Dennis M Staley
Current research focuses on landslide hazards in Alaska, specifically on tsunamigenic landslides in Prince William Sound. Past research includes post-wildfire debris flow hazards in the western United States, the geomorphology of alluvial and debris-flow fans and talus deposits in arid and alpine environments, and the assessment of aquatic, riparian and wetland ecosystem health and function.
I am a Research Physical Scientist in the Alaska Volcano Observatory in Anchorage, Alaska, where I currently lead a project related to landslide hazards in Prince William Sound. This project is currently aimed at improving our understanding of the tsunamigenic potential and corresponding risk associated with large rock slope failures in recently deglaciated fiords.
Prior to moving to Alaska in the fall of 2021, I worked at the Geologic Hazards Science Center in Golden, Colorado, where I studied post-fire debris flows. This research focused on advancing our understanding of the topographic, geologic, hydrologic, and meteorological conditions that influence the location, timing, and magnitude of post-fire debris flows for the purpose of improving hazard assessment and early warning.
Before starting my career at the U.S. Geological Survey, I was a Physical Scientist at the U.S. Forest Service in Golden, Colorado, where I focused on developing protocols for assessing the health and function of aquatic, riparian, and wetland ecosystems of the Rocky Mountains.
Professional Experience
2007 - Present: Research Physical Scientist, U.S. Geological Survey, Golden CO and Anchorage AK
2001 - 2007: Physical Scientist, U.S. Forest Service, Golden CO
Education and Certifications
Ph.D. in Earth Sciences, University of Memphis, Memphis TN, 2006.
MSc. in Geography, University of Memphis, Memphis TN, 2000.
BA in Geography, State University of New York - College at Geneseo, Geneseo NY, 1998.
Affiliations and Memberships*
Fellow, Geological Society of America (2020)
E.B. Burwell Jr. Award, Geological Society of America Environmental and Engineering Geology Division (2019)
Honor Award for Superior Service, U.S. Department of Interior (2016)
Meritorious Service Award, Environmental and Engineering Geology Division of the Geological Society of America (2015)
Best Paper Award in Landslides, International Landslide Consortium (2013)
Science and Products
Filter Total Items: 58
Topographic change detection at Chalk Cliffs, Colorado, USA, using Airborne LiDAR and UAS-based Structure-from-Motion photogrammetry Topographic change detection at Chalk Cliffs, Colorado, USA, using Airborne LiDAR and UAS-based Structure-from-Motion photogrammetry
The Chalk Cliffs debris-flow site is a small headwater catchment incised into highly fractured and hydrothermally altered quartz monzonite in a semi-arid climate. Over half of the extremely steep basin is exposed bedrock. Debris flows occur multiple times per year in response to rainstorm events, typically during the summer monsoon season. The frequency of debris flows, and the...
Authors
Katherine R Barnhart, Francis K. Rengers, Ghent Jessica N, Gregory E. Tucker, Jeffrey A. Coe, Jason W. Kean, Joel B. Smith, Dennis M. Staley, William Kleiber, Ashton M Wiens
Post-fire rockfall and debris-flow hazard zonation in the Eagle Creek Fire burn area, Columbia River Gorge, Oregon: a tool for emergency managers and first responders Post-fire rockfall and debris-flow hazard zonation in the Eagle Creek Fire burn area, Columbia River Gorge, Oregon: a tool for emergency managers and first responders
The Eagle Creek Fire engulfed 48,832 acres (196 km2) within the Columbia River Gorge, Oregon beginning September 2nd and was 100% contained by November 30th, 2017. The Columbia River Gorge area is steep and heavily forested characterized by cliffs and flanking talus slopes, receiving > 100 inches (> 254 cm) of precipitation annually. The Columbia River Gorge is a critical lifeline for...
Authors
Nancy C. Calhoun, William J. Burns, S.H. Hayduk, Dennis M. Staley, Jason W. Kean
Inundation, flow dynamics, and damage in the 9 January 2018 Montecito Debris-Flow Event, California, USA: Opportunities and challenges for post-wildfire risk assessment Inundation, flow dynamics, and damage in the 9 January 2018 Montecito Debris-Flow Event, California, USA: Opportunities and challenges for post-wildfire risk assessment
Shortly before the beginning of the winter rainy season, one of the largest fires in California history (Thomas Fire) substantially increased the susceptibility of steep slopes in Santa Barbara and Ventura Counties to debris flows. On January 9, 2018, before the fire was fully contained, an intense burst of rain fell on the portion of the burn area above Montecito, CA. The rainfall and...
