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Multimedia

Browse our photos and videos of landslide research and post-landslide investigations.

Images

Map showing the location of the tsunamigenic landslide in Tracy Arm southeast of Sawyer Island.
2025 Tracy Arm Landslide Overview Map
2025 Tracy Arm Landslide Overview Map
2025 Tracy Arm Landslide Overview Map

Overview map and location of the Tracy Arm landslide-generated tsunami event. The imagery is not current, and the South Sawyer Glacier has retreated over a kilometer from what is depicted. 

Overview map and location of the Tracy Arm landslide-generated tsunami event. The imagery is not current, and the South Sawyer Glacier has retreated over a kilometer from what is depicted. 

Aerial photo of landslide deposit at bottom of mountain and into the water
2025 Tracy Arm Landslide Aerial Photo Facing West
2025 Tracy Arm Landslide Aerial Photo Facing West
2025 Tracy Arm Landslide Aerial Photo Facing West

Oblique aerial photo of the August 10, 2025 landslide captured during a field reconnaissance overflight on August 13, 2025. Look direction is to the west.​

Aerial photo of steep mountainside showing the landslide source area.
2025 Tracy Arm Landslide Source Area
2025 Tracy Arm Landslide Source Area
2025 Tracy Arm Landslide Source Area

Oblique aerial photo of the August 10, 2025 landslide source area captured during a field reconnaissance overflight on August 13, 2025. Look direction is approximately north.​

Oblique aerial photo of the August 10, 2025 landslide source area captured during a field reconnaissance overflight on August 13, 2025. Look direction is approximately north.​

Photo of shoreline with debris showing tsunami-inundated area
2025 Tracy Arm Landslide Tsunami-Inundated Shoreline
2025 Tracy Arm Landslide Tsunami-Inundated Shoreline
2025 Tracy Arm Landslide Tsunami-Inundated Shoreline

Photo of tsunami-inundated shoreline at Williams Cove, near the mouth of Tracy Arm. Look direction is approximately north.​

Aerial photo of landslide taken across the fiord
2025 Tracy Arm Landslide Across the Fiord Facing North
2025 Tracy Arm Landslide Across the Fiord Facing North
2025 Tracy Arm Landslide Across the Fiord Facing North

Oblique aerial photo of the August 10, 2025 landslide taken from across the fiord during a field reconnaissance overflight on August 13, 2025. Look direction is approximately north.​

Photo of a mountainous landscape with the landslide on the right
2025 Tracy Arm Landslide and Tsunami Trimline
2025 Tracy Arm Landslide and Tsunami Trimline
2025 Tracy Arm Landslide and Tsunami Trimline

Oblique aerial photo of the August 10, 2025 landslide source area captured during a field reconnaissance overflight on August 13, 2025. Look direction is approximately north.​

Oblique aerial photo of the August 10, 2025 landslide source area captured during a field reconnaissance overflight on August 13, 2025. Look direction is approximately north.​

Videos

mud and trees flowing through a channel mud and trees flowing through a channel
Postfire debris flow in the 2024 Elk Fire burn area
Postfire debris flow in the 2024 Elk Fire burn area

A debris flow recorded by a USGS Landslide Monitoring Station in the 2024 Elk Fire burn area near Dayton, Wyoming. The flow was triggered by intense rainfall during a thunderstorm on the evening of July 15, 2025.

A debris flow recorded by a USGS Landslide Monitoring Station in the 2024 Elk Fire burn area near Dayton, Wyoming. The flow was triggered by intense rainfall during a thunderstorm on the evening of July 15, 2025.

Side view of a rocky peak partially covered in snow Side view of a rocky peak partially covered in snow
Geologic Controls on Deep-Seated Landslides
Geologic Controls on Deep-Seated Landslides

The frequency and scale of landslides in a region are determined by both external forcing and inherent, site-specific susceptibility.

The frequency and scale of landslides in a region are determined by both external forcing and inherent, site-specific susceptibility.

snowcapped mountain peak surrounded by tree-covered hillslopes 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

The effects of deglaciation on the slope stability of glacial valleys have increasing importance in the context of climate change, with a role on the susceptibility to large-volume rock slides or rock avalanches and catastrophic cascading geohazards.

Controls on post-fire debris flows in Oregon

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.

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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