This project uses geologic and geomorphic mapping in the context of societally relevant problems in the Earth’s critical zone. Leveraging interdisciplinary research ties and interagency collaborations, it utilizes remote sensing data, corroborated with field observations, to determine i) the spatial distribution of geomorphic processes and ages of Quaternary deposits in the context of active tectonics, landsliding, and ecosystem function in coastal California, ii) the discharge of land-based pollutants, such as sediment and nutrients, degrading coral reef ecosystems in the Hawaiian Islands, and iii) the record of earthquake-triggered terrestrial Quaternary landslides in the west. Working with land-use manager partners, answers to the following questions should result in readily applied science:
Where in the landscape are Quaternary materials and where are they geomorphically active?
What are their sources, rates of deposition with respect to frequency and magnitude, and thresholds for re-mobilization?
Science Issue and Relevance:
Active geomorphic processes, surface erosion, and landslides
Mapping the distribution of earth materials is essential to understanding the location, timing, and magnitude of surface-water availability, ecosystem function, and erosion hazards. Bedrock and Quaternary surficial maps provide different information for analyzing processes that span the surface and subsurface. Supplemental geomorphic process maps, expressing modes of sediment transport tied to triggering functions, can be used to estimate future mobilization thresholds. Additionally, efforts to estimate 3D thickness, with refinements of deposit architecture and material properties, elucidate potential landslide volumes and potential runout lengths.
Active Tectonics
Constraining connectivity between faults, past displacement rates, and cumulative displacements are critical to modeling future deformation and relative hazard to life and property. While most existing geologic maps focus on fault deformation in bedrock, providing context for long-term deformation patterns and mineral resources, knowledge of Quaternary fault activity is critical to estimate hazard and risk. Opportunities exist to map offset of Quaternary materials associated with on- and off-fault deformation patterns. Quaternary surficial mapping, at scales commensurate with fault-displaced materials, coupled with robust numerical dating campaigns will refine frequency/magnitude relations.
Surface and Ground Water
As industrial, agricultural, and residential demands continue to stress available resources, surface water and groundwater reserves will be in higher demand. Understanding the spatial distribution of earth materials is critical to forecasting where water reserves exist. Quaternary surficial maps, including unit thicknesses, could inform estimates of transmissivity and water delivery rates. Albeit, thin-skinned, this avenue can enrich geologic maps with 3-D data.
Post-event response
In the wake of natural disasters, decision makers have timely needs for accurate earth science information. Improving the collection of potentially time-sensitive, spatially relevant data for map representation of source and inundation areas for immediate planning and extrapolation to future events is high-visibility science. Map-based interpretations promote richer interpretations of geomorphic indicators of pre-historic ground ruptures, multi-disciplinary research, integrated assessments, predictive modeling, and knowledge transfer to land managers.
Methodology to Address Issues:
Geologic Maps and associated Geodatabases
Although this project generates traditional Quaternary surficial geologic maps, it also forges new directions demonstrating the utility of geomorphic transport process mapping. This new mapping will address topical research problems with collaborating partners. Mapping strategies will employ remotely sensed image analysis, field control for characteristic map units, stratigraphic, paleontologic, geochronological, and geochemical studies. Maps will be released on scale-appropriate base materials such as high-resolution, lidar-derived topography.
Watershed Erosion Rates
Mapping the geomorphic processes, coupled with monitoring the erosion rates and modeling the sediment budget, locates and quantifies the sediment sources and sediment flux from a watershed. We can estimate the magnitude and recurrence interval of erosion-causing events. The resulting products enable community members and relevant stakeholders to make informed decisions about how to efficiently protect resources to maintain long-term viability.
Structure from Motion to estimate ground-deformation
Structure from Motion (SfM) from fixed wing or UAV platforms provides a cost-effective means to rapidly acquire imagery that can be transformed to digital topography using photogrammetry. The inherent high spatial and temporal resolution of coupled imagery and topography, as well as potential for time series data, allow for enhanced mapping of deposits and joining them to transport mechanisms (wind, rain, etc.). Target areas include constraining crustal deformation associated with tectonics and deep-seated landsliding. Such an approach is essential to responding to post-event natural disaster recovery mission as the UAV platform can be used to generate both imagery and topography for process mapping.
