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Landslide Hazards Program

The primary objective of the National Landslide Hazards Program is to reduce long-term losses from landslide hazards by improving our understanding of the causes of ground failure and suggesting mitigation strategies.

News

Hurricane Helene’s Deadly Landslide Legacy

USGS Awards a Dozen Landslide Risk Reduction Grants to Enhance Public Safety and Hazard Preparedness Nationwide

USGS Seeks Landslide Risk Reduction Proposals (FY25)

Publications

Preliminary field report of landslide hazards following Hurricane Helene Preliminary field report of landslide hazards following Hurricane Helene

Executive SummaryThis report reflects our knowledge regarding the widespread landslide activity associated with Hurricane Helene observed during the U.S. Geological Survey’s (USGS) mission assignment to North Carolina in October 2024. The material in this report was originally prepared for the Federal Emergency Management Agency under mission assignment DR-4827-NC. The data and...
Authors
Kate E. Allstadt, Sara K. McBride, Jonathan W. Godt, Stephen L. Slaughter, Kelli W. Baxstrom, Steven Sobieszczyk, Anna Stull

Constraining landslide frequency across the United States to inform county-level risk reduction Constraining landslide frequency across the United States to inform county-level risk reduction

Informative landslide hazard estimates are needed to support landslide mitigation strategies to reduce landslide risk across the United States. Whereas existing national-scale landslide susceptibility products assess where landslides are likely to occur, they do not address how often, which is a critical element of landslide hazard and risk assessments. In particular, the U.S. Federal...
Authors
Lisa Victoria Luna, Jacob Bryson Woodard, Janice L. Bytheway, Gina Marie Belair, Benjamin B. Mirus

Uncertainty reduction for subaerial landslide-tsunami hazards Uncertainty reduction for subaerial landslide-tsunami hazards

Subaerial rock slopes may generate a tsunami by rapidly moving into the water. Large uncertainty in landslide characteristics propagates into large uncertainty in tsunami hazard, making hazard assessment more difficult for land and emergency managers. Once a potentially tsunamigenic landslide is identified, it may not be clear which landslide characteristics contribute most significantly...
Authors
Katherine R. Barnhart, David L. George, Andrew L. Collins, Lauren N. Schaefer, Dennis M. Staley

Science

Brights Creek, North Carolina

The USGS and its cooperators at the North Carolina Geological Survey have installed instruments in a steep hillside at Brights Creek, approximately 15 km east of Hendersonville, North Carolina. Data collection at this site supports research on hydrologic factors that control landslide initiation and is provided here for situational awareness before and during major storm events.
Brights Creek, North Carolina

Brights Creek, North Carolina

The USGS and its cooperators at the North Carolina Geological Survey have installed instruments in a steep hillside at Brights Creek, approximately 15 km east of Hendersonville, North Carolina. Data collection at this site supports research on hydrologic factors that control landslide initiation and is provided here for situational awareness before and during major storm events.
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Shumont Mountain, North Carolina

The USGS and its cooperators have installed instruments in a steep hillside at Shumont Mountain, approximately 4 km north of Chimney Rock, North Carolina . Data collection at this site supports research on hydrologic factors that control landslide initiation and is provided here for situational awareness before and during major storm events.
Shumont Mountain, North Carolina

Shumont Mountain, North Carolina

The USGS and its cooperators have installed instruments in a steep hillside at Shumont Mountain, approximately 4 km north of Chimney Rock, North Carolina . Data collection at this site supports research on hydrologic factors that control landslide initiation and is provided here for situational awareness before and during major storm events.
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Poplar Cove, Nantahala National Forest, North Carolina Landslide Monitoring Site

Poplar Cove, Nantahala National Forest, North Carolina Landslide Monitoring Site

Recent Monitoring Data
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Multimedia

Side view of a rocky peak partially covered in snow Geologic Controls on Deep-Seated Landslides
Geologic Controls on Deep-Seated Landslides
snowcapped mountain peak surrounded by tree-covered hillslopes Understanding large rock slides in deglaciated valleys in the Central and Patagonian Andes
Understanding large rock slides in deglaciated valleys in the Central and Patagonian Andes
person standing in canyon on top of mud, rocks, and vegetation
Debris flow in the 2025 Eaton Fire burn area, California
Debris flow in the 2025 Eaton Fire burn area, California
person holding notebook and wearing hardhat lies on ground watching graduated cylinder and recording measurements
Soil property measurements in the Eaton Fire burn area, Angeles National Forest, California
Soil property measurements in the Eaton Fire burn area, Angeles National Forest, California
burned hillside with no ash and very sparse vegetation
A steep, burned hillside in the 2025 Eaton Fire, Los Angeles County, California.
A steep, burned hillside in the 2025 Eaton Fire, Los Angeles County, California.
hillslope partially covered by burned vegetation
Burned and unburned hillslopes, Eaton Fire, California
Burned and unburned hillslopes, Eaton Fire, California
Steep hillslope denuded of vegetation
A steep, burned hillside in the 2025 Eaton Fire, Los Angeles County, California.
A steep, burned hillside in the 2025 Eaton Fire, Los Angeles County, California.
Steep hillslope with loose sediment and burned vegetation
Dry ravel in the 2025 Eaton Fire burn area.
Dry ravel in the 2025 Eaton Fire burn area.
a dump truck and front loader remove debris in a mostly empty basin at the mountain front
West Ravine debris basin in Los Angeles County, California on January 20, 2025.
West Ravine debris basin in Los Angeles County, California on January 20, 2025.
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