Debris flow deposit at the outlet of the Tumalt Creek drainage basin, Columbia River Gorge, Oregon, following storms in January 2021.
2024 Elk Fire
Bighorn National Forest, Wyoming
2021 Muckamuck Fire burn area
Okanogan County, Washington
2020 Cameron Peak Fire burn area
Roosevelt National Forest, Colorado
2020 Dolan Fire
Los Padres National Forest, California
Wildfires can dramatically alter how water moves across the landscape. After a fire, vegetation is removed and soil properties change, reducing the ground’s ability to absorb rainfall. As a result, even modest rainstorms can trigger dangerous flash floods and debris flows in steep burned areas.
Postfire debris flows are fast-moving mixtures of water, mud, rocks, and vegetation that can surge downslope like flowing concrete. These flows often move faster than a person can run and may travel far beyond the burned area, posing risks to people, homes, roads, and infrastructure. They are typically triggered by short bursts of intense rainfall and can occur during the first storm following a wildfire.
This project develops rapid methods to evaluate postfire debris-flow hazards and advances research on the processes that control their initiation and growth. The goal is to provide reliable scientific information that helps federal, state, and local agencies reduce risks and improve preparedness in recently burned landscapes.
A postfire debris flow in the area burned by the 2016 Fish Fire, Los Angeles county, California. The flow was triggered by heavy rainfall on January 20, 2017.
USGS Postfire Debris-Flow Hazard Assessments
The USGS conducts postfire debris-flow hazard assessments for select fires in the Western U.S. These assessments use information about watershed properties, rainfall characteristics, and soil properties to answer a few key questions:
What burned watersheds are most susceptible to debris flows?
During what types of rainstorms are debris flows likely to be triggered?
How much mud and other debris are these flows capable of carrying?
Click the image below to access the postfire debris-flow hazard assessment dashboard. You can use the dashboard to view or download the data for all recent postfire hazard assessments conducted by the USGS.
More information about hazard assessments
Frequently asked questions
Scientific Background
GIS Services
Request an assessment
Learn more about postfire debris flows
RECOVERY
How long does the hazard last?
As the burn area recovers and the landscape returns to prefire conditions the level of debris-flow hazard decreases. Understanding this recovery process and how debris-flow hazards change in the years following the fire is an active area of research at the USGS.
Use the link below to learn more about fire recovery and postfire debris flows.
RUNOUT
How far can flows travel?
Understanding how far debris flows can travel and what the impacts may be is one of the most important questions we face to effectively protect life and property from debris-flow hazards.
Use the link below to learn more about debris-flow runout research at the USGS.
MONITORING
How well do our hazard models work?
Monitoring stations are installed in select burn areas to better understand the processes that control postfire debris-flow initiation and growth.
Use the link below to learn more about postfire watershed monitoring at the USGS.
Below is a list of science sites associated with this project.
Scientific Background
Rainfall, Volumetric soil-water content, Video, and Geophone Data from the Calwood Fire Burn Area, Colorado, April 2021 to November 2023 Rainfall, Volumetric soil-water content, Video, and Geophone Data from the Calwood Fire Burn Area, Colorado, April 2021 to November 2023
Rainfall, Video, and Geophone Data from the Hermit's Peak/ Calf Canyon Fire Burn Area, New Mexico, June 2022 to June 2024 Rainfall, Video, and Geophone Data from the Hermit's Peak/ Calf Canyon Fire Burn Area, New Mexico, June 2022 to June 2024
Inventory of debris flows in burned (2020-2022) and unburned (1995-2020) areas in the western Cascade Range of Oregon Inventory of debris flows in burned (2020-2022) and unburned (1995-2020) areas in the western Cascade Range of Oregon
Postfire erosion estimates for large California wildfires that occurred between 1984 and 2021 Postfire erosion estimates for large California wildfires that occurred between 1984 and 2021
Compilation of runoff-generated debris-flow inventories for 18 fires across Arizona, California, Colorado, New Mexico, Utah, and Washington, USA Compilation of runoff-generated debris-flow inventories for 18 fires across Arizona, California, Colorado, New Mexico, Utah, and Washington, USA
Postfire Debris-Flow Database (Literature Derived) Postfire Debris-Flow Database (Literature Derived)
Postfire Debris Flow Science Infographic
Post-wildfire debris flow: 2016 Fish Fire, Las Lomas Canyon
The June 2016 Fish Fire burned over 12 km^2 in Los Angeles County, California. After the fire, the USGS installed an automated rain-triggered camera to monitor post-wildfire flooding and debris flow in a small canyon above the Las Lomas debris basin in Duarte. This video shows the peak flow triggered by an intense rainstorm on January 20, 2017.
