Southern California is home to nearly 24 million people and countless visitors who live, recreate, consume resources, and face the risk of natural hazards in the region. This project produces high-quality, multi-purpose geologic maps, databases, and reports that portray our understanding of the region’s four-dimensional geologic framework. We conduct stratigraphic, structural, geomorphological, geophysical, geochronological, and paleontological studies, and we assist other stakeholders in applying our findings toward establishing geologic context for diverse land-use management issues; for assessing water, mineral, and energy resources; and for understanding natural hazards.
The geologic and landscape evolution of southern California is framed by plate tectonic interactions between the North America and Pacific plates, leading most recently to the growth of the San Andreas Fault system. Our project studies are helping to document the evolving formation and deformation of crustal blocks—accompanied by the growth and subsequent disruption of mountain ranges and flanking basins—that record the magnitude, timing, and interactive roles of faults comprising this plate-margin system.
Science Issue and Relevance:
Plate-margin deformation leads either directly (through seismic events) or indirectly (by creating steep range-front relief) to high-risk of natural hazards in southern California, home to more than 24 million people. USGS and USGS-sponsored studies have made and continue to make essential contributions to our understanding of the overall geologic and tectonic framework for these hazards. Because the region contained crustal faults before the initiation of the San Andreas system, these studies will consider the full timespan of plate margin evolution. This will allow the greatest insight into the distribution of seismic hazards.
Methodology to Address Issue:
FEDMAP Geologic Mapping - FEDMAP Geologic Mapping advances nationwide geologic mapping and associated research as mandated by the National Geologic Mapping Act of 1992 (Public Law 102-285). The FEDMAP program produces world-class digital geologic maps and 3D framework models based on state-of-the art observation and scientific interpretation directed by high priority national issues.
Within the Fedmap framework we will
- Conduct geologic mapping, stratigraphic, geochronologic, and geophysical studies that contribute to our understanding of fault interactions in the San Andreas system in Southern California
- Conduct geomorphic mapping and carry out tectonic landform analyses that help us understand landscape evolution and hazards in southern CA, and
- Conduct paleontologic and paleogeographic studies in Eocene, Miocene, and Pliocene strata along the San Andreas fault
Below are publications associated with this project.
Insights into the geometry and evolution of the southern San Andreas Fault from geophysical data, southern California
Geology and hydrogeology of the Yucaipa groundwater subbasin, San Bernardino and Riverside Counties, California
Benthic foraminiferal biotic events related to the Paleocene–Eocene Thermal Maximum along the California Margin
Distributed fault slip in the eastern California shear zone: Adding pieces to the puzzle near Barstow, California
Geologic map and database of the Chocolate Mountain Aerial Gunnery Range, Riverside and Imperial Counties, California
Punctuated sediment discharge during early Pliocene birth of the Colorado River: Evidence from regional stratigraphy, sedimentology, and paleontology
Subsurface geometry of the San Andreas fault in southern California: Results from the Salton Seismic Imaging Project (SSIP) and strong ground motion expectations
Geologic map of the Morena Reservoir 7.5-minute quadrangle, San Diego County, California
High-resolution gravity and seismic-refraction surveys of the Smoke Tree Wash area, Joshua Tree National Park, California
Geology of Joshua Tree National Park geodatabase
Crustal-scale tilting of the central Salton block, southern California
Late Quaternary slip history of the Mill Creek strand of the San Andreas fault in San Gorgonio Pass, southern California: The role of a subsidiary left-lateral fault in strand switching
Below are partners associated with this project.
- Overview
Southern California is home to nearly 24 million people and countless visitors who live, recreate, consume resources, and face the risk of natural hazards in the region. This project produces high-quality, multi-purpose geologic maps, databases, and reports that portray our understanding of the region’s four-dimensional geologic framework. We conduct stratigraphic, structural, geomorphological, geophysical, geochronological, and paleontological studies, and we assist other stakeholders in applying our findings toward establishing geologic context for diverse land-use management issues; for assessing water, mineral, and energy resources; and for understanding natural hazards.
The geologic and landscape evolution of southern California is framed by plate tectonic interactions between the North America and Pacific plates, leading most recently to the growth of the San Andreas Fault system. Our project studies are helping to document the evolving formation and deformation of crustal blocks—accompanied by the growth and subsequent disruption of mountain ranges and flanking basins—that record the magnitude, timing, and interactive roles of faults comprising this plate-margin system.
