 200,000 well-determined earthquake focal mechanisms since 1981. These extensive catalogs need to be carefully examined and analyzed—not only for the accuracy and resolution of the earthquake hypocenters [e.g., Richards-Dinger and Ellsworth, 2001]—but also for the spatial pattern of fault slip and the orientation of 3D fault surfaces. As demonstrated by the 2010 M7.2 El Mayor-Cucapah earthquake and other events, rupture along major through-going faults in southern California can be quite complex and strongly affected by both local fault geometry and the interaction with adjacent secondary structures, such as sub-parallel fault strands, left-lateral cross faults, and basal detachments [e.g., Nicholson et al., 1986; Hudnut et al., 1989; Seeber and Armbruster, 1995; Nicholson, 1996; Carena et al., 2004; Lin et al., 2007; Nicholson et al., 2009, 2011, 2012; Hudnut et al., 2010; Fletcher et al., 2010]. Identification of these important fault features prior to a major earthquake, especially at seismogenic depths, often depends on careful analysis of microearthquake hypocenters and focal mechanisms in both space and time. To help address these issues, this project was part of an on-going, multi-year collaborative effort within SCEC to systematically upgrade and improve the Community Fault Model (CFM). Since 2010 and working in close cooperation with Andreas Plesch, John Shaw, and Egill Hauksson, we have continued to make steady and significant improvements to the CFM and its associated fault database [Nicholson et al., 2010, 2011, 2012; Plesch et al., 2010]. These improvements include more detailed and complex 3D representations of major active fault systems (Fig.1), additional detailed fault surface trace data, and finalization of our new naming and numbering scheme for CFM that allows for closer links to the USGS Qfault database. A systematic revision of CFM fault models was triggered by unexpected discrepancies between previous CFM-v.3 fault representations and the newer Qfault surface traces, as well as by the availability of the extensive relocated earthquake catalogs to better define the complex subsurface geometry of active faults. Although a draft version of CFM-v.4 was sent out for review and comment, this upgrade to CFM-v.4 is not yet complete. Many fault models in CFM-v.3 still need to be re-registered to the more detailed Qfault surface traces and, together with recent relocated hypocenters, require newer, more complex and more realistic 3D fault models for CFM. Such on-going efforts to update the 3D fault set for CFM are critical to the USGS NEHRP research priorities. This is because better knowledge of active 3D 3 fault geometry and improved 3D fault representations are fundamental to a better understanding of both fault kinematics and earthquake rupture dynamics, and are essential to improved computations of accurate strong ground motion predictions and seismic hazard assessments.

Figure 1. Oblique 3D view looking NE of new, revised CFM-v.4 fault representations developed in 2011 and 2012, plus Qfault surface traces (red lines), and relocated seismicity (dots color-coded by depth) [Nicholson et al., 2011; 2012]. New CFM 3D faults are now registered to the Qfault surface traces and major strike-slip faults are no longer assumed to be vertical, but change dip and dip direction along strike and with depth to better correlate with the relocated hypocenters. Seismicity from Hauksson et al. [2012]. Offshore Carlsbad, Coronado Bank, and Descanso faults recently provided to CFM by Chris Sorlien [Bennett et al., 2012].

Thus, the purpose of this project was primarily to continue our on-going evaluation of active 3D fault geometry and development of new, updated digital 3D fault representations for CFM. In areas of unusually complex fault geometry, like San Gorgonio Pass or the El Mayor-Cucapah rupture, this project also allowed for more detailed studies of the active subsurface faults to be conducted. As a result, substantial progress was made on implementing newly revised 3D models for several major fault zones, including sections of the San Andreas from Parkfield to the Salton Sea, San Jacinto, Elsinore-Laguna Salada, Agua Tibia-Earthquake Valley, Garlock, Imperial-Brawley, Landers- Joshua Tree, San Gabriel, Oak Ridge-Northridge and the San Fernando/Sierra Madre faults, as well as for several major intervening cross faults (Fig.1) [Nicholson et al., 2012]. These new models allow for more non-planar, multi-stranded 3D fault geometry, including changes in dip and dip direction along strike and down dip, based on the changing patterns of earthquake hypocenter and focal-mechanism nodal plane alignments, rather than projecting faults to depth assuming a constant (often vertical) dip and dip direction, as is the case for many of the previous preliminary fault models in CFM-v.3. Where these faults intersect the surface, the new 3D fault models are also now properly registered to both USGS DEM and Qfault surface traces [Bryant, 2005; USGS, 2006]. In addition to updating 3D fault models for CFM, we, together with Tom Rockwell, Jerry Treiman and others have finalized a new CFM fault database hierarchical naming and numbering scheme. This allows CFM to properly organize, name and number the increasing variety and complexity of modeled, multi-stranded principal slip surfaces and associated secondary faults, while maintaining more consistency with fault nomenclature from the CGS Fault Activity database. 4 Data and Methods The primary data sets used in this and related SCEC projects are the most recent, revised catalogs of relocated earthquake hypocenters and earthquake focal mechanism solutions [Hauksson et al., 2012; Yang et al., 2012], plus USGS Digital Elevation Models of surface topography, and mapped Quaternary fault surface traces (Qfault)[Bryant, 2005; USGS, 2006]. All of these data sets are readily available online. The revised earthquake hypocenters were calculated using a procedure that involved initial relocations with absolute travel-times, source-specific station terms and a 3D velocity model, waveform cross-correlation to improve clustering and identify related earthquake pairs, and differential travel times from cross-correlated pairs to determine relative relocation within clusters [Hauksson and Shearer, 2005; Shearer et al., 2005; Lin et al., 2007; Hauksson et al., 2012]. Focal mechanisms were then determined from these revised earthquake hypocenters using both P- wave first-motions and S/P amplitude ratios [Hardebeck and Shearer, 2003; Yang et al., 2012]. For faults associated with the recent 2010 El Mayor-Cucapah sequence, the zone, or found in the Sierra Cucapah and Yuha Desert area, we had supplemental fault surface trace maps and InSAR fault models courtesy of John Fletcher, Ken Hudnut, Jerry Treiman, and Mike Oskin [e.g., Fletcher et al., 2010; Treiman et al., 2010; Teran et al., 2011; Oskin et al., 2012]. In addition, sets of surface geologic maps, interpreted geologic cross sections and subsurface structure contour maps of stratigraphic reference horizons were used where available to help define near-surface and subsurface fault geometry in the shallow section of the fault that often exhibits little or no seismicity. These maps and cross sections are based on integrated correlations of surface geologic mapping, industry well logs and seismic reflection data [c.f., Yeats et al, 1977; Yeats, 1987, 2001; Wright, 1991; Hopps et al., 1992; Huftile and Yeats, 1995; Tsutsumi and Yeats, 1999] and can often provide geologic control of subsurface fault geometry to depths of 3 to 4 km. Similar geological and geophysical data sets, as well as maps and cross sections are also available for offshore structures [c.f., Kamerling et al., 1998, 2003; Sorlien and Kamerling, 2000; Sorlien et al., 1998, 2000, 2006, 2013; Redin et al., 2005; Nicholson et al., 2007, 2011; Hubbard, 2011; Marshall et al., 2012], and were used to generate digital 3D fault models for inclusion in CFM (Fig.1) [Kamerling et al., 2001; Schindler et al., 2007; Bennett et al., 2012]. Many of these once proprietary industry well files and seismic reflection data sets are now publicly available on-line or by request from DOGGR (c.f., http://owr.conservation.ca.gov/WellSearch/WellSearch.aspx for well files), USGS (http://walrus.wr.usgs.gov/NAMSS/ for marine seismic reflection data) and BOEMRE. The basic procedure we use is actually quite simple. We start with the earthquake hypocenters and look for alignments in map, cross section or in 3D that define discrete principal slip surfaces (Fig.2, top). These surfaces can be planar or non-planar. We then overlay the earthquake focal mechanisms (Fig.2, bottom), but generally plot only one of the two possible nodal planes and the associated slip vector (inset) [Seeber and Armbruster, 1995]. If the alignment of the dominant focal mechanism nodal planes is consistent with the alignment of hypocenters, then the principal slip surface is considered well resolved. Generally, the best orientation for identifying such principal slip surfaces is to look in 3D down-dip or along strike in the plane of slip for the fault. Digital 3D fault surfaces were then generated in several ways, depending on the available data, and the quality and distribution of the hypocenters and nodal planes. If the hypocenters could define a discrete slip surface with non-planar fault geometry, a best-fitting gridded surface with varying smoothing constraints was constructed with these events. If the events only defined a general linear trend, then a best-fitting median plane was constructed through the earthquake distribution. Faults with a mapped surface traces were generally constructed by projecting a smoothed version of the surface trace to depth, but with changing dip and fault geometry along strike, that best matched the changing geometry of discrete hypocenter clusters or dip of the predominant nodal plane (Figs.3-5). 5

Map view

MCF

SAF

San Gorgonio Pass

Inset

MCFMCF

SAFSAF San Gorgonio Pass

Hypocenters from Lin et al., 2007

Focal mechanisms from Hauksson, 2000; Hardebeck and Shearer, 2003

Figure 2. (top) Map and cross section of relocated hypocenters [Lin et al., 2007] for the region around San Gorgonio Pass. Linear trends in hypocenter alignment denoted by dashed red lines; boundary between upper and lower crustal deformation shown by dashed blue line. Some older fault strands, like the Mill Creek fault (MCF) are best defined by where they sharply truncate adjacent seismicity. (bottom) Map and cross section with overlay of single nodal planes and associated slip vectors (inset, Seeber and Armbruster, 1995). Note that a steeply dipping through-going predominantly strike-slip active strand of the San Andreas fault (SAF) can be defined through San Gorgonio Pass based on the alignment of earthquake hypocenters and focal mechansims nodal planes, but only at depths below ~10 km. 6

Mill Creek Mission Creek SAF-Banning North Palm Springs Garnet Hill Palm Springs Figure 3. Map view looking NE of San Gorgonio Pass region with seismicity color coded by depth and some of the new 3D fault models for CFM-v4. Mission San Andreas fault system Creek, Banning and Garnet Hill faults typically dip 70° to 80°NE, and each is a distinctly separate PSF fault to 8-10 km. Different interpretations are permissible, e.g., the orange North Palm Springs fault could be the active down-dip extension of the gray

San Jacinto fault system San Gorgonio Pass thrust that has been offset in a right-lateral sense by the more steeply dipping Banning fault strand. San Gorgonio Pass thrust

Figure 4. Oblique 3D view looking NE, but now looking down-dip of the Palm Springs fault (PSF). Earthquakes along the PSF define a narrow linear trend, as they should San Andreas fault system if most represent slip along this PSF principal slip surface. Additional oblique to strike-slip faults with similar dips are also revealed by this rotated frame of reference (white arrows). These faults define a set of NW-striking, NE-dipping

San Jacinto fault system en echelon blind faults at depths >10 km that help accommodate plate boundary slip through San Gorgonio Pass.

Figure 5. Enlarged oblique 3D view of Fig.3 looking down-dip of the Palm Springs fault (PSF), but now showing some of the new updated 3D fault surfaces created for CFM-v4 that represent the set of deep en echelon NE-dipping blind faults defined by PSF San Andreas fault zone linear trends in hypocenter and nodel plane alignments. Several of these fault models, including the Palm Springs fault, are nearly identical to previous independently derived 3D fault models based on earlier relocated catalogs and different surface-fitting algorithms [Carena et al., 2004]. 7

This kinematic technique of using the spatial distribution of earthquake hypocenters and focal mechanisms to define the geometry of active subsurface faults has proven to be very effective in southern California [Nicholson et al., 1986; Nicholson and Seeber, 1989; Seeber and Armbruster, 1995; Carena et al., 2004]. The power of this technique lies in the internal consistency between two relatively independent datasets: (1) the spatial distribution of the earthquake hypocenters in 3D defined by earthquake travel-times, and (2) the kinematic compatibility and alignment in 3D of individual nodal planes defined by earthquake first-motions and amplitude ratios. A simple example of this technique is demonstrated by a set of steeply dipping, blind, oblique to predominantly strike-slip en echelon faults that occur at depths below about 10 km beneath San Gorgonio Pass. Figure 3 shows a map view looking NE of this deep seismicity, together with some of the new revised 3D fault models we developed for CFM-v4. This includes the Mill Creek, Mission Creek, Banning, and Garnet Hill fault strands, as well as other secondary faults such as the San Gorgonio Pass thrust, the North Palm Springs fault, and the new blind Palm Springs fault (green, PSF). The Palm Springs fault represents one of these deep blind, oblique en echelon faults. The reason we believe we can confidently identify and map these structures as distinctly separate faults is because of the consistency produced by the hypocenter and nodal plane alignments when looking down-dip or along strike in the plane of slip of each fault. Thus, if we rotate the entire frame of reference of this earthquake and fault volume until we are looking down-dip and in the plane of slip of the Palm Springs fault (Fig.4), the earthquakes along the Palm Springs fault (PSF) now define a very narrow linear trend, as they should if most of the events represent slip along this single principal slip surface. This geometry is also consistent with the geometry of the predominant NW-striking, NE-dipping nodal plane many of these earthquakes exhibit in their focal mechanism solutions [e.g., Carena et al., 2004]. Moreover, this frame of reference, highlights other faults in this set of deep, en echelon strike-slip to oblique slip faults that have remarkably similar NE dips. These faults are in addition and sub-parallel to the principal slip surfaces of the San Andreas fault zone, and thus help accommodate plate boundary strain through San Gorgonio Pass. This fault set was first identified by Seeber and Armbruster [1995] and confirmed by Carena et al. [2004], and the resulting 3D fault models developed for CFM-v4 (Fig.5) are virtually identical to previous non- planar 3D fault surfaces independently created using an earlier catalog of relocated focal mechanism solutions and different surface-fitting algorithms [Carena et al., 2004]. Results For this project and in collaboration with other members of the Community Model Development Team, substantial progress was made on implementing newly revised 3D models for several major fault zones, including sections of the San Andreas from Parkfield to Cajon Pass, Garlock, Imperial- Brawley, Laguna Salada-Sierra Cucapah, Lenwood-Lockhart, Landers-Joshua Tree, San Gabriel, Oak Ridge-Northridge and the San Fernando/Sierra Madre faults, as well as for several major cross faults (Fig.1)[Nicholson et al., 2012]. These new models expand the lexicon of revised 3D fault models previously developed for CFM-v.4 that include the San Andreas fault from San Gorgonio Pass to the Salton Sea, the adjacent sub-parallel Mecca Hills-Hidden Springs fault zone, and the San Jacinto, Elsinore-Laguna Salada, and Agua Tibia-Earthquake Valley fault systems [Nicholson et al., 2011]. Several of these earlier CFM-v4 fault models were subsequently revised and updated as part of this project based on additional information and after community review and comment. In addition, this project was able to support more detailed studies in areas of particularly complex fault geometry where multiple fault sets and sub-parallel fault zones strongly interact. This included the complex San Gorgonio Pass region along the San Andreas fault, and the Laguna Salada-Indiviso- Sierra Cucapah region at the southern end of the Elsinore-Laguna Salada fault zone and associated with the El Mayor-Cucapah sequence. This report will focus on many of these special fault areas. 8 Southern San Andreas and Mecca Hills-Hidden Springs fault zones In constructing 3D fault models for CFM, special care was taken to distinguish between sub- parallel fault strands or secondary fault systems. For example, Figure 6 shows a slightly oblique map view of some of our new CFM-v4 3D fault representations along the southern San Andreas fault (SSAF) extending from San Gorgonio Pass through the to the Salton Sea [Nicholson et al., 2011, 2012]. This includes active strands and down-dip splays of the Banning, Garnet Hill, Mission Creek, North Palm Springs, San Gorgonio Pass thrust, and Southern San Andreas faults, as well as a 3D model for the adjacent, sub-parallel Mecca Hills-Hidden Springs fault. The Mecca Hills-Hidden Springs fault is an active NE-dipping sub-parallel structure adjacent to the SSAF that is responsible for the bulk of the seismicity located east of the southern San Andreas surface trace. Previous investigators have inferred that this seismicity may be produced by a dipping SSAF that dips NE at about 65°-67° [e.g., Fuis et al., 2007] based mainly on the projection of seismicity and nodal plane alignments near Salt Creek [Lin et al., 2007]. However, further study of this seismicity, clearly shows that this dipping principal slip surface strikes oblique to the SSAF surface trace and progressively projects to crop out several kilometers farther east as one moves north [Nicholson et al., 2010]. In all cases along strike of this structure, including at Salt Creek, the earthquake and nodal plane alignments project to intersect the down-dip extension of mapped intervening surface faults, like the Hidden Springs, Mecca Hills and Painted Canyon faults.

Figure 6. Slightly oblique 3D view looking NE and nearly down-dip of the Mecca Hills-Hidden Springs fault adjacent to the Southern San Andreas fault (SSAF). This secondary fault system strikes oblique to the SSAF and is responsible for the dipping seismicity found east of the SSAF surface trace, the mapped surface faults east of the SSAF surface trace (like Indio Hills, Painted Canyon, Mecca Hills and Hidden Springs), and regional topography not explained by SSAF slip.

The presence of both a dipping Mecca Hills-Hidden Springs fault system and a vertical or near- vertical SSAF has significant implications. First, it can help explain observations that are otherwise difficult to reconcile. For example, a few scattered earthquakes do occur directly beneath the SSAF surface trace, seismic reflection data along the SSAF suggest a steep to near vertical fault [Rymer et al, 2012; Catchings et al., 2012; Goldman et al., 2012], and the SSAF is clearly vertical at Bombay 9 Beach where it intersects the based on earthquake and nodal plane alignments [Nicholson et al., 2010]. However, geodetic data along the SSAF indicate that maximum shear strain is displaced about 7 km NE of the SSAF surface trace [Fialko, 2006]. This could be the result of the active NE-dipping Mecca Hills-Hidden Springs fault working in combination with a vertical SSAF, rather than shear strain only accumulating on what would otherwise be an inferred dipping SSAF. The presence of two active fault systems side-by-side implies, however, that some plate motion is already being diverted from the SSAF onto the Eastern California shear zone as far south as Bombay Beach, and not necessarily only at the Indio Hills where the southernmost end of the Landers-Joshua Tree sequences begin to splay off from the main SSAF system. San Gorgonio Pass Along the San Andreas fault proper, there is no place more complex, more enigmatic, or more important to properly understand in 3D than San Gorgonio Pass (SGP)[Yule, 2009] and its extension to Cajon Pass where the major San Andreas and San Jacinto fault zones intersect (Figs.1-3,7). Knowing the subsurface geometry of active faults in this area is critical for properly extrapolating near-surface observations to depth, and is particularly important in such complex areas where principal slip surfaces can be multi-stranded, exhibit significant non-planar subsurface fault geometry, and/or intersect other adjacent major faults. The geometry and nature of active fault strands is also crucial to resolving the potential for large through-going rupture, and the resulting strong ground motion predictions for different SSAF rupture scenarios. San Gorgonio Pass and its surrounding region are currently designated a SCEC Special Fault Study Area [Yule et al., 2012]. Accurate representations of 3D fault surfaces through the Pass are thus not only fundamental to the basic seismic hazard estimation for southern California, but provide the necessary framework for all such future integrated tectonic, geologic, and geophysical studies of this particular fault area. 10

Figure 7. Map of relocated earthquake hypocenters color-coded by depth [Hauksson et al., 2012]. To first-order, the geometry of the major through-going fault is defined by the San Andreas- Banning surface trace (red line) and the down-dip NE extent of the deeper earthquakes (solid orange line). Dashed red line is the actual linear trend of deeper seismicity that defines a steeply dipping, through-going predominantly strike-slip San Andreas fault strand, while the cluster of green to yellow events farther east represent oblique thrust faults in its hangingwall.

A major question has always been: what is the geometry of the principal active strand of the San Andreas fault (SAF) through San Gorgonio Pass? Figure 7 shows a map of the most recent relocated hypocenters [Hauksson et al., 2012] with the earthquakes color-coded by depth. This figure actually shows the geometry of this fault quite well. It is basically defined by the SAF surface trace (red line) and the down-dip NE extent of the deeper earthquakes shown by the dark blue and magenta colors (orange line). In actuality, the alignment in 3D of the earthquake hypocenters and nodal planes tends to suggest something a bit more linear (dashed red line), but the general shape is still one of a steep NE-dipping through-going fault with a dip in the northern Coachella Valley of about 70°. The light blue, green and yellow events at shallower levels farther east are mostly aftershocks of the 1986 North Palms Springs earthquake. They help define moderately dipping secondary oblique thrust faults in the hanging-wall of this more steeply dipping San Andreas fault. This interpretation of a through-going, steeply dipping SAF, and one or more moderately dipping oblique thrust faults in its hanging-wall is not new. Both Seeber and Armbruster [1995] and Carena et al. [2004] were able to identify nearly identical fault structures based on the alignment of relocated hypocenters and focal mechanism nodal planes. This fault geometry is also not surprising as it is very similar to the geometry of the San Andreas fault through the Santa Cruz Mountains, where similar oblique motion is again partitioned between a near-vertical SAF, and a more moderately dipping oblique dip-slip fault that produced the 1989 Loma Prieta earthquake [Seeber and Armbruster, 1990]. The new, more extensive relocated earthquake catalogs we use for CFM-v4 basically reaffirm this earlier interpretation. The only difference is that in CFM-v4, we distinguish between the shallow San Gorgonio Pass thrust fault that is largely defined by surface geologic mapping, and the deeper North Palm Springs fault defined by seismicity to emphasize that these two sections are defined by different data sets, and that this structure, if continuous, appears to be offset both vertically and horizontally by the through-going Banning fault strand of the SAF. In previous interpretations, the North Palm Springs fault would be simply labeled as the down-dip extension of the San Gorgonio Pass thrust. This is a very viable, reasonable interpretation and both alternative representations, as well as those from Carena et al. [2004] are included in CFM-v4. Figure 8 shows a map view of the many new 3D fault models through San Gorgonio Pass we developed for CFM [Nicholson et al., 2012]. In developing these new 3D fault representations, care was taken that fault models were first smoothed to reduce artifacts of model construction, and if the fault extended to surface outcrop, the fault was registered to both DEM and the Qfault surface trace. In this way, 3D models for active strands and down-dip splays of Banning, Garnet Hill, Mission Creek, Mill Creek, San Gorgonio Pass thrust, North Palm Springs, and southern San Andreas faults (SSAF) were created. Subsequently, faults in the Crafton Hills complex and representations for the set of blind en echelon faults (Fig.5), like Palm Springs and other secondary faults beneath San Gorgonio Pass were also added. The advantage of these new models is that they allow for more variability in dip along strike and with depth, are more consistent with alignments of relocated hypocenters and focal mechanism nodal planes, and have a higher concentration of hypocenters within close proximity (±1 km) of the modeled 3D slip surface [Hauksson, 2012] than previous CFM fault models. The new 3D fault models also help characterize a more complex pattern of fault 11 interactions at depth between various fault sets and linked fault systems, while providing more continuous, multiple, through-going fault surfaces through San Gorgonio Pass.

Figure 8. New CFM-v.4 fault models for the San Andreas fault system through San Gorgonio Pass [Nicholson et al., 2012]. Three distinctly separate fault strands (Mission Creek, Banning, and Garnet Hill) are now defined in the northern Coachella Valley, and are typically steeply dipping and sub-parallel to depths of 8–10 km. The presence of the principal through-going Banning strand at depth increases the possibility of dynamic rupture through the pass [Shi et al., 2012], while the Crafton Hills complex affects SAF slip rates [Herbert, 2012].

