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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.
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.
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.
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.
A debris-flow fan near the outlet of the North Fork Cedar Creek in the South Fork Fire burn area. Floods and debris flows occurred during rain events following the summer wildfire. This drainage is located near the center of the burn area and the photo was taken approximately 4 months following the wildfire.
A debris-flow fan near the outlet of the North Fork Cedar Creek in the South Fork Fire burn area. Floods and debris flows occurred during rain events following the summer wildfire. This drainage is located near the center of the burn area and the photo was taken approximately 4 months following the wildfire.
Mud- to boulder-sized sediment fill a channel in the 2024 South Fork Fire burn area. The sediment was deposited by flooding and debris flows during rain events following the summer wildfire. The coarsest material (including several large boulders) was deposited on the south side of the channel, forming a debris-flow levee.
Mud- to boulder-sized sediment fill a channel in the 2024 South Fork Fire burn area. The sediment was deposited by flooding and debris flows during rain events following the summer wildfire. The coarsest material (including several large boulders) was deposited on the south side of the channel, forming a debris-flow levee.
A mud- to boulder-sized debris-flow deposit in the South Fork Fire burn area, New Mexico. Flooding and debris-flows occurred as a result of rain events shortly following the summer wildfire. This photo was taken in the South Fork Cedar Creek drainage near the center of the burn area approximately 4 months following the wildfire.
A mud- to boulder-sized debris-flow deposit in the South Fork Fire burn area, New Mexico. Flooding and debris-flows occurred as a result of rain events shortly following the summer wildfire. This photo was taken in the South Fork Cedar Creek drainage near the center of the burn area approximately 4 months following the wildfire.
A boulder-rich postfire debris-flow deposit in the 2024 Salt fire burn area. Flooding and debris flows occurred near Ruidoso, New Mexico during rain events shortly following the 2024 wildfires. This photo was taken in Bear Canyon, on the Mescalero Reservation, near the central portion of the burn area.
A boulder-rich postfire debris-flow deposit in the 2024 Salt fire burn area. Flooding and debris flows occurred near Ruidoso, New Mexico during rain events shortly following the 2024 wildfires. This photo was taken in Bear Canyon, on the Mescalero Reservation, near the central portion of the burn area.
A poorly-sorted, debris-flow levee deposited during a rain event following the 2024 South Fork Fire. Levees form at the margins of debris flows are matrix-supported, and comprised of variably-sized sediment. Levees are useful for field identification of debris flow deposits and help to differentiate them from flood deposits.
A poorly-sorted, debris-flow levee deposited during a rain event following the 2024 South Fork Fire. Levees form at the margins of debris flows are matrix-supported, and comprised of variably-sized sediment. Levees are useful for field identification of debris flow deposits and help to differentiate them from flood deposits.
Post-fire debris flow depositing ash and sediment on a steep hillside, 2021 Dixie Fire in northern CA.
Post-fire debris flow depositing ash and sediment on a steep hillside, 2021 Dixie Fire in northern CA.
Boulders deposited by post-fire debris flow at the site of the 2020 Dolan Fire in California.
Boulders deposited by post-fire debris flow at the site of the 2020 Dolan Fire in California.
Flooding and debris flows during rain events following the 2024 South Fork Fire near Ruidoso, New Mexico.
Flooding and debris flows during rain events following the 2024 South Fork Fire near Ruidoso, New Mexico.
The USGS Postfire Landslide Monitoring Station “Maria Ygnacio” is located within the Los Padres National Forest in the Santa Ynez Mountains of southern California. The site consists of surface and subsurface instrumentation that is monitoring the hillslope shown in this image.
The USGS Postfire Landslide Monitoring Station “Maria Ygnacio” is located within the Los Padres National Forest in the Santa Ynez Mountains of southern California. The site consists of surface and subsurface instrumentation that is monitoring the hillslope shown in this image.
A range of flow types can be observed in steep, recently-burned terrain, but predicting the spatial distribution of debris flows resulting from a single storm event remains challenging.
A range of flow types can be observed in steep, recently-burned terrain, but predicting the spatial distribution of debris flows resulting from a single storm event remains challenging.
Debris-flow deposits downstream of the 2022 Pipeline Fire burn scar, north of Flagstaff, Arizona.
Debris-flow deposits downstream of the 2022 Pipeline Fire burn scar, north of Flagstaff, Arizona.
On July 4, 2022, intense rainfall triggered this debris flow that damaged a home in the 2021 Muckamuck Fire in north-central Washington.
On July 4, 2022, intense rainfall triggered this debris flow that damaged a home in the 2021 Muckamuck Fire in north-central Washington.
The Grizzly Creek Fire initiated in August 2020, and widespread destructive debris flow activity followed the during the summer of 2021. This image shows damage from the summer 2021 debris flow in Glenwood Canyon, Colorado.