Results
1. Quaternary Geologic Mapping of Channel Islands National Park (CHIS)
Tectonics
Located in the western Transverse Range (WTR) of California, Channel Islands National Park (CHIS) is part of the active broad San Andreas transform plate margin with dramatic Neogene and Quaternary transpressional faulting, folding, and clockwise vertical-axis rotations of crustal blocks. Geologically youthful manifestations of tectonism include regions of concentrated seismicity and recent to active crustal uplift, associated basinal subsidence, and local drainage capture. Significant seismic hazard exists, exemplified by the 2018 M 5.3 earthquake south of Santa Cruz Island that triggered coastal landslides.

Surface Water Availability
Recent repeat surveys of surface-water distribution conducted by NPS-CHIS scientists reveal spring and sink points that correlate with geologic contacts and faults juxtaposing rocks and deposits with contrasting hydrologic properties. Spatial correlations between independent geologic and hydrologic mapping provide the opportunity to evaluate causal mechanisms for surface water presence in the water-limited landscape and assist restoration efforts.

Ecosystem Restoration
Disturbance caused by heavy grazing, introduction of non-native vegetation, and associated erosion complicates NPS land management. Grazing of native vegetation on steep slopes resulted in significantly increased erosion rates and, in some cases, complete stripping of hillslope soil. Presently, endemic vegetation is competing with non-natives, especially shrubs and grasses, or has been completely replaced by invasive species. The Channel Islands are unique in that the grazing ungulates have been removed and the landscape is now managed for conservation with concomitant restoration efforts.
Big Sur Coast Landslides
Faulting and associated uplift in the Santa Lucia Range of central California has generated steep, high-relief hillslopes with abundant active landslides suppling sediment to the adjacent national marine sanctuary in the Pacific Ocean and impacting California Hwy. 1. The 2017 Mud Creek landslide closed Hwy. 1 for 15 months with a present cost of $54 million to re-open the road. Hwy. 1, the only transportation artery along the coast has an average daily traffic count of ~ 4000. Closures have been common since its inauguration in 1937, with long-term deep-seated landslide-induced closures occurring in years of heavy rainfall. Structure from Motion (SfM) was used to estimate the timing of deformation and volume of the Mud Creek landslide.
2. Geomorphic Process Mapping, Monitoring and Modeling to Non-Point Source Erosion Impacting Coral Reef Health in the Hawaiian Islands
Coral reef ecosystems, and the fishing and tourism industries they support, depend on clean waters. Fine sediment pollution from nearshore watersheds threatens these economies across the Hawaiian Islands. The terrestrial sediment sources are largely unknown and vary by location due to geology and land-use history. To effectively mitigate sediment pollution, it is critical to know where the sediment is coming from, how fast it erodes, and when it moves. These questions are either unanswered or unquantified, and relevant to stakeholders trying to mitigate the problem. USGS, in collaboration with federal and local partners, is working in watersheds across the Hawaiian Islands to: 1) map geomorphic processes generating fine sediment, 2) monitor erosion rates, 3) determine thresholds for sediment mobilization, and 4) determine the likely frequency of triggering events. The products delivered provide data stakeholders use to make informed mitigation decisions.

3. Evaluating the record of earthquake-triggered terrestrial Quaternary landslides
The Pacific Northwest and Coastal California face a myriad of landslide hazards ranging from subduction zone megathrust earthquakes in the north, shallow crustal earthquakes along the central and southern California coast, and heavy precipitation in the form of atmospheric river events across much of the region. However, our understanding of the terrestrial landscape response to these events is lacking. In collaboration with academic colleagues, personnel are convening a series of workshops through USGS Powell Center to integrating geological and geophysical datasets to understand subduction zone earthquake recurrence and hazards.
Below are data or web applications associated with this project.
Field measurements of rainfall and soil moisture data used to support understanding of infiltration and runoff following the 2007 Canyon Fire, Malibu, CA, USA
Sr concentrations and 87Sr/86Sr data used to determine the Sr-chronostratigraphic age of sirenian fossils on Santa Rosa Island, Channel Islands National Park, California, USA
Field-saturated hydraulic conductivity time series and sediment accumulations following the 2017 Nuns and Tubbs wildfires, Napa and Sonoma Counties, CA, USA
Root thread strength, landslide headscarp geometry, and observed root characteristics at the monitored CB1 landslide, Oregon, USA
Field, geotechnical, and meteorological data of the 22 March 2018 narrow cold frontal rainband (NCFR) and its effects, Tuolumne River canyon, Sierra Nevada Foothills, California
Field observations of ground failure triggered by the 2020 Puerto Rico earthquake sequence
Below are publications associated with this project.
