USGS Hurricane Helene Landslide Dashboard. Screenshot taken on October 3, 2024 at 10:18pm UTC. This is an ongoing, multi-agency effort to map landslides from Hurricane Helene. This dashboard is updated as more information is available.
Multimedia
Browse our photos and videos of landslide research and post-landslide investigations.
Images
USGS Hurricane Helene Landslide Dashboard. Screenshot taken on October 3, 2024 at 10:18pm UTC. This is an ongoing, multi-agency effort to map landslides from Hurricane Helene. This dashboard is updated as more information is available.
Relative landslide hazard from Hurricane Helene. Dark purple shows locations expected to have experienced the highest landslide occurrence. Map based on cumulative precipitation estimate (NWS Greenville-Spartanburg from 9/24-9/28) and the USGS Landslide Susceptibility Map.
Relative landslide hazard from Hurricane Helene. Dark purple shows locations expected to have experienced the highest landslide occurrence. Map based on cumulative precipitation estimate (NWS Greenville-Spartanburg from 9/24-9/28) and the USGS Landslide Susceptibility Map.
ÂżDĂłnde Ocurren los Deslizamientos de Tierra?
(Mapa Nacional de Susceptibilidad a Deslizamientos de Tierra, 2024)
ÂżDĂłnde Ocurren los Deslizamientos de Tierra?
(Mapa Nacional de Susceptibilidad a Deslizamientos de Tierra, 2024)
A map of the United States including Hawaii, Alaska, and Puerto Rico shows landslide susceptibility from yellow (low) to red (high), where the areas without shading represent negligible potential for landslides.
A map of the United States including Hawaii, Alaska, and Puerto Rico shows landslide susceptibility from yellow (low) to red (high), where the areas without shading represent negligible potential for landslides.
Geologist conducts a survey of the tsunami damage following the 2024 Pedersen Lagoon Landslide in Alaska.
Geologist conducts a survey of the tsunami damage following the 2024 Pedersen Lagoon Landslide in Alaska.
Photo looking towards the landslide source, with debris from the subsequent tsunami in the foreground.
Photo looking towards the landslide source, with debris from the subsequent tsunami in the foreground.
Videos
Atmospheric rivers cause the majority of precipitation-induced landslides in Western North America
linkAtmospheric 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
linkAtmospheric rivers (ARs) are transient channels of intense horizontal water vapor transport in the lower atmosphere.
The development of a Geologic Hazards Program for the USDA Forest Service is a challenging undertaking.
The development of a Geologic Hazards Program for the USDA Forest Service is a challenging undertaking.
Debris 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.
Debris 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.
This video provides a brief overview of the Prince William Sound Landslide Hazards Project in Alaska. The video describes each of the congressional mandates that makes up the project tasks. This is the first video in a series about the project.
This video provides a brief overview of the Prince William Sound Landslide Hazards Project in Alaska. The video describes each of the congressional mandates that makes up the project tasks. This is the first video in a series about the project.
In 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.
In 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.
How debris flows erode and deposit material along their paths is difficult to determine in natural settings due to the lack of warning and the rapid pace at which they occur. Post-event field measurements or controlled flume experiments are commonly used to evaluate debris flows between the head and the distalmost deposit.
How debris flows erode and deposit material along their paths is difficult to determine in natural settings due to the lack of warning and the rapid pace at which they occur. Post-event field measurements or controlled flume experiments are commonly used to evaluate debris flows between the head and the distalmost deposit.