The Grizzly Creek Fire initiated in August 2020, and widespread destructive debris flow activity followed the during the summer of 2021. This image shows damage from the summer 2021 debris flow in Glenwood Canyon, Colorado.
Debris flow in Glenwood Canyon during the summer of 2021. This event followed the 2020 Grizzly Creek Fire in Glenwood Canyon, Colorado.
Debris flow in Glenwood Canyon during the summer of 2021. This event followed the 2020 Grizzly Creek Fire in Glenwood Canyon, Colorado.
Scientists assess post wildfire debris flow following the 2020 Grizzly Creek fire.
Scientists assess post wildfire debris flow following the 2020 Grizzly Creek fire.
USGS scientist assesses debris flow in Glenwood Canyon, Colorado. This post-wildfire debris flow follows the 2020 Grizzly Creek Fire.
USGS scientist assesses debris flow in Glenwood Canyon, Colorado. This post-wildfire debris flow follows the 2020 Grizzly Creek Fire.
Calwood burn area, Calwood post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:06 MDT to 14:13:05 MDT.
Calwood burn area, Calwood post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:06 MDT to 14:13:05 MDT.
Calwood burn area, Heil Ranch post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:07 MDT to 14:13:11 MDT.
Calwood burn area, Heil Ranch post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:07 MDT to 14:13:11 MDT.
Ground level view of debris covering the eastbound lane of I-70 following the June 26-27, 2021, storms. The green sign in the background indicating Milepost 120 is mostly buried by mud.
Ground level view of debris covering the eastbound lane of I-70 following the June 26-27, 2021, storms. The green sign in the background indicating Milepost 120 is mostly buried by mud.
The atmospheric river, a narrow, powerful track of water vapor that can deliver tremendous volumes of rain, hit the central California coast and stalled there between January 26 and 28, 2021 — with catastrophic consequences.
The atmospheric river, a narrow, powerful track of water vapor that can deliver tremendous volumes of rain, hit the central California coast and stalled there between January 26 and 28, 2021 — with catastrophic consequences.
On Sunday, August 16, 2020 at approximately 3:00 PM PST, the River wildfire ignited in Monterey County, California, just west of the Salinas River Valley.
On Sunday, August 16, 2020 at approximately 3:00 PM PST, the River wildfire ignited in Monterey County, California, just west of the Salinas River Valley.
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.
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.
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.
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.
A debris-flow fan near the outlet of the North Fork Cedar Creek in the South Fork Fire burn area. Floods and debris flows occurred during rain events following the summer wildfire. This drainage is located near the center of the burn area and the photo was taken approximately 4 months following the wildfire.
A debris-flow fan near the outlet of the North Fork Cedar Creek in the South Fork Fire burn area. Floods and debris flows occurred during rain events following the summer wildfire. This drainage is located near the center of the burn area and the photo was taken approximately 4 months following the wildfire.
Mud- to boulder-sized sediment fill a channel in the 2024 South Fork Fire burn area. The sediment was deposited by flooding and debris flows during rain events following the summer wildfire. The coarsest material (including several large boulders) was deposited on the south side of the channel, forming a debris-flow levee.
Mud- to boulder-sized sediment fill a channel in the 2024 South Fork Fire burn area. The sediment was deposited by flooding and debris flows during rain events following the summer wildfire. The coarsest material (including several large boulders) was deposited on the south side of the channel, forming a debris-flow levee.
A mud- to boulder-sized debris-flow deposit in the South Fork Fire burn area, New Mexico. Flooding and debris-flows occurred as a result of rain events shortly following the summer wildfire. This photo was taken in the South Fork Cedar Creek drainage near the center of the burn area approximately 4 months following the wildfire.
A mud- to boulder-sized debris-flow deposit in the South Fork Fire burn area, New Mexico. Flooding and debris-flows occurred as a result of rain events shortly following the summer wildfire. This photo was taken in the South Fork Cedar Creek drainage near the center of the burn area approximately 4 months following the wildfire.
A boulder-rich postfire debris-flow deposit in the 2024 Salt fire burn area. Flooding and debris flows occurred near Ruidoso, New Mexico during rain events shortly following the 2024 wildfires. This photo was taken in Bear Canyon, on the Mescalero Reservation, near the central portion of the burn area.
A boulder-rich postfire debris-flow deposit in the 2024 Salt fire burn area. Flooding and debris flows occurred near Ruidoso, New Mexico during rain events shortly following the 2024 wildfires. This photo was taken in Bear Canyon, on the Mescalero Reservation, near the central portion of the burn area.
A poorly-sorted, debris-flow levee deposited during a rain event following the 2024 South Fork Fire. Levees form at the margins of debris flows are matrix-supported, and comprised of variably-sized sediment. Levees are useful for field identification of debris flow deposits and help to differentiate them from flood deposits.