Science Issue and Relevance:
Plate-margin deformation leads either directly (through seismic events) or indirectly (by creating steep range-front relief) to high-risk of natural hazards in southern California, home to more than 24 million people. USGS and USGS-sponsored studies have made and continue to make essential contributions to our understanding of the overall geologic and tectonic framework for these hazards. Because the region contained crustal faults before the initiation of the San Andreas system, these studies will consider the full timespan of plate margin evolution. This will allow the greatest insight into the distribution of seismic hazards.
Photograph from summit of San Jacinto Peak looking north across San Gorgonio Pass toward San Gorgonio Mountain. San Gorgonio River and Interstate Highway 10 traverse the Pass lowland; the Whitewater River drains the San Bernardino Mountains and flows eastward into the Salton Trough. San Gorgonio Pass is known as a geologically complex segment of the San Andreas Fault that traverses the landscape from southeast to northwest (white arrows mark the approximate trace of one of the multiple fault lines in the Pass region). Methodology to Address Issue:
FEDMAP Geologic Mapping - FEDMAP Geologic Mapping advances nationwide geologic mapping and associated research as mandated by the National Geologic Mapping Act of 1992 (Public Law 102-285). The FEDMAP program produces world-class digital geologic maps and 3D framework models based on state-of-the art observation and scientific interpretation directed by high priority national issues.
Oblique orbital view of California looking NNW from above NW Sonora, Mexico, and northern Gulf of California (NASA Space Shuttle Photgraph STS103-701-39) Within the Fedmap framework we will
- Conduct geologic mapping, stratigraphic, geochronologic, and geophysical studies that contribute to our understanding of fault interactions in the San Andreas system in Southern California
- Conduct geomorphic mapping and carry out tectonic landform analyses that help us understand landscape evolution and hazards in southern CA, and
- Conduct paleontologic and paleogeographic studies in Eocene, Miocene, and Pliocene strata along the San Andreas fault
The image shown displays a portion of the lidar data collected by the USGS for the SAFSOC Project. Our goal is to study and map surficial processes and landforms related to tectonism, specifically the San Andreas Fault system. With computer processing to remove vegetation, highly accurate, bare-earth digital elevation models of the ground surface are derived to aid in more accurately mapping fault scarps, lineaments, landslides, and geology. - Publications
Below are publications associated with this project.
Filter Total Items: 15Insights into the geometry and evolution of the southern San Andreas Fault from geophysical data, southern California
Two new joint gravity-magnetic models in northern Coachella Valley provide additional evidence for a steep northeast dip of the Mission Creek strand of the southern San Andreas fault (southern California, USA). Gravity modeling indicates a steep northeast dip of the Banning fault in the upper 1–2 km in northern Coachella Valley. The Mission Creek strand and its continuation to the southeast (CoachAuthorsVictoria Langenheim, Gary S. FuisGeology and hydrogeology of the Yucaipa groundwater subbasin, San Bernardino and Riverside Counties, California
The Yucaipa groundwater subbasin (referred to in this report as the Yucaipa subbasin) is located about 75 miles (mi) east of of Los Angeles and about 12 mi southeast of the City of San Bernardino. In the Yucaipa subbasin, as in much of southern California, limited annual rainfall and large water demands can strain existing water supplies; therefore, understanding local surface water and groundwateAuthorsGeoffrey Cromwell, Jonathan C. MattiBenthic foraminiferal biotic events related to the Paleocene–Eocene Thermal Maximum along the California Margin
The faunal expression of the Paleocene-Eocene Thermal Maximum (PETM) is well documented in deep-sea sediments. However, few studies have examined continental margin sections, especially active margins. The Moreno and Lodo formations, Central California, were deposited along the eastern margin of a north-south trending forearc basin on the convergent margin of California during the Cretaceous throuAuthorsKristin McDougall-Reid, Cedric M JohnDistributed fault slip in the eastern California shear zone: Adding pieces to the puzzle near Barstow, California
We investigate the dextral Lockhart and Mt. General faults, which are among four active structures in the northwestern portion of the eastern California shear zone (ECSZ). Early mapping depicts the Lockhart and Mt. General faults as discontinuous fault traces that continue northwest of the Lenwood Fault. Recent work indicates that the Lenwood Fault slips at ~0.2-1.0 mm/yr over the past ~8 ka and 0AuthorsElizabeth K. Haddon, David M. Miller, Victoria Langenheim, Shannon A. MahanGeologic map and database of the Chocolate Mountain Aerial Gunnery Range, Riverside and Imperial Counties, California