The degree of fault complexity in San Gorgonio Pass is exemplified by the fact that at least 4 different sets of interacting fault structures have been identified, and each set needs to be mapped in detail if the pattern of stress and strain is to be properly modeled and understood. These fault sets include: 1) the principal NW-striking slip surfaces inferred to accommodate the bulk of strike-slip motion along the fault zone (Fig.8). These are typically steeply (~70°–80°) NE-dipping faults, such as the Banning, Garnet Hill and Mission Creek strands, and can extend throughout the seismogenic crust; 2) sets of NE-striking, high-angle secondary cross faults found primarily in the upper 10 km, such as the Crafton Hills fault complex; 3) predominantly NE-dipping moderate-to-low-angle (~30°–45°) oblique thrust faults that occur at depths below ~8-10 km. These would include faults involved in the 1986 North Palm Springs sequence, like the North Palm Springs fault, as well as other mid-crustal and basal detachments; and 4) the series of previously mentioned en echelon NW- striking oblique strike-slip faults that typically dip ~65°NE, such as the blind Palm Springs fault (PSF)(Fig.5), and which also occur primarily below ~10 km [Nicholson et al., 1986; Nicholson and Lees, 1992; Seeber and Armbruster, 1995; Nicholson, 1996; Carena et al., 2004; Nicholson et al., 2010]. As with the PSF, many of these secondary fault sets are best expressed by looking down-dip or along strike within the plane of slip (e.g., Fig.4), and Figure 9 shows a vertical cross section looking nearly along strike of the Banning and Garnet Hill fault strands (Fig.4, red box + arrow). In cross section, the first-order feature we see in the seismicity is a fairly distinct separation of seismic activity in the upper and lower crust. The upper crust exhibits less seismicity that defines a 12 few steeply dipping strike-slip to oblique-slip faults, while in the lower crust, the higher level of earthquake activity tends to define a wedge-shaped volume that contains more low-angle reverse or oblique-reverse faults. The boundary between these two crustal layers appears to be at about 10 to 12 km depth (dashed white line, Fig.9). In places, this very low-angle dipping interface appears to be seismically active, as it exhibits alignments of hypocenters and low-angle nodal planes (inset, Nicholson and Lees, 1992). It may also have been responsible for truncating the down-dip extent of the North Palm Springs rupture in 1986 [Nicholson, 1996]. As such, this interface or detachment may reflect a significant mechanical layering to the seismogenic crust, and may help explain why the shallow mapped geologic structures and other near-surface observations in San Gorgonio Pass may not necessarily correlate well with the deeper active faults.

Figure 9. Cross section looking NW along strike of Banning fault (see Fig.4 for orientation) showing how the steeply dipping Garnet Hill (GHF, yellow), Banning (BF, purple) & Mission Creek (MCF) fault strands intersect and merge with a set of low-angle oblique thrust faults. Seismicity appears to exhibit mechanical layering (dashed line) that may be active (inset) and controlled the down-dip extent of rupture in 1986 [Nicholson and Lees, 1992]. Through-going BF & GHF may remain steeply dipping and relatively planar (Option #1), become more listric (Option #2), or do both to splay down- dip and become multi-stranded at depth. Alternatively, these can just be considered separate fault sets.

This mechanical layering may also affect to some extent the geometry and behavior of major through-going faults. Earthquakes currently occur along the through-going Banning fault strand, but primarily at depths below this mid-crustal detachment (Fig.2). In the upper crust, the Garnet Hill, Banning and Mission Creek fault strands remain steeply dipping and sub-parallel down to about 8- 10 km, or about the depth of this detachment (Fig.9). At deeper levels, however, they begin to interact and merge with a set of moderately-dipping oblique thrust faults. Thus, faults like the 13 Garnet Hill strand can remain steeply-dipping (Option #1), it can become more listric (Option #2), or do both and splay down-dip to become multi-stranded at depth. This is also true for the Banning which can remain steeply-dipping (Option #1), it can become more listric (Option #2), or merge with the faults active during the 1986 North Palm Springs sequence (Option #3). The main point is that both fault sets: steeply dipping through-going predominantly strike-slip faults (like the Banning and Garnet Hill strands), and more moderately dipping oblique thrust faults (like the North Palm Springs fault), are present, active and interacting with each other. This allows the fault system to accommodate both through-going predominantly strike-slip motion along the more steeply dipping planar fault strands, like the Banning, but also a secondary component of crustal shortening and reverse slip on the more moderately dipping oblique thrust faults present in the hangingwall. The new 3D fault models developed for CFM-v4 thus help characterize a more complex pattern of fault interactions at depth between various fault sets, while providing more continuous, steeply dipping and smoothly varying rupture surfaces through San Gorgonio Pass. These more complete, detailed, and more complex multiple 3D fault models may help explain some of the more enigmatic fault behavior and patterns of deformation that may be otherwise difficult to understand. For example, the failure of the 1986 North Palm Springs mainshock to develop into a full-scale rupture of the SSAF could be the result of it occurring primarily on the adjacent secondary North Palm Springs fault (Fig.9), rather than on what might be considered the primary, more steeply dipping through-going Banning fault strand (Option #1, Fig.9). Moreover, the decrease in slip rate observed SE along strike of the San Bernardino strand of San Andreas fault in San Gorgonio Pass may be related to adjacent secondary faults, like the Crafton Hills complex [Herbert and Cooke, 2012] and to slip being more distributed as the fault becomes multi-stranded at depth (Fig.8), rather than changing geometry of a single fault as was once believed [Dair and Cooke, 2009]. Laguna Salada and Sierra Cucapah faults, and the 2010 El Mayor-Cucapah sequence Besides developing updated 3D fault models along major mapped surface traces (e.g., Fig.1), substantial effort was also made to develop preliminary 3D fault models for several major recent earthquake ruptures. This included fault models for the 1971 San Fernando, 1979 , 1986 North Palm Springs, 1987 Elmore Ranch-Superstition Hills, 1992 Landers-Joshua Tree, 1994 Northridge, and 2010 El Mayor-Cucapah earthquakes and their associated aftershocks. The 2010 El Mayor-Cucapah earthquake was particularly complex [Hudnut et al., 2010; Kroll et al., 2012], and demonstrated that major earthquakes can occur on adjacent sub-parallel faults in close proximity to previous large earthquakes on distinctly separate structures (e.g., 1892 M7 Laguna Salada earthquake). Figure 10 shows an oblique 3D view of some of the new fault models we developed for this 2010 sequence, as well as for various cross faults and active strands of the Laguna Salada fault, based on an integrated analysis of the relocated aftershocks [Hauksson et al., 2011; 2012], and near-surface geologic mapping and InSAR studies of fault surface traces [e.g., Fletcher et al., 2010; Oskin et al., 2011, 2012; Teran et al., 2011; Treiman et al., 2010]. Several of these CFM models were subsequently revised following comment and review of preliminary ones presented at the 2011 SCEC meeting. The new CFM 3D models include fault representations for the Borrego, Pescadores, Paso Superior, Paso Inferior, Sierra Cucapah, and Indiviso faults, as well as adjacent dipping strands of the Laguna Salada fault and various associated cross faults like Painted Gorge Wash, Devil's Canyon, Yuha Well, Shell Beds, Yuha Wash, Yuha, and El Mayor-Cucapah cross faults. In constructing these new 3D models, we distinguished between the predominantly steep to E- dipping shallow faults and related fault splays that we correlate to the major, deep E-dipping Sierra Cucapah fault, and the predominantly steep to W-dipping strands and down-dip splays related to the Laguna Salada fault. Numerous cross faults and other secondary faults were triggered by the 2010 event. Many of these correlated well with mapped surface fault traces, while others remained blind. 14

Figure 10. Oblique 3D view looking East across various preliminary CFM 3D fault representations for the 2010 M7.2 El Mayor-Cucapah rupture and its associated aftershocks [Nicholson et al., 2012]. CFM-v4 3D fault models were developed for the steep to east-dipping Pescadores, Borrego, Paso Superior, Paso Inferior, deep Sierra Cucapah and related fault splays, for the steep to west-dipping Indiviso, Laguna Salada and other related faults, and for a number of curved to planar cross faults, including the Painted Gorge Wash, Devil's Canyon, Yuha Well, Shell Beds, Yuha, and various other El Mayor-Cucapah cross faults. Relocated aftershock hypocenters from Hauksson et al. [2012]; mapped fault surface trace data courtesy of Ken Hudnut, John Fletcher and Jerry Treiman.

Reorganization of the CFM fault database In collaboration with the Community Model Development Team and the SCEC Earthquake Group, the CFM-v4 fault database was reorganized with a new hierarchical name and numbering scheme. This reorganization allows CFM to properly organize, name and number the increasing variety and complexity of modeled, multi-stranded principal slip surfaces, adjacent secondary faults, and alternative fault representations that have been or will be developed for CFM, while maintaining a greater consistency with fault nomenclature from the CGS Fault Activity database. The new CFM database naming scheme provides unique identifiers (including number, name and abbreviation) for each level of the fault hierarchy under which a particular fault segment is classified. Levels of hierarchy include Fault Area, Fault Zone or System, Fault Section, Fault Name, Fault Strand or Model, and Fault Component (Fig.11). These additional hierarchical levels allow for more flexible database searches and easier identification of fault components and possible system-level associations of individual 3D fault elements that comprise CFM. This scheme also allows for grouping related individual faults under a higher-level fault system (e.g., Southern Frontal Fault System for the Raymond, Hollywood, Santa Monica, and Malibu Coast faults) to help facilitate identification of potentially larger earthquake ruptures between such kinematically linked and geometrically similar multiple fault segments. In 2012, a draft version this new fault database was sent out for review, comment and ranking of alternative fault models in CFM. Appendix 1 provides a partial listing of the database with current revised CFM fault names, numbers and abbreviations. However, this spreadsheet is still a work in progress, as it needs to more fully incorporate feedback, review comments, and fault rankings provided to us by the USGS, CGS and other SCEC colleagues. 01 10 13 11 09 08 SCEC CFM-v4 Fault Database - Fault Area/Major Boundary 08 01 - San Andreas fault system 02 - fault area 12 03 - fault area 07 04 - Offshore Continental Borderland 01 05 - Western area 05 06 - Eastern Transverse Ranges area 01 07 - Mojave fault area 08 - system 06 09 - Basin and Range fault area Figure 11. The SCEC CFM fault database now includes 10 - fault area a hierarchical ID naming and numbering scheme that 11 - Great Valley fault area provides unique identifiers (number, name, abbreviation) 12 - Coast Ranges fault area for each level under which a particular fault segment is 03 13 - Offshore Central California area classified. Levels of fault hierarchy include Fault Area, Fault Zone or System, Section, Name, Fault Strand or 04 Model, and Fault Component (see Table). Fault areas or major fault boundaries for southern California are shown 02 at right. The table below gives a simplified, brief partial example of the hierarchical tree for assigning individual faults to related fault systems and larger fault areas.

No Fault Area/Major Boundary Abbrev No. Fault Zone or System Abbrev No Fault Section Abbrev No Fault Name Abbrev No Fault Strand or Model Abbrev

01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 06 Parkfield PARK 01 San Andreas fault SAF 01 Yule CFMA model YULE 02 San Gorgonio Pass fault region SGPR 07 Cholame-Carrizo CLCZ 02 Banning fault strand BNFS 02 70dip Nicholson model NICH 03 Mecca Hills-Hidden Springs fault zoneMHFZ 08 Mojave MJVS 03 Mill Creek fault strand MLCS 02 listric Nicholson model NICH 02 Salton Trough Fault Area SALT 01 Brawley Seismic Zone BSZ 09 San Bernardino Mountains SBMT 04 Mission Creek fault strand MSCS 02 Nicholson model w/splay NICH 02 IMFZ 10 Coachella COAV 05 Garnet Hill fault strand GHFS 01 Yule CFMA model YULE 03 fault zone CPFZ 11 1812 Rupture-Mojave 1812 01 San Andreas fault SAF 01 1812 CFMA model CFMA

03 Peninsular Ranges Fault Area PNRA 01 San Jacinto fault zone SJFZ 01 San Bernardino SBRN 01 San Jacinto-Claremont fault SJCF 01 90dip CFMA model CFMA 04 Offshore Continental Borderland OCBA 02 Elsinore-Laguna Salada fault zone ELSZ 02 San Jacinto Valley SJNV 01 Claremont fault CLMF 01 90dip CFMA model CFMA 05 Western Transverse Ranges Area WTRA 03 Agua Tibia-Erthquake Valley fault zoneATEV 03 Anza ANZA 01 Clark fault CLRF 01 CFMA model CFMA 06 Eastern Transverse Ranges Area ETRA 04 Newport-Inglewood-Rose Canyon NIRC 04 Coyote Creek CCRS 02 Buck Ridge fault BKRF 01 variable dip model VDIP 07 Mojave Fault Area MJVA 05 Compton-Lower systemCLEP 05 Borrego Mountain BRMT 01 Coyote Creek fault CCRF 01 CFMA model CFMA 08 Garlock Fault System GRFS 01 Garlock Fault zone GRFZ 06 Superstition Hills SSHS 01 Superstition Hills fault SHF 01 90dip CFMA model CFMA 09 Basin and Range Area BNRA 01 Black Mountain fault zone BMFZ 07 Superstition Mountain SSMT 01 Superstition Mountain fault SMTF 01 90dip CFMA model CFMA 10 Area SNFA 01 fault zone OVFZ 08 Imperial Valley IMPV 01 Weinert-El Centro fault WECF 11 Great Valley Fault Area GVFA 01 zone WWFZ 12 Coast Ranges Fault Area CRFA 01 Rinconada-East Huasana fault systemRNEH 15 13 Offshore Central California Area OCCA 01 zone HSGZ 16

