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Geologic Hazards Science Center images.

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View of debris flows on hillslope in Puerto Rico from above
Hurricane Maria debris flows - Naranjito, Puerto Rico 2017
Hurricane Maria debris flows - Naranjito, Puerto Rico 2017
Hurricane Maria debris flows - Naranjito, Puerto Rico 2017

Numerous debris flows caused by intense rainfall from Hurricane Maria in September 2017 in Puerto Rico. Trees are bare due to the hurricane force winds that stripped the leaves. 

Numerous debris flows caused by intense rainfall from Hurricane Maria in September 2017 in Puerto Rico. Trees are bare due to the hurricane force winds that stripped the leaves. 

A hillside showing landslides with debris from one landslide impacting a house at the bottom of the slope.
Rainfall and Landslides in Northern CA
Rainfall and Landslides in Northern CA
Rainfall and Landslides in Northern CA

Shallow landslides damaged homes and closed many roads in the San Francisco East Bay region as a result of storms in January and February, 2017.

Shallow landslides damaged homes and closed many roads in the San Francisco East Bay region as a result of storms in January and February, 2017.

landslide destruction to the exterior of a home in King County, WA
Home damaged by rainfall-triggered debris flow - King County, Washington
Home damaged by rainfall-triggered debris flow - King County, Washington
Home damaged by rainfall-triggered debris flow - King County, Washington

Landslide caused by intense rainfall in February 2017 in King County, WA. The rapid landslide destroyed a garage and a large propane tank. 

view of Salt Creek rock avalanche in Western Colorado from the top
Salt Creek Rock Avalanche in Western Colorado
Salt Creek Rock Avalanche in Western Colorado
Salt Creek Rock Avalanche in Western Colorado

Photograph taken from a Colorado National Guard helicopter looking north down the West Salt Creek rock avalanche deposit. On May 25, 2014, the central core of the rock avalanche deposit continued to move for 1-2 hours after the main rock avalanche deposit had stopped moving.

Photograph taken from a Colorado National Guard helicopter looking north down the West Salt Creek rock avalanche deposit. On May 25, 2014, the central core of the rock avalanche deposit continued to move for 1-2 hours after the main rock avalanche deposit had stopped moving.

Home with large crack in foundation
Slow landslide building damage - Boyd County, Kentucky
Slow landslide building damage - Boyd County, Kentucky
Slow landslide building damage - Boyd County, Kentucky

Building damage caused by a slow landslide in Boyd County, Kentucky. Previous repairs reveal that the landslide has moved in the past. 

Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.
Geomagnetism Fredericksburg
Geomagnetism Fredericksburg
Geomagnetism Fredericksburg

Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.

landslide
Catastrophic landslide near Oso, WA, Mar. 22, 2014.
Catastrophic landslide near Oso, WA, Mar. 22, 2014.
large crack in ground in forested area
Potential landslide indicator - Snohomish County, Washington
Potential landslide indicator - Snohomish County, Washington
Potential landslide indicator - Snohomish County, Washington

Cracks on a gravel road formed during the reactivation of a slow, deep landslide. The cracks can be indicators of local movement in or around the road or in this case, are a sign of a much larger landslide. 

Cracks on a gravel road formed during the reactivation of a slow, deep landslide. The cracks can be indicators of local movement in or around the road or in this case, are a sign of a much larger landslide. 

large crack in residential yard
Potential landslide indicator - Island County, Washington
Potential landslide indicator - Island County, Washington
Potential landslide indicator - Island County, Washington

Large cracks formed in this yard after a large landslide occurred downslope of a home. Though the home wasn't directly impacted by the landslide, the cracks in the yard are indicators of potential additional movement and increased landslide risk.

Large cracks formed in this yard after a large landslide occurred downslope of a home. Though the home wasn't directly impacted by the landslide, the cracks in the yard are indicators of potential additional movement and increased landslide risk.

two cracks on a gravel slope in residential yard
Potential landslide indicator - Island County, Washington
Potential landslide indicator - Island County, Washington
Potential landslide indicator - Island County, Washington

Cracks on a gravel road formed during the initial movement of a slow, deep landslide. The cracks can be indicators of local movement in or around the road or in this case, a much larger landslide and damaged many homes. 

Cracks on a gravel road formed during the initial movement of a slow, deep landslide. The cracks can be indicators of local movement in or around the road or in this case, a much larger landslide and damaged many homes. 

severe damage to home foundation, homes built on landslide
Home damaged by debris flow - Island County, Washington
Home damaged by debris flow - Island County, Washington
Home damaged by debris flow - Island County, Washington

A reactivated landslide destroyed this home that was built on the landslide. Initial, slow landslide movement allowed the occupant to escape. Island County, WA. March 2013

Data logger suspended above a channel with a person pointing up at it from the bottom of the channel
Millicoma Meander study basin
Millicoma Meander study basin
Millicoma Meander study basin

Photograph of the channel station showing the laser distance meter (in red circle) high above the channel used to measure stage (height) of flow in the channel.

Photograph of the channel station showing the laser distance meter (in red circle) high above the channel used to measure stage (height) of flow in the channel.

Top: The global tectonic regions modified from García et al. (2012), with each region shown in