The northwest-trending Chocolate Mountains are situated along the northeastern margin of the southern Salton Trough. The Chocolate Mountain Aerial Gunnery Range occupies most of the 75-km-long part of the Chocolate Mountains that lies between Salt Creek to the north and California State Highway 78 to the south. Mapping studies in the Chocolate Mountains within the gunnery range are few and this stAuthorsRobert E. Powell, Robert J. Fleck, Pamela M. CossettePunctuated sediment discharge during early Pliocene birth of the Colorado River: Evidence from regional stratigraphy, sedimentology, and paleontology
The Colorado River in the southwestern U.S. provides an excellent natural laboratory for studying the origins of a continent-scale river system, because deposits that formed prior to and during river initiation are well exposed in the lower river valley and nearby basinal sink. This paper presents a synthesis of regional stratigraphy, sedimentology, and micropaleontology from the southern Bouse FoAuthorsRebecca J. Dorsey, Brennan O’Connell, Kristin McDougall-Reid, Mindy B. HomanSubsurface geometry of the San Andreas fault in southern California: Results from the Salton Seismic Imaging Project (SSIP) and strong ground motion expectations
The San Andreas fault (SAF) is one of the most studied strike‐slip faults in the world; yet its subsurface geometry is still uncertain in most locations. The Salton Seismic Imaging Project (SSIP) was undertaken to image the structure surrounding the SAF and also its subsurface geometry. We present SSIP studies at two locations in the Coachella Valley of the northern Salton trough. On our line 4, aAuthorsGary S. Fuis, Klaus Bauer, Mark R. Goldman, Trond Ryberg, Victoria E. Langenheim, Daniel S. Scheirer, Michael J. Rymer, Joann M. Stock, John A. Hole, Rufus D. Catchings, Robert Graves, Brad T. AagaardGeologic map of the Morena Reservoir 7.5-minute quadrangle, San Diego County, California
IntroductionMapping in the Morena Reservoir 7.5-minute quadrangle began in 1980, when the Hauser Wilderness Area, which straddles the Morena Reservoir and Barrett Lake quadrangles, was mapped for the U.S. Forest Service. Mapping was completed in 1993–1994. The Morena Reservoir quadrangle contains part of a regional-scale Late Jurassic(?) to Early Cretaceous tectonic suture that coincides with theAuthorsVictoria R. ToddHigh-resolution gravity and seismic-refraction surveys of the Smoke Tree Wash area, Joshua Tree National Park, California
We describe high-resolution gravity and seismic refraction surveys acquired to determine the thickness of valley-fill deposits and to delineate geologic structures that might influence groundwater flow beneath the Smoke Tree Wash area in Joshua Tree National Park. These surveys identified a sedimentary basin that is fault-controlled. A profile across the Smoke Tree Wash fault zone reveals low gravAuthorsVictoria E. Langenheim, Michael J. Rymer, Rufus D. Catchings, Mark R. Goldman, Janet Watt, Robert E. Powell, Jonathan C. MattiGeology of Joshua Tree National Park geodatabase
The database in this Open-File Report describes the geology of Joshua Tree National Park and was completed in support of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey (USGS) and in cooperation with the National Park Service (NPS). The geologic observations and interpretations represented in the database are relevant to both the ongoing scientific interests of theAuthorsRobert E. Powell, Jonathan C. Matti, Pamela M. CossetteCrustal-scale tilting of the central Salton block, southern California
The southern San Andreas fault system (California, USA) provides an excellent natural laboratory for studying the controls on vertical crustal motions related to strike-slip deformation. Here we present geologic, geomorphic, and gravity data that provide evidence for active northeastward tilting of the Santa Rosa Mountains and southern Coachella Valley about a horizontal axis oriented parallel toAuthorsRebecca Dorsey, Victoria E. LangenheimLate Quaternary slip history of the Mill Creek strand of the San Andreas fault in San Gorgonio Pass, southern California: The role of a subsidiary left-lateral fault in strand switching
The fault history of the Mill Creek strand of the San Andreas fault (SAF) in the San Gorgonio Pass region, along with the reconstructed geomorphology surrounding this fault strand, reveals the important role of the left-lateral Pinto Mountain fault in the regional fault strand switching. The Mill Creek strand has 7.1–8.7 km total slip. Following this displacement, the Pinto Mountain fault offset tAuthorsKatherine J. Kendrick, Jonathan C. Matti, Shannon A. Mahan - Partners
Below are partners associated with this project.