Conclusions For this project, alignments of relocated earthquake hypocenters and focal mechanism nodal planes were thus used to define the subsurface 3D geometry of active faults and to construct updated digital 3D fault representations for CFM (Fig.1). These new models allow for more non- planar, multi-stranded 3D fault geometry, including changes in dip and dip direction along strike and down dip, based on the changing patterns of earthquake hypocenter and focal-mechanism nodal plane alignments, rather than projecting faults to depth assuming a constant (often vertical) dip and dip direction, as was the case for many of the previous preliminary fault models in CFM. These fault surfaces are often best resolved when looking in 3D down-dip or along strike within the plane of slip for each fault (Figs.2,4,6&9). Along major through-going faults in southern California, recent earthquake fault ruptures, such as the 2010 El Mayor-Cucapah earthquake that involved the deep Sierra Cucapah fault and associated fault splays (Fig.10), appear to be strongly affected by local fault geometry, as well as the sense of slip and relative orientation of secondary structures, such as left-lateral conjugate cross faults, tear faults, and low-angle detachments. Identification of these features, especially at seismogenic depths, often depends on careful kinematic analysis of the earthquake hypocenters and focal mechanisms in both space and time. In the Coachella Valley and at its intersection with the Brawley Seismic zone below the Salton Sea, alignments of hypocenters and nodal planes, together with seismic reflection data strongly suggest the Southern San Andreas fault (SSAF) is vertical to steeply dipping, while earthquakes located farther east define a separate Mecca Hills-Hidden Springs fault zone (Fig.6) that dips NE at about 65° to 70°. This principal slip surface strikes oblique to the SSAF and so would project to crop out several kilometers east of the SSAF surface trace at the latitude of the Indio Hills. This dipping fault zone, sub-parallel and adjacent to the SSAF, is responsible for the mapped secondary faults and elevated, tectonically deformed topography found in this area that can not be explained by strike-slip motion on a vertical or near-vertical SSAF. The presence of both fault zones side-by- side implies that some plate boundary motion is likely diverted onto the Eastern California shear zone as far south as Bombay Beach. Through San Gorgonio Pass (SGP), seismicity appears to define a mechanically layered crust with predominantly high-angle strike-slip to oblique slip faults in the upper crust, while beneath ~10 km depth, intersecting sets of strike-slip, oblique slip and low-angle thrust faults define a more complex wedge-shaped volume deformation of the lower crust (Figs.2-5,8&9). In some places, this interface between upper and lower crustal deformation appears to be seismically active and may have controlled the down-dip extent of seismic rupture in 1986. Alignments of hypocenters and nodal planes define multiple principal slip surfaces through SGP (Figs.8-9), including a through- going steeply-dipping (~70°) predominantly strike-slip Banning strand at depth and a more moderately-dipping (40°-50°) oblique North Palm Springs fault that both project upwards towards the San Andreas fault (SAF) surface trace. The North Palm Springs fault may be the active down- dip extension of the San Gorgonio Pass thrust offset at depth by the principal, through-going steeply dipping Banning strand of the SAF. In the northern Coachella Valley, seismicity indicates that the Garnet Hill and Banning strands of the SAF are most likely sub-parallel and steeply dipping (~70°NE) to depths of 8–10 km, where they intersect and merge with a stack of moderately dipping to low-angle oblique thrust faults (Fig.9). Although the dense wedge of deep seismicity below SGP contains multiple secondary fault sets of different orientations, the predominant fault set appears to be a series of en echelon NW- striking strike-slip to oblique-slip faults that dip NE and strike slightly oblique to the SAF (Figs.4- 5). These faults also help accommodated plate boundary motion through SGP. 17 These revised 3D models for the principal slip surfaces through San Gorgonio Pass and into the Coachella Valley, including the Mecca Hills-Hidden Springs fault, have already proven useful to modeling dynamic earthquake rupture along the San Andreas fault [Shi et al., 2012; Tarnowski and Oglesby, 2012], as well as providing a better match to the observed patterns of geodetic strain [Fialko, 2006], tectonic uplift and regional topography in the Coachella Valley and adjacent Little San Bernardino Mountains [Fattaruso and Cooke, 2012]. Furthermore, the presence of additional active secondary faults, such as the Crafton Hills complex and blind faults at depth below San Gorgonio Pass, like the Palm Springs fault (Fig.8), are also important as they can strongly influence modeled slip rates along the San Andreas fault itself [e.g., Herbert and Cooke, 2012]. The new 3D fault models developed for CFM-v4 help characterize a more complex pattern of fault interactions at depth between various fault sets, sub-parallel fault systems, and intersecting secondary cross faults and low-angle detachments. To properly organize, name and number the increasing variety and complexity of these modeled, multi-stranded principal slip surfaces, adjacent secondary faults, and alternative fault representations, the SCEC CFM database was reorganized with a new hierarchical name and numbering scheme (Fig.11 & Appendix 1). This new fault ID scheme allows for more flexible database searches, and easier identification of possible system- level associations of individual 3D fault elements that comprise CFM to help facilitate identification of potentially larger earthquake ruptures between various kinematically linked and geometrically similar faults and multiple fault segments. Data and Product Availability The primary earthquake datasets used for this research are available from the SCEC Data Center (http://data.scec.org/research-tools/altcatalogs.html). Most mapped fault surface trace data we used were provided by the California Geological Survey primarily through the USGS Quaternary Fault and Fold database website (http://earthquake.usgs.gov/hazards/qfaults/). Products and updated digital representations of 3D fault surfaces generated by this project are available from the SCEC Community Fault Model website (http://structure.rc.fas.harvard.edu/cfm/modelaccess.html). Reports and Outreach Presentations Nicholson, C., E. Hauksson and A. Plesch, Active fault geometry and crustal deformation in San Gorgonio Pass: The view from below and in 3D from seismicity, SCEC SFSA Workshop on San Gorgonio Pass, June, 2012. Nicholson, C., A. Plesch, J.H. Shaw and E. Hauksson, Upgrades and improvements to the SCEC Community Fault Model: Increasing 3D fault complexity and compliance with surface and subsurface data, 2012 SCEC Annual Meeting Proceedings & Abstracts, XXII, p.125-126 (2012). Nicholson, C., Earthquake hazards and earthquake rupture scenario for the Santa Barbara area, County Earthquake Exercise, Santa Barbara County Office of Emergency Services, Oct. 23 (2012). Invited speaker. Nicholson, C., E. Hauksson and A. Plesch, Active fault geometry and crustal deformation along the San Andreas fault system through San Gorgonio Pass, California: The view in 3D from seismicity, Eos (Transactions of AGU), 93 (52), Abstract T22C-03 (2012). Nicholson, C., Evaluating 3D fault geometry in Special Fault Study Areas and improving the SCEC Community Fault Model (CFM), 2012 SCEC Annual Report, 7 pp. (2013). 18 Sorlien, C.C, C.J. Marshall, C. Nicholson et al., Post-1 Ma deformation history of the anticline forelimb above the Pitas Point-North Channel fault in Santa Barbara Channel, California, 2012 SCEC Annual Meeting Proceedings & Abstracts, XXII, p.139-140 (2012). Non-technical Summary Detailed analysis of well-determined earthquake locations and focal mechanisms are used to define the geometry of active subsurface faults and to create improved, updated digital 3D fault surface models for the SCEC Community Fault Model (CFM). Newly revised 3D models for several major fault zones, including the San Andreas from Parkfield to the Salton Sea, San Jacinto, Elsinore-Laguna Salada, Agua Tibia-Earthquake Valley, Garlock, Imperial-Brawley, Mecca Hills- Hidden Springs, Pinto Mountain, Landers-Joshua Tree, San Gabriel, Oak Ridge-Northridge and the San Fernando/Sierra Madre faults were developed, including detailed models for the San Gorgonio Pass and El Mayor-Cucapah regions. These new models allow for more non-planar, multi-stranded 3D fault geometry, including changes in dip and dip direction along strike and down dip, based on the changing patterns of earthquake hypocenter and focal-mechanism nodal plane alignments. These new CFM fault surfaces describe a more complex pattern of interacting fault sets at depth accommodating crustal deformation in southern California, and have already provided the basis for improved dynamic earthquake rupture models, variable fault slip rate models, and correlations with associated regional topography. References Bennett, J., C.C. Sorlien, et al., Quaternary deformation of the Newport-Inglewood-Carlsbad- Coronado Bank-Descanso Fault System: Long Beach to , California, 2012 SCEC Annual Meeting Proceedings & Abstracts, XXII, p.90 (2012). Bryant, W. A. (compiler), 2005, Digital Database of Quaternary and Younger Faults from the Fault Activity Map of California, version 2.0: accessed July 2010 from California Geological Survey Web Page, http://www.consrv.ca.gov/cgs/information/publications/Pages/QuaternaryFaults_ver2.aspx. Bullard, T.F. and W.R. Lettis, 1993, Quaternary fold deformation associated with blind thrust faulting, basin, California, J. Geophys. Res., 98, p. 8349–8369. Carena, S., J. Suppe and H. Kao, Lack of continuity of the San Andreas fault in southern California: Three-dimensional fault models and earthquake scenarios, J. Geophys. Res, 109, doi:10.1029/2003JB002643, B04313, 17 pp (2004). Catchings, R.D.; G. Fuis; M.J. Rymer; M. Goldman et al., Salton Seismic Imaging Project Line 6: San Andreas Fault and Northern Coachella Valley Structure, Riverside and San Bernardino Counties, California, Eos (Trans. AGU), v.93, n.52, abstract T51B-2583, Fall meeting, 2012. Dair, L. and M.L. Cooke, San Andreas fault geometry through the San Gorgonio Pass, California, Geology, 37, n.2, p.119-122 (2009). Davis, T.L., J. Namson and R.F. Yerkes, 1989, A cross section of the Los Angeles area: Seismically active fold and thrust belt, the 1987 Whittier Narrows earthquake, and earthquake hazard, J. Geophys. Res., 94, p. 9644–9664. De Hoogh, G.L., C. Nicholson, C.C. Sorlien and R.D. Francis, Neogene Basin and Plate Boundary Development in the Outer Continental Borderland Offshore Southern California, Eos (Transactions of AGU), 90(52), Abstract T13C-1891 (2009). Dolan, J.F., J.H. Shaw and T.K. Rockwell, The Ventura Region Special Fault Study Area: Towards an understanding of the potential for large, multi-segment thrust ruptures in the Transverse Ranges, 2012 SCEC Annual Meeting Proc. & Abstracts, XXII, p.99-100 (2012). 19 Fattaruso, L. and M. Cooke The influence of complex fault geometry on uplift patterns in the Coachella Valley and Mecca Hills of Southern California, 2012 SCEC Annual Meeting Proc. & Abstracts, XXII, p.102 (2012). Fialko, Y., Interseismic strain accumulation and earthquake potential on the southern San Andreas fault system, Nature, 441, p.968-971 (2006). Fletcher, J.M, T.K. Rockwell, et al., Distribution and kinematics of surface ruptures associated with the El Mayor-Cucapah earthquake, 2010 SCEC Annual Meeting Proceedings & Abstracts, XX, p.213-214 (2010). Fuis, G.S., D. Scheirer, V. Langenheim and M. Kohler, The San Andreas fault in southern California is almost nowhere vertical—Implications for , 2007 SCEC Annual Meeting Proc. & Abstracts, XVII, p.112 (2007). Goldman, M.; G. Fuis; R.D. Catchings; M.J. Rymer et al., Salton Seismic Imaging Project Line 7: Data and Analysis to Date, Eos (Trans. AGU), 93, n.52, abstract T51B-2581, Fall meeting, 2012. Hardebeck, J.L. and P.M. Shearer, Using S/P amplitude ratios to constrain the focal mechanisms of small earthquakes, Bull. Seismol. Soc. Am., v.93, n.6, p.2434–2444 (2003). Hauksson, E., Understanding seismicity in the context of complex fault systems and crustal geophysics, 2012 SCEC Annual Meeting Proc. & Abstracts, XXII, p.108 (2012). Hauksson, E. and P. Shearer, Southern California hypocenter relocation with waveform cross- correlation; Part 1, Results using the double-difference method, Bull. Seismol. Soc. Am., v.95, n.3, p.893-903, 2005. Hauksson, E., W. Yang and P. Shearer, Waveform relocated earthquake catalog for Southern California (1981 to June 2011), Bull. Seismol. Soc. Am., v.102, n.4, p.2239-2238, doi:10.1785/0120110241, 2012. Hauksson, E., J. Stock, K. Hutton, W. Yang, J. A. Vidal-Villegas and H. Kanamori, The 2010 Mw 7.2 El Mayor-Cucapah Earthquake Sequence, , and Southernmost California, USA: Active Seismotectonics along the Mexican Pacific Margin, Pure Appl. Geophys., 168, p. 1255–1277, 2011. Herbert, J., The role of fault complexity and secondary faults on fault slip, SCEC Special Fault Study Area Workshop on San Gorgonio Pass, June, 2012. Herbert, J. and M. Cooke, 2012, Sensitivity of the Southern San Andreas fault system to tectonic boundary conditions and fault configuration, Bull. Seismol. Soc. Am., 102, p.2046-2062, doi:10.1785/0120110316. Hester, R.J. and J.N. Truex (1977). field trip, AAPG Pacific Section Guidebook, 35 pp. Hopps, T.E., H.E. Stark, and R.J. Hindle, Subsurface geology of Ventura Basin, California, Ventura Basin Study Group Report, 45 pp., 17 structure contour maps and 84 structure panels comprising 21 cross sections, Rancho Energy Consultants, Inc., Santa Paula, CA, 1992. Hopps, T.E., H.E. Stark, R.J. Hindle, J.H. Thompson, and G.C. Brown, CS30: Correlated section across Central Ventura Basin from T5N/R19W to T1N/R18W, California, Pacific Section–Am. Assoc. Petrol. Geol. Cross Section, April, 1995. Hubbard, J., Structural linkage of onshore and offshore thrust systems across the and prospects for large earthquakes in the Transverse Ranges, SCEC Annual Meeting Proc. & Abstracts, XXI, p.7, 2011. Hudnut, K.W., J.M. Fletcher et al., Earthquake rupture complexity evidence from field observations, Eos (Transactions of AGU). 91 (52), Abstract T51E-02 (2010). Hudnut, K., L. Seeber and J. Pacheco, Cross-fault triggering in the November 1987 Superstition Hills earthquake sequence, southern California, Geophys. Res. Lett., 16, p. 199–202, 1989. 20 Huftile, G. and R.S. Yeats, Convergence rates across a displacement transfer zone in the western Transverse Ranges, Ventura basin, California, J. Geophys. Res., v. 100, p. 2043–2068 (1995). Kamerling, M. and C. Nicholson, The Oak Ridge fault and fold system, Eastern Santa Barbara Channel, California, 1995 SCEC Annual Report, v. II, p. C26–C30 (1996). Kamerling, M.J., C.C. Sorlien, and C. Nicholson (1998), Subsurface faulting and folding onshore and offshore of Ventura basin: 3D map restoration across the Oak Ridge fault, SCEC 1998 Annual Meeting Report, V, p.68-69. Kamerling, M.J., C.C. Sorlien and C. Nicholson (2003), 3D development of an active oblique fault system, northern Santa Barbara Channel, California, Seismol. Res. Lett., v. 74, n.2, p. 248. Kamerling, M. J., Sorlien, C. C., Archuleta, R., and Nicholson, C., 2001, Three-dimensional geometry and interactions of faults and structures along the northern margin of the Santa Barbara Channel, California: Geol. Soc. Am. Abstracts with Prog., v. 33, no. 3, p. A-41. Kroll, K., E. Cochran, K.B. Richards-Dinger and D.F. Sumy, Complex fault interaction in the Yuha Desert, Eos (Trans. AGU), v.93, n.52, abstract S13B-05, Fall meeting, 2012. Lees, J. M., Geotouch: Software for Three and Four-Dimensional GIS in the Earth Sciences, Computers & Geosciences, 1999. Lin, G., P. M. Shearer, and E. Hauksson, Applying a three-dimensional velocity model, waveform cross-correlation, and cluster analysis to locate southern California seismicity from 1981 to 2005, J. Geophys. Res., v.112, n.B12, 14 pp, B12309, doi:10.1029/2007JB004986, 2007. Lozos, J.C. and D.D. Oglesby, Seemingly minor details of fault geometry may strongly affect rupture propagation, Seismol. Res. Lett., 83, n.2, p.370, 2012. Marshall, C.J., C. Sorlien, C. Nicholson, R.J. Behl and J.P. Kennett, Sedimentation in an active fold and thrust belt, Santa Barbara Basin, California: Local and regional influences on the spatial and temporal evolution of sedimentation from 1.0 Ma to Present, AAPG National Meeting, Long Beach, CA (2012). Meade, B.J. and B.H. Hager, Block models of crustal motion in southern California constrained by GPS measurements, J. Geophys. Res., 110, B03403, doi:10.1029/2004JB003209 (2005). Mori, J., D. Wald and R. Wesson, Overlapping fault planes of the 1971 San Fernando and 1994 Northridge, California earthquakes, Geophys. Res. Lett., 22, n.9, p.1033-1036, 1995. Nicholson, C., Seismic behavior of the San Andreas fault in the Northern Coachella Valley, California: Comparison of the 1948 and 1986 earthquake sequences, Bulletin of the Seismological Society of America, v.86, n. 5, p. 1331-1349 (1996). Nicholson, C., E. Hauksson, A. Plesch and P. Shearer, Resolving 3D fault geometry at depth along active strike-slip faults: Simple or complex?, 2008 SCEC Annual Meeting Proceedings & Abstracts, XVIII, p.143-144 (2008). Nicholson, C., E. Hauksson, and A. Plesch, Revised 3D fault models for the Southern San Andreas fault system extending from San Gorgonio Pass to the Salton Sea, Pacific Section AAPG-GSA Cordilleran Joint Meeting Abstracts w/Program, v.42, n.4, Abstract 21-8, p.69, Anaheim, CA (2010). Nicholson, C., E. Hauksson and A. Plesch, Active fault geometry and crustal deformation along the San Andreas fault system through San Gorgonio Pass, California: The view in 3D from seismicity, Eos (Transactions of AGU), 93 (52), Abstract T22C-03 (2012). Nicholson, C. and M.J. Kamerling, Reliability of 2D kinematic fold models to infer deep fault structure in the western Transverse Ranges, California, Proceedings of the NEHRP Conference and Workshop on the Northridge, California Earthquake of January 17, 1994, v. II, p. 299–306 (1998). Nicholson, C., M.J. Kamerling, C.C. Sorlien, T.E. Hopps and J.-P. Gratier, Subsidence, compaction and gravity-sliding: Implications for 3D geometry, dynamic rupture and seismic hazard of active 21 basin-bounding faults in southern California, Bull. Seismol. Soc. Am., 97, n.5, p.1607-1620 (2007). Nicholson, C., A. Plesch, J. Shaw, E. Hauksson and P. Shearer, Improvements in SCEC Community Fault Model for Version 4.0, UCERF-3 California Statewide Fault Model & Paleoseismic Workshop, Pomona, CA (2011). Nicholson, C., A. Plesch, J.H. Shaw and E. Hauksson, Upgrades and improvements to the SCEC Community Fault Model: Increasing 3D fault complexity and compliance with surface and subsurface data, 2012 SCEC Annual Meeting Proceedings & Abstracts, XXII, p.125-126 (2012). Nicholson, C., L. Seeber, P. Williams and L.R. Sykes. Seismicity and fault kinematics through the eastern Transverse Ranges, California: Block rotations, strike-slip faulting and low-angle thrusts, Journal of Geophysical Research, 91, p. 4891-4908, (1986). Nicholson, C., L. Seeber, P. Williams and L.R. Sykes. Seismic evidence for conjugate slip and block rotation within the San Andreas fault system, southern California, Tectonics, 5, p. 629-648 (1986). Nicholson, C., C.C. Sorlien, C.S. Schindler, and G. DeHoogh, Large vertical motions and basin evolution in the Outer Continental Borderland off Southern California associated with plate boundary development and continental rifting, Eos (Transactions of AGU), 92 (52), Invited Abstract T31F-04 (2011). Oglesby, D.D. and P.M. Mai, Fault geometry, rupture dynamics and ground motion from potential earthquakes on the North Anatolian Fault under the Sea of Marmara, Geophys. J. Inter., v.188, n.3, p.1071-1087 (2012). Olsen, K.B, S.M. Day, et al., Strong shaking in Los Angeles expected from southern San Andreas earthquake, Geophys. Res. Lett., 33, L07305, doi:10.1029/2005GL025472, 4pp (2006). Oskin, M.E., J.R. Arrowsmith, et al., Near-field coseismic deformation quantified from differential airborne LiDAR of the El Mayor-Cucapah earthquake , 2011 SCEC Annual Meeting, XXI, p.210 (2011). Oskin, M.E. J.R. Arrowsmith, et al., Near-field deformation from the El Mayor-Cucapah earthquake revealed by differential LiDAR, Science, v.335, n.6069, p. 702-705 (2012). Plesch, A., C. Nicholson, J.H. Shaw, E. Hauksson and P.M. Shearer, New developments for the SCEC Community Fault Model and its associated fault database, 2010 SCEC Annual Meeting Proceedings & Abstracts, XX, p.261-262 (2010). Plesch, A., J. Shaw et. al., Community Fault Model (CFM) for Southern California, Bulletin of the Seismological Society of America, v.97, n.6, p.1793–1802, doi: 10.1785/0120050211 (2007). Redin, T., J. Forman and M.J. Kamerling, 2005, Santa Barbara Channel structure and correlation sections, Pacific Section AAPG Cross Sections CS-32 through CS-42, Bakersfield, CA. Richards-Dinger, K.B. and W.L. Ellsworth, A comparison of earthquake (Re)Location methods Seismol. Res. Lett, v.72, n.2, p. 229 (2001). Rockwell, T., Large co-seismic uplift of coastal terraces across the Ventura Avenue Anticline: Implications for the size of earthquakes and the potential for tsunami generation, 2011 SCEC Annual Meeting Proceedings & Abstracts, XXI, p.7 (2011). Rymer, M.J.; G. Fuis; R.D. Catchings; M. Goldman et al., Salton Seismic Imaging Project Line 5— the San Andreas Fault and Northern Coachella Valley Structure, Riverside County, California, Eos (Trans. AGU), v.93, n.52, abstract T51B-2584, Fall meeting, 2012 Seeber, L. and J. Armbruster, The San Andreas fault system through the Transverse Ranges as illuminated by earthquakes, J. Geophys. Res, 100, p. 8285-8310 (1995). Seeber, L., J.G. Armbruster, and P. Geiser, The 1994 Northridge and 1971 fault ruptures and surrounding seismogenic faults as illuminated by small earthquakes, Geol. Soc. Am. Abstracts w/Prog., v. 33, n.3, p.A-63 (2001). 22 Schindler, C.S., C. Nicholson and C. Sorlien, 3D Fault Geometry and Basin Evolution in the Northern Continental Borderland Offshore Southern California, Eos (Trans. AGU), 88, n.52, T32A-1100 (2007). Shaw, J.H. and P.M. Shearer, An elusive blind-thrust fault beneath metropolitan Los Angeles, Science, v.283, p. 1,516-1,518, 1999. Shaw, J. H., and J. Suppe (1996). Earthquake hazards of active blind-thrust faults under the central , California, J. Geophys. Res. 101, 8623-8642. Shearer, P., E. Hauksson and G. Lin, Southern California hypocenter relocation with waveform cross-correlation, Part 2 Results using Source-specific station terms and cluster analysis, Bull. Seismol. Soc. Am., v.95, n.3, p.904-915, 2005. Shi, Z. and S.M. Day, Studying the effect of fault roughness on strong ground motion, Seismol. Res. Lett., 81, n.2, p.311, 2010. Shi, Z., S. Ma, S.M. Day and G.P. Ely, Dynamic rupture along the San Gorgonio Pass section of the San Andreas fault, Seismol. Res. Lett., 83, n.2, p. 423, 2012. Sorlien, C.C, B.A. Campbell, W.S. Alward, L. Seeber. M.R. Legg, and M. Cormier, Transpression along strike-slip restraining segments vs regional thrusting in the Inner California Continental Borderland, 2009 SCEC Annual Meeting Proceedings & Abstracts, XIX, p.264-265 (2009). Sorlien, C. C., J. P. Gratier, B. P. Luyendyk, J. S. Hornafius, and T. E. Hopps, Map restoration of folded and faulted late Cenozoic strata across the Oak Ridge fault, onshore and offshore Ventura basin, California, Geol. Soc. America Bull., v. 112, p. 1080-1090, 2000. Sorlien, C. C., and Kamerling, M. J., 2000, Fault displacement and fold contraction estimated by unfolding of Quaternary strata, onshore and offshore Ventura basin, California, Final Report to U.S. Geological Survey NEHRP, contract 99HQGR0080. Sorlien, C. C., M. J. Kamerling, L. Seeber, and K. G. Broderick (2006), Restraining segments and reactivation of the Santa Monica–Dume–Malibu Coast fault system, offshore Los Angeles, California, J. Geophys. Res., 111, B11402, doi:10.1029/2005JB003632. Sorlien, C.C. and C. Nicholson, Suggestions for SCEC3: Providing a Unified Structural Representation for Active Faults, Folds, and Basin Development, 2004 SCEC Annual Meeting XIV, p.162-163, (2004). Sorlien, C.C, C.J. Marshall, C. Nicholson et al., Post-1 Ma deformation history of the anticline forelimb above the Pitas Point-North Channel fault in Santa Barbara Channel, California, 2012 SCEC Annual Meeting Proceedings & Abstracts, XXII, p.139-140 (2012). Sorlien, C. C., L. Seeber, K. G. Broderick, B.P. Luyendyk, M.A. Fisher, R.W. Sliter, W.R. Normark (2013), The Palos Verdes Anticlinorium along the Los Angeles, CAlifornia coast: Implications for underlying thrust faulting, G-Cubed, 14, doi:10.1002/ggge.20112. Tarnowski, J.M. and D.D. Oglesby, Dynamic models of potential earthquakes in the San Gorgonio Pass, CA, Eos (Transactions of AGU), 93 (52), Abstract S21B-2519 (2012). Teran, O.J., J.M. Fletcher, T.R. Rockwell, K.W. Hudnut, M.E. Oskin, et al., Structural controls on the surface rupture associated with the M7.2 El Mayor-Cucapah earthquake: A comparative analysis of scarp array kinematics, orientation, lithology and width, 2011 SCEC Annual Meeting, XXI, p. 236-237 (2011). Thibaut, M., J.P. Gratier, M. Léger, and J.M. Morvan (1996). An inverse method for determining three-dimensional fault geometry with thread criterion: application to strike-slip and thrust faults, J. Structural Geol., v.18, p. 1127–1138. Treiman, J.A. K.J. Kendrick, M.J. Rymer, and E.J. Fielding, Fault rupture in the Yuha Desert, California, from the El Mayor-Cucapah earthquake, and the contribution of InSAR imagery to its documentation, 2010 SCEC Annual Meeting Proceedings and Abstracts, XX, p.284 (2010). 23 Tsutsumi, H. and R.S. Yeats, Tectonic setting of the 1971 and 1994 Northridge earthquakes in the , California, Bull. Seismol. Soc. Am., v.89, n.5, p. 1,232-1,249 (1999). U.S. Geological Survey and California Geological Survey, 2006, Quaternary fault and fold database for the United States, accessed July 2010 from USGS web site: http://earthquake.usgs.gov/hazards/qfaults/. Wright, T.L., 1991, Structural geology and tectonic evolution of the Los Angeles basin, California, in Active Tectonic Basins, T.K. Biddle, ed., AAPG Memoir 52, p.35-134. Yeats, R.S.. Late Cenozoic structure of the Santa Susana fault zone, in Recent Reverse Faulting in the Transverse Ranges, California, USGS Professional Paper, 1339, p. 137-160, 1987. Yeats, R.S., Neogene tectonics of the East Ventura and San Fernando Basins, in Geology and Tectonics of the San Fernando Valley and East Ventura Basin, California, T.L. Wright and R.S. Yeats, eds, Pacific Section AAPG Guidebook, GB77, p. 9-36, 2001. Yeats, R.S., Butler, M.L., Schlueter, J.C., 1977, Geology of the central Santa Susana fault area, Ventura and Los Angeles counties, California: NEHRP final technical report, 28 p., 11 plates. Yeats, R.S. and G.J. Huftile (1995). Oak Ridge fault system and the 1994 Northridge, California, earthquake, Nature, v.373, p. 418–420. Yeats, R.S., G.J. Huftile, and L.T. Sitt, Late Cenozoic tectonics of the east Ventura basin, California, Am. Asoc. Petrol. Geol. Bull., v. 78, p.1040-1074, 1994. Yeats, R.S., Late Quaternary slip rate on the Oak Ridge Fault, Transverse Ranges, California: Implications for seismic risk, Journal of Geophysical Research, v. 93, p. 12,137-12,149, 1988. Yule, D., Research Focus: The enigmatic San Gorgonio Pass, Geology, 37, n.2, p.191-192 (2009). Yule, D, M.L. Cooke and D. Oglesby, SCEC Workshop on San Gorgonio Pass: Structure, stress, slip, and the likelihood of through-going rupture, 2012 SCEC Annual Meeting Proc. & Abstracts, XXII, p.75 (2012). Yule, D. and K. Sieh, Complexities of the San Andreas fault newar San Gorgonio Pass: Implications for large earthquakes, J. Geophys. Res., 109, n.B11, 2548, doi:10.1029/2001JB000451 (2003).

New CFM 4.0 Name & Number ID ---> Fault Area/Major Boundary Fault zone/system Fault Section Fault name Fault Strand/Branch/Model OLD CFM 3.0 Filename number name abbrev number name abbrev number name abbrev number name abbrev number name abbrev

./peninsular_ranges/anza_san_jacinto/alt1/extents/cfma_anza_san_jacinto_complete.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 03 Anza ANZA 01 Clark fault CLRF CFMA model CFMA ./peninsular_ranges/borrego_san_jacinto/alt1/extents/cfma_borrego_san_jacinto_complete.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 05 Borrego Mountain BRMT 01 Coyote Creek fault CCRF CFMA model CFMA ./peninsular_ranges/cerro_prieto/alt1/extents/cfma_cerro_prieto_extruded_90_trace_100m.ts02 Salton Trough Fault Area SALT 03 zone CPFZ 01 Cerro Prieto Basin CRPR 01 Cerro Prieto fault CRPF 90dip, extruded CFMA CFMA

