Wildfire often amplifies the likelihood and magnitude of debris flows in steep terrain. In arid climates (e.g. US Mountain West and Southwest), post-fire debris flows typically occur during the first rains following fire, suggesting that rainfall-driven erosion is a strong control on in-channel preconditioning and triggering of these hazards.
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a pile of large boulders and tree parts up against a guardrail next to a road
Wildfire often amplifies the likelihood and magnitude of debris flows in steep terrain. In arid climates (e.g. US Mountain West and Southwest), post-fire debris flows typically occur during the first rains following fire, suggesting that rainfall-driven erosion is a strong control on in-channel preconditioning and triggering of these hazards.
At the USGS National Earthquake Information Center (NEIC), our team locates and researches earthquakes to provide information on how to reduce risk from earthquakes.
At the USGS National Earthquake Information Center (NEIC), our team locates and researches earthquakes to provide information on how to reduce risk from earthquakes.
At the USGS National Earthquake Information Center (NEIC), our team locates and researches earthquakes to provide information on how to reduce risk from earthquakes.
At the USGS National Earthquake Information Center (NEIC), our team locates and researches earthquakes to provide information on how to reduce risk from earthquakes.
Ever wonder what it is like to work as a USGS intern? Dive into these intern stories of how students are making science their superpower while studying earthquakes!
Ever wonder what it is like to work as a USGS intern? Dive into these intern stories of how students are making science their superpower while studying earthquakes!
Every 11 years the Sun's magnetic field flips. This period is referred to as a solar cycle. As we approach the peak of Solar Cycle 25, activity on the Sun’s surface will increase, including more solar flares, sunspots, and coronal mass ejections.
Every 11 years the Sun's magnetic field flips. This period is referred to as a solar cycle. As we approach the peak of Solar Cycle 25, activity on the Sun’s surface will increase, including more solar flares, sunspots, and coronal mass ejections.
Every 11 years the Sun's magnetic field flips. This period is referred to as a solar cycle. As we approach the peak of Solar Cycle 25, activity on the Sun’s surface will increase, including more solar flares, sunspots, and coronal mass ejections.
Every 11 years the Sun's magnetic field flips. This period is referred to as a solar cycle. As we approach the peak of Solar Cycle 25, activity on the Sun’s surface will increase, including more solar flares, sunspots, and coronal mass ejections.
Atmospheric rivers cause the majority of precipitation-induced landslides in Western North America
Atmospheric rivers cause the majority of precipitation-induced landslides in Western North AmericaAtmospheric rivers (ARs) are transient channels of intense horizontal water vapor transport in the lower atmosphere.
Atmospheric rivers cause the majority of precipitation-induced landslides in Western North America
Atmospheric rivers cause the majority of precipitation-induced landslides in Western North AmericaAtmospheric rivers (ARs) are transient channels of intense horizontal water vapor transport in the lower atmosphere.
Cascading Hazards: Earthquake Triggered Landslides
Cascading Hazards: Earthquake Triggered LandslidesOn February 6, 2023, magnitude 7.8 and 7.5 earthquakes struck Turkey near the Syrian border. Over 50,000 people lost their lives. Earthquake shaking was not the only hazard. The quake triggered landslides, liquefaction, and other cascading hazards.
Cascading Hazards: Earthquake Triggered Landslides
Cascading Hazards: Earthquake Triggered LandslidesOn February 6, 2023, magnitude 7.8 and 7.5 earthquakes struck Turkey near the Syrian border. Over 50,000 people lost their lives. Earthquake shaking was not the only hazard. The quake triggered landslides, liquefaction, and other cascading hazards.
Measuring Landslide Thickness: Seismic Equipment Used for More Than Earthquakes
Measuring Landslide Thickness: Seismic Equipment Used for More Than EarthquakesEver wonder how scientists measure how thick landslides are? There are a few ways, but the one Kate Allstadt explains might surprise you.
Measuring Landslide Thickness: Seismic Equipment Used for More Than Earthquakes
Measuring Landslide Thickness: Seismic Equipment Used for More Than EarthquakesEver wonder how scientists measure how thick landslides are? There are a few ways, but the one Kate Allstadt explains might surprise you.
Landslide risk evaluation: tools and tips for risky decisions
Landslide risk evaluation: tools and tips for risky decisionsWhen a landslide is recognized to be life-threatening, difficult decisions follow. Like, should the house be evacuated? Is the community safe enough? How much should be invested in mitigation? For the past two decades, we have been applying a quantitative risk management framework to inform these types of decisions.
Landslide risk evaluation: tools and tips for risky decisions
Landslide risk evaluation: tools and tips for risky decisionsWhen a landslide is recognized to be life-threatening, difficult decisions follow. Like, should the house be evacuated? Is the community safe enough? How much should be invested in mitigation? For the past two decades, we have been applying a quantitative risk management framework to inform these types of decisions.