Hunting for landslides from Cascadia's great earthquakes
Inversions of landslide strength as a proxy for subsurface weathering
From data to interpretable models: Machine learning for soil moisture forecasting
Comparing root cohesion estimates from three models at a shallow landslide in the Oregon Coast Range
Multi-stage soil-hydraulic recovery and limited ravel accumulations following the 2017 Nuns and Tubbs wildfires in Northern California
Developing landslide chronologies using landslide-dammed lakes in the Oregon Coast Range
When hazard avoidance is not an option: Lessons learned from monitoring the postdisaster Oso landslide, USA
Sediment budget for watersheds of West Maui, Hawaii
Unsaturated flow processes and the onset of seasonal deformation in slow-moving landslides
Renewing the National Cooperative Geologic Mapping Program as the Nation’s authoritative source for modern geologic knowledge
Toward an integrative geological and geophysical view of Cascadia subduction zone earthquakes
Linking mesoscale meteorology with extreme landscape response: Effects of narrow cold frontal rainbands (NCFR)
Rainfall triggers more deep-seated landslides than Cascadia earthquakes in the Oregon Coast Range, USA
- Overview
This project uses geologic and geomorphic mapping in the context of societally relevant problems in the Earth’s critical zone. Leveraging interdisciplinary research ties and interagency collaborations, it utilizes remote sensing data, corroborated with field observations, to determine i) the spatial distribution of geomorphic processes and ages of Quaternary deposits in the context of active tectonics, landsliding, and ecosystem function in coastal California, ii) the discharge of land-based pollutants, such as sediment and nutrients, degrading coral reef ecosystems in the Hawaiian Islands, and iii) the record of earthquake-triggered terrestrial Quaternary landslides in the west. Working with land-use manager partners, answers to the following questions should result in readily applied science:
Where in the landscape are Quaternary materials and where are they geomorphically active?
What are their sources, rates of deposition with respect to frequency and magnitude, and thresholds for re-mobilization?
Science Issue and Relevance:
Active geomorphic processes, surface erosion, and landslides
Mapping the distribution of earth materials is essential to understanding the location, timing, and magnitude of surface-water availability, ecosystem function, and erosion hazards. Bedrock and Quaternary surficial maps provide different information for analyzing processes that span the surface and subsurface. Supplemental geomorphic process maps, expressing modes of sediment transport tied to triggering functions, can be used to estimate future mobilization thresholds. Additionally, efforts to estimate 3D thickness, with refinements of deposit architecture and material properties, elucidate potential landslide volumes and potential runout lengths.
Active Tectonics
Constraining connectivity between faults, past displacement rates, and cumulative displacements are critical to modeling future deformation and relative hazard to life and property. While most existing geologic maps focus on fault deformation in bedrock, providing context for long-term deformation patterns and mineral resources, knowledge of Quaternary fault activity is critical to estimate hazard and risk. Opportunities exist to map offset of Quaternary materials associated with on- and off-fault deformation patterns. Quaternary surficial mapping, at scales commensurate with fault-displaced materials, coupled with robust numerical dating campaigns will refine frequency/magnitude relations.
Surface and Ground Water
As industrial, agricultural, and residential demands continue to stress available resources, surface water and groundwater reserves will be in higher demand. Understanding the spatial distribution of earth materials is critical to forecasting where water reserves exist. Quaternary surficial maps, including unit thicknesses, could inform estimates of transmissivity and water delivery rates. Albeit, thin-skinned, this avenue can enrich geologic maps with 3-D data.
Post-event response
In the wake of natural disasters, decision makers have timely needs for accurate earth science information. Improving the collection of potentially time-sensitive, spatially relevant data for map representation of source and inundation areas for immediate planning and extrapolation to future events is high-visibility science. Map-based interpretations promote richer interpretations of geomorphic indicators of pre-historic ground ruptures, multi-disciplinary research, integrated assessments, predictive modeling, and knowledge transfer to land managers.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologist Jonathan Perkins adjusting tension in infiltrometer to evaluate post-fire recovery conditions in the Pepperwood Preserve, Santa Rosa, CA following the October 2017 Tubbs Fire to better understand how landscapes heal after wildfire. Methodology to Address Issues:
Geologic Maps and associated Geodatabases
Although this project generates traditional Quaternary surficial geologic maps, it also forges new directions demonstrating the utility of geomorphic transport process mapping. This new mapping will address topical research problems with collaborating partners. Mapping strategies will employ remotely sensed image analysis, field control for characteristic map units, stratigraphic, paleontologic, geochronological, and geochemical studies. Maps will be released on scale-appropriate base materials such as high-resolution, lidar-derived topography.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologist Scott Minor searching for fossils on uplifted marine terrace on San Miguel Island, Channel Islands National Park, CA. Watershed Erosion Rates
Mapping the geomorphic processes, coupled with monitoring the erosion rates and modeling the sediment budget, locates and quantifies the sediment sources and sediment flux from a watershed. We can estimate the magnitude and recurrence interval of erosion-causing events. The resulting products enable community members and relevant stakeholders to make informed decisions about how to efficiently protect resources to maintain long-term viability.