A poorly-sorted, debris-flow levee deposited during a rain event following the 2024 South Fork Fire. Levees form at the margins of debris flows are matrix-supported, and comprised of variably-sized sediment. Levees are useful for field identification of debris flow deposits and help to differentiate them from flood deposits.
Post-fire debris flow depositing ash and sediment on a steep hillside, 2021 Dixie Fire in northern CA.
Post-fire debris flow depositing ash and sediment on a steep hillside, 2021 Dixie Fire in northern CA.
Boulders deposited by post-fire debris flow at the site of the 2020 Dolan Fire in California.
Boulders deposited by post-fire debris flow at the site of the 2020 Dolan Fire in California.
Flooding and debris flows during rain events following the 2024 South Fork Fire near Ruidoso, New Mexico.
Flooding and debris flows during rain events following the 2024 South Fork Fire near Ruidoso, New Mexico.
The USGS Postfire Landslide Monitoring Station “Maria Ygnacio” is located within the Los Padres National Forest in the Santa Ynez Mountains of southern California. The site consists of surface and subsurface instrumentation that is monitoring the hillslope shown in this image.
The USGS Postfire Landslide Monitoring Station “Maria Ygnacio” is located within the Los Padres National Forest in the Santa Ynez Mountains of southern California. The site consists of surface and subsurface instrumentation that is monitoring the hillslope shown in this image.
A range of flow types can be observed in steep, recently-burned terrain, but predicting the spatial distribution of debris flows resulting from a single storm event remains challenging.
A range of flow types can be observed in steep, recently-burned terrain, but predicting the spatial distribution of debris flows resulting from a single storm event remains challenging.
Debris-flow deposits downstream of the 2022 Pipeline Fire burn scar, north of Flagstaff, Arizona.
Debris-flow deposits downstream of the 2022 Pipeline Fire burn scar, north of Flagstaff, Arizona.
On July 4, 2022, intense rainfall triggered this debris flow that damaged a home in the 2021 Muckamuck Fire in north-central Washington.
On July 4, 2022, intense rainfall triggered this debris flow that damaged a home in the 2021 Muckamuck Fire in north-central Washington.
The Grizzly Creek Fire initiated in August 2020, and widespread destructive debris flow activity followed the during the summer of 2021. This image shows damage from the summer 2021 debris flow in Glenwood Canyon, Colorado.
The Grizzly Creek Fire initiated in August 2020, and widespread destructive debris flow activity followed the during the summer of 2021. This image shows damage from the summer 2021 debris flow in Glenwood Canyon, Colorado.
Debris flow in Glenwood Canyon during the summer of 2021. This event followed the 2020 Grizzly Creek Fire in Glenwood Canyon, Colorado.
Debris flow in Glenwood Canyon during the summer of 2021. This event followed the 2020 Grizzly Creek Fire in Glenwood Canyon, Colorado.
Scientists assess post wildfire debris flow following the 2020 Grizzly Creek fire.
Scientists assess post wildfire debris flow following the 2020 Grizzly Creek fire.
USGS scientist assesses debris flow in Glenwood Canyon, Colorado. This post-wildfire debris flow follows the 2020 Grizzly Creek Fire.
USGS scientist assesses debris flow in Glenwood Canyon, Colorado. This post-wildfire debris flow follows the 2020 Grizzly Creek Fire.
Calwood burn area, Calwood post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:06 MDT to 14:13:05 MDT.
Calwood burn area, Calwood post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:06 MDT to 14:13:05 MDT.
Calwood burn area, Heil Ranch post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:07 MDT to 14:13:11 MDT.
Calwood burn area, Heil Ranch post-fire debris-flow monitoring station video footage from rainstorm on July 31, 2021 from 14:07 MDT to 14:13:11 MDT.
Ground level view of debris covering the eastbound lane of I-70 following the June 26-27, 2021, storms. The green sign in the background indicating Milepost 120 is mostly buried by mud.
Ground level view of debris covering the eastbound lane of I-70 following the June 26-27, 2021, storms. The green sign in the background indicating Milepost 120 is mostly buried by mud.
The atmospheric river, a narrow, powerful track of water vapor that can deliver tremendous volumes of rain, hit the central California coast and stalled there between January 26 and 28, 2021 — with catastrophic consequences.
The atmospheric river, a narrow, powerful track of water vapor that can deliver tremendous volumes of rain, hit the central California coast and stalled there between January 26 and 28, 2021 — with catastrophic consequences.
On Sunday, August 16, 2020 at approximately 3:00 PM PST, the River wildfire ignited in Monterey County, California, just west of the Salinas River Valley.
On Sunday, August 16, 2020 at approximately 3:00 PM PST, the River wildfire ignited in Monterey County, California, just west of the Salinas River Valley.