./peninsular_ranges/chino/alt3/extents/cfma_chino_extruded_65_upper_complete.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 02 Chino CHNO 01 CHNF 65dip, extruded CFMA CFMA APPENDIX 1 ./peninsular_ranges/chino/alt1/extents/cfma_chino_extruded_65_crosscut_trace_100m.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 02 Chino CHNO 01 Chino fault CHNF 65 dip, cross cut CFMA CFMA ./peninsular_ranges/coachella_san_andreas/alt2/extents/cfma_san_andreas_coachella_alt2_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 05 Coachella Valley COAV 01 Southern San Andreas fault SSAF CFMA model CFMA ./peninsular_ranges/coachella_san_andreas/alt1/extents/cfma_san_andreas_coachella_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 05 Coachella Valley COAV 01 Southern San Andreas fault SSAF CFMA model CFMA ./peninsular_ranges/coyote_creek_san_jacinto/alt1/extents/cfma_coyote_creek_san_jacinto_extruded_90dip_complete.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 04 Coyote Creek CCRS 01 Coyote Creek fault CCRF 90dip, extruded CFMA CFMA ./peninsular_ranges/coyote_mountain_elsinore/alt1/extents/cfma_coyote_mountain_elsinore_complete.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 07 Coyote Mountain CYMT 01 Elsinore fault ELSF CFMA model CFMA ./peninsular_ranges/earthquake_valley_elsinore/alt2/extents/cfm_earthquake_valley_extrapolated_elongated_complete.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 06 Earthquake Valley EQVS 02 Earthquake Valley fault EQVF extrapolated CFM model CFM ./peninsular_ranges/earthquake_valley_elsinore/alt1/extents/cfma_earthquake_valley_extruded_90dip_complete.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 06 Earthquake Valley EQVS 02 Earthquake Valley fault EQVF 90dip, extruded CFMA CFMA ./peninsular_ranges/elmore_ranch/alt1/extents/cfma_elmore_ranch_extruded_90_complete.ts03 Salton Trough Fault Area SALT 01 Cross Fault 06 Imperial Valley IMPV 02 Elmore Ranch fault ELRF 90dip, extruded CFMA CFMA ./peninsular_ranges/imperial/alt1/extents/cfma_imperial_complete.ts 02 Salton Trough Fault Area SALT 02 Imperial fault zone IMFZ 01 Imperial Valley IMPV 01 Imperial fault IMPF CFMA model CFMA ./peninsular_ranges/julian_elsinore/alt1/extents/cfma_julian_elsinore_complete.ts 03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 05 Julian JULN 01 Elsinore fault ELSF CFMA model CFMA ./peninsular_ranges/san_bernardino_san_andreas/alt2/extents/cfma_san_andreas_san_bernardino_alt2_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 01 San Andreas fault SAF Mill Creek strand, CFMA MCS ./peninsular_ranges/san_bernardino_san_andreas/alt1/extents/cfma_san_bernardino_san_andreas_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 01 San Andreas fault SAF Garnet Hill strand, Yule model GHS ./peninsular_ranges/san_bernardino_san_jacinto/alt2/extents/cfm_san_bernardino_valley_san_jacinto_complete.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 00 San Bernadino-San Jacinto Valley MULT 01 San Jacinto-Claremont fault SJCF CFM model CFM ./peninsular_ranges/san_bernardino_san_jacinto/alt2/extents/cfma_san_bernardino_valley_san_jacinto_extruded_90dip.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 00 San Bernadino-San Jacinto Valley MULT 01 San Jacinto-Claremont fault SJCF 90dip, extruded CFMA CFMA ./peninsular_ranges/san_jacinto_valley_san_jacinto/alt1/extents/cfma_san_jacinto_valley_san_jacinto_extruded_90dip_complete.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 02 San Jacinto Valley SJVS 01 Casa Loma fault CSLF 90dip, extruded CFMA CFMA ./peninsular_ranges/superstition_hills_san_jacinto/alt1/extents/cfma_superstition_hills_san_jacinto_extruded_90dip_complete.ts03 Peninsular Ranges PNRA 01 San Jacinto fault zone SJFZ 06 Superstition Hills SSHS 01 Superstition Hills fault SHF 90dip, extruded CFMA CFMA ./peninsular_ranges/superstition_mountain_san_jacinto/alt1/extents/cfma_superstition_mountain_san_jacinto_extruded_90dip_comple03 Peninsular Ranges PNRA te.ts01 San Jacinto fault zone SJFZ 07 Superstition Mountain SSMT 01 Superstition Mountain fault SMF 90dip, extruded CFMA CFMA ./peninsular_ranges/temecula_elsinore/alt3/extents/cfm_temecula_elsinore_short_complete.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 04 Temecula TMCL 01 Willard fault WLRF short CFM model CFM ./peninsular_ranges/brawley_seismic_zone/alt1/extents/cfma_brawley_seismic_zone_complete.ts02 Salton Trough Fault Area SALT 01 Brawley Seismic Zone BRSZ 01 Brawley seismic zone BSZ 01 Brawley seismic zone BSZ CFMA model CFMA ./peninsular_ranges/glen_ivy_elsinore/alt3/extents/cfma_glen_ivy_complete_3.ts 03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 03 Glen Ivy GLIV 01 Glen Ivy North fault GINF CFMA model CFMA ./peninsular_ranges/laguna_salada/alt1/extents/cfma_laguna_salada_extruded_90_complete.ts03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 08 Laguna Salada LGSD 01 Laguna Salada fault LSF 90dip, extruded CFMA CFMA ./peninsular_ranges/banning/alt1/extents/cfma_banning_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 02 Banning fault BNNF 90dip, Yule model YULE ./peninsular_ranges/garnet_hill/alt1/extents/cfma_garnet_hill_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 00 San Bernardino Mtns-Coachella ValleyMULT 05 Garnet Hill fault GHF Yule model YULE ./peninsular_ranges/gorgonio_pass/alt1/extents/cfma_gorgonio_pass_complete.ts 01 San Andreas Fault System SAFS 02 San Gorgonio Pass fault region SGPS 01 San Gorgonio Pass SGP 01 San Gorgonio Pass fault SGPF Yule model YULE ./peninsular_ranges/mill_creek/alt3/extents/mill_complete_90_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 03 Mill Creek fault MLCF 90dip, CFMA CFMA ./peninsular_ranges/mill_creek/alt1/extents/mill_creek_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 03 Mill Creek fault MLCF CFMA model CFMA ./peninsular_ranges/mill_creek/alt2/extents/mill_creek_truncated_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 03 Mill Creek fault MLCF CFMA model CFMA ./peninsular_ranges/mission_creek/alt1/extents/mission_creek_65_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 04 Mission Creek fault MSCF 65dip, CFMA CFMA /peninsular_ranges/mission_creek/alt2/extents/mission_creek_alt2_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 04 Mission Creek fault MSCF CFMA model CFMA ./peninsular_ranges/canada_david/alt1/extents/cfm_canada_david_detachment_extruded_complete.ts03 Peninsular Ranges PNRA Northern Baja Detachments? NBJD Canada-David CDS Canada-David detachment CDD extruded CFM model CFM ./peninsular_ranges/cerro_centinela/alt1/extents/cfm_cerro_centinela_detachment_extruded_complete.ts03 Peninsular Ranges PNRA Northern Baja Detachments? NBJD Cerro Centinela CCS Cerro Centinela detachment CCD extruded CFM model CFM 01 San Andreas Fault System San Andreas fault zone SAFZ Coachella Valley COAV North Palm Springs NPSF 01 San Andreas Fault System San Gorgonio Pass deformation region SGPR San Jacinto Mountain SGP Palm Springs fault PLSF 01 San Andreas Fault System San Gorgonio Pass deformation region SGPR Crafton Hills SGP Crafton Hills fault CRHF 01 San Andreas Fault System San Gorgonio Pass deformation region SGPR San Gorgonio Pass SGP west Banning fault WBNF ./san_andreas_garlock/owl_lake/alt1/extents/cfma_owl_lake_w_to_e_extruded_90_complete.ts08 Garlock Fault System GRFS 01 Garlock fault zone GRFZ 03 Eastern EAST 02 Owl Lake fault OWLF 01 90dip, extruded CFMA CFMA ./san_andreas_garlock/1857_rupture/alt1/extents/cfma_1857_rupture_extruded_1_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 06 1857 rupture-Parkfield-Mojave 1857 01 San Andreas fault SAF 1857 rupture, extruded CFMA 1857 ./san_andreas_garlock/carrizo/alt1/extents/cfma_carrizo_extruded_1_complete.ts 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 02 Cholame-Carrizo CLCZ 01 San Andreas fault SAF Carrizo extruded CFMA CFMA ./san_andreas_garlock/mojave/alt1/extents/cfm_san_andreas_mojave_extruded_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 03 Mojave MJVS 01 San Andreas fault SAF Mojave extruded CFM CFM ./san_andreas_garlock/parkfield/alt1/extents/cfma_sa_parkfield_extruded_90dip_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 01 Parkfield PARK 01 San Andreas fault SAF 90dip, Parkfield extruded CFMA CFMA ./san_andreas_garlock/cholame/alt1/extents/cfma_sa_cholame_extrapolated_complete.ts01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 02 Cholame-Carrizo CLCZ 01 San Andreas fault SAF Cholame extrapolated CFMA CFMA ./san_andreas_garlock/garlock/alt1/extents/cfma_garlock_complete.ts 08 Garlock Fault System GRFS 01 Garlock fault zone GRFZ 00 Western-Eastern MULT 01 Garlock fault GRLF CFMA model CFMA ./san_andreas_garlock/coalinga/alt1/extents/cfm_coalinga_complete.ts 11 Great Valley Fault Area GVFA Temblor-Diablo Range fault system TDRS Coalinga COAL Coalinga COAL CFM model CFM ./san_andreas_garlock/kettleman_hills_north_dome/alt1/extents/cfm_kettleman_hills_north_dome_complete.ts11 Great Valley Fault Area GVFA Temblor-Diablo Range fault system TDRS Kettleman Hills KTLM Kettleman Hills KMHF CFM model CFM ./san_andreas_garlock/lost_hills/alt1/extents/cfm_lost_hills_ramp_complete.ts 11 Great Valley Fault Area GVFA Temblor-Diablo Range fault system TDRS Lost Hills LSTH Lost Hills LSHF CFM model CFM ./san_andreas_garlock/pleito/alt2/extents/cfm_pleito_truncated_complete.ts 11 Great Valley Fault Area GVFA Pleito fault zone PLFZ 00 Western-Eastern MULT 01 Pleito fault PLTF truncated CFM model CFM ./san_andreas_garlock/pleito/alt1/extents/cfma_pleito_extruded_complete.ts 11 Great Valley Fault Area GVFA Pleito fault zone PLFZ 00 Western-Eastern MULT 02 Pleito fault PLTF extruded CFMA model CFMA ./san_andreas_garlock/scodie/alt1/extents/cfma_scodie_lineament_68_deep_complete.ts11 Great Valley Fault Area GVFA White Wolf fault zone WWFZ 03 Eastern EAST 02 Scodie lineament SCOL 68dip, CFMA model CFMA ./san_andreas_garlock/lake_isabella_seismicity/alt1/extents/cfm_lake_isabella_seismicity_extruded_complete.ts11 Great Valley Fault Area GVFA Lake Isabelle Lineamnet zone LILZ Central CNTR Isabelle seismicity lineament ISBS extruded CFM model CFMA ./san_andreas_garlock/white_wolf/alt1/extents/cfma_white_wolf_long_complete.ts 11 Great Valley Fault Area GVFA White Wolf fault zone WWFZ 00 Western-Central MULT 01 White Wolf fault WWF long CFMA model CFMA ./death_valley/death_valley/alt1/extents/cfma_death_valley_complete.ts 09 Basin and Range Fault Area BNRA fault zone DVFZ 00 Northern-Southern MULT 01 Death Valley fault DVF CFMA model CFMA ./death_valley/death_valley/alt2/extents/cfm_death_valley_smooth_complete.ts 09 Basin and Range Fault Area BNRA DVFZ 00 Northern-Southern MULT 01 Death Valley fault DVF smooth, CFM model CFM ./death_valley/death_valley/alt3/extents/cfm_death_valley_split_complete.ts 09 Basin and Range Fault Area BNRA Death Valley fault zone DVFZ 00 Northern-Southern MULT 01 Death Valley fault DVF split, CFM model CFM ./death_valley/furnace_creek/alt1/extents/cfma_furnace_creek_complete.ts 09 Basin and Range Fault Area BNRA FCFZ 01 Furnace Creek FCRS 01 Furnace Creek fault FCRF CFMA model CFMA ./death_valley/furnace_creek/alt2/extents/cfm_furnace_creek_long_complete.ts 09 Basin and Range Fault Area BNRA Furnace Creek fault zone FCFZ 01 Furnice Creek FCRS 01 Furnace Creek fault FCRF long, CFM model CFM ./death_valley/hunter_mountain_saline_valley/alt1/extents/cfma_hunter_mountain_complete.ts10 Sierra Nevada Fault Area SNFA Hunter Mountain fault zone HMFZ 00 Hunter Mtn-Saline Valley MULT 01 Hunter Mountain fault HMTF CFMA model CFMA ./death_valley/independence/alt1/extents/cfma_independance_complete.ts 10 Sierra Nevada Fault Area SNFA Southern Sierra Nevada fault zone SNFZ 01 Independence INDP 01 Independence fault INDF CFMA model CFMA ./death_valley/owens_valley/alt1/extents/cfma_owens_valley_complete.ts 10 Sierra Nevada Fault Area SNFA Owens Valley fault zone OVFZ 01 1872 rupture 1872 01 Owens Valley fault OVF CFMA model CFMA ./death_valley/little_lake/alt1/extents/cfma_little_lake_complete.ts 10 Sierra Nevada Fault Area SNFA Little Lake fault zone LLFZ 01 Central CNTR 01 Little Lake fault LLF CFMA model CFMA ./death_valley/panamint_valley/alt2/extents/cfm_panamint_valley_low_dip_truncated_at_garlock_complete.ts10 Sierra Nevada Fault Area SNFA Panamint Valley fault zone PMVZ 00 Northern Panamint-Brown Mtn MULT 01 Panamint Valley fault PMVF low-dip, truncated@GARF CFM ./death_valley/panamint_valley/alt1/extents/cfma_panamint_valley_complete.ts 10 Sierra Nevada Fault Area SNFA Panamint Valley fault zone PMVZ 00 Northern Panamint-Brown Mtn MULT 01 Panamint Valley fault PMVF CFMA model CFMA ./death_valley/sierra_nevada/alt2/extents/cfma_sierra_nevada_truncated_at_garlock_complete.ts10 Sierra Nevada Fault Area SNFA Southern Sierra Nevada fault zone SNFZ 00 Independence-Haiwee Reservoir MULT Independence-Sierra Nevada fault ISNF truncated @ GARF, CFMA CFMA ./death_valley/tank_canyon/alt2/extents/cfm_tank_canyon_truncated_at_panamint_complete.ts10 Sierra Nevada Fault Area SNFA Ash Hill-Tank Canyon fault system AHTC 02 Tank Canyon TANK 01 Tank Canyon fault TNCF truncated@PNMF, CFM CFM ./death_valley/tank_canyon/alt1/extents/cfma_tank_canyon_complete.ts 10 Sierra Nevada Fault Area SNFA Ash Hill-Tank Canyon fault system AHTC 02 Tank Canyon TANK 01 Tank Canyon fault TNCF CFMA model CFMA ./death_valley/ash_hill/alt1/extents/cfm_ash_hill_extruded_cut_to_pv_complete.ts 10 Sierra Nevada Fault Area SNFA Ash Hill-Tank Canyon fault system AHTC 01 Ash Hill ASHH 01 Ash Hill fault ASHF cut 2 PV extruded CFM CFM ./los_angeles/fontana_seismicity/alt1/extents/cfma_fontana_seismicity_bestfit_complete.ts03 Peninsular Ranges PNRA Cross fault CRSF 01 Upper Santa Ana Valley USAV Fontana Seismicity lineament FNTS bestfit, CFMA model CFMA ./los_angeles/las_cienagas/alt1/extents/cfma_las_cienagas_extrapolated.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 03 Los Angeles basin LAB 02 Las Cienagas LCGF extrapolated CFMA ./los_angeles/lower_elysian_park/alt1/extents/pre_cfma_lower_elysian_park_deep_complete.tsPeninsular Ranges PNRA Compton-Lower Elysian Park fault system CEPS 01 Los Angeles basin LAB 02 Lower Elysian Park fault LEPF lower-deep, CFMA model CFMA ./los_angeles/north_salt_lake/alt1/extents/cfma_north_salt_lake_1_complete.ts Western Tranverse Ranges WTRA Southern Frontal fault system SFFS 02 Los Angeles basin LAB North Salt Lake fault NSLF CFMA model CFMA ./los_angeles/san_jose/alt1/extents/cfma_san_jose_74dip_complete.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 01 Upper Santa Ana Valley USAV 02 San Jose fault SNJF 01 74dip, CFMA model CFMA ./los_angeles/san_jose/alt2/extents/cfma_san_jose_50_74dip_complete.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 01 Upper Santa Ana Valley USAV 02 San Jose fault SNJF 02 50-74dip, CFMA model CFMA ./los_angeles/san_jose/alt3/extents/cfma_san_jose_extruded_50dip_complete.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 01 Upper Santa Ana Valley USAV 02 San Jose fault SNJF 03 50dip, extruded CFMA CFMA ./los_angeles/san_vicente/alt1/extents/cfma_san_vicente_extrapolated.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 03 Los Angeles basin LAB 01 San Vicente fault SNVF extrapolated CFMA Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 04 SMMT 01 Santa Monica thrust SMCT ./los_angeles/santa_monica/alt1/extents/cfma_santa_monica_complete.ts 05 Western Tranverse Ranges WTRA Southern Frontal fault system SFFS 02 Santa Monica Mountains SMMT 01 Santa Monica fault SMCF CFMA model CFMA ./los_angeles/upper_elysian_park/alt1/extents/pre_cfma_upper_elysian_park_constant_dip_50_complete.tsWestern Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 03 Los Angeles basin LAB 03 Upper Elysian Park fault EPF 01 50dip, upper pre-CFMA PCFM ./los_angeles/upper_elysian_park/alt2/extents/pre_cfma_upper_elysian_park_constant_dip_45_30_complete.tsWestern Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 03 Los Angeles basin LAB 03 Upper Elysian Park fault EPF 02 30-45dip, upper pre-CFMA PCFM ./los_angeles/upper_elysian_park/alt3/extents/pre_cfma_upper_elysian_park_constant_dip_60_complete.tsWestern Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 03 Los Angeles basin LAB 03 Upper Elysian Park fault EPF 03 60dip, upper pre-CFMA PCFM ./los_angeles/peralta_hills/alt1/extents/cfma_peralta_hills_complete.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 02 Puente Hills PHS 02 Peralta Hills fault PRHF CFMA model CFMA ./los_angeles/richfield_blind/alt1/extents/cfma_richfield_complete.ts Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 02 Puente Hills PHS 01 Puente Hills thrust PHT 02 Richfield fault CFMA ./los_angeles/compton/alt1/extents/cfma_compton_complete.ts 03 Peninsular Ranges PNRA Compton-Lower Elysian Park fault system CEPS 01 Los Angeles basin LAB 01 Compton thrust CPTF CFMA model CFMA ./los_angeles/hollywood/alt1/extents/cfma_hollywood_complete.ts 05 Western Tranverse Ranges WTRA Southern Frontal fault system SFFS 02 Los Angeles basin LAB 02 HWDF CFMA model CFMA ./los_angeles/clamshell_sawpit/alt1/extents/cfma_clamshell_sawpit_complete.ts Western Tranverse Ranges WTRA SMFZ 05 Clamshell-Sawpit Canyon CSPC 01 Clamshell-Sawpit Canyon fault CSPF CFMA model CFMA ./los_angeles/anaheim_blind/alt1/extents/cfma_anaheim_complete.ts 03 Peninsular Ranges PNRA Compton-Lower Elysian Park fault system CEPS 01 Los Angeles basin LAB 03 Anaheim fault ANHF 03 CFMA model CFMA ./los_angeles/anaheim_blind/alt2/extents/cfma_anaheim_highway_extruded_35dip_complete.ts03 Peninsular Ranges PNRA Compton-Lower Elysian Park fault system CEPS 01 Los Angeles basin LAB 03 Anaheim fault ANHF 04 35dip, extruded CFMA CFMA ./los_angeles/newport_inglewood/alt1/extents/cfma_newport_inglewood_complete.ts03 Peninsular Ranges PNRA Newport-Inglewood fault zone NIFZ 00 North-South Los Angeles Basin MULT 01 Newport-Inglewood- NIF CFMA model CFMA ./los_angeles/newport_inglewood/alt2/extents/cfma_newport_inglewood_branches_complete.ts03 Peninsular Ranges PNRA Newport-Inglewood fault zone NIFZ 00 North-South Los Angeles Basin MULT 01 Newport-Inglewood-Rose Canyon fault NIF branches, CFMA model CFMA ./los_angeles/newport_inglewood/alt3/extents/cfma_newport_inglewood_split_complete.ts03 Peninsular Ranges PNRA Newport-Inglewood fault zone NIFZ 00 North-South Los Angeles Basin MULT 01 Newport-Inglewood-Rose Canyon fault NIF split CFMA model CFMA ./los_angeles/puente_hills/alt1/extents/cfma_puente_hills_complete.ts 03 Peninsular Ranges PNRA Southern Boundary Thrust system SBTS 02 Puente Hills PHS 01 Puente Hills thrust PHT 01 CFMA model CFMA Los Angeles Santa Fe Springs Coyote Hills

./los_angeles/raymond/alt1/extents/cfma_raymond_complete.ts 05 Western Tranverse Ranges WTRA Southern Frontal fault system SFFS 01 SGV 01 RYMF CFMA model CFMA 24 ./los_angeles/cucamonga/alt2/extents/cfm_cucamonga_extruded_truncated_at_sa_complete.ts05 Western Tranverse Ranges WTRA Sierra Madre fault zone SMFZ 06 Cucamonga CUCM 02 Cucamonga fault CMGF 01 truncated@SAF, extruded CFM CFM ./los_angeles/cucamonga/alt1/extents/cfma_cucamonga_complete.ts 05 Western Tranverse Ranges WTRA Sierra Madre fault zone SMFZ 06 Cucamonga CUCM 02 Cucamonga fault CMGF 02 CFMA model CFMA ./los_angeles/sierra_madre/alt1/extents/cfma_sierra_madre_complete.ts 05 Western Tranverse Ranges WTRA Sierra Madre fault zone SMFZ 00 Sections B-E MULT 01 Sierra Madre fault SMDF 01 CFMA model CFMA ./los_angeles/sierra_madre/alt2/extents/cfm_sierra_madre_extruded_complete.ts 05 Western Tranverse Ranges WTRA Sierra Madre fault zone SMFZ 00 Sections B-E MULT 01 Sierra Madre fault SMDF 02 extruded CFM model CFM ./los_angeles/upland/alt1/extents/cfma_upland_strikeslip_complete.ts 05 Western Tranverse Ranges WTRA Southern Boundary thrust system SBTS 01 Upper Santa Ana Valley USAV 01 Upland fault UPLF 01 strike-slip CFMA model CFMA