Structure from Motion to estimate ground-deformation
Structure from Motion (SfM) from fixed wing or UAV platforms provides a cost-effective means to rapidly acquire imagery that can be transformed to digital topography using photogrammetry. The inherent high spatial and temporal resolution of coupled imagery and topography, as well as potential for time series data, allow for enhanced mapping of deposits and joining them to transport mechanisms (wind, rain, etc.). Target areas include constraining crustal deformation associated with tectonics and deep-seated landsliding. Such an approach is essential to responding to post-event natural disaster recovery mission as the UAV platform can be used to generate both imagery and topography for process mapping.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologists Elisabeth Haddon and Skye Corbett mounting camera to UAV for flight of Big Sur deep-seated landslides. Results
1. Quaternary Geologic Mapping of Channel Islands National Park (CHIS)
Tectonics
Located in the western Transverse Range (WTR) of California, Channel Islands National Park (CHIS) is part of the active broad San Andreas transform plate margin with dramatic Neogene and Quaternary transpressional faulting, folding, and clockwise vertical-axis rotations of crustal blocks. Geologically youthful manifestations of tectonism include regions of concentrated seismicity and recent to active crustal uplift, associated basinal subsidence, and local drainage capture. Significant seismic hazard exists, exemplified by the 2018 M 5.3 earthquake south of Santa Cruz Island that triggered coastal landslides.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologists Scott Minor and David Bedford pointing out Santa Rosa Island fault in the Channel Island National Park, CA Surface Water Availability
Recent repeat surveys of surface-water distribution conducted by NPS-CHIS scientists reveal spring and sink points that correlate with geologic contacts and faults juxtaposing rocks and deposits with contrasting hydrologic properties. Spatial correlations between independent geologic and hydrologic mapping provide the opportunity to evaluate causal mechanisms for surface water presence in the water-limited landscape and assist restoration efforts.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologist Scott Minor testing rock permeability along the Santa Rosa Island fault in the Channel Island National Park, CA. Surface water, a limited resource, is partially controlled by contrasting permeabilities of rock juxtaposed by faulting. Ecosystem Restoration
Disturbance caused by heavy grazing, introduction of non-native vegetation, and associated erosion complicates NPS land management. Grazing of native vegetation on steep slopes resulted in significantly increased erosion rates and, in some cases, complete stripping of hillslope soil. Presently, endemic vegetation is competing with non-natives, especially shrubs and grasses, or has been completely replaced by invasive species. The Channel Islands are unique in that the grazing ungulates have been removed and the landscape is now managed for conservation with concomitant restoration efforts.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Instrument array to monitor fog, rainfall, and soil moisture on Santa Rosa Island, Channel Islands National Park, CA. The study is evaluating the effectiveness of plants and fog to modulate soil moisture in the root zone to advise on ecosystem restoration strategies. Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologist Jonathan Perkins measuring soil infiltration in vegetation recovery area on Santa Rosa Island, Channel Islands National Park, CA Big Sur Coast Landslides
Faulting and associated uplift in the Santa Lucia Range of central California has generated steep, high-relief hillslopes with abundant active landslides suppling sediment to the adjacent national marine sanctuary in the Pacific Ocean and impacting California Hwy. 1. The 2017 Mud Creek landslide closed Hwy. 1 for 15 months with a present cost of $54 million to re-open the road. Hwy. 1, the only transportation artery along the coast has an average daily traffic count of ~ 4000. Closures have been common since its inauguration in 1937, with long-term deep-seated landslide-induced closures occurring in years of heavy rainfall. Structure from Motion (SfM) was used to estimate the timing of deformation and volume of the Mud Creek landslide.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologist Mark Reid monitoring landslide displacement along Big Sur Coast using campaign-style differential GPS measurements. Paul's slide shown here intermittently closes CA State Highway 1. Sources/Usage: Some content may have restrictions. Visit Media to see details.Aerial image of lateral margin of Big Sur landslide highlighted by recent asphalt patches in road. Note how asphalt patches align with vegetation break upslope of the road. Image obtained by UAV, truck for scale in hairpin curve. 2. Geomorphic Process Mapping, Monitoring and Modeling to Non-Point Source Erosion Impacting Coral Reef Health in the Hawaiian Islands