Debris flow deposit at the outlet of the Tumalt Creek drainage basin, Columbia River Gorge, Oregon, following storms in January 2021.
Home damaged by post-wildfire debris flow in Montecito, CA.
Home damaged by post-wildfire debris flow in Montecito, CA.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
Home damaged by post-wildfire debris flow in Montecito, CA.
Home damaged by post-wildfire debris flow in Montecito, CA.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
Damage from a major post-wildfire landslide that occurred on 25 December 2003 near Devore, San Bernardino County as a result of the Old/Grand Prix fires that ran through the San Bernardino Mountains.
Damage from a major post-wildfire landslide that occurred on 25 December 2003 near Devore, San Bernardino County as a result of the Old/Grand Prix fires that ran through the San Bernardino Mountains.
Montecito home damaged by post-wildfire debrisflow.
Montecito home damaged by post-wildfire debrisflow.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
Montecito home damaged by post-wildfire debrisflow.
Montecito home damaged by post-wildfire debrisflow.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
The Dec. 4, 2017 Thomas fire, Southern California's largest wildfire on record, burned more than 280,000 acres across Ventura and Santa Barbara counties for nearly a month.
The Dec. 4, 2017 Thomas fire, Southern California's largest wildfire on record, burned more than 280,000 acres across Ventura and Santa Barbara counties for nearly a month.
Geologists assess boulders displaced during the Montecito debris flow event on Jan. 9, 2018.
Geologists assess boulders displaced during the Montecito debris flow event on Jan. 9, 2018.
USGS geologists deployed to Santa Barbara County to support a geohazard assessment of the Montecito area
USGS geologists deployed to Santa Barbara County to support a geohazard assessment of the Montecito area
Post-wildfire Flood and Debris Flow: 2014 Silverado Fire
Post-wildfire Flood and Debris Flow: 2014 Silverado FireIn 2014, the Silverado Fire burned approximately 4 km^2 in Orange County, California. After the fire, the USGS installed an automated rain-triggered camera to monitor post-wildfire flooding and debris flow at the outlet of a small 0.6 km^2 basin within the burn area.
Post-wildfire Flood and Debris Flow: 2014 Silverado Fire
Post-wildfire Flood and Debris Flow: 2014 Silverado FireIn 2014, the Silverado Fire burned approximately 4 km^2 in Orange County, California. After the fire, the USGS installed an automated rain-triggered camera to monitor post-wildfire flooding and debris flow at the outlet of a small 0.6 km^2 basin within the burn area.
House engulfed by debris flows generated in response to a rainstorm on February 6, 2010. This house was west of Briar Wood Canyon in southern California. The small, but steep and rugged drainage basin above this home was burned the previous summer by the Station Fire, the largest fire in the history of Los Angeles County.
House engulfed by debris flows generated in response to a rainstorm on February 6, 2010. This house was west of Briar Wood Canyon in southern California. The small, but steep and rugged drainage basin above this home was burned the previous summer by the Station Fire, the largest fire in the history of Los Angeles County.
Debris Flow in Cable Canyon following the 2003 Old Fire in the San Bernardino Mountains, California.
Debris Flow in Cable Canyon following the 2003 Old Fire in the San Bernardino Mountains, California.
Evaluation of debris-flow building damage forecasts Evaluation of debris-flow building damage forecasts
Post-wildfire debris flows Post-wildfire debris flows
How long do runoff-generated debris-flow hazards persist after wildfire? How long do runoff-generated debris-flow hazards persist after wildfire?
Forecasting the inundation of postfire debris flows Forecasting the inundation of postfire debris flows
Runout model evaluation based on back-calculation of building damage Runout model evaluation based on back-calculation of building damage
Postfire hydrologic response along the central California (USA) coast: Insights for the emergency assessment of postfire debris-flow hazards Postfire hydrologic response along the central California (USA) coast: Insights for the emergency assessment of postfire debris-flow hazards
View the geonarratives (Esri Storymap) below to learn more about recent post-fire debris flow events.