./los_angeles/upland/alt2/extents/cfma_upland_dipslip_complete.ts 05 Western Tranverse Ranges WTRA Southern Boundary Thrust system SBTS 01 Upper Santa Ana Valley USAV 01 Upland fault UPLF 02 dip-slip CFMA model CFMA ./los_angeles/verdugo/alt2/extents/cfma_verdugo_complete.ts 05 Western Tranverse Ranges WTRA San Fernando fault system SFNS VRMS Verdugo fault VRDF 02 CFMA model CFMA APPENDIX 1 ./los_angeles/verdugo/alt1/extents/cfma_verdugo_complete.ts 05 Western Tranverse Ranges WTRA San Fernando fault system SFNS Verdugo Mountains VRMS Verdugo fault VRDF 01 CFMA model CFMA ./los_angeles/whittier/alt4/extents/cfm_whittier_split_complete.ts 03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 01 Whittier WHIT 01 WHTF split CFM model CFM ./los_angeles/whittier/alt3/extents/cfma_whittier_complete.ts 03 Peninsular Ranges PNRA 02 Elsinore-Laguna Salada fault zone ELSZ 01 Whittier WHIT 01 Whittier fault WHTF CFMA model CFMA ./los_angeles/yorba_linda/alt1/extents/cfm_yorba_linda_extruded_complete.ts 03 Peninsular Ranges PNRA 02 Cross fault CRSF CHNH Yorba Linda lineation YLL extruded CFM model CFM ./los_angeles/east_montebello/alt1/extents/cfma_alhambra_complete.ts 03 Peninsular Ranges PNRA Elsinore-Laguna Salada fault zone ELSZ East Montebello EMTB Alhambra fault ALHF CFMA model CFMA ./los_angeles/san_joaquin_hills/alt1/extents/cfm_san_joaquin_hills_extruded_complete.ts03 Peninsular Ranges PNRA Coastal faults CSTL San Joaqin Hills SJQH San Joaqin Hills fault? SJHF extruded CFM model CFM ./los_angeles/workman_hill/alt1/extents/cfma_workman_hill_extruded_75dip_complete.ts03 Peninsular Ranges PNRA Elsinore-Laguna Salada fault zone ELSZ Whittier WHIT Workman Hill fault WMHF 75dip, extruded CFMA CFMA 03 Peninsular Ranges PNRA Cross fault CRSF San Jose Hills SJSH Walnut Creek fault WNCF 03 Peninsular Ranges PNRA Elsinore-Laguna Salada fault zone Whittier WHIT Whittier Heights WTHF ./mojave/bicycle_lake/alt1/extents/cfma_bicycle_lake_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA 01 Northeast NE Bicycle Lake fault BCLF 90dip, extruded CFMA CFMA ./mojave/blackwater/alt1/extents/cfma_blackwater_extruded_90_trace_100m.ts 07 Mojave Fault Area MJVA Blackwater fault zone BWFZ 00 Northern-Southern MULT Blackwater fault BWF 90dip, extruded CFMA CFMA ./mojave/burnt_mountain-east_wide_canyon/alt1/extents/cfm_burnt_mountain_east_wide_canyon_extruded_complete.ts06 Eastern Transverse Ranges ETRA Little San Bernardino Mtns fault system LSBM 02 Burnt Mountain BRMT 02 East Wide Canyon fault EWCF extruded CFM model CFM ./mojave/burnt_mountain/alt1/extents/cfma_burnt_mountain_extruded_1_complete.ts06 Eastern Transverse Ranges ETRA Little San Bernardino Mtns fault system LSBM 02 Burnt Mountain BRMT 01 Burnt Mountain fault BMTF extruded CFMA model CFMA ./mojave/cady/alt1/extents/cfma_cady_extruded_90_complete.ts 07 Mojave Fault Area MJVA 02 Central CNTR Cady fault CDYF 90dip, extruded CFMA CFMA ./mojave/calico_hidalgo/alt1/extents/cfma_calico_hidalgo_extruded_90_complete.ts07 Mojave Fault Area MJVA Calico-Hildalgo fault zone CHFZ 00 Calico-Hildalgo MULT 01 Calico-Hidalgo fault CHF 90dip, extruded CFMA CFMA ./mojave/cleghorn/alt1/extents/cfma_cleghorn_extruded_1_complete.ts 07 Mojave Fault Area MJVA Cleghorn fault zone CLFZ 00 Northern-Southern MULT 01 Cleghorn fault CLHF extruded CFMA model CFMA ./mojave/coyote_canyon/alt1/extents/cfma_coyote_canyon_extruded_90_complete.ts07 Mojave Fault Area MJVA Tiefort Mountains fault zone TMFZ 01 Central CNTR Coyote Canyon fault CCYF 90dip, extruded CFMA CFMA ./mojave/coyote_lake/alt1/extents/cfma_coyote_lake_extruded_90_trace_100m.ts 07 Mojave Fault Area MJVA Coyote Lake fault zone CLFZ 01 Central CNTR Coyote Lake fault CLKF 90dip, extruded CFMA CFMA ./mojave/east_north_frontal_zone/alt1/extents/cfma_east_north_frontal_zone_extruded_1_complete.ts06 Eastern Transverse Ranges ETRA North Frontal thrust system NFTS 02 Eastern EAST Eastern North Frontal thrust ENFT extruded CFMA model CFMA ./mojave/east_north_frontal_zone/alt2/extents/cfm_east_north_frontal_zone_smooth_extruded_complete.ts06 Eastern Transverse Ranges ETRA North Frontal thrust system NFTS 02 Eastern EAST Eastern North Frontal thrust ENFT smooth, extruded CFM CFM ./mojave/garlic_springs/alt1/extents/cfma_garlic_springs_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA 01 Northeast NE Garlic Spring fault GSPF 90dip, extruded CFMA CFMA ./mojave/goldstone_lake/alt1/extents/cfma_goldstone_lake_extruded_90_complete.ts07 Mojave Fault Area MJVA Goldstone Lake-Paradise fault system GLPS 01 Goldstone Lake GLDS Goldstone Lake fault GSLF 90dip, extruded CFMA CFMA ./mojave/gravel_hills_harper_lake/alt1/extents/cfma_gravel_hills_harper_lake_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA Harper fault zone 00 Gravel Hills-Harper Lake MULT Gravel Hills-Harper Lake fault GHLF 90dip, extruded CFMA CFMA ./mojave/hector_mine/alt1/extents/cfma_hector_mine_extruded_90_complete.ts 07 Mojave Fault Area MJVA Eastern California shear zone ECSZ 02 Lavic Lake-Bullion-Mesquite Lake 1994 Hector Mine rupture HCMR 90dip, extruded CFMA CFMA ./mojave/helendale_south_lockhardt/alt1/extents/cfma_helendale_south_lockhardt_extruded_90_complete.ts07 Mojave Fault Area MJVA Helendale-South Lockhart fault zone HSLZ 00 South Lockhart-San Bernardino MtnsMULT Helendale-South Lockhart fault HSLF 90dip, extruded CFMA CFMA ./mojave/johnson_valley/alt2/extents/cfm_johnson_valley_extruded_90_100m.ts 07 Mojave Fault Area MJVA Johnson Valley fault zone JVFZ 00 Northern-Southern MULT Johnson Valley fault JVF 90dip, extruded CFM CFM ./mojave/johnson_valley/alt1/extents/cfma_johnson_valley_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA Johnson Valley fault zone JVFZ 00 Northern-Southern MULT Johnson Valley fault JVF 90dip, extruded CFMA CFMA ./mojave/landers/alt2/extents/cfm_landers_detailed_complete.ts 07 Mojave Fault Area MJVA Eastern California shear zone ECSZ 01 Camp Rock-Homestead-Johnson Valley1992 Landers rupture LNDR CFM model CFM ./mojave/landers/alt3/extents/cfm_landers_detailed_splays_complete.ts 07 Mojave Fault Area MJVA Eastern California shear zone ECSZ 01 Camp Rock-Homestead-Johnson Valley1992 Landers rupture LNDR CFM model CFM ./mojave/lenwood_lockhardt_old_woman_springs/alt1/extents/cfma_lenwood_lockhardt_old_woman_springs_extruded_90_complete.ts07 Mojave Fault Area MJVA Lenwood-Lockhart fault zone LLFZ 00 Lenwood-Lockhart- Old Woman SpringsMULT 01 Lenwood-Lockhart fault LLOF 90dip, extruded CFMA CFMA ./mojave/ludlow/alt1/extents/cfma_ludlow_extruded_90_trace_100m.ts 07 Mojave Fault Area MJVA Ludlow fault zone LDWZ 00 North-South MULT Ludlow fault LDLF 90dip, extruded CFMA CFMA ./mojave/manix_afton_hills/alt1/extents/cfma_manix_afton_hills_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA Manix fault zone MNXZ 00 East-West MULT Manix fault MNXF 90dip, extruded CFMA CFMA ./mojave/mclean_lake_drink_water_lake/alt1/extents/cfma_mclean_lake_drinkwater_lake_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA Granite Mountains fault system GMFS 02 Northern East-West NEW McLean-Drinkwater Lake fault? MDLF 90dip, extruded CFMA CFMA ./mojave/nelson_lake/alt1/extents/cfma_nelson_lake_extruded_90_complete.ts 07 Mojave Fault Area MJVA Granite Mountains fault system GMFS 01 Southern East-West SEW Nelson Lake fault? NLF 90dip, extruded CFMA CFMA ./mojave/paradise/alt1/extents/cfma_paradise_extruded_90_complete.ts 07 Mojave Fault Area MJVA Goldstone Lake-Paradise fault system GLPS 02 Paradise PRDS Paradise fault PRDF 90dip, extruded CFMA CFMA ./mojave/pinto_mountain/alt1/extents/cfma_pinto_mountain_extruded_90_trace_100m.ts06 Eastern Transverse Ranges ETRA Pinto Mountain fault zone PMFZ 00 East-West MULT 01 Pinto Mountain fault PMF 90dip, extruded CFMA CFMA ./mojave/pisgah_bullion_mountain_mesquite_lake/alt1/extents/cfma_pisgah_bullion_mesquite_lake_extruded_90_trace_100m.ts07 Mojave Fault Area MJVA Pisgah-Bullion fault zone PBFZ 00 Pisgah-Bullion-Mesquite Lake MULT Pisgah-Bullion-Mesquite Lake fault PBMF 90dip, extruded CFMA CFMA ./mojave/red_pass/alt1/extents/cfma_red_pass_extruded_90_complete.ts 07 Mojave Fault Area MJVA 01 Northeast NE Red Pass fault RDPF 90dip, extruded CFMA CFMA ./mojave/south_emerson_copper_mountain/alt1/extents/cfma_south_emerson_copper_mountain_extruded_90_complete.ts07 Mojave Fault Area MJVA Camp Rock-Emerson-Copper Mtn fault zone CREC 00 Emerson-Copper Mtn MULT Emerson-Copper Mtn fault ECMF 90dip, extruded CFMA CFMA ./mojave/west_north_frontal_zone/alt1/extents/cfma_west_north_frontal_zone_extruded_1_complete.ts06 Eastern Transverse Ranges ETRA Northern Frontal thrust system NFTS 01 Western-Ord Mtn-White Mtn thrust WEST Western North Frontal thrust WNFT extruded CFMA model CFMA ./mojave/blue_cut/alt1/extents/cfm_blue_cut_extruded_complete.ts 06 Eastern Transverse Ranges ETRA Blue Cut fault zone BCFZ East-West MULT Blue Cut fault BCTF extruded CFM model CFM ./mojave/eureka_peak-west_deception_canyon/alt1/extents/cfm_eureka_peak_west_deception_canyon_extruded_100m.ts06 Eastern Transverse Ranges ETRA Little San Bernardino Mtns fault system LSBM 01 Eureka Peak ERPK 02 West Deception Canyon fault WDCF extruded CFM model CFM ./mojave/eureka_peak/alt1/extents/cfma_eureka_peak_extruded_1_complete.ts 06 Eastern Transverse Ranges ETRA Little San Bernardino Mtns fault system LSBM 01 Eureka Peak ERPK 01 Eureka Peak fault EPKF extruded CFMA model CFMA ./mojave/galway_lake/alt1/extents/cfm_galway_lake_complete.ts 07 Mojave Fault Area MJVA Camp Rock-Emerson-Copper Mtn fault zone CREC 02 Emerson EMRS Galway lake fault GLKF CFM model CFM ./mojave/big_bear/alt1/extents/cfm_big_bear_rupture_complete.ts 06 Eastern Transverse Ranges ETRA Big Bear fault system BBFS 01 San Bernardino Mountains 1992 Big Bear rupture BGBR CFM model CFM ./mojave/camp_rock/alt1/extents/cfm_camp_rock_complete.ts 07 Mojave Fault Area MJVA Camp Rock-Emerson-Copper Mtn fault zone CREC 00 Camp Rock-Copper Mtn MULT 01 Camp Rock-Emerson-Copper Mtn faultCREF CFM model CFM ./mojave/joshua_tree_seismicity/alt1/extents/cfm_joshua_tree_seismicity_extruded_complete.ts06 Eastern Transverse Ranges ETRA Little San Bernardino Mtns fault system LSBM 03 Joshua Tree sequence 1992 Joshua Tree seismicity JTEQ extruded CFM model CFM ./ventura_c_transverse_ranges/delvalle/alt3/extents/cfma_del_valle_complete_cut_at_ss.ts05 Western Transverse Ranges WTRA San Cayetano fault zone SCFZ SCVA Del Valle fault DVLF CFMA model CFMA ./ventura_c_transverse_ranges/delvalle/alt1/extents/cfma_del_valle_complete.ts 05 Western Transverse Ranges WTRA San Cayetano fault zone SCFZ Santa Clarita Valley SCVA Del Valle fault DVLF CFMA model CFMA ./ventura_c_transverse_ranges/holser/alt2/extents/cfma_holser_complete_cut_at_ss.ts05 Western Transverse Ranges WTRA San Cayetano fault zone SCFZ Santa Clarita Valley SCVA Holser fault HLSF CFMA model CFMA ./ventura_c_transverse_ranges/holser/alt1/extents/cfma_holser_complete.ts 05 Western Transverse Ranges WTRA San Cayetano fault zone SCFZ Santa Clarita Valley SCVA Holser fault HLSF CFMA model CFMA ./ventura_c_transverse_ranges/oakridge_onshore/alt1/extents/cfma_oakridge_on_complete.ts05 Western Transverse Ranges WTRA Oak Ridge fault zone ORFZ Ventura basin VNTB Oak Ridge fault ORF CFMA model CFMA ./ventura_c_transverse_ranges/san_cayetano/alt1/extents/cfma_san_cayetano_complete.ts05 Western Transverse Ranges WTRA San Cayetano fault zone SCFZ Western+Modelo Lobe MULT San Cayetano fault SCTF CFMA model CFMA ./ventura_c_transverse_ranges/san_cayetano/alt2/extents/cfma_san_cayetano_extruded_complete.ts05 Western Transverse Ranges WTRA San Cayetano fault zone SCFZ Western+Modelo Lobe MULT San Cayetano fault SCTF extruded CFMA model CFMA ./ventura_c_transverse_ranges/santa_susana/alt1/extents/cfma_santa_susana_complete.ts05 Western Transverse Ranges WTRA Santa Susana fault zone SSFZ 00 Santa Susana Mts-San Fernando ValleyMULT 01 Santa Susana fault SSF CFMA model CFMA ./ventura_c_transverse_ranges/anacapa_dume/alt2/extents/cfma_dume_connected_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS 02 Anacapa Anacapa-Dume fault ANDF connected CFMA model CFMA ./ventura_c_transverse_ranges/malibu_coast/alt3/extents/cfma_malibu_coast_extrapolated_truncated_complete.ts05 Western Transverse Ranges WTRA Southern Frontal fault system SFFS 02 Santa Monica Mountains SMMT Malibu Coast fault MBCF truncated, extrapolated CFMA CFMA ./ventura_c_transverse_ranges/malibu_coast/alt1/extents/cfma_malibu_coast_extrapolated_complete.ts05 Western Transverse Ranges WTRA Southern Frontal fault system SFFS 02 Santa Monica Mountains SMMT Malibu Coast fault MBCF extrapolated CFMA model CFMA ./ventura_c_transverse_ranges/northridge/alt3/extents/cfm_northridge_smoothed_truncated_at_top_complete.ts05 Western Transverse Ranges WTRA Oak Ridge fault zone ORFZ San Fernando Valley SFNV Northridge fault NRDF truncated@top, smooth CFM CFM ./ventura_c_transverse_ranges/northridge/alt1/extents/cfma_northridge_complete.ts05 Western Transverse Ranges WTRA Oak Ridge fault zone ORFZ San Fernando Valley SFNV Northridge fault NRDF CFMA model CFMA ./ventura_c_transverse_ranges/simi_santa_rosa/alt1/extents/cfma_simi_complete.ts05 Western Transverse Ranges WTRA Simi-Santa Rosa fault zone SSRZ 00 Springfield-Camarillo- Santa Rosa MULT Simi-Santa Rosa fault SSRF CFMA model CFMA ./ventura_c_transverse_ranges/sisar/alt1/extents/cmfa_sisar_complete.ts 05 Western Transverse Ranges WTRA Sisar-Lion Canyon fault zone SLCZ Ventura Basin VNTB Sisar fault SISF CFMA model CFMA ./ventura_c_transverse_ranges/sisar/alt2/extents/pre_cfma_sisar_lion_canyon_interpolated_complete.ts05 Western Transverse Ranges WTRA Sisar-Lion Canyon fault zone SLCZ Ventura Basin VNTB Sisar-Lion Canyon fault SLCF interpolated pre-CFMA PCFM ./ventura_c_transverse_ranges/ventura_pitas_point/alt1/extents/cfma_ventura_pitas_point_complete_extrapolated.ts05 Western Transverse Ranges WTRA North Channel fault system NCFS Pitas Point-Ventura PPTV Ventura-Pitas Point fault VPPF extrapolated CFMA model CFMA ./ventura_c_transverse_ranges/northridge_hills/alt1/extents/cfm_northridge_hills_extruded_complete.ts05 Western Transverse Ranges WTRA San Fernando fault system SFNS San Fernando Valley SFNV Northridge Hills fault NHLF extruded CFM model CFM ./ventura_c_transverse_ranges/north_san_gabriel/alt1/extents/cfma_north_san_gabriel_extruded_60_complete.ts05 Western Transverse Ranges WTRA zone SGFZ 01 Palomas PLMS Northern San Gabriel fault NSGF 60dip, extruded CFMA CFMA ./ventura_c_transverse_ranges/south_san_gabriel/alt1/extents/cfma_south_san_gabriel_extruded_60_complete.ts05 Western Transverse Ranges WTRA San Gabriel fault zone SGFZ 02 Honor Rancho-San Gabriel River MULT Southern San Gabriel fault SSGF 60dip, extruded CFMA CFMA ./ventura_c_transverse_ranges/san_gabriel/alt1/extents/cfma_san_gabriel_extruded_complete.ts05 Western Transverse Ranges WTRA San Gabriel fault zone SGFZ 00 Palomas-Honor Rancho-San Gabriel MULTRiver San Gabriel fault SGF extruded CFMA model CFMA ./santa_barbara_w_transverse_ranges/channel_islands/alt1/extents/cfma_channel_islands_interpolated_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS Santa Cruz-Anacapa Islands MULT Channel Islands thrust CIT interpolated CFMA model CFMA ./santa_barbara_w_transverse_ranges/channel_islands/alt2/extents/cfma_channel_islands_interpolated_with_flats_west_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS Santa Cruz-Anacapa Islands MULT Channel Islands thrust CIT interpolated w/flats CFMA CFMA ./santa_barbara_w_transverse_ranges/mission_ridge_arroyo_parida_santa_ana/alt2/extents/cfma_mission_ridge_arroyo_parida_santa_a05 Western Transverse Ranges WTRA na_extruded_complete.tsMission Ridge fault system MRFS 00 Mission Ridge-Arroyo Parida-Santa AnaMULT Mission Ridge-Arroyo Parida fault MRAF extruded CFMA model CFMA ./santa_barbara_w_transverse_ranges/lower_pitas_point_montalvo/alt1/extents/cfma_lower_pitas_point_montalvo_complete.ts05 Western Transverse Ranges WTRA Santa Barbara Channe faults SBCF Pitas Point-Mid-Channel trend PPMC Pitas Point fault PPTF Shaw CFMA model SHAW ./santa_barbara_w_transverse_ranges/north_channel/alt1/extents/cfma_north_channel_extrapolated2_complete.ts05 Western Transverse Ranges WTRA North Channel fault system NCFS North Channel-Pitas Point NCPP North Channel fault NCHF CFMA model CFMA ./santa_barbara_w_transverse_ranges/oakridge/alt1/extents/cfma_oak_ridge_off_extrapolated_complete.ts05 Western Transverse Ranges WTRA Oak Ridge fault zone ORFZ 02 Offshore OFFS Oak Ridge fault ORF CFMA model CFMA ./ventura_c_transverse_ranges/red_mountain/alt1/extents/cfma_red_mountain_complete.ts05 Western Transverse Ranges WTRA North Channel fault system NCFS Red Mountain RDMT Red Mountain fault RMF CFMA model CFMA ./santa_barbara_w_transverse_ranges/santa_cruz_island/alt1/extents/cfma_santa_cruz_extruded_90_complete.ts05 Western Transverse Ranges WTRA Channel Islands fault system CIFS Santa Cruz SNCZ fault SCIF 90dip, extruded CFMA CFMA ./santa_barbara_w_transverse_ranges/santa_rosa_island/alt1/extents/cfma_santa_rosa_island_extruded_complete.ts05 Western Transverse Ranges WTRA Channel Islands fault system CIFS Santa Rosa SNRS Santa Rosa Island fault SRIF extruded CFMA model CFMA 05 Western Transverse Ranges WTRA Channel Islands fault system CIFS Anacapa ANCP Anacapa Island fault ACIF ./santa_barbara_w_transverse_ranges/santa_ynez/alt1/extents/cfma_santa_ynez_extruded_70dip_complete.ts05 Western Transverse Ranges WTRA zone SYFZ 00 Western-Eastern MULT Santa Ynez fault SYF 70dip, extruded CFMA CFMA ./santa_barbara_w_transverse_ranges/big_pine/alt3/extents/cfm_big_pine_east_complete.ts12 Coast Ranges Fault Area CRFA Big Pine-Pine Mountain fault system BPPM 05 Eastern+Lockwood Valley MULT East Big Pine fault EBPF CFM model CFM ./santa_barbara_w_transverse_ranges/big_pine/alt1/extents/cfma_big_pine_extrapolated_complete.ts12 Coast Ranges Fault Area CRFA Big Pine-Pine Mountain fault system BPPM 06 Western-Eastern-Lockwood Valley MULT Big Pine fault BPF extrapolated CFMA model CFMA Big Pine-Pine Mountain fault system BPPM 03 Eastern EAST Big Pine fault BPF Big Pine-Pine Mountain fault system BPPM 04 Lockwood Valley LCKV Lockwood Valley fault LCWV ./santa_barbara_w_transverse_ranges/western_big_pine/alt1/extents/cfm_big_pine_west_extrapolated_complete.ts12 Coast Ranges Fault Area CRFA Big Pine-Pine Mountain fault system BPPM 02 Western Big Pine WEST West Big Pine fault WBPF extrapolated CFM model CFM ./santa_barbara_w_transverse_ranges/hosgri/alt1/extents/cfma_hosgri_san_simeon_extrapolated_complete.ts13 Offshore Central California OCCA Hosgi fault zone HFZ 00 Northern-Southern MULT 01 Hosgri fault HSGF extrapolated CFMA model CFMA ./santa_barbara_w_transverse_ranges/western_deep_ramp/alt1/extents/cfma_worlds_end_complete.ts05 Western Transverse Ranges WTRA Santa Barbara Channe faults SBCF Western WEST Worlds End fault WEF CFMA model CFMA ./santa_barbara_w_transverse_ranges/upper_pitas_point/alt1/extents/cfma_upper_pitas_point_extrapolated_complete.ts05 Western Transverse Ranges WTRA North Channel fault system NCFS Pitas Point PPT Pitas Point fault PPTF extrapolated CFMA model CFMA ./santa_barbara_w_transverse_ranges/nacimiento/alt1/extents/cfm_nacimiento_complete.ts12 Coast Ranges Fault Area CRFA Nacimiento fault zone NAFZ Northern-Southern MULT Nacimiento fault NCMF CFM model CFM ./santa_barbara_w_transverse_ranges/pine_mountain/alt1/extents/cfm_pine_mountain_complete.ts12 Coast Ranges Fault Area CRFA Big Pine-Pine Mountain fault system BPPM 01 Pine Mountain PNMT Pine Mountain fault PMTF CFM model CFM ./inner_borderlands/carlsbad/alt1/extents/pre_cfma_carlsbad_interpolated_complete.ts04 Offshore Continental Borderland OCBA San Onofre-Carlsbad fault zone SOCZ 00 San Mateo-San Onofre-Oceanside-CarlsbadMULT San Onofre-Carlsbad fault SOCF interpolated pre-CFMA PCFM ./inner_borderlands/coronado_bank/alt1/extents/cfma_coronado_banks_complete.ts04 Offshore Continental Borderland OCBA Coronado Bank fault zone CBFZ Coronado Bank-Oceanside-Palos VerdesMULT Coronado Bank fault CBF CFMA model CFMA ./inner_borderlands/oceanside/alt1/extents/cfma_oceanside_complete.ts 04 Offshore Continental Borderland OCBA Oceanside-San Mateo fault system OSMS Oceanside Oceanside thrust OCNT CFMA model CFMA ./inner_borderlands/palos_verdes/alt1/extents/cfma_palos_verdes_complete.ts 04 Offshore Continental Borderland OCBA Palos Verdes fault zone PVFZ 00 Santa Monica Basin-Oceanside MULT 01 Palos Verdes fault PVF CFMA model CFMA ./inner_borderlands/palos_verdes/alt3/extents/cfm_palos_verdes_complete.ts 04 Offshore Continental Borderland OCBA Palos Verdes fault zone PVFZ 00 Santa Monica Basin-Oceanside MULT 01 Palos Verdes fault PVF CFM model CFM 25 ./inner_borderlands/san_clemente_escarpment/alt1/extents/cfma_san_clemente_complete.ts04 Offshore Continental Borderland OCBA San Clemente fault zone SCFZ Northern-Southern MULT 01 San Clemente fault SCLF CFMA model CFMA ./inner_borderlands/san_diego_trough/alt1/extents/cfma_san_diego_trough_complete.ts04 Offshore Continental Borderland OCBA San Diego Trough fault zone SDTZ Northern-Southern MULT 01 San Diego Trough fault SDTF CFMA model CFMA ./inner_borderlands/thirty_miles/alt1/extents/pre_cfma_thirty_miles_rivero_complete.ts04 Offshore Continental Borderland OCBA Inner Borderland fault system IBFS Thirty Mile Bank TMBK Thirty-Mile Bank fault TMBF Rivero CFMA model RVRO ./inner_borderlands/newport_inglewood_rose_canyon/alt1/extents/cfm_newport_inglewood_rose_canyon_complete.ts04 Peninsular Ranges PNRA Newport-Inglewood-Rose Canyon fault zone NIRC 00 Los Angeles basin-San Diego MULT 01 Newport-Inglewood-Rose Canyon fault NIRF CFM model CFM ./inner_borderlands/redondo_canyon/alt1/extents/cfm_redondo_canyon_extruded_zioni_trace_100m.ts04 Offshore Continental Borderland OCBA Cross Fault CF Redondo Canyon RDNC 02 Redondo Canyon fault RDCF extruded Zioni CFM ZION ./inner_borderlands/redondo_canyon/alt2/extents/cfm_redondo_canyon_extruded_bohannon_trace_100m.ts04 Offshore Continental Borderland OCBA Cross Fault CF Redondo Canyon RDNC 02 Redondo Canyon fault RDCF extruded Bohannon CFM BOHN ./inner_borderlands/san_pedro_basin/alt1/extents/cfm_san_pedro_basin_complete.ts04 Offshore Continental Borderland OCBA San Pedro Basin fault zone SPBZ San Pedro basin SPDB 01 San Pedro Basin fault SPBF CFM model CFM ./inner_borderlands/santa_cruz-santa_catalina_ridge/alt1/extents/cfm_sant_cruz-catalina_ridge_fault_zone_extruded_complete.ts04 Offshore Continental Borderland OCBA Santa Cruz-Catalina Ridge fault zone SCCR Northern-Southern MULT 01 Santa Cruz-Catalina Ridge fault SCCF extruded CFM model CFM ./santa_barbara_w_transverse_ranges/big_pine/alt2/extents/pre_cfma_big_pine_cdmg_complete.ts12 Coast Ranges Fault Area CRFA Big Pine-Pine Mountain fault system BPPM 00 Western-Eastern-Lockwood Valley MULT 01 Big Pine fault BGPF 03 CDMG pre-CFMA model CDMG ./death_valley/black_mountain/alt1/extents/cfm_black_mountain_low_dip_complete.ts Black Mountain fault zone BMFZ 00 Mustard Hills-Smith Mtn MULT 01 Black Mountain fault BMTF low-dip CFM model CFM ./mojave/camp_rock/alt2/extents/cfm_camp_rock_alt2_complete.ts 07 Mojave Fault Area MJVA Camp Rock-Emerson-Copper Mtn fault zone CREC 01 Camp Rock CMRK 01 Camp Rock fault CMPF CFM model CFM ./peninsular_ranges/canada_david/alt2/extents/cfm_canada_david_detachment_connected_complete.ts03 Peninsular Ranges PNRA Northern Baja Detachments? NBJD Canada-David CDS Canada David detachment CDD connected CFM model CFM APPENDIX 1 ./los_angeles/clamshell_sawpit/alt3/extents/cfm_clamshell_sawpit_cut_at_sag_complete.ts05 Western Transverse Ranges WTRA Sierra Madre fault zone SMFZ 03 Clamshell-Sawpit Canyon CSPC Clamshell-Sawpit Canyon fault CSCF cut at sag, CFM model CFM ./los_angeles/eagle_rock/alt1/extents/cfm_eagle_rock_complete.ts 05 Western Transverse Ranges WTRA San Fernando fault system SFNS Verdugo Mountains VRDM Eagle Rock fault ERKF CFM model CFM ./ventura_c_transverse_ranges/anacapa_dume/alt1/extents/cfma_dume_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS 02 Santa Monica Mountains SMMT Anacapa-Dume fault ANDF CFMA model CFMA ./ventura_c_transverse_ranges/anacapa_dume/alt3/extents/cfm_dume_cut_at_mal_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS 02 Santa Monica Mountains SMMT Anacapa-Dume fault ANDF cut@mal, CFM model CFM ./peninsular_ranges/extra/alt1/extents/cfm_extra_extruded_90_complete.ts 02 Salton Trough Fault Area SALT 01 Cross Fault CF 02 Salton Sea SALT 01 Extra fault EXTF 90dip, extruded CFM CFM ./mojave/homestead_valley/alt1/extents/cfm_homestead_valley_complete.ts 07 Mojave Fault Area MJVA Homestead Valley fault zone HVFZ Homestead Valley HMSV Homestead Valley fault HMVF CFM model CFM ./mojave/johnson_valley/alt3/extents/cfm_johnson_valley_alt3_complete.ts 07 Mojave Fault Area MJVA Johnson Valley fault zone JVFZ 00 Johnson Valley JNSV Johnson Valley fault JVF CFM model CFM ./los_angeles/las_cienagas/alt2/extents/cfm_las_cienagas_cut_at_pht_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system Los Angeles Basin LAB Las Cienagas LCGF cut@pht, CFM model CFM ./los_angeles/las_cienagas/alt3/extents/cfm_las_cienagas_cut_at_lep_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system Los Angeles Basin LAB Las Cienagas LCGF cut@lep, CFM model CFM ./mojave/lavic_lake/alt1/extents/cfm_lavic_lake_complete.ts 07 Mojave Fault Area MJVA Lavic Lake fault zone LLFZ Lavic Lake Lavic Lake fault LVLF CFM model CFM ./ventura_c_transverse_ranges/malibu_coast/alt2/extents/pre_cfma_malibu_coast_cdmg_complete.ts05 Western Transverse Ranges WTRA Southern Frontal fault system SFFS 02 Santa Monica Mountains SMMT Malibu Coast fault MBCF CDMG pre-CFMA model CDMG ./ventura_c_transverse_ranges/malibu_coast/alt4/extents/cfm_malibu_coast_long_complete.ts05 Western Transverse Ranges WTRA Southern Frontal fault system SFFS 02 Santa Monica Mountains SMMT Malibu Coast fault MBCF long CFM model CFM ./peninsular_ranges/mill_creek/alt4/extents/cfm_mill_creek_cut_at_SA_complete.ts01 San Andreas Fault System SAFS San Andreas fault zone SAFZ 04 San Bernardino Mtns SBMT 02 Mill Creek fault MLCF cut@SAF, CFM model CFM ./santa_barbara_w_transverse_ranges/morales/alt1 05 Coast Ranges Fault Area CRFA San Juan-Morales fault zone SJMZ Morales MRLS Morales fault MRLF CFM model CFM ./mojave/north_emerson/alt1/extents/cfm_north_emerson_complete.ts 07 Mojave Fault Area MJVA Camp Rock-Emerson-Copper Mtn fault zone CREC 02 Emerson EMRS North Emerson fault NEMF CFM model CFM ./los_angeles/north_salt_lake/alt2/extents/cfm_north_salt_lake_cut_at_hol_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS Los Angeles Basin LAB North Salt Lake Cut NSLC cut@hol, CFM model CFM ./death_valley/northern_death_valley/alt1/extents/cfm_northern_death_valley_100m_trace.ts09 Basin and Range Fault Area BNRA Northern Death Valley fault zone NDVZ 00 Grapevine Mtns-Kit Fox Hills MULT Northern Death Valley fault NDVF CFM model CFM ./santa_barbara_w_transverse_ranges/oceanic/alt1/extents/cfm_oceanic_from_san_simeon_complete.ts12 Coast Ranges Fault Area CRFA Oceanic fault zone OFZ Santa Lucia Range SLRS Oceanic fault OCNF CFM model CFM ./santa_barbara_w_transverse_ranges/oceanic/alt2/extents/cfm_oceanic_90dip_complete.ts12 Coast Ranges Fault Area CRFA Oceanic fault zone OFZ Santa Lucia Range SLRS Oceanic fault OCNF 90dip, CFM model CFM ./santa_barbara_w_transverse_ranges/oceanic/alt3/cfm_oceanic_58dip_complete.ts12 Coast Ranges Fault Area CRFA Oceanic fault zone OFZ Santa Lucia Range SLRS Oceanic fault OCNF 58dip, CFM model CFM ./santa_barbara_w_transverse_ranges/pine_mountain/alt2/extents/cfm_pine_mountain_cut_at_sag_complete.ts12 Coast Ranges Fault Area CRFA Big Pine-Pine Mountain fault system BPPM 00 Pine Mountain PMTS Pine Mountain fault PMTF cut@sag, CFM model CFM ./mojave/pinto_mountain/alt2/extents/cfm_pinto_mountain_90dip_complete.ts 06 Eastern Transverse Ranges ETRA Pinto Mountain fault zone PMFZ 01 Pinto Mountain PNMT 01 Pinto Mountain fault PNTF 90dip, CFM model CFM 06 Eastern Transverse Ranges ETRA Pinto Mountain fault zone PMFZ 02 Morongo Valley MRGV Morongo Valley fault MRVF ./mojave/pisgah_bullion_mountain_mesquite_lake/alt2/extents/cfm_pisgah_bullion_mesquite_lake_complete.ts07 Mojave Fault Area MJVA Pisgah-Bullion fault zone PBFZ 00 Pisgah-Mesquite Lake MULT 01 Pisgah-Bullion-Mesquite Lake fault PBML CFM model CFM ./santa_barbara_w_transverse_ranges/rinconada/alt1/extents/cfm_rinconada_complete.ts12 Coast Ranges Fault Area CRFA Rinconada fault zone RNFZ 00 Espinoza-Rinconada MULT 01 Rinconada fault RNCF CFM model CFM ./los_angeles/san_antonio_canyon/alt1/extents/cfm_san_antonio_canyon_90dip_complete.ts05 Western Transverse Ranges WTRA San Gabriel Mountain faults SGMF San Antonio Canyon SANC San Antonio Canyon fault? SACF 90dip, CFM model CFM ./los_angeles/san_joaquin_hills/alt2/extents/cfm_san_joaquin_hills_curved_complete.ts03 Peninsular Ranges PNRA Coastal faults CSTF San Joquin Hills SJQH San Joaquin Hills fault SJHF CFM model CFM 03 Peninsular Ranges PNRA Compton-Lower Elysian Park fault system CEPS Coastal CSTL Wilmington thrust WLMT 03 Peninsular Ranges PNRA Compton-Lower Elysian Park fault system CEPS Offshore OFFS San Pedro Escarpment fault SPEF ./santa_barbara_w_transverse_ranges/santa_barbara_channel_western_segment_boundary/alt105 Western Transverse Ranges WTRA Santa Barbara Channel faults SBCF Western WEST Western Segment fault WSGF CFM model CFM ./los_angeles/santa_monica/alt2/extents/cfm_santa_monica_75dip_extrapolated.ts05 Western Transverse Ranges WTRA Southern Frontal fault system SFFS 02 Santa Monica Mountains SMMT Santa Monica fault SMF 75dip, extrapolated CFM CFM ./inner_borderlands/santa_monica_bay/alt1/extents/cfm_santa_monica_bay_larson_extruded_complete.ts05 Western Transverse Ranges WTRA Southern Boundary Thrust system SBTS Santa Monica basin SMNB 01 Santa Monica Bay fault SMBF extruded CFM model CFM ./santa_barbara_w_transverse_ranges/south_cuyama/alt1/ 12 Coast Ranges Fault Area CRFA South Cuyama fault zone SCFZ South Cuyama fault SCYF CFM model CFM ./death_valley/southern_death_valley/alt1/extents/cfm_southern_death_valley_dipping_complete.ts09 Basin and Range Fault Area BNRA Southern Death Valley fault zone SDVZ 00 Confidence Hills-Nobel Hills MULT Southern Death Valley fault SDVF dipping, CFMA CFM ./death_valley/southern_death_valley/alt2/extents/cfm_southern_death_valley_90dip_complete.ts09 Basin and Range Fault Area BNRA Southern Death Valley fault zone SDVZ 00 Confidence Hills-Nobel Hills MULT Southern Death Valley fault SDVF 90dip, CFMA CFM Basic CFM Fault ID Naming and Numbering Scheme 00 Multiple faults MULT New CFM4 Fault Object Name Fault Area/Major Fault System Fault Zone/Region Fault Section Fault Name Fault Strand/Model Description Alternative