Coral reef ecosystems, and the fishing and tourism industries they support, depend on clean waters. Fine sediment pollution from nearshore watersheds threatens these economies across the Hawaiian Islands. The terrestrial sediment sources are largely unknown and vary by location due to geology and land-use history. To effectively mitigate sediment pollution, it is critical to know where the sediment is coming from, how fast it erodes, and when it moves. These questions are either unanswered or unquantified, and relevant to stakeholders trying to mitigate the problem. USGS, in collaboration with federal and local partners, is working in watersheds across the Hawaiian Islands to: 1) map geomorphic processes generating fine sediment, 2) monitor erosion rates, 3) determine thresholds for sediment mobilization, and 4) determine the likely frequency of triggering events. The products delivered provide data stakeholders use to make informed mitigation decisions.
Sources/Usage: Some content may have restrictions. Visit Media to see details.Research Geologists Corina Cerovski-Darriau and Jonathan Stock measure how, when, and where erosion occurs in Pelekane to understand the sources of fine sediment polluting the coastal waters of West Hawai'i Sources/Usage: Some content may have restrictions. Visit Media to see details.USGS Research Geologist Jonathan Stock and student contractor Madison Douglas install an anemometer to measure wind conditions at one of hte monitoring sites in Pelekane. 3. Evaluating the record of earthquake-triggered terrestrial Quaternary landslides
The Pacific Northwest and Coastal California face a myriad of landslide hazards ranging from subduction zone megathrust earthquakes in the north, shallow crustal earthquakes along the central and southern California coast, and heavy precipitation in the form of atmospheric river events across much of the region. However, our understanding of the terrestrial landscape response to these events is lacking. In collaboration with academic colleagues, personnel are convening a series of workshops through USGS Powell Center to integrating geological and geophysical datasets to understand subduction zone earthquake recurrence and hazards.
- Data
Below are data or web applications associated with this project.
Field measurements of rainfall and soil moisture data used to support understanding of infiltration and runoff following the 2007 Canyon Fire, Malibu, CA, USA
This data release includes information used to support interpretations of relations between precipitation and soil moisture for a U.S. Geological Survey post-fire monitoring array installed near Malibu, CA following the 2007 Canyon fire. The 3 datasets are: 1) a time series of precipitation from three tipping bucket rain gages in individual files (Schmidt_2020_CANVQRG1.csv, Schmidt_2020_CANVQRG2.cSr concentrations and 87Sr/86Sr data used to determine the Sr-chronostratigraphic age of sirenian fossils on Santa Rosa Island, Channel Islands National Park, California, USA
This data release includes a table of Sr concentrations and 87Sr/86Sr data used to evaluate primary seawater isotope compositions of marine invertebrate shell material used to estimate the Sr-chronostratigraphic age of sediments hosting early Miocene sirenian fossils on Santa Rosa Island of the Channel Island National Park, Ventura County, CaliforniaField-saturated hydraulic conductivity time series and sediment accumulations following the 2017 Nuns and Tubbs wildfires, Napa and Sonoma Counties, CA, USA
This dataset comprises repeat surveys of field-saturated hydraulic conductivity and sorptivity following the October 2017 Nuns and Tubbs wildfires as part of an effort to document soil-hydraulic recovery. A summary table includes associated physiographic properties for each site, including: pre-burn vegetation, lithology, soil burn severity, location, soil texture, and associated van Genuchten parRoot thread strength, landslide headscarp geometry, and observed root characteristics at the monitored CB1 landslide, Oregon, USA
This data release supports interpretations of field-observed root distributions within a shallow landslide headscarp (CB1) located below Mettman Ridge within the Oregon Coast Range, approximately 15 km northeast of Coos Bay, Oregon, USA. (Schmidt_2021_CB1_topo_far.png and Schmidt_2021_CB1_topo_close.png). Root species, diameter (greater than or equal to 1 mm), general orientation relative to the sField, geotechnical, and meteorological data of the 22 March 2018 narrow cold frontal rainband (NCFR) and its effects, Tuolumne River canyon, Sierra Nevada Foothills, California
This data release includes information used to support the manuscript "Linking mesoscale meteorology with extreme landscape response: effects of narrow cold frontal rainbands (NCFR)". The included datasets and supplement include information related to the 22 March 2018 NCFR and associated shallow landslides in the Toulumne Canyon triggered by this event. The three datasets and one supplemental infField observations of ground failure triggered by the 2020 Puerto Rico earthquake sequence
This dataset consists of over 800 field observations of ground failure (landslides, lateral spreading, and liquefaction) and other damage triggered by the 2019-2020 Puerto Rico earthquake sequence. The sequence started with a M4.7 earthquake on 28 December 2019, followed by many more earthquakes, including 15 larger than M5 (as of 7 July 2020). The M6.4 mainshock, which is thought to have triggere - Publications
Below are publications associated with this project.