Cameron Peak Fire
Columbia River Gorge Landslides
pfdf 2.0.0 pfdf 2.0.0
pfdf 1.1.0 pfdf 1.1.0
pfdf 1.0.0 pfdf 1.0.0
digger: A python package for D-Claw model inputs digger: A python package for D-Claw model inputs
Wildfires can dramatically alter how water moves across the landscape. After a fire, vegetation is removed and soil properties change, reducing the ground’s ability to absorb rainfall. As a result, even modest rainstorms can trigger dangerous flash floods and debris flows in steep burned areas.
Postfire debris flows are fast-moving mixtures of water, mud, rocks, and vegetation that can surge downslope like flowing concrete. These flows often move faster than a person can run and may travel far beyond the burned area, posing risks to people, homes, roads, and infrastructure. They are typically triggered by short bursts of intense rainfall and can occur during the first storm following a wildfire.
This project develops rapid methods to evaluate postfire debris-flow hazards and advances research on the processes that control their initiation and growth. The goal is to provide reliable scientific information that helps federal, state, and local agencies reduce risks and improve preparedness in recently burned landscapes.
A postfire debris flow in the area burned by the 2016 Fish Fire, Los Angeles county, California. The flow was triggered by heavy rainfall on January 20, 2017.
USGS Postfire Debris-Flow Hazard Assessments
The USGS conducts postfire debris-flow hazard assessments for select fires in the Western U.S. These assessments use information about watershed properties, rainfall characteristics, and soil properties to answer a few key questions:
What burned watersheds are most susceptible to debris flows?
During what types of rainstorms are debris flows likely to be triggered?
How much mud and other debris are these flows capable of carrying?
Click the image below to access the postfire debris-flow hazard assessment dashboard. You can use the dashboard to view or download the data for all recent postfire hazard assessments conducted by the USGS.
More information about hazard assessments
Frequently asked questions
Scientific Background
GIS Services
Request an assessment
Learn more about postfire debris flows
RECOVERY
How long does the hazard last?
As the burn area recovers and the landscape returns to prefire conditions the level of debris-flow hazard decreases. Understanding this recovery process and how debris-flow hazards change in the years following the fire is an active area of research at the USGS.
Use the link below to learn more about fire recovery and postfire debris flows.
RUNOUT
How far can flows travel?
Understanding how far debris flows can travel and what the impacts may be is one of the most important questions we face to effectively protect life and property from debris-flow hazards.
Use the link below to learn more about debris-flow runout research at the USGS.
MONITORING
How well do our hazard models work?
Monitoring stations are installed in select burn areas to better understand the processes that control postfire debris-flow initiation and growth.
Use the link below to learn more about postfire watershed monitoring at the USGS.
Below is a list of science sites associated with this project.
Scientific Background
Rainfall, Volumetric soil-water content, Video, and Geophone Data from the Calwood Fire Burn Area, Colorado, April 2021 to November 2023 Rainfall, Volumetric soil-water content, Video, and Geophone Data from the Calwood Fire Burn Area, Colorado, April 2021 to November 2023
Rainfall, Video, and Geophone Data from the Hermit's Peak/ Calf Canyon Fire Burn Area, New Mexico, June 2022 to June 2024 Rainfall, Video, and Geophone Data from the Hermit's Peak/ Calf Canyon Fire Burn Area, New Mexico, June 2022 to June 2024
Inventory of debris flows in burned (2020-2022) and unburned (1995-2020) areas in the western Cascade Range of Oregon Inventory of debris flows in burned (2020-2022) and unburned (1995-2020) areas in the western Cascade Range of Oregon
Postfire erosion estimates for large California wildfires that occurred between 1984 and 2021 Postfire erosion estimates for large California wildfires that occurred between 1984 and 2021
Compilation of runoff-generated debris-flow inventories for 18 fires across Arizona, California, Colorado, New Mexico, Utah, and Washington, USA Compilation of runoff-generated debris-flow inventories for 18 fires across Arizona, California, Colorado, New Mexico, Utah, and Washington, USA
Postfire Debris-Flow Database (Literature Derived) Postfire Debris-Flow Database (Literature Derived)
Postfire Debris Flow Science Infographic
Post-wildfire debris flow: 2016 Fish Fire, Las Lomas Canyon
The June 2016 Fish Fire burned over 12 km^2 in Los Angeles County, California. After the fire, the USGS installed an automated rain-triggered camera to monitor post-wildfire flooding and debris flow in a small canyon above the Las Lomas debris basin in Duarte. This video shows the peak flow triggered by an intense rainstorm on January 20, 2017.