San Andreas Fault System SAFS-SAFZ-MULT-San_Andreas-alt1-single 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 00 Parkfield-Coachella Valley MULT 01 San Andreas fault SAF 01 CFM3+CFM4-merged-single M3M4 SAFS-SAFZ-MULT-San_Andreas-alt2-complex 02 CFM3+CFM4-merged-complex M3M4 SAFS-SAFZ-MULT-San_Andreas_fault-Fuis 01 FUIS propeller model-shallow FUIS SAFS-SAFZ-MULT-San_Andreas_fault-Fuis-18km 02 FUIS propeller model-18km FUIS SAFS-SAFZ-MULT-Banning_fault_strand-alt1 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 00 San Bernardino-Coachella Valley MULT 02 Banning fault strand BNFS 01 CFM4 model ALT1 SAFS-SAFZ-MULT-Banning_fault_strand-deep-dip1 02 CFM4 deep model DEEP SAFS-SAFZ-MULT-Banning_fault_strand-upper-alt1 03 CFM4 upper model UPPR SAFS-SAFZ-MULT-Banning_fault_strand-YULE 04 Yule model YULE SAFS-SAFZ-PARK-San_Andreas_fault 01 San Andreas Fault System SAFS 01 San Andreas fault zone SAFZ 06 Parkfield PARK 01 San Andreas fault SAF SAFS-SAFZ-CLCZ-San_Andreas_fault-CHLM 07 Cholame-Carrizo CLCZ 01 San Andreas fault SAF 01 Cholame section CHLM SAFS-SAFZ-CLCZ-San_Andreas_fault-CRRZ 02 Carrizo section CRRZ SAFS-SAFZ-MJVS-San_Andreas_fault 08 Mojave MJVS 01 San Andreas fault SAF SAFS-SAFZ-SBMT-San_Andreas_fault-alt1 09 San Bernardino Mountains SBMT 01 San Andreas fault SAF 01 ALT1 SAFS-SAFZ-SBMT-San_Andreas_fault-CFMA 02 CFMA SAFS-SAFZ-SBMT-Banning_fault_strand 02 Banning fault strand BNFS SAFS-SAFZ-SBMT-Mission_Creek_fault_strand-alt1 03 Mission Creek fault strand MSCS 01 CFM4 model- dipping ALT1 SAFS-SAFZ-SBMT-Mission_Creek_fault_strand-alt2 02 CFM4 model- steep dip ALT2 SAFS-SAFZ-SBMT-Garnet_Hill_fault_strand-alt1 04 Garnet Hill fault strand GHFS 01 CFM4 model ALT1 SAFS-SAFZ-SBMT-Garnet_Hill_fault_strand-YULE 02 Yule model YULE SAFS-SAFZ-SBMT-Mill_Creek_fault_strand-alt1 05 Mill Creek fault strand MLCS 01 ALT1 SAFS-SAFZ-SBMT-Mill_Creek_fault_strand-CFM1 02 CFM1 SAFS-SAFZ-SBMT-Mill_Creek_fault_strand-CFM2 03 CFM2 SAFS-SAFZ-SBMT-Mill_Creek_fault_strand-CFM3 04 CFM3 SAFS-SAFZ-SBMT-Mill_Creek_fault_strand-CFM4 05 CFM4 SAFS-SAFZ-COAV-Southern_San_Andreas_fault-alt1 10 Coachella COAV 01 Southern San Andreas fault SSAF 01 CFM4 model ALT1 SAFS-SAFZ-COAV-Southern_San_Andreas_fault-CFM1 02 CFM1 SAFS-SAFZ-COAV-Southern_San_Andreas_fault-CFM2 03 CFM2 SAFS-SAFZ-COAV-Banning_fault_strand 02 Banning fault strand BNFS 01 CFM4 model CFM4 SAFS-SAFZ-COAV-Banning_fault_strand-south 02 CFM4 model-south SAFS-SAFZ-COAV-Mission_Creek_fault_strand-south 03 Mission Creek fault strand MSCS 01 CFM4 model-south SAFS-SAFZ-COAV-Mission_Creek_fault_strand-SAF-connector 02 SAF-connector SAFC SAFS-SAFZ-COAV-Garnet_Hill_fault_strand 04 Garnet Hill fault strand GHFS 01 CFM4 model ALT1 SAFS-SAFZ-COAV-North_Palm_Springs_fault 05 North Palm Springs fault NPSF 01 CFM4 model-blind CFM4 SAFS-SAFZ-COAV-North_Palm_Springs_fault-CRNA 02 Sara Carena model CRNA SAFS-SAFZ-1812-San_Andreas_fault 11 1812 Rupture-Mojave 1812 01 San Andreas fault SAF SAFS-SAFZ-1857-San_Andreas_fault 12 1857 Rupture-Parkfield-Mojave 1857 01 San Andreas fault SAF 13 1906 Rupture-Cape Mendocino-SC Mtn1906 01 San Andreas fault SAF 14 1989 Loma Prieta rupture 1989 01 Loma Prieta fault LPRF SAFS-SGPR-SGPS-San_Gorgonio_Pass_thrust 02 San Gorgonio Pass fault region SGPR 01 San Gorgonio Pass SGPS 01 San Gorgonio Pass thrust SGPT 01 CFM4 model ALT1 SAFS-SGPR-SGPS-San_Gorgonio_Pass_thrust-YULE 02 Yule model YULE SAFS-SGPR-SGPS-San_Gorgonio_Pass_thrust-CRNA 02 Sara Carena model CRNA SAFS-SGPR-SJMT-Palm_Springs_blind_fault 02 San Jacinto Mountains SJMT 02 Palm Springs fault 01 CFM4 model-blind CFM4 SAFS-SGPR-SJMT-Palm_Springs_blind_fault-CRNA 02 Sara Carena model CRNA SAFS-SGPR-SJMT-Potato_Chip-1_fault 03 Potato Chip-1 fault 01 CFM4 model-blind CFM4 SAFS-SGPR-SJMT-Potato_Chip-1_fault-CRNA 02 Sara Carena model CRNA SAFS-SGPR-SJMT-Potato_Chip-2_fault 04 Potato Chip-2 fault 01 CFM4 model-blind CFM4 SAFS-SGPR-SJMT-Potato_Chip-2_fault-CRNA 02 Sara Carena model CRNA SAFS-SGPR-SJMT-Potato_Chip-3_fault 05 Potato Chip-3 fault SAFS-SGPR-SJMT-Potato_Chip-4_fault 06 Potato Chip-4 fault SAFS-SGPR-SJMT-Potato_Chip-5_fault 07 Potato Chip-5 fault SAFS-SGPR-CRFH-Crafton_Hills_fault 03 Crafton Hills CRFH 01 Crafton Hills fault SAFS-SGPR-YUCA-Banning fault 04 Yucaipa YUCA 01 Banning fault 01 CFM

05 San Bernardino SBRN 01 San Bernardino cross fault 26 02 cross fault SAFS-MHFZ-MULT-Mecca_Hills-Hidden_Springs_fault-deep 03 Mecca Hills-Hidden Springs fault zone MHFZ 00 Multiple sections MULT 01 Mecca Hills-Hidden Springs deep fault SAFS-MHFZ-LSBM-Indio_Hills_fault 01 Little San Bernardino Mts LSBM 01 Indio Hills fault SAFS-MHFZ-LSBM-Berdoo_Canyon_fault 02 Berdoo Canyon fault SAFS-MHFZ-MCHS-Painted_Canyon_fault 02 Mecca Hills MCHS 01 Painted Canyon fault SAFS-MHFZ-MCHS-Mecca_Hills_fault 02 Mecca Hills fault 01 CFM4 model CFM4 SAFS-MHFZ-MCHS-Mecca_Hills_fault-alt1 02 ALT1 SAFS-MHFZ-MCHS-Hidden_Springs_fault 03 Hidden Springs fault 01 CFM4 model CFM4 04 Eagle Canyon fault 05 Platform fault Salton Trough Fault Area SALT-BRSZ-BSZ-Brawley_Seismic_Zone_boundary-CFMA 02 Salton Trough Fault Area SALT 01 Brawley Seismic Zone BRSZ 01 Brawley Seismic Zone BSZ 01 Brawley Seismic zone BSZ SALT-BRSZ-BSZ-Brawley_fault 02 Brawley fault BRWF APPENDIX 1 SALT-IMFZ-IMPV-Imperial_fault 02 Imperial fault zone IMFZ 01 Imperial Valley IMPV 01 Imperial fault IMPF 01 near vertical at north end SALT-IMFZ-IMPV-Imperial_fault-alt1-FUIS E-dipping at north end-FUIS FUIS SALT-IMFZ-IMPV-Imperial_fault-north_end IMPF 02 small segment at north end NSEG SALT-IMFZ-IMPV-Imperial_fault-east_branch-north 02 Imperial fault-east branch IMPE 03 inferred east branch-north NRTH SALT-IMFZ-IMPV-Imperial_fault-east_branch-south IMPE 04 inferred east branch-south SOTH SALT-CPFZ-CRPR-Cierro_Prieto_fault-CFM 03 Cerro Prieto fault zone CPFZ 01 Cerro Prieto basin CRPR 01 Cerro Prieto fault CRPF SALT-CRSF-SLTS-Extra_fault 04 Cross Faults CRSF 01 Salton Sea SLTS 01 Extra fault EXTF SALT-CRSF-IMPV-Elmore_Ranch_fault 02 Imperial Valley IMPV 01 Elmore Ranch fault ELRF 01 CFM SALT-CRSF-IMPV-Westmorland_fault-main 02 Imperial Valley IMPV 02 Westmorland fault WSTF 01 main MAIN SALT-CRSF-IMPV-Westmorland_fault-splay 02 splay SPLY Peninsular Ranges Area PNRA-SJFZ-SBRN-San_Jacinto-Claremont_fault-alt1 03 Peninsular Ranges Area PNRA 01 San Jacinto fault zone SJFZ 01 San Bernardino SBRN 01 San Jacinto-Claremont fault SJCF 01 ALT1 PNRA-SJFZ-SBRN-San_Jacinto-Claremont_fault-alt2 02 ALT2 PNRA-SJFZ-SBRN-San_Jacinto-Claremont_fault-CFM 03 CFM PNRA-SJFZ-SBRN-Loma_Linda_fault 02 Loma Linda fault 01 CFM4 model CFM4 PNRA-SJFZ-SBRN-Rialto-Colton_fault 03 Rialto-Colton fault 01 CFM4 model CFM4 PNRA-SJFZ-SBRN-Glen_Helen_fault-alt1 04 Glen Helen fault 01 ALT1 PNRA-SJFZ-SBRN-Glen_Helen_fault-CFM 02 CFM PNRA-SJFZ-SBRN-Lytle_Creek_fault 05 Lytle Creek fault 01 CFM4 PNRA-SJFZ-SJCV-Claremont_fault 02 San Jacinto Valley SJNV 01 Claremont fault CLMF 01 Main CFM4 PNRA-SJFZ-SJCV-Claremont_fault-E 02 east branch EAST PNRA-SJFZ-SJCV-Casa_Loma_fault-alt1 02 Casa Loma fault 01 ALT1 PNRA-SJFZ-SJCV-Casa_Loma_fault-CFMA 02 CFMA PNRA-SJFZ-SJCV-Hot_Springs_fault-main-alt1 03 Hot Springs fault 01 ALT1 PNRA-SJFZ-SJCV-Hot_Springs_fault-main-alt2 02 ALT2 PNRA-SJFZ-SJCV-Hot_Springs_fault-W 03 west branch WEST PNRA-SJFZ-ANZA-Clark_fault-CFMA 03 Anza ANZA 01 Clark fault CLRF 01 CFMA PNRA-SJFZ-ANZA-Clark_fault-alt1-north-alt1 02 north-main NRTH PNRA-SJFZ-ANZA-Clark_fault-alt1-north-alt2-lower 03 north-lower NLWR PNRA-SJFZ-ANZA-Clark_fault-alt1-north-alt2-upper1 04 north-upper1 NUP1 PNRA-SJFZ-ANZA-Clark_fault-alt1-north-alt2-upper2 05 north-upper2 NUP2 PNRA-SJFZ-ANZA-Clark_fault-alt1-south-main-alt1 06 south-main SOTH PNRA-SJFZ-ANZA-Clark_fault-alt1-south-E-alt1 07 south-east1 SE1 PNRA-SJFZ-ANZA-Clark_fault-alt1-south-E-alt2 08 south-east2 SE2 PNRA-SJFZ-ANZA-Clark_fault-alt1-south-ext 09 south-extension SEXT PNRA-SJFZ-ANZA-Buck_Ridge_fault 02 Buck Ridge fault 01 CFM4 model CFM4 PNRA-SJFZ-ANZA-Hot_Springs-Buck_Ridge_Link_fault 03 Buck Ridge-Hot Springs link LINK PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt1 04 Coyote Creek CCRS 01 Coyote Creek fault CCRF 01 ALT1 PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt2-north-lower 02 north-lower PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt2-north-upper 03 north-upper PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt2-south 04 south-main PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt2-south-ext 05 south-extension PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt2-south-link 06 sotuh-link PNRA-SJFZ-CYTC-Coyote_Creek_fault-alt2-south-splay 07 south-splay PNRA-SJFZ-BRMT-Coyote_Creek_fault-CFMA 05 Borrego Mountain BRMT 01 Coyote Creek fault CCRF 01 CFMA PNRA-SJFZ-BRMT-Coyote_Creek_fault-alt1-north 02 north-lower PNRA-SJFZ-BRMT-Coyote_Creek_fault-alt1-south 03 south PNRA-SJFZ-BRMT-Coyote_Creek_fault-alt1-east 04 east PNRA-SJFZ-BRMT-Coyote_Creek_fault-alt1-n-s-link1 05 n-s-link1 PNRA-SJFZ-BRMT-Coyote_Creek_fault-alt1-n-s-link1-ext 06 n-s-link1-ext PNRA-SJFZ-BRMT-Coyote_Creek_fault-alt1-n-s-link2 07 n-s-link2 PNRA-SJFZ-SSHS-Superstition_Hills_fault-alt1 06 Superstition Hills SSHS 01 Superstition Hills fault SHF 01 CFM4 model CFM4 PNRA-SJFZ-SSHS-Superstition_Hills_fault-CFMA CFMA PNRA-SJFZ-SSMT-Superstition_Mountain_fault-main 07 Superstition Mountain SSMT 01 Superstition Mountain fault SMTF 01 CFM4 model CFM4 PNRA-SJFZ-SSMT-Superstition_Mountain_fault-main CFMA PNRA-SJFZ-IMPV-Weinert_El_Centro_fault 08 Imperial Valley IMPV 01 Weinert-El Centro fault 01 CFM4 model CFM4 PNRA-SJFZ-IMPV-Weinert_Superstition_Hills_link 02 Weinert-Superstition Hills link 01 CFM4 model CFM4 PNRA-SJFZ-IMPV-Dixieland_fault-north previously Superstition_Mtn-New_River_extension 03 Dixieland_fault 01 north NRTH PNRA-SJFZ-IMPV-Dixieland_fault-center 02 center CNTR PNRA-SJFZ-IMPV-Dixieland_fault-south 03 south SOTH PNRA-ELSZ-WHIT-Whittier_fault 02 Elsinore-Laguna Salada fault zone ELSZ 01 Whittier WHIT 01 Whittier fault WHTF 01 CFM4 model CFM4 PNRA-ELSZ-WHIT-Whittier_fault-CFM 02 CFM PNRA-ELSZ-WHIT-Whittier_fault-CFMA 03 CFMA PNRA-ELSZ-WHIT-Whittier_Heights_fault 02 Whittier Heights fault PNRA-ELSZ-WHIT-Workman_Hill_fault 03 Workman Hill fault PNRA-ELSZ-WHIT-East_Montebello_fault 04 East Montebello fault PNRA-ELSZ-CHNO-Chino_fault-main 02 Chino CHNO 01 Chino Fault CHNF 01 main MAIN PNRA-ELSZ-CHNO-Chino_fault-Central_Ave 02 Central Avenue CTLA PNRA-ELSZ-CHNO-Chino_fault-CFM1 03 CFM1 PNRA-ELSZ-CHNO-Chino_fault-CFM2 04 CFM2 PNRA-ELSZ-GLIV-Glen_Ivy_North_fault 03 Glen Ivy GLIV 01 Glen Ivy North fault GINF 01 CFM4 model CFM4 PNRA-ELSZ-GLIV-Glen_Ivy_North_ fault-CFMA 02 CFMA PNRA-ELSZ-GLIV-Glen_Ivy_South_fault 02 Glen Ivy South fault GISF 01 CFM4 model CFM4 PNRA-ELSZ-TMCL-Wildomar_fault 04 Temecula TMCL 01 Wildomar fault WLDF 01 CFM4 model CFM4 PNRA-ELSZ-TMCL-Willard_fault-alt1 02 Willard fault WLRF 01 CFM4 model CFM4 PNRA-ELSZ-TMCL-Willard_fault-CFM 02 CFM PNRA-ELSZ-JULN-Elsinore_fault-north 05 Julian JULN 01 Elsinore fault-north ELNF 01 CFM4 model CFM4 PNRA-ELSZ-JULN-Elsinore_fault-CFMA 02 CFMA PNRA-ELSZ-JULN-Elsinore_fault-south 02 Elsinore fault-south ELSF 01 CFM4 model CFM4 PNRA-ELSZ-JULN-Elsinore_fault-Wildomar-link 03 Elsinore-Wildomar link ELWL 01 Wildomar-link LINK PNRA-ELSZ-CYMT-Elsinore_fault 06 Coyote Mountain CYMT 01 Elsinore fault ELSF 01 CFM4 PNRA-ELSZ-CYMT-Elsinore_fault-CFMA 02 CFMA PNRA-ELSZ-LGSD-Laguna_Salada_fault 07 Laguna Salada LGSD 01 Laguna Salada fault LGSF 01 full fault w/ branches FULL PNRA-ELSZ-LGSD-Laguna_Salada_fault-main main single (WBRC+north+south) MAIN PNRA-ELSZ-LGSD-Laguna_Salada_fault-east branch-dipping 04 east branch-dipping EAST PNRA-ELSZ-LGSD-Laguna_Salada_fault-west branch-west 08 West Branch-west WBRW PNRA-ELSZ-LGSD-Laguna_Salada_fault-west branch-west-upper West Branch-west WBRW PNRA-ELSZ-LGSD-Laguna_Salada_fault-west branch-west-deep West Branch-west WBRW PNRA-ELSZ-LGSD-Laguna_Salada_fault-west branch-center 07 West Branch-center WBRC PNRA-ELSZ-LGSD-Laguna_Salada_fault-west-branch-east 05 West Branch-east WBRE PNRA-ELSZ-LGSD-Laguna_Salada_fault-west-branch-deep_splay_east 06 West Branch-deep_splay_east WBRE PNRA-ELSZ-LGSD-Laguna_Salada_fault-north 02 north section-main NRTH PNRA-ELSZ-LGSD-Laguna_Salada_fault-south 03 south section-main SOTH 27 PNRA-ELSZ-LGSD-Laguna_Salada_fault-south-upper south section-main SOTH PNRA-ELSZ-LGSD-Laguna_Salada_fault-south-deep south section-main SOTH PNRA-ELSZ-LGSD-Laguna_Salada_fault-CFMA 09 vertical from trace CFMA PNRA-ELSZ-INDV-Indiviso_fault 08 Indiviso INDV 01 Indiviso fault INDF 01 CFM4 model-main MAIN PNRA-ELSZ-INDV-Indiviso_fault-splay 02 CFM4 model-splay SPLY PNRA-ELSZ-YUHA-Sierra_Cucapah_fault-nw_splay previously -NW-extension-Laguna Salada fault-Treiman 09 Yuha Desert YUHA 01 Sierra Cucapah fault SCPF 01 northwest splay w/trace NWST PNRA-ELSZ-YUHA-Sierra_Cucapah_fault-nw_splay-deep PNRA-ELSZ-YUHA-Sierra_Cucapah_fault-nw_splay-upper PNRA-ELSZ-YUHA-Sierra_Cucapah_fault-blind_north 01 Blind northern NRTH PNRA-ELFZ-YUHA-Yuha_Desert_blind_fault 02 Yuha Desert blind fault YDBF Blind east-side of cross faults EAST PNRA-ELSZ-SRCP-Sierra_Cucapah_fault-deep 09 Sierra Cucapah SRCP 01 Sierra Cucapah fault SCPF 01 deep from seismicity DEEP PNRA-ELSZ-SRCP-Sierra_Cucapah_fault-deep-bot 02 deep from seismicity PNRA-ELSZ-SRCP-Sierra_Cucapah_fault-deep-mid 03 deep from seismicity APPENDIX 1 PNRA-ELSZ-SRCP-Pescadores_fault 02 Pescadores fault PSDF 01 shallow SCPF from trace SSCF PNRA-ELSZ-SRCP-Borrego_fault 03 Borrego fault BRGF 01 shallow SCPF from trace SSCF PNRA-ELSZ-SRCP-Paso_Inferior_fault 04 Paso Inferior fault PSIF 01 shallow SCPF from trace SSCF PNRA-ELSZ-SRCP-Paso_Superior_fault 05 Paso Superior detachment PSSD 01 shallow SCPF from trace SSCF PNRA-ELSZ-SRCP-Paso_Superior_fault-top 02 PNRA-ELSZ-SRCP-Paso_Superior_fault-mid 03 06 Cucapah fault 07 Cucapah Range fault 08 Canon Rojo fault 09 Chupamirtos fault 10 Chupamirtos Norte fault 11 Central Mayor