One Way to Develop a Geologic Hazards Program: Lessons Learned and Anecdotes
One Way to Develop a Geologic Hazards Program: Lessons Learned and AnecdotesThe development of a Geologic Hazards Program for the USDA Forest Service is a challenging undertaking.
One Way to Develop a Geologic Hazards Program: Lessons Learned and Anecdotes
One Way to Develop a Geologic Hazards Program: Lessons Learned and AnecdotesThe development of a Geologic Hazards Program for the USDA Forest Service is a challenging undertaking.
Forecasting and seismic detection of debris flows at Mount Rainier National Park
Forecasting and seismic detection of debris flows at Mount Rainier National ParkDebris flows occur as a result of glacial outburst floods or intense fall storms prior to snow accumulations and occur commonly at the glaciated Mount Rainier, WA. Over 60 such events have been documented since 1928, 35+ of which have occurred in Tahoma Creek on the southwest side of the park.
Forecasting and seismic detection of debris flows at Mount Rainier National Park
Forecasting and seismic detection of debris flows at Mount Rainier National ParkDebris flows occur as a result of glacial outburst floods or intense fall storms prior to snow accumulations and occur commonly at the glaciated Mount Rainier, WA. Over 60 such events have been documented since 1928, 35+ of which have occurred in Tahoma Creek on the southwest side of the park.
Kinematic evolution of a large paraglacial landslide in the Barry Arm fjord of Alaska
Kinematic evolution of a large paraglacial landslide in the Barry Arm fjord of AlaskaIn the Barry Arm fjord of Alaska, repeat, high-resolution aerial and satellite data provide a unique opportunity to learn how a large bedrock landslide with a receding and thinning glacier at the toe is deforming.
Kinematic evolution of a large paraglacial landslide in the Barry Arm fjord of Alaska
Kinematic evolution of a large paraglacial landslide in the Barry Arm fjord of AlaskaIn the Barry Arm fjord of Alaska, repeat, high-resolution aerial and satellite data provide a unique opportunity to learn how a large bedrock landslide with a receding and thinning glacier at the toe is deforming.
Communicating landslide information and hazards with maps and graphics at the Washington Geological Survey
Communicating landslide information and hazards with maps and graphics at the Washington Geological SurveyThe Washington Geological Survey works to increase public and scientific understanding of landslide hazards in Washington State. One of the ways that we do this is through use of interpretive maps, illustrations, and other types of graphics. I will show several examples of these products and will discuss some of the methods used to construct them.
Communicating landslide information and hazards with maps and graphics at the Washington Geological Survey
Communicating landslide information and hazards with maps and graphics at the Washington Geological SurveyThe Washington Geological Survey works to increase public and scientific understanding of landslide hazards in Washington State. One of the ways that we do this is through use of interpretive maps, illustrations, and other types of graphics. I will show several examples of these products and will discuss some of the methods used to construct them.
Modeling post-fire flood and debris-flow hazards considering infrastructure sedimentation
Modeling post-fire flood and debris-flow hazards considering infrastructure sedimentationWhile California has been known to experience a fire-flood cycle for about a century, post-fire flood and debris-flow risks are increasing due to increases in the frequency and intensity of wildfires and storms and urbanization in fire- and flood-prone areas.
Modeling post-fire flood and debris-flow hazards considering infrastructure sedimentation
Modeling post-fire flood and debris-flow hazards considering infrastructure sedimentationWhile California has been known to experience a fire-flood cycle for about a century, post-fire flood and debris-flow risks are increasing due to increases in the frequency and intensity of wildfires and storms and urbanization in fire- and flood-prone areas.
The spatial distribution of post-fire debris flows in relation to observed rainfall anomalies: Insights from the Dolan Fire, California
The spatial distribution of post-fire debris flows in relation to observed rainfall anomalies: Insights from the Dolan Fire, CaliforniaA 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.
The spatial distribution of post-fire debris flows in relation to observed rainfall anomalies: Insights from the Dolan Fire, California
The spatial distribution of post-fire debris flows in relation to observed rainfall anomalies: Insights from the Dolan Fire, CaliforniaA 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.
Liquefaction or liquefiction? Anthropogenic regulation and the influence of evaporite dissolution on ground failure in the 2019 Mw 7.1 Ridgecrest Earthquake and beyond
Liquefaction or liquefiction? Anthropogenic regulation and the influence of evaporite dissolution on ground failure in the 2019 Mw 7.1 Ridgecrest Earthquake and beyondOptical remote sensing observations of the 2019 Ridgecrest, California, earthquake sequence revealed a significant amount of surface ejecta in the nearby Searles Lake, including one area where the surface ejecta was arranged in a repeating hexagonal “honeycomb” pattern.