Debris flow deposit at the outlet of the Tumalt Creek drainage basin, Columbia River Gorge, Oregon, following storms in January 2021.
Debris flow deposit at the outlet of the Tumalt Creek drainage basin, Columbia River Gorge, Oregon, following storms in January 2021.
Home damaged by post-wildfire debris flow in Montecito, CA.
Home damaged by post-wildfire debris flow in Montecito, CA.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
Home damaged by post-wildfire debris flow in Montecito, CA.
Home damaged by post-wildfire debris flow in Montecito, CA.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
Damage from a major post-wildfire landslide that occurred on 25 December 2003 near Devore, San Bernardino County as a result of the Old/Grand Prix fires that ran through the San Bernardino Mountains.
Damage from a major post-wildfire landslide that occurred on 25 December 2003 near Devore, San Bernardino County as a result of the Old/Grand Prix fires that ran through the San Bernardino Mountains.
Montecito home damaged by post-wildfire debrisflow.
Montecito home damaged by post-wildfire debrisflow.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
Montecito home damaged by post-wildfire debrisflow.
Montecito home damaged by post-wildfire debrisflow.Damage from a major post-wildfire landslide that occurred on 9 January 2018 near Montecito, Santa Barbara County as a result of the 2017 Thomas Fire.
The Dec. 4, 2017 Thomas fire, Southern California's largest wildfire on record, burned more than 280,000 acres across Ventura and Santa Barbara counties for nearly a month.
The Dec. 4, 2017 Thomas fire, Southern California's largest wildfire on record, burned more than 280,000 acres across Ventura and Santa Barbara counties for nearly a month.
Geologists assess boulders displaced during the Montecito debris flow event on Jan. 9, 2018.
Geologists assess boulders displaced during the Montecito debris flow event on Jan. 9, 2018.
USGS geologists deployed to Santa Barbara County to support a geohazard assessment of the Montecito area
USGS geologists deployed to Santa Barbara County to support a geohazard assessment of the Montecito area
Post-wildfire Flood and Debris Flow: 2014 Silverado Fire
Post-wildfire Flood and Debris Flow: 2014 Silverado FireIn 2014, the Silverado Fire burned approximately 4 km^2 in Orange County, California. After the fire, the USGS installed an automated rain-triggered camera to monitor post-wildfire flooding and debris flow at the outlet of a small 0.6 km^2 basin within the burn area.
Post-wildfire Flood and Debris Flow: 2014 Silverado Fire
Post-wildfire Flood and Debris Flow: 2014 Silverado FireIn 2014, the Silverado Fire burned approximately 4 km^2 in Orange County, California. After the fire, the USGS installed an automated rain-triggered camera to monitor post-wildfire flooding and debris flow at the outlet of a small 0.6 km^2 basin within the burn area.
House engulfed by debris flows generated in response to a rainstorm on February 6, 2010. This house was west of Briar Wood Canyon in southern California. The small, but steep and rugged drainage basin above this home was burned the previous summer by the Station Fire, the largest fire in the history of Los Angeles County.
House engulfed by debris flows generated in response to a rainstorm on February 6, 2010. This house was west of Briar Wood Canyon in southern California. The small, but steep and rugged drainage basin above this home was burned the previous summer by the Station Fire, the largest fire in the history of Los Angeles County.
Debris Flow in Cable Canyon following the 2003 Old Fire in the San Bernardino Mountains, California.
Debris Flow in Cable Canyon following the 2003 Old Fire in the San Bernardino Mountains, California.
Evaluation of debris-flow building damage forecasts Evaluation of debris-flow building damage forecasts
Post-wildfire debris flows Post-wildfire debris flows
How long do runoff-generated debris-flow hazards persist after wildfire? How long do runoff-generated debris-flow hazards persist after wildfire?
Forecasting the inundation of postfire debris flows Forecasting the inundation of postfire debris flows
Runout model evaluation based on back-calculation of building damage Runout model evaluation based on back-calculation of building damage
Postfire hydrologic response along the central California (USA) coast: Insights for the emergency assessment of postfire debris-flow hazards Postfire hydrologic response along the central California (USA) coast: Insights for the emergency assessment of postfire debris-flow hazards
View the geonarratives (Esri Storymap) below to learn more about recent post-fire debris flow events.