Hunting for landslides from Cascadia's great earthquakes
No abstract available.AuthorsJonathan P. Perkins, Joshua J. Roering, William J. Burns, William Strubel, Bryan A. Black, Kevin Schmidt, Alison Duvall, Nancy C. CalhounFilter Total Items: 23Inversions of landslide strength as a proxy for subsurface weathering
Distributions of landslide size are hypothesized to reflect hillslope strength, and consequently weathering patterns. However, the association of weathering and critical zone architecture with mechanical strength properties of parent rock and soil are poorly-constrained. Here we use three-dimensional stability to analyze 7330 landslides in western Oregon to infer combinations of strength - frictioAuthorsStefano Alberti, Ben Leshchinksy, Joshua J. Roering, Jonathan P. Perkins, Michael OlsenFrom data to interpretable models: Machine learning for soil moisture forecasting
Soil moisture is critical to agricultural business, ecosystem health, and certain hydrologically driven natural disasters. Monitoring data, though, is prone to instrumental noise, wide ranging extrema, and nonstationary response to rainfall where ground conditions change. Furthermore, existing soil moisture models generally forecast poorly for time periods greater than a few hours. To improve suchAuthorsAniruddha Basak, Kevin M. Schmidt, Ole MengshoelComparing root cohesion estimates from three models at a shallow landslide in the Oregon Coast Range
Although accurate root cohesion model estimates are essential to quantify the effect of vegetation roots on shallow slope stability, few means exist to independently validate such model outputs. One validation approach for cohesion estimates is back-calculation of apparent root cohesion at a landslide site with well-documented failure conditions. The catchment named CB1, near Coos Bay, Oregon, USAAuthorsCollin Cronkite-Ratcliff, Kevin M. Schmidt, Charlotte WirionMulti-stage soil-hydraulic recovery and limited ravel accumulations following the 2017 Nuns and Tubbs wildfires in Northern California
Wildfire can impact soil-hydraulic properties by reducing saturated hydraulic conductivity and sorptivity, making recently burned landscapes prone to debris flows and flash floods. The post-fire hazard window can range from years to decades. In Northern California, where wildfire frequency is steadily increasing, the impact and soil-hydraulic recovery from wildfires is unknown. Following the OctobAuthorsJonathan P. Perkins, Carlos Diaz, Skye C. Corbett, Corina Cerovski-Darriau, Jonathan D. Stock, Jeffrey Paul Prancevic, Lisa Micheli, Jay JasperseDeveloping landslide chronologies using landslide-dammed lakes in the Oregon Coast Range
The Oregon Coast Range is a dynamic landscape that is continually shaped by shallow and deep-seated landslides that can have disastrous consequences to infrastructure and human lives. Searching for evidence of potentially coseismic mass wasting is incredibly difficult, particularly when historical observations are limited. Landslide-dammed lakes with submerged “ghost forests” in the Oregon Coast RAuthorsLogan Wetherell, William Struble, Sean Richard LaHusenWhen hazard avoidance is not an option: Lessons learned from monitoring the postdisaster Oso landslide, USA
On 22 March 2014, a massive, catastrophic landslide occurred near Oso, Washington, USA, sweeping more than 1 km across the adjacent valley flats and killing 43 people. For the following 5 weeks, hundreds of workers engaged in an exhaustive search, rescue, and recovery effort directly in the landslide runout path. These workers could not avoid the risks posed by additional large-scale slope collapsAuthorsMark E. Reid, Jonathan W. Godt, Richard G LaHusen, Stephen L Slaughter, Thomas C. Badger, Brian D. Collins, William Schulz, Rex L. Baum, Jeffrey A. Coe, Edwin L Harp, Kevin M. Schmidt, Richard M. Iverson, Joel B. Smith, Ralph Haugerud, David L. GeorgeSediment budget for watersheds of West Maui, Hawaii