Authors
Jason W. Kean, Dennis M. Staley, Jeremy T. Lancaster, Francis K. Rengers, Brian J. Swanson, Jeffrey A. Coe, Janis Hernandez, Aaron Sigman, Kate E. Allstadt, Donald N. Lindsay
Estimating post-fire debris-flow hazards prior to wildfire using a statistical analysis of historical distributions of fire severity from remote sensing data Estimating post-fire debris-flow hazards prior to wildfire using a statistical analysis of historical distributions of fire severity from remote sensing data
Following wildfire, mountainous areas of the western United States are susceptible to debris flow during intense rainfall. Convective storms that can generate debris flows in recently burned areas may occur during or immediately after the wildfire, leaving insufficient time for development and implementation of risk mitigation strategies. We present a method for estimating post-fire...
Authors
Dennis M. Staley, Anne C. Tillery, Jason W. Kean, Luke McGuire, Hannah Pauling, Francis K. Rengers, Joel B. Smith
Incorporating spatially heterogeneous infiltration capacity into hydrologic models with applications for simulating post‐wildfire debris flow initiation Incorporating spatially heterogeneous infiltration capacity into hydrologic models with applications for simulating post‐wildfire debris flow initiation
Soils in post‐wildfire environments are often characterized by a low infiltration capacity with a high degree of spatial heterogeneity relative to unburned areas. Debris flows are frequently initiated by run‐off in recently burned steeplands, making it critical to develop and test methods for incorporating spatial variability in infiltration capacity into hydrologic models. We use Monte...
Authors
Luke A. McGuire, Francis K. Rengers, Jason W. Kean, Dennis M. Staley, Benjamin B. Mirus
The science and prediction of post-fire debris flows in the western United States The science and prediction of post-fire debris flows in the western United States
No abstract available.
Authors
Dennis M. Staley, Jason W. Kean
Debris flow initiation by runoff in a recently burned basin: Is grain-by-grain sediment bulking or en masse failure to blame? Debris flow initiation by runoff in a recently burned basin: Is grain-by-grain sediment bulking or en masse failure to blame?
Postwildfire debris flows are frequently triggered by runoff following high-intensity rainfall, but the physical mechanisms by which water-dominated flows transition to debris flows are poorly understood relative to debris flow initiation from shallow landslides. In this study, we combined a numerical model with high-resolution hydrologic and geomorphic data sets to test two different...
Authors
Luke McGuire, Francis K. Rengers, Jason W. Kean, Dennis M. Staley
Prediction of spatially explicit rainfall intensity–duration thresholds for post-fire debris-flow generation in the western United States Prediction of spatially explicit rainfall intensity–duration thresholds for post-fire debris-flow generation in the western United States
Early warning of post-fire debris-flow occurrence during intense rainfall has traditionally relied upon a library of regionally specific empirical rainfall intensity–duration thresholds. Development of this library and the calculation of rainfall intensity-duration thresholds often require several years of monitoring local rainfall and hydrologic response to rainstorms, a time-consuming...
Authors
Dennis M. Staley, Jacquelyn Negri, Jason W. Kean, Jayme L. Laber, Anne C. Tillery, Ann M. Youberg
Post-fire debris flows in southern California: Science, prediction, and implications for practitioners Post-fire debris flows in southern California: Science, prediction, and implications for practitioners
No abstract available.
Authors
Dennis M. Staley, Jason W. Kean
Constraining the relative importance of raindrop- and flow-driven sediment transport mechanisms in postwildfire environments and implications for recovery time scales Constraining the relative importance of raindrop- and flow-driven sediment transport mechanisms in postwildfire environments and implications for recovery time scales
Mountain watersheds recently burned by wildfire often experience greater amounts of runoff and increased rates of sediment transport relative to similar unburned areas. Given the sedimentation and debris flow threats caused by increases in erosion, more work is needed to better understand the physical mechanisms responsible for the observed increase in sediment transport in burned...
Authors
Luke McGuire, Jason W. Kean, Dennis M. Staley, Francis K. Rengers, Thad A. Wasklewicz
Model simulations of flood and debris flow timing in steep catchments after wildfire Model simulations of flood and debris flow timing in steep catchments after wildfire
Debris flows are a typical hazard on steep slopes after wildfire, but unlike debris flows that mobilize from landslides, most post-wildfire debris flows are generated from water runoff. The majority of existing debris-flow modeling has focused on landslide-triggered debris flows. In this study we explore the potential for using process-based rainfall-runoff models to simulate the timing...