PNRA-ATEV-EQVS-Earthquake_Valley_fault-main 03 Agua Tibia-Earthquake Valley fault zone ATEV 01 Earthquake Valley EQVS 01 Earthquake Valley fault EQVF 01 MAIN PNRA-ATEV-EQVS-Earthquake_Valley_fault-CFM 02 CFM PNRA-ATEV-EQVS-Earthquake_Valley_East fault 02 Earthquake Valley East fault EQVE 01 EAST PNRA-ATEV-EQVS-Earthquake_Valley_West_fault 03 Earthquake Valley West fault EQVW 01 WEST PNRA-ATEV-ACHS-Agua_Caliente_fault-east 02 Agua Caliente-Hot Springs ACHS 01 Agua Caliente East fault ACEF 01 MAIN PNRA-ATEV-ACHS-Agua_Caliente_fault-west 02 Agua Caliente West fault ACWF 01 MAIN PNRA-ATEV-ACHS-Agua_Caliente_fault-west-splay1 02 splay1 SPL1 PNRA-ATEV-ACHS-Agua_Caliente_fault-west-splay2 03 splay2 SPL2 PNRA-ATEV-ACHS-Agua_Caliente_fault-west-splay3 04 splay3 SPL3 PNRA-ATEV-ACHS-Hot_Springs_fault 03 Hot Springs fault HTSF 01 PNRA-ATEV-ACHS-Murrieta-Hotsprings_fault 04 Murietta-Hot Springs fault MRHS 01 PNRA-NIFZ-LABS-Newport_Inglewood_fault-CFM3 04 Newport-Inglewood-Rose Canyon fault zone NIRC 00 Multiple-Los Angeles basin LABS 01 Newport-Inglewood fault NIWF 01 LAB CFM3 PNRA-NIFZ-LABS-Newport_Inglewood_fault-CFM1 02 LAB CFM1 PNRA-NIFZ-LABS-Newport_Inglewood_fault-CFM2 03 LAB CFM2 PNRA-NIRC-OFFS-Newport_Inglewood_fault 00 Dana Point-Oceanside OFFS 02 Newport-Inglewood fault-south NIWS 01 offshore PNRA-NIRC-MULT-Rose_Canyon_fault 00 Del Mar-San Diego MULT 03 Rose Canyon fault RSCF 01 01 North Los Angeles Basin NLAB 01 Newport-Inglewood fault NIWF 02 South Los Angeles Basin SLAB 01 Newport-Inglewood fault NIWF 03 Dana Point DNPT 01 Newport-Inglewood fault NIWF 04 Oceanside OCNS 01 Newport-Inglewood fault NIWF PNRA-NIRC-OCNS-Newport_Inglewood-RC-link 02 Newport-Inglewood-RC-link NIRC 05 Del Mar DLMR 01 Rose Canyon fault RSCF 06 San Diego SNDG 01 Rose Canyon fault RSCF 07 Silver Strand SLVS 01 San Diego fault 02 Coronado fault PNRA-CEPS-LABS-Lower_Elysian_Park_fault-CFMA 05 Compton-Lower Elysian Park fault system CLEP 01 Los Angeles Basin LABS 01 Lower Elysian Park fault 01 CFMA PNRA-CEPS-LABS-Anaheim_fault-CFM1 02 Anaheim fault 01 CFM1 PNRA-CEPS-LABS-Anaheim_fault-CFM2 02 CFM2 PNRA-CEPS-CMPT-Compton-Los_Alamitos_fault 02 Compton CMPT 01 Compton-Los_Alamitos fault PNRA-CEPS-BLDH-Compton-Los_Alamitos_fault 03 Baldwin Hills BLDH 01 Compton-Los_Alamitos fault PNRA-CRSF-USAV-Fontana seismicity lineament-CFMA 06 Cross Faults CRSF 01 Upper Santa Ana Valley USAV 01 Fontana Seismicity lineament FNTS bestfit, CFMA model CFMA PNRA-CRSF-SJSH-Walnut_Creek_fault 02 San Jose Hills SJSH 01 Walnut Creek fault WNCF 02 San Jose fault(?) SJSF PNRA-CRSF-CHNH-Yorba_Linda_lineament 03 Chino Hills CHNH 01 Yorba Linda Lineament CFM PNRA-CRSF-ALCM-Sawtooth_Range_fault 04 Allicito Mountains ALCM 01 Sawtooth Range fault 01 CFM4 model CFM4 PNRA-CRSF-OCOT-Devil's_Canyon_fault 05 Ocotillo OCOT 01 Devil's Canyon fault 01 CFM4 model CFM4 PNRA-CRSF-OCOT-Ocotillo_fault 02 Ocotillo fault PNRA-CRSF-PGWS-Painted Gorge Wash fault 06 Painted Gorge Wash 01 Painted Gorge Wash fault 01 CFM4 model CFM4 PNRA-CRSF-YUHA-Yuha_Well_fault 07 Yuha Desert YUHA 01 Yuha Well fault 01 CFM4 model CFM4 PNRA-CRSF-YUHA-Shell_Beds_fault 02 Shell Beds fault 01 CFM4 model CFM4 PNRA-CRSF-YUHA-Shell_Beds_fault-alt2 02 ALT2 PNRA-CRSF-YUHA-Yuha_Wash_fault 03 Yuha Wash fault 01 CFM4 model CFM4 PNRA-CRSF-YUHA-Yuha_fault 04 Yuha fault 01 CFM4 model CFM4 PNRA-CRSF-EMCP-El_Mayor-Cucapah-normal_fault 08 El Mayor-Cucapah EMCP 01 El Mayor-Cucapah normal fault 01 CFM4 model CFM4 PNRA-CRSF-EMCP-El_Mayor-Cucapah-west_fault 02 El Mayor-Cucapah west fault 01 CFM4 model CFM4 PNRA-CSTF-SJQH-San_Joaquin_Hills_fault 07 Coastal Faults CSTF 01 San Joaquin Hills SJQH San Joaquin Hills fault SJHF CFM model CFM PNRA-DVVZ-DVSV-Davies Valley fault 08 Davies Valley fault zone DVVZ 01 Davies Valley DVSV 01 Davies Valley fault PNRA-DVVZ-DVSV-West Davies Valley fault 02 West Davies Valley fault PNRA-DVVZ-DVSV-Northern Davies Valley fault 03 Northern Davies Valley fault PNRA-NBJD-SRCP-Cerro-Centinela_fault 09 Northern Baja detachments NBJD 01 Sierra Cucapah SRCP Cerro-Centinela fault PNRA-NBJD-CDVD-Canada-David-Detachment_fault 02 Canada David CDVD Canada David detachment Offshore Continental Borderland Area OCBA-PVFZ-MULT-Palos_Verdes_fault-CFM 04 Offshore Continental Borderland AreaOCBA 01 Palos Verdes fault zone PVFZ 00 Multiple sections MULT Palos Verdes fault 01 CFM OCBA-PVFZ-MULT-Palos_Verdes_fault-Brankman 02 Brankman BRKM OCBA-PVFZ-MULT-Palos_Verdes_fault-CFMA 03 CFMA 01 Santa Monica Bay SMBS 02 Palos Verdes Hills PVHS 03 San Pedro Shelf SPDS 04 San Pedro Basin SPDB OCBA-SMCS-MULT-San_Onofre-Carlsbad_fault 02 San Mateo-San Onofre-Carlsbad fault system SMCS 00 Multiple sections MULT 01 San Onofre-Carlsbad fault SOCF OCBA-SMCS-SMTO-San_Mateo-Carlsbad_fault 01 San Mateo SMTO 01 San Mateo-Carlsbad fault SMCF 02 San Onofre-Oceanside SONO OCBA-SMCS-CRLB-San_Mateo-Carlsbad_fault 03 Carlsbad CRLB 01 San Mateo-Carlsbad fault SMCF 03 Descanso fault system DSCS 01 Northern main NRTH 01 Descanso fault DSCF main 02 Southern main SOTH 01 Descanso fault DSCF 03 Eastern splay EAST 01 Descanso east splay fault DSES east 04 Newport-Inglewood transfer NITR 01 Descanso-NI transfer fault DNIT 04 Oceanside detachment system OCSD 00 Multiple sections MULT 01 Oceanside detachment OCND 01 San Mateo SMTO OCBA-OCSD-OCNS-Oceanside_fault 02 Oceanside OCNS 01 Oceanside fault OCNF OCBA-CBFZ-MULT-Coronado_Bank_fault 05 Coronado Bank fault zone CBFZ 00 Multiple sections MULT 01 Coronado Bank fault CRBF 02 Coronado Bank detachment CRBD 01 Northern Coronado-PV NCPV 01 Coronado Bank fault CRBF 02 Coronado Bank CRDB 01 Coronado Bank fault CRBF 03 Eastern splays EAST 01 Coronado splay2 02 Coronado splay3 03 Coronado splay4 06 San Pedro Basin fault zone SPBZ 00 Multiple Sections MULT 01 San Pedro Basin fault SPBF OCBA-SPBZ-SMBS-San_Pedro_Basin_fault-north 01 Santa Monica Bay SMBS 01 San Pedro Basin fault SPBF OCBA-SPBZ-SPDB-San_Pedro_Basin_fault-south 02 San Pedro Basin SPDB 01 San Pedro Basin fault SPBF OCBA-SDTZ-MULT-San_Diego_Trough_fault 07 San Diego Trough fault zone SDTZ 00 Multiple Sections MULT 01 San Diego Trough fault SDTF 28 OCBA-IBFS-TMBK-Thirty_Mile_Bank_fault-CFMA 08 Inner Borderland fault system IBFS 01 Thirtymile Bank TMBK 01 Thirtymile Bank detachment TMBD OCBA-SCCR-MULT-Santa_Cruz-Catalina_Ridge_fault 09 Santa Cruz-Catalina Ridge fault system SCCR 00 Multiple Sections MULT 01 Santa Cruz-Catalina Ridge fault SCRF OCBA-SCFZ-MULT-San_Clemente_fault 10 San Clemente fault zone SCFZ 00 Multiple Sections MULT 01 San Clemente fault SCLF 11 East Santa Cruz Basin fault system ESCS 01 Channel Islands Thrust CIT 01 ESCB-CIT fault OCBA-ESCS-ESCB-East_Santa_Cruz_Basin fault 02 East Santa Cruz Basin ESCB 01 East Santa Cruz Basin fault 03 San Nicolas Basin SNCB 01 East Santa Cruz Basin fault-SE 01 Sorlien-Schindler model SRSN 02 East Santa Cruz Basin fault-SW 01 Sorlien-Schindler model SRSN OCBA-FRFZ-SRSR-Ferrelo_fault-SRLN 12 Ferrelo fault zone FRFZ 01 Santa Rosa Ridge SRSR 01 Ferrelo fault FRLF 01 Sorlien model SRLN 02 Tanner-Cortez Bank TNCB 01 Ferrelo fault FRLF 01 Sorlien model SRLN OCBA-CRSF-RDNC-Redondo_Canyon_fault-BOHN 13 Cross faults CRSF 01 Redondo Canyon RDNC 01 Redondo Canyon fault RDCF 01 Bohn model BOHN OCBA-CRSF-RDNC-Redondo_Canyon_fault-ZION 02 Zioni model ZION 03 Sorlien model SRLN APPENDIX 1 OCBA-CRSF-NCLR-Nicolas_Ridge_NE_fault-SRDH 02 Nicolas Ridge NCLR 01 Nicolas Ridge NE fault NRNF 01 Sorlien-De Hoogh model SRDH OCBA-CRSF-NCLR-Nicolas_Ridge_South_fault-SRDH 02 Nicolas Ridge South fault NRSF 01 Sorlien-De Hoogh model SRDH OCBA-TCBK-TNRB-Tanner Bank NW fault-SRDH 14 Tanner-Cortez Bank-Blake Knolls faults TCBK 01 Tanner Bank TNRB 01 Tanner Bank NW fault TBNF 01 Sorlien-De Hoogh model SRDH OCBA-TCBK-TNRB-Tanner Bank Central fault-SRDH 02 Tanner Bank Central fault TBCF 01 Sorlien-De Hoogh model SRDH OCBA-TCBK-TNRB-Tanner Bank SE fault-SRDH 03 Tanner Bank SE fault TBSF 01 Sorlien-De Hoogh model SRDH OCBA-TCBK-BLKS-Blake Knolls fault-SRDH 02 Blake Knolls BLKS 01 Blake Knolls fault 01 Sorlien-De Hoogh model SRDH 15 Cortez-Velero Basin faults CVBF 01 East Cortez Basin ECRB 02 West Cortez Basin WCRB 03 Velero Basin VLRB Western Transverse Ranges Area WTRA-SGFZ-MULT-San_Gabriel_fault 05 Western Transverse Ranges Area WTRA 01 San Gabriel fault zone SGFZ 00 Multiple sections MULT 01 San Gabriel fault WTRA-SGFZ-MULT-Southern_San_Gabriel_fault 02 San Gabriel fault-south WTRA-SGFZ-PLMS-Northern_San_Gabriel_fault 01 Palomas PLMS 02 Honor Rancho 03 Newhall 04 San Gabriel River 05 Big Tujunga WTRA-SYFZ-MULT-Santa_Ynez_fault 02 Santa Ynez fault zone SYFZ 00 Multiple sections MULT Santa Ynez fault 01 Pacifico PCFC Pacifico fault 02 Western WEST North Branch Santa Ynez fault 03 South Branch SBRC South Branch Santa Ynez fault 04 Eastern EAST Santa Ynez fault 03 Santa Ynez River fault zone SYRZ 00 Multiple sections MULT WTRA-SMFZ-MULT-Sierra_Madre_fault-east 04 Sierra Madre fault zone SMFZ 00 Multiple sections MULT 01 Sierra Madre fault-east east WTRA-SMFZ-MULT-Sierra_Madre_fault-west 02 Sierra Madre fault-west west ALT1 WTRA-SMFZ-MULT-Sierra_Madre_fault-west-CFM 03 Sierra Madre fault-west west CFM 01 Sierra Madre A section SMDA Sierra Madre fault 02 Sierra Madre B section SMDB 01 Sierra Madre fault 02 Gould Canyon thrust 03 Sierra Madre C section SMDC Sierra Madre fault WTRA-SMFZ-CSPC-Clamshell-Sawpit_Canyon_fault 04 Clamshell-Sawpit CSPC Clamshell-Sawpit Canyon fault 05 Sierra Madre D section SMDD 01 Sierra Madre fault 02 Duarte fault 06 Sierra Madre E section SMDE 01 Sierra Madre fault WTRA-SMFZ-SMDE-Sierra_Madre-Cucamonga_Connector 02 Sierra Madre-Cucamonga connector WTRA-SMFZ-CCMG-Cucamonga_fault-CFM 07 Cucamonga CCMG 01 Cucamonga fault 01 CFM WTRA-SMFZ-CCMG-Cucamonga_fault-CFMA 02 CFMA 05 San Fernando fault system SFNS 00 Multiple sections MULT WTRA-SFNS-SFNV-San_Fernando_fault-alt1 01 San Fernando Valley SFNV 01 San Fernando fault 01 ALT1 WTRA-SFNS-SFNV-San_Fernando_fault-alt2 02 ALT2 WTRA-SFNS-SFNV-Northridge_Hills_fault 02 Northridge Hills fault 01 02 Mission Hills MSNH 01 Mission Hills fault 01 WTRA-SFNS-VRDM-Verdugo_fault-CFM 03 Verdugo Mountains VRDM 01 Verdugo fault 01 WTRA-SFNS-VRDM-Eagle_Rock_fault-alt1 02 Eage Rock fault 01 ALT1 WTRA-SFNS-VRDM-Eagle_Rock_fault-CFMA 02 CFMA WTRA-SSFZ-MULT-Santa_Susana_fault 06 Santa Susana fault zone SSFZ 00 Multiple sections MULT 01 Santa Susana fault Olive View fault WTRA-SCFZ-MULT-San_Cayetano_fault-CFM 07 San Cayetano fault zone SCFZ 00 Multiple sections MULT 01 San Cayetano fault SCTF 01 WTRA-SCFZ-MULT-San_Cayetano_fault-CFMA 02 01 Western WEST 01 San Cayetano fault SCTF WTRA-SCFZ-MULT-San_Cayetano_Red_Mtn_link 02 San Cayetano-Red Mtn link 02 Modelo Lobe MDLB 01 San Cayetano fault SCTF 03 Eastern EAST 01 San Cayetano fault SCTF WTRA-SCFZ-SCVA-Del_Valle_fault-CFM2 04 Santa Clarita Valley SCLV 01 Del Valle fault 01 CFM2 WTRA-SCFZ-SCVA-Del_Valle_fault-CFM1 02 CFM1 WTRA-SCFZ-SCVA-Holser_fault-CFM2 02 Holser fault 01 CFM2 WTRA-SCFZ-SCVA-Holser_fault-CFM1 02 CFM1 WTRA-SLCZ-SLMT-Sisar_fault 08 Sisar-Lion Canyon fault zone SLCZ 01 Sulphur Mountain SLMT 01 Sisar fault 02 Lion Canyon fault 03 Sulphur Mountain fault WTRA-MRFS-MULT-Mission_Ridge-Arroyo_Parida_fault-CFM1 09 Mission Ridge fault system MRFS 00 Multiple sections MULT 01 Mission Ridge-Arroyo Parida fault 01 CFM1 WTRA-MRFS-MULT-Mission_Ridge-Arroyo_Parida_fault-CFM2 02 CFM2 01 More Ranch MORE 01 More Ranch fault 02 Mission Ridge MSRD 01 Mission Ridge fault 03 Arroyo Parida ARPR 01 Arroyo Parida fault 04 Santa Ana SANA 01 Santa Ana fault 10 North Channel fault system NCFS 00 Multiple sections MULT WTRA-NCFS-RDMT-Red_Mountain_fault-CFM1 01 Red Mountain RDMT 01 Red Mountain fault RMTF 01 CFM1 WTRA-NCFS-RDMT-Red_Mountain_fault-CFM2 02 CFM2 02 Red Mountain north branch RMTN North branch NBRN 03 Red Mountain south branch RMTS South branch SBRN WTRA-NCFS-NCPP-North_Channel_fault 02 North Channel NCHN 01 North Channel fault NCHF WTRA-NCFS-PPTV-Pitas_Point_fault 03 Pitas Point-Ventura PPTV 01 Pitas Point fault PPTF WTRA-NCFS-PPTV-Ventura-Pitas_Point_fault 02 Ventura fault VNTF WTRA-NCFS-PPMC-Lower_Pitas_Point_fault-SHAW 04 Pitas Point-Mid-Channel PPMC 01 Lower Pitas Point fault LPPT 01 Shaw model SHAW 11 Oak Ridge fault zone ORFZ 00 Multiple sections MULT Oak Ridge fault ORF WTRA-ORFZ-OFFS-Oak_Ridge_fault-CFM4 01 Offshore (Mid-Channel trend) OFFS 01 Oak Ridge fault ORF CFM4 WTRA-ORFZ-OFFS-Oak_Ridge_fault-CFMA CFMA 02 Mid-Channel fault MCHF WTRA-ORFZ-VNTB-Oak_Ridge_fault 02 Ventura basin VNTR 01 Oak Ridge fault ORF WTRA-ORFZ-SFNV-Northridge-Frew_fault-CFM 03 San Fernando Valley SNFV 01 Northridge-Frew fault NRDF 01 CFM WTRA-ORFZ-SFNV-Northridge-Frew_fault-CFMA 02 CFMA WTRA-SSRZ-MULT-Simi-Santa_Rosa_fault 12 Simi-Santa Rosa fault zone SSRZ 00 Multiple sections MULT 13 Southern Frontal fault system SFFS 00 Multiple sections MULT WTRA-SFFS-SGVS-Raymond_fault-CFM1 01 San Gabriel Valley SGVS 01 Raymond fault WTRA-SFFS-LABS-Hollywood_fault-CFM 01 Los Angeles Basin LABS 01 Hollywood fault WTRA-SFFS-LABS-North_Salt_Lake_fault 02 North Salt Lake fault WTRA-SFFS-SMMT-Santa_Monica_fault-CFM2 02 Santa Monica Mountains SMMT 01 Santa Monica fault WTRA-SFFS-SMMT-Santa_Monica_fault-CFM1-E WTRA-SFFS-SMMT-Santa_Monica_fault-CFM1-C WTRA-SFFS-SMMT-Santa_Monica_fault-CFM1-W WTRA-SFFS-SMMT-Malibu_Coast_fault-CFM4 02 Malibu Coast fault WTRA-SFFS-SMMT-Malibu_Coast_fault-CFM1 WTRA-SFFS-SMMT-Malibu_Coast_fault-CFM2 29 WTRA-SFFS-SMMT-Malibu_Coast_fault-CFM3 WTRA-SFFS-SNCZ-Santa_Cruz_Island_fault-CFM-hw 03 Santa Cruz Island SNCZ 01 Santa Cruz Island fault WTRA-SFFS-SNRS-Santa_Rosa_Island_fault 04 Santa Rosa-San Miguel Islands SNRS 01 Santa Rosa Island fault WTRA-SBTS-MULT-Channel_Islands_thrust-CFM1 14 Southern Boundary thrust system SBTS 00 Santa Cruz Is-Anacapa MULT 01 Channel Islands thrust 01 CFM1 WTRA-SBTS-MULT-Channel_Islands_thrust-CFM2 02 CFM2 WTRA-SBTS-USAV-San_Jose_fault-CFM1 01 Upper Santa Ana Valley USAV 01 San Jose fault 01 CFM1 WTRA-SBTS-USAV-San_Jose_fault-CFM2 02 CFM2 WTRA-SBTS-USAV-San_Jose_fault-CFM3 03 CFM3 WTRA-SBTS-USAV-Upland_fault-CFM1 02 Upland fault 01 CFM1 WTRA-SBTS-USAV-Upland_fault-CFM2 02 CFM2 WTRA-SBTS-PHLS-Puente_Hills_thrust 02 Los Angeles Basin LABS 02 Puente Hills thrust 00 full fault FULL WTRA-SBTS-PHLS-Puente_Hills_thrust-LAB 01 LA subsection LABS APPENDIX 1 WTRA-SBTS-PHLS-Puente_Hills_thrust-SFS 02 Sante Fe Springs subsection SFSS WTRA-SBTS-PHLS-Puente_Hills_thrust-CHS 03 Coyote Hills subsection CYHS WTRA-SBTS-PHLS-Puente_Hills_thrust-RCHF 04 Richfield subsection RCHS WTRA-SBTS-PHLS-Peralta_Hills_fault 03 Peralta Hills fault WTRA-SBTS-LABS-Las_Cienagas_fault-CFM1 03 Los Angeles Basin LABS 04 Las Cienagas fault 01 CFM1 WTRA-SBTS-LABS-Las_Cienagas_fault-CFM2 02 CFM2 WTRA-SBTS-LABS-Las_Cienagas_fault-CFMA 03 CFMA WTRA-SBTS-LABS-San_Vicente_fault 05 San Vicente fault 01 WTRA-SBTS-LABS-Upper_Elysian_Park_fault-CFM1 01 Upper Elysian Park fault 01 CFM1 WTRA-SBTS-LABS-Upper_Elysian_Park_fault-CFM2 02 CFM2 WTRA-SBTS-LABS-Upper_Elysian_Park_fault-CFM3 03 CFM3 WTRA-SBTS-SMNB-Santa_Monica_thrust 03 Santa Monica Bay SMNB 01 Santa Monica thrust WTRA-SBTS-SMNB-Santa_Monica_Bay_fault 02 Santa Monica Bay fault WTRA-SBTS-ANCP-Anacapa-Dume_fault-CFM1 04 Anacapa-Dume ANCP 01 Anacapa-Dume fault WTRA-SBTS-ANCP-Anacapa-Dume_fault-CFM2 WTRA-SBTS-ANCP-Anacapa-Dume_fault-CFMA 02 Channel Islands thrust WTRA-SBTS-SCZI-Channel_Islands_thrust-CFM2 05 Santa Cruz Island SCZI 01 Channel Islands thrust 06 Santa Rosa-San Miguel Islands SRMI 01 Channel Islands thrust WTRA-SGMF-SANC-San_Antonio_Canyon_fault 15 San Gabriel Mountain faults SGMF 01 San Antonio Canyon SANC 01 San Antonio Canyon fault 16 Ventura Basin faults VBNF WTRA-SBCF-WEST-Western_Segment_Boundary_fault 17 Santa Barbara Channel faults SBCF 01 Western WEST 01 Western Segment Boundary fault WTRA-SBCF-CNTR-Worlds_End_fault 02 Central CNTR 01 World's End fault 03 Eastern EAST Eastern Transverse Ranges Area ETRA-CLGZ-MULT-Cleghorn_fault 06 Eastern Transverse Ranges Area ETRA 01 Cleghorn fault zone CLGZ 00 Multiple sections 01 Cleghorn fault 01 Southern Cleghorn 01 Cleghorn fault 02 Tunnel Ridge fault 03 Arrastre Canyon Narrows fault 02 Northern Cleghorn 01 Grass Valley fault 02 North Frontal thrust system NFTS 00 Multiple sections MULT 01 North Frontal thrust ETRA-NFTS-WEST-Western_North_Frontal_Thrust_fault 01 Western WEST 01 Ord Mountains fault 02 Sky High Ranch fault 03 White Mountains thrust ETRA-NFTS-EAST-Eastern_North_Frontal_Thrust_fault-CFM 02 Eastern EAST 01 Eastern North Frontal fault CFM CFM ETRA-NFTS-EAST-Eastern_North_Frontal_Thrust_fault-CFMA CFMA CFMA ETRA-BBFS-1992-Big_Bear_rupture_fault 03 Big Bear Fault system BBFS 01 1992 Big Bear rupture 1992 01 Big Bear rupture 04 Santa Ana fault zone SANA 00 Multiple sections MULT 01 Arrowhead 01 Arrowhead fault 02 Santa Ana 01 Santa Ana fault 05 San Bernardino Mountains fault region SBMT 01 Western 01 Waterman Canyon fault 02 Eastern 01 Pipes Canyon fault ETRA-PMFZ-YUCV-Pinto_Mountain_fault 06 Pinto Mountain fault zone PMFZ 01 Yucca Valley YUCV 01 Pinto Mountain fault 02 Morongo Valley MORV 01 Morongo Valley fault 07 Little San Bernadino Mountains fault region LSBM 00 Multiple sections MULT ETRA-LSBM-BRMT-Burnt_Mountain_fault-CFMA 01 Burnt Mountain BRMT 01 Burnt Mountain fault 02 East Wide Canyon fault ETRA-LSBM-MULT-Burnt_Mountain-East-Wide_Canyon_fault-CFM 03 Burnt Mountain-East Wide Canyon ETRA-LSBM-ERPK-Eureka_Peak_fault-CFMA 02 Eureka Peak ERPK 01 Eureka Peak fault CFMA 02 West Deception Canyon fault ETRA-LSBM-MULT-Eureka_Peak-West_Deception_Canyon_fault-CFM 03 Eureka Peak-West Deception Canyon ETRA-LSBM-1992-Joshua_Tree_Sequence_fault 03 1992 Joshua Tree rupture 1992 01 Joshua Tree sequence ETRA-BCFZ-MULT-Blue_Cut_fault 08 Blue Cut fault zone BCFZ 00 Multiple sections MULT 01 Blue Cut fault ETRA-BCFZ-WEST-Blue_Cut_fault 01 Western WEST ETRA-BCFZ-EAST-Blue_Cut_fault 02 Eastern EAST 09 Chiriaco fault zone CHRC 00 Multiple sections MULT 01 Chiriaco fault Mojave Fault Area 07 Mojave Fault Area MJVA 01 Eastern California shear zone ECSZ 01 Landers rupture 1992 01 Landers sequence LNDS 02 Landers-Barstow trend LNBT 02 Hector Mine rupture 1999 MJVA-HSLZ-MULT-Helendale-South_Lockhart_fault 02 Helendale-South Lockhart fault zone HSLZ 00 Multiple sections MULT 01 Helendale-South Lockhart fault 01 South Lockhart 02 Helendale 03 Northern San Bernardino Mtns MJVA-LWLZ-MULT-Lenwood_Lockhart_fault 03 Lenwood-Lockhart fault zone LWLZ 00 MULT 01 01 Lockhart 01 Lockhart fault 02 Lenwood 01 Lenwood fault MJVA-JVFZ-JNSV-Johnson_Valley_fault-CFM1 04 Johnson Valley-Homestead Valley fault zone JVHZ 00 North-South Johnson Valley MULT 01 Johnson Valley fault JSVF 01 MJVA-JVFZ-JNSV-Johnson_Valley_fault-CFMA 02 01 Northern Johnson Valley NJVS 01 Johnson Valley fault JSVF MJVA-JVHZ-SJVS-Johnson_Valley_fault-CFM2-south 02 Southern Johnson Valley SJVS 01 Johnson Valley fault JSVF 02 Kickapoo fault KCPF MJVA-JVHZ-HMSV-Homestead_Valley_fault Separate Homestead Valley FZ? 03 Homestead Valley HMSV 01 Homestead Valley fault HSVF MJVA-HPFZ-MULT-Gravel_Hills-Harper_Lake_fault 05 Harper fault zone HPFZ 00 Gravel Hills-Harper Lake MULT 01 Gravel Hills-Harper Lake fault GHLF 01 Harper Valley 01 Harper Lake fault HPLF 02 Harper Valley fault HPVF 02 Gravel Hills 01 Gravel Hills fault GVHF 02 Black Mountain fault BKMF MJVA-CREC-MULT-Camp_Rock-Emerson-Copper_Mtn_fault-alt2 06 Camp Rock-Emerson-Copper Mountain fault zone CREC 00 Camp Rock-Copper Mtn MULT 01 Camp Rock-Emerson-Copper Mtn faultCECF 01 MJVA-CREC-MULT-Camp_Rock-Emerson-Copper_Mtn_fault-alt1 MULT 02 MJVA-CREC-MULT-Emerson-Copper_Mtn_fault 00 Emerson-Copper Mountain MULT 02 Emerson-Copper Mtn fault ECMF 01 Camp Rock 01 Camp Rock fault CPRF MJVA-CREC-EMRS-North_Emerson_fault 02 Emerson EMRS 01 North Emerson fault NEMF MJVA-CREC-EMRS-Galway_Lake_fault 02 Galway Lake fault GLWF 03 Copper Mountain 01 Copper Mountain fault CMTF MJVA-BWFZ-MULT-Blackwater_fault 07 Blackwater fault zone BWFZ 00 Multiple sections MULT 01 Blackwater fault BWTF Coon Canyon fault Fossil Canyon fault Owl Canyon fault Rainbow Canyon fault MJVA-CHFZ-MULT-Calico-Hidalgo_fault 08 Calico-Hildalgo fault zone CHFZ 00 Multiple sections MULT 01 Calico-Hildalgo fault CLHF 01 Calico 01 Calico fault CLCF 02 west Calico 01 West Calico fault WCLF 03 Hildalgo 01 Hildalgo fault HLDF 30 MJVA-PBMZ-MULT-Pisgah_Bullion_Mesquite_Lake_fault-CFM2 09 Pisgah-Bullion-Mesquite Lake fault zone PBMZ 00 Pisgah-Mesquite Lake MULT 01 Pisgah-Bullion-Mesquite Lake fault 01 MJVA-PBMZ-MULT-Pisgah_Bullion_Mesquite_Lake_fault 02 MJVA-PBMZ-MULT-Pisgah_Bullion_Mesquite_Lake_fault-CFMA 03 01 Pisgah 01 Pisgah fault 02 Bullion 01 Bullion fault 03 East Bullion 01 East Bullion fault 02 Valley Mountain fault 04 West Bullion 01 West Bullion fault 05 Mesquite Lake 01 Mesquite Lake fault 02 Airfield fault 10 Lavic Lake-Bullion Mountains fault zone LLBM 00 Multiple sections MULT MJVA-LLBM-LVLK-Lavic_Lake_fault 01 Lavic Lake LVLK 01 Lavic Lake fault LVLF APPENDIX 1 02 Bullion Mountains BLNM 01 Bullion Mountains fault BLMF 11 Ludlow-Cleghorn Lake fault zone LCLZ 00 Multiple sections MULT MJVA-LCLZ-LDLW-Ludlow_fault 01 Ludlow LDLW 01 Ludlow fault LDLF 02 Cleghorn Lake CLGL 01 Cleghorn Lake fault CLGF MJVA-GLPS-GLDS-Goldstone_Lake_fault 12 Goldstone Lake-Paradise fault system GLPS 01 Goldstone Lake GLDS 01 Goldstone Lake fault GLSF MJVA-GLPS-PRDS-Paradise_fault 02 Paradise PRDS 01 Paradise fault PRDF MJVA-CRSF-GNTM-McLean_Lake-Drinkwater_Lake_fault 13 Cross Faults CRSF 01 Granite Mountains GNTM 01 McLean Lake-Drinkwater Lake fault MDLF MJVA-CRSF-GNTM-Nelson_Lake_fault 02 Nelson Lake fault NSLF 03 Granite Mountains fault GRMF MJVA-CRSF-TFMT-Coyote_Canyon_fault 02 Tiefort Mountains TFMT 01 Coyote Canyon fault CYCF 02 Tiefort Mountain fault TFMF MJVA-CRSF-BCYL-Bicycle_Lake_fault 03 Bicycle Lake BCYL 01 Bicycle Lake fault BCLF MJVA-CRSF-CYTL-Coyote_Lake_fault 04 Coyote Lake CYTL 01 Coyote Lake fault CYLF MJVA-CRSF-MANX-Manix_fault 05 Manix MANX 01 Manix fault MNXF MJVA-CRSF-CADY-Cady_fault 06 Cady CADY 01 Cady fault CDYF 14 West Mojave faults WMVF 01 Mirage Valley MRGV 01 Mirage Valley fault MRVF 02 Blake Ranch BLKR 01 Blake Ranch fault BLRF 03 Kramer Hills KRMH 01 Kramer Hills fault KRHF MJVA-NEMV-RDPS-Red_Pass_fault 15 Northeast Mojave faults NEMV 01 Red Pass RDPS 01 Red Pass fault RDPF MJVA-NEMV-GRLS-Garlic_Springs_fault 02 Garlic Springs GRLS 01 Garlic Springs fault GRSF Garlock Fault System 08 Garlock Fault System GRFS 01 Garlock falt zone GRFZ 00 Multiple sections MULT 01 Garlock fault GRLF GRFS-GRFZ-WEST-Garlock_fault 01 Western WEST 01 Garlock fault GRLF 02 Central CNTL 01 Garlock fault GRLF GRFS-GRFZ-EAST-Garlock_fault 03 Eastern EAST 01 Garlock fault GRLF GRFS-GRFZ-EAST-Owl_Lake_fault 02 Owl Lake fault OWLF Basin and Range Area BNRA-BMFZ-MULT-Black_Mountain_fault 09 Basin and Range Area BNRA 01 Black Mountain fault zone BMFZ 00 Multiple sections MULT 01 Black Mountain fault BMTF 01 Mustard Hills 02 Artist's Canyon 03 Copper Canyon 04 Smith Mountain