Episodic runoff brings suspended sediment to West Maui’s nearshore waters, turning them from blue to brown. This pollution degrades the ecological, cultural, and recreational value of these iconic nearshore waters. We used mapping, monitoring, and modeling to identify and quantify the watershed sources for fine sediment that pollutes the nearshore each year. These results focus strategies to reducAuthorsJonathan D. Stock, Corina Cerovski-DarriauUnsaturated flow processes and the onset of seasonal deformation in slow-moving landslides
Predicting rainfall-induced landslide motion is challenging because shallow groundwater flow is extremely sensitive to the preexisting moisture content in the ground. Here, we use groundwater hydrology theory and numerical modeling combined with five years of field monitoring to illustrate how unsaturated groundwater flow processes modulate the seasonal pore water pressure rise and therefore the oAuthorsNoah J. Finnegan, Jonathan P. Perkins, Alexander Lewis Nereson, Alexander L. HandwergerRenewing the National Cooperative Geologic Mapping Program as the Nation’s authoritative source for modern geologic knowledge
This document presents the renewed vision, mission, and goals for the National Cooperative Geologic Mapping Program (NCGMP). The NCGMP, as authorized by the National Cooperative Geologic Mapping Act of 1992 (Public Law 102-285, 106 Stat. 166 and its reauthorizations), is tasked with expediting the production of a geologic database for the Nation based on modern geologic maps and their supporting dAuthorsJohn Brock, Karen Berry, James Faulds, Richard Berg, Kyle House, Michael Marketti, Darcy McPhee, Kevin M. Schmidt, James Schmitt, David Soller, David Spears, Ren A. Thompson, Harvey Thorleifson, Gregory J. WalshToward an integrative geological and geophysical view of Cascadia subduction zone earthquakes
The Cascadia subduction zone (CSZ) is an exceptional geologic environment for recording evidence of land level changes, tsunamis, and ground motion that reveals at least 19 great megathrust earthquakes over the past 10 kyr. Such earthquakes are among the most impactful natural hazards on Earth, transcend national boundaries, and can have global impact. Reducing the societal impacts of future eventAuthorsMaureen A. L. Walton, Lydia M. Staisch, Tina Dura, Jessie Kathleen Pearl, Brian L. Sherrod, Joan S. Gomberg, Simon E. Engelhart, Anne Trehu, Janet Watt, Jonathan P. Perkins, Robert C. Witter, Noel Bartlow, Chris Goldfinger, Harvey Kelsey, Ann Morey, Valerie J. Sahakian, Harold Tobin, Kelin Wang, Ray Wells, Erin WirthLinking mesoscale meteorology with extreme landscape response: Effects of narrow cold frontal rainbands (NCFR)
Landscapes evolve in response to prolonged and/or intense precipitation resulting from atmospheric processes at various spatial and temporal scales. Whereas synoptic (large‐scale) features (e.g., atmospheric rivers and hurricanes) govern regional‐scale hydrologic hazards such as widespread flooding, mesoscale features such as thunderstorms or squall lines are more likely to trigger localized geomoAuthorsBrian D. Collins, N. S. Oakley, Jonathan P. Perkins, Amy E. East, Skye C. Corbett, Benjamin J. HatchettRainfall triggers more deep-seated landslides than Cascadia earthquakes in the Oregon Coast Range, USA
The coastal Pacific Northwest USA hosts thousands of deep-seated landslides. Historic landslides have primarily been triggered by rainfall, but the region is also prone to large earthquakes on the 1100-km-long Cascadia Subduction Zone megathrust. Little is known about the number of landslides triggered by these earthquakes because the last magnitude 9 rupture occurred in 1700 CE. Here, we map 9938AuthorsSean R LaHusen, Alison R Duvall, Adam M. Booth, Alex R. R. Grant, Benjamin A Mishkin, David R. Montgomery, William Struble, Joshua J. Roering, Joseph Wartman