Liquefaction or liquefiction? Anthropogenic regulation and the influence of evaporite dissolution on ground failure in the 2019 Mw 7.1 Ridgecrest Earthquake and beyond
Liquefaction or liquefiction? Anthropogenic regulation and the influence of evaporite dissolution on ground failure in the 2019 Mw 7.1 Ridgecrest Earthquake and beyondLiquefaction or liquefiction? Anthropogenic regulation and the influence of evaporite dissolution on ground failure in the 2019 Mw 7.1 Ridgecrest Earthquake and beyond
Liquefaction or liquefiction? Anthropogenic regulation and the influence of evaporite dissolution on ground failure in the 2019 Mw 7.1 Ridgecrest Earthquake and beyondOptical remote sensing observations of the 2019 Ridgecrest, California, earthquake sequence revealed a significant amount of surface ejecta in the nearby Searles Lake, including one area where the surface ejecta was arranged in a repeating hexagonal “honeycomb” pattern.
Blockslides, summit grabens, and collapsing highwalls of the Appalachian Valley and Ridge: Using lidar-derived imagery to reevaluate a thoroughly studied landscape
Blockslides, summit grabens, and collapsing highwalls of the Appalachian Valley and Ridge: Using lidar-derived imagery to reevaluate a thoroughly studied landscapeIn the mid-1980s, Art Schultz (USGS, ret.) drew on experiences in the Colorado Front Range to identify numerous large, stratigraphically intact, kilometer-scale bedrock landslides on interbedded sandstone-shale dip slopes in the Virginia Valley and Ridge.
Blockslides, summit grabens, and collapsing highwalls of the Appalachian Valley and Ridge: Using lidar-derived imagery to reevaluate a thoroughly studied landscape
Blockslides, summit grabens, and collapsing highwalls of the Appalachian Valley and Ridge: Using lidar-derived imagery to reevaluate a thoroughly studied landscapeBlockslides, summit grabens, and collapsing highwalls of the Appalachian Valley and Ridge: Using lidar-derived imagery to reevaluate a thoroughly studied landscape
Blockslides, summit grabens, and collapsing highwalls of the Appalachian Valley and Ridge: Using lidar-derived imagery to reevaluate a thoroughly studied landscapeIn the mid-1980s, Art Schultz (USGS, ret.) drew on experiences in the Colorado Front Range to identify numerous large, stratigraphically intact, kilometer-scale bedrock landslides on interbedded sandstone-shale dip slopes in the Virginia Valley and Ridge.
Dr. Annemarie Baltay talks about the October 25th, 2022 M5.1 earthquake in Seven Trees, California.
Dr. Annemarie Baltay talks about the October 25th, 2022 M5.1 earthquake in Seven Trees, California.
Landslide susceptibility in Minnesota: Insight from landslide inventory mapping and lidar change detection
Landslide susceptibility in Minnesota: Insight from landslide inventory mapping and lidar change detectionThe recently published landslide inventory for most landslide-prone areas in Minnesota provides the basis for generation of landslide susceptibility maps. These maps are derived from logistic regression analysis of mapped landslide occurrences, terrain characteristics, and Quaternary geological mapping.
Landslide susceptibility in Minnesota: Insight from landslide inventory mapping and lidar change detection
Landslide susceptibility in Minnesota: Insight from landslide inventory mapping and lidar change detectionThe recently published landslide inventory for most landslide-prone areas in Minnesota provides the basis for generation of landslide susceptibility maps. These maps are derived from logistic regression analysis of mapped landslide occurrences, terrain characteristics, and Quaternary geological mapping.
black and white image of mountain with text
Virtual Field Excursion to Glenwood Canyon, Colorado: and the post-fire debris flows from the 2020 Grizzly Creek Fire
Virtual Field Excursion to Glenwood Canyon, Colorado: and the post-fire debris flows from the 2020 Grizzly Creek FireThis video serves as a virtual fieldtrip to document the debris flow activity following the Grizzly Creek Fire in the Glenwood Canyon, CO, USA. The Grizzly Creek Fire initiated in August 2020, and widespread destructive debris flow activity followed the during the summer of 2021.
Virtual Field Excursion to Glenwood Canyon, Colorado: and the post-fire debris flows from the 2020 Grizzly Creek Fire
Virtual Field Excursion to Glenwood Canyon, Colorado: and the post-fire debris flows from the 2020 Grizzly Creek FireThis video serves as a virtual fieldtrip to document the debris flow activity following the Grizzly Creek Fire in the Glenwood Canyon, CO, USA. The Grizzly Creek Fire initiated in August 2020, and widespread destructive debris flow activity followed the during the summer of 2021.