BNRA-NDVZ-MULT-Northern_Death_Valley_fault 02 Northern Death Valley fault zone NDVZ 00 Multiple sections MULT Northern Death Valley fault 01 Grapevine Mountains 02 Mesquite Flat-Screwbean Spring 03 Kit Fox Hills

BNRA-SDVZ-MULT-Southern_Death_Valley_fault-CFM1 03 Southern Death Valley fault zone SDVZ 00 Multiple sections MULT 01 Southern Death Valley fault SDVF 01 CFM1 CFM1 BNRA-SDVZ-MULT-Southern_Death_Valley_fault-CFM2 01 Confidence Hills 01 02 CFM2 CFM2 02 Nobel Hills 01 BNRA-FCFZ-FCRS-Furnace_Creek_fault-CFMA 04 Furnace Creek fault zone FCFZ Furnace Creek fault(?) FRCF Sierra Nevada Fault Area 10 Sierra Nevada Fault Area SNFA 01 Owens Valley fault zone OVFZ 00 Multiple sections MULT 01 Owens Valley fault ONVF 01 Northern 01 Owens Valley fault 02 Southern 01 Owens Valley fault 02 Lone Pine fault SNFA-OVFZ-1872-Owens_Valley_fault 03 1872 rupture 1872 01 Owens Valley fault SNFA-SSNZ-MULT-Independance-Sierra_Nevada_fault 02 Southern Sierra Nevada fault zone SSNZ 00 Independence-Haiwee Reservoir MULT 01 Independence-Sierra Nevada fault SNFA-SSNZ-INDP-Independance_fault 01 Independence 01 Independence fault 02 Haiwee Reservoir 01 Sierra Nevada fault 02 Cliff Canyon fault SNFA-HMFZ-MULT-Hunter_Mountain_fault 03 Hunter Mountain fault zone HMFZ 00 Hunter Mtn-Saline Valley MULT 01 Hunter Mountain fault 01 Saline Valley 01 Saline Valley fault 02 Hunter Mountain 01 Hunter Mountain fault SNFA-PMVZ-MULT-Panamint_Valley_fault-CFM 04 Panamint Valley fault zone PMVZ 00 Northern Panamint-Brown Mtn MULT 01 Panamint Valley fault CFM SNFA-PMVZ-MULT-Panamint_Valley_fault-CFMA CFMA 01 Northern Panamint Valley 01 Panamint Valley fault 02 Wildrose 01 Wildrose graben fault 03 Southern Panamint 01 Panamint Valley fault 04 Brown Mountain 01 Brown Mountain fault SNFA-AHTC-ASHH-Ash_Hill_fault-CFM 05 Ash Hill-Tank Canyon fault system AHTC 01 Ash Hill 01 Ash Hill fault SNFA-AHTC-TANK-Tank_Canyon_fault-CFM 02 Tank Canyon 01 Tank Canyon fault CFM SNFA-AHTC-TANK-Tank_Canyon_fault-CFMA CFMA SNFA-LLFZ-CNTR-Little_Lake_fault-CFM 06 Little Lake fault zone LLFZ 01 Central CNTL Little Lake fault CFM SNFA-LLFZ-CNTR-Little_Lake_fault-CFMA CFMA Great Valley Fault Area GVFA-WWFZ-MULT-White_Wolf_fault 11 Great Valley Fault Area GVFA 01 White Wolf fault zone WWFZ 00 Multiple Sections MULT 01 White Wolf fault 01 Western WEST 01 White Wolf fault 02 Eastern EAST 01 White Wolf fault GVFA-WWFZ-EAST-Scodie_Lineament 02 Scodie Lineament GVFA-PLFZ-MULT-Pleito_fault-CFM 02 Pleito fault zone PLFZ 00 Multiple sections MULT 01 Pleito fault 01 CFM GVFA-PLFZ-MULT-Pleito_fault-CFMA 02 CFMA 01 Western WEST 01 Pleito fault 02 Oak Hill fault 02 Eastern EAST 01 Pleito fault 03 Kern Front fault system KRFS 01 Kern Front 01 Kern Front fault 02 Kern Gorge 01 Kern Gorge fault GVFA-TDRS-COAL-Coalinga_fault 04 Temblor-Diablo Range thrust system TDRS 01 Coalinga COAL 01 Coalinga fault GVFA-TDRS-KTLM-Kettleman_Hills_fault 02 Kettleman Hills KTLM 01 Kettleman Hills fault GVFA-TDRS-LSTH-Lost_Hills_fault 03 Lost Hills LSTH 01 Lost Hills fault GVFA-LILZ-CNTR-Lake_Isabella_Lineament 05 Lake Isabella Lineament zone LILZ Coast Ranges Fault Area 12 Coast Ranges Fault Area CRFA 01 Rinconada-East Huasna fault system RNEH 00 Multiple sections 01 Rinconada 01 Espinoza 01 Espinoza fault 02 San Marcos 01 SAn Marcos fault 03 Rinconada 01 Rinconada fault 04 East Huasna 01 East Huasna fault CRFA-SCFZ-MULT-South_Cuyama_fault 02 South Cuyama-Ozena fault zone SCFZ 01 South Cuyama 01 South Cuyuma fault 02 Ozena 01 Ozena fault 03 San Juan-Morales fault zone SJMZ 01 San Juan 01 San Juan fault 02 Big Spring fault 03 Chimineas fault 04 Gillis Canyon 31 05 Red hills CRFA-SJMZ-MRLS-Morales_fault 02 Morales 01 Morales fault 04 La Pana fault zone LPNZ 05 Big Pine-Pine Mountain fault zone BPPM 00 Multiple sections MULT 01 Big Pine faut CRFA-BPPM-WEST-West_Big_Pine_fault 01 Western Big Pine 01 Big Pine fault 01 North Branch 01 02 South Branch CRFA-BPPM-EAST-Big_Pine_fault 02 Eastern Big Pine 01 Big Pine fault CRFA-BPPM-MULT-East_Big_Pine_fault-CFMA 02 San Guillermo fault CRFA-BPPM-LCKV-Lockwood_Valley_fault 03 Lockwood Valley 01 Lockwood Valley fault 02 South Lockwood Valley fault CRFA-BPPM-PMTS-Pine_Mountain_fault-CFM1 04 Pine Mountain 01 Pine Mountain fault CFM1 CRFA-BPPM-PMTS-Pine_Mountain_fault-CFM2 CFM2 APPENDIX 1 CRFA-NAFZ-MULT-Nacimiento_fault 06 Nacimiento fault zone NAFZ 00 Multiple sections MULT 01 Nacimiento fault 07 Oceanic fault zone OCNZ 01 Santa Lucia Range 01 Oceanic fault 02 Serrano fault 02 West Huasna 01 West Huasna fault 03 Cambria 01 Cambria fault 08 San Luis Range fault system SLRZ 01 Los Osos 01 Los Osos fault 02 Edna 01 Edna fault 03 Little Pine 01 Little Pine fault 09 Casmalia fault zone CSMZ 00 Multiple sections MULT 01 Casmalia fault 10 Lions Head fault zone LNHZ 00 Multiple sections MULT 01 Lion's Head fault Offshore Central California Area OCCA-HSFZ-MULT-Hosgri_fault 13 Offshore Central California Area OCCA 01 Hosgri fault zone HSFZ 00 Multiple sections MULT 01 Hosgri fault 01 Northern 02 San Luis-Pismo 03 San Luis Obispo BAy 04 Point Sal 05 Southern 02 San Simeon fault zone SSMZ 00 Multiple sections MULT 01 San Simeon fault 02 Arroyo del Oso fault 03 Santa Lucia Bank fault zone SLBZ 00 Multiple sections MULT 01 Santa Lucia Bank fault 32