Lower portion of the landslide runout along the Pedersen Glacier from the 2024 Pedersen Lagoon landslide in Alaska.
Multimedia
The Geologic Hazards Science Center produces many images as part of our earthquake, landslides, geologic, and geomagnetic research. Also, check out our growing educational video selection.
Images
Lower portion of the landslide runout along the Pedersen Glacier from the 2024 Pedersen Lagoon landslide in Alaska.
Landslide source area and upper portion of the landslide runout. The upper reaches of the landslide source material of the 2024 Pedersen Lagoon landslide in Alaska.
Landslide source area and upper portion of the landslide runout. The upper reaches of the landslide source material of the 2024 Pedersen Lagoon landslide in Alaska.
Tsunami damage between the upper and lower portions of the lagoon from the landslide-generated tsunami from the 2024 Pedersen Lagoon landslide in Alaska. It moved toward the east at the western shore and uplands of the landform between the lagoons.
Tsunami damage between the upper and lower portions of the lagoon from the landslide-generated tsunami from the 2024 Pedersen Lagoon landslide in Alaska. It moved toward the east at the western shore and uplands of the landform between the lagoons.
Carousel Banner for the "Meet the USGS Interns - Earthquakes Edition" video pointing visitors to the latest recap on intern stories at NEIC.
Carousel Banner for the "Meet the USGS Interns - Earthquakes Edition" video pointing visitors to the latest recap on intern stories at NEIC.
Video Thumbnail for the video "USGS NEIC Earthquake Response". Showcases three USGS scientists working at the National Earthquakes Information Center.
Video Thumbnail for the video "USGS NEIC Earthquake Response". Showcases three USGS scientists working at the National Earthquakes Information Center.
ShakeMap of 1906 San Francisco Earthquake constructed using historical data. Compare to Macroseismic data version.
ShakeMap of 1906 San Francisco Earthquake constructed using historical data. Compare to Macroseismic data version.
Videos
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
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.