Authors
Francis K. Rengers, Luke McGuire, Jason W. Kean, Dennis M. Staley, D.E.J Hobley
The influence of vegetation cover on debris-flow density during an extreme rainfall in the northern Colorado Front Range The influence of vegetation cover on debris-flow density during an extreme rainfall in the northern Colorado Front Range
We explored regional influences on debris-flow initiation throughout the Colorado Front Range (Colorado, USA) by exploiting a unique data set of more than 1100 debris flows that initiated during a 5 day rainstorm in 2013. Using geospatial data, we examined the influence of rain, hillslope angle, hillslope aspect, and vegetation density on debris-flow initiation. In particular we used a...
Authors
Francis K. Rengers, Luke McGuire, Jeffrey A. Coe, Jason W. Kean, Rex L. Baum, Dennis M. Staley, Jonathan W. Godt
Filter Total Items: 17
No Result Found
Science and Products
Filter Total Items: 58
Topographic change detection at Chalk Cliffs, Colorado, USA, using Airborne LiDAR and UAS-based Structure-from-Motion photogrammetry Topographic change detection at Chalk Cliffs, Colorado, USA, using Airborne LiDAR and UAS-based Structure-from-Motion photogrammetry
The Chalk Cliffs debris-flow site is a small headwater catchment incised into highly fractured and hydrothermally altered quartz monzonite in a semi-arid climate. Over half of the extremely steep basin is exposed bedrock. Debris flows occur multiple times per year in response to rainstorm events, typically during the summer monsoon season. The frequency of debris flows, and the...
Authors
Katherine R Barnhart, Francis K. Rengers, Ghent Jessica N, Gregory E. Tucker, Jeffrey A. Coe, Jason W. Kean, Joel B. Smith, Dennis M. Staley, William Kleiber, Ashton M Wiens
Post-fire rockfall and debris-flow hazard zonation in the Eagle Creek Fire burn area, Columbia River Gorge, Oregon: a tool for emergency managers and first responders Post-fire rockfall and debris-flow hazard zonation in the Eagle Creek Fire burn area, Columbia River Gorge, Oregon: a tool for emergency managers and first responders
The Eagle Creek Fire engulfed 48,832 acres (196 km2) within the Columbia River Gorge, Oregon beginning September 2nd and was 100% contained by November 30th, 2017. The Columbia River Gorge area is steep and heavily forested characterized by cliffs and flanking talus slopes, receiving > 100 inches (> 254 cm) of precipitation annually. The Columbia River Gorge is a critical lifeline for...
Authors
Nancy C. Calhoun, William J. Burns, S.H. Hayduk, Dennis M. Staley, Jason W. Kean
Inundation, flow dynamics, and damage in the 9 January 2018 Montecito Debris-Flow Event, California, USA: Opportunities and challenges for post-wildfire risk assessment Inundation, flow dynamics, and damage in the 9 January 2018 Montecito Debris-Flow Event, California, USA: Opportunities and challenges for post-wildfire risk assessment
Shortly before the beginning of the winter rainy season, one of the largest fires in California history (Thomas Fire) substantially increased the susceptibility of steep slopes in Santa Barbara and Ventura Counties to debris flows. On January 9, 2018, before the fire was fully contained, an intense burst of rain fell on the portion of the burn area above Montecito, CA. The rainfall and...
Authors
Jason W. Kean, Dennis M. Staley, Jeremy T. Lancaster, Francis K. Rengers, Brian J. Swanson, Jeffrey A. Coe, Janis Hernandez, Aaron Sigman, Kate E. Allstadt, Donald N. Lindsay
Estimating post-fire debris-flow hazards prior to wildfire using a statistical analysis of historical distributions of fire severity from remote sensing data Estimating post-fire debris-flow hazards prior to wildfire using a statistical analysis of historical distributions of fire severity from remote sensing data
Following wildfire, mountainous areas of the western United States are susceptible to debris flow during intense rainfall. Convective storms that can generate debris flows in recently burned areas may occur during or immediately after the wildfire, leaving insufficient time for development and implementation of risk mitigation strategies. We present a method for estimating post-fire...
Authors
Dennis M. Staley, Anne C. Tillery, Jason W. Kean, Luke McGuire, Hannah Pauling, Francis K. Rengers, Joel B. Smith
Incorporating spatially heterogeneous infiltration capacity into hydrologic models with applications for simulating post‐wildfire debris flow initiation Incorporating spatially heterogeneous infiltration capacity into hydrologic models with applications for simulating post‐wildfire debris flow initiation
Soils in post‐wildfire environments are often characterized by a low infiltration capacity with a high degree of spatial heterogeneity relative to unburned areas. Debris flows are frequently initiated by run‐off in recently burned steeplands, making it critical to develop and test methods for incorporating spatial variability in infiltration capacity into hydrologic models. We use Monte...
Authors
Luke A. McGuire, Francis K. Rengers, Jason W. Kean, Dennis M. Staley, Benjamin B. Mirus
The science and prediction of post-fire debris flows in the western United States The science and prediction of post-fire debris flows in the western United States
No abstract available.
Authors
Dennis M. Staley, Jason W. Kean
Debris flow initiation by runoff in a recently burned basin: Is grain-by-grain sediment bulking or en masse failure to blame? Debris flow initiation by runoff in a recently burned basin: Is grain-by-grain sediment bulking or en masse failure to blame?
Postwildfire debris flows are frequently triggered by runoff following high-intensity rainfall, but the physical mechanisms by which water-dominated flows transition to debris flows are poorly understood relative to debris flow initiation from shallow landslides. In this study, we combined a numerical model with high-resolution hydrologic and geomorphic data sets to test two different...
Authors
Luke McGuire, Francis K. Rengers, Jason W. Kean, Dennis M. Staley
Prediction of spatially explicit rainfall intensity–duration thresholds for post-fire debris-flow generation in the western United States Prediction of spatially explicit rainfall intensity–duration thresholds for post-fire debris-flow generation in the western United States
Early warning of post-fire debris-flow occurrence during intense rainfall has traditionally relied upon a library of regionally specific empirical rainfall intensity–duration thresholds. Development of this library and the calculation of rainfall intensity-duration thresholds often require several years of monitoring local rainfall and hydrologic response to rainstorms, a time-consuming...
Authors
Dennis M. Staley, Jacquelyn Negri, Jason W. Kean, Jayme L. Laber, Anne C. Tillery, Ann M. Youberg
Post-fire debris flows in southern California: Science, prediction, and implications for practitioners Post-fire debris flows in southern California: Science, prediction, and implications for practitioners
No abstract available.
Authors
Dennis M. Staley, Jason W. Kean
Constraining the relative importance of raindrop- and flow-driven sediment transport mechanisms in postwildfire environments and implications for recovery time scales Constraining the relative importance of raindrop- and flow-driven sediment transport mechanisms in postwildfire environments and implications for recovery time scales
Mountain watersheds recently burned by wildfire often experience greater amounts of runoff and increased rates of sediment transport relative to similar unburned areas. Given the sedimentation and debris flow threats caused by increases in erosion, more work is needed to better understand the physical mechanisms responsible for the observed increase in sediment transport in burned...
Authors
Luke McGuire, Jason W. Kean, Dennis M. Staley, Francis K. Rengers, Thad A. Wasklewicz
Model simulations of flood and debris flow timing in steep catchments after wildfire Model simulations of flood and debris flow timing in steep catchments after wildfire
Debris flows are a typical hazard on steep slopes after wildfire, but unlike debris flows that mobilize from landslides, most post-wildfire debris flows are generated from water runoff. The majority of existing debris-flow modeling has focused on landslide-triggered debris flows. In this study we explore the potential for using process-based rainfall-runoff models to simulate the timing...
Authors
Francis K. Rengers, Luke McGuire, Jason W. Kean, Dennis M. Staley, D.E.J Hobley
The influence of vegetation cover on debris-flow density during an extreme rainfall in the northern Colorado Front Range The influence of vegetation cover on debris-flow density during an extreme rainfall in the northern Colorado Front Range
We explored regional influences on debris-flow initiation throughout the Colorado Front Range (Colorado, USA) by exploiting a unique data set of more than 1100 debris flows that initiated during a 5 day rainstorm in 2013. Using geospatial data, we examined the influence of rain, hillslope angle, hillslope aspect, and vegetation density on debris-flow initiation. In particular we used a...
Authors
Francis K. Rengers, Luke McGuire, Jeffrey A. Coe, Jason W. Kean, Rex L. Baum, Dennis M. Staley, Jonathan W. Godt
Filter Total Items: 17
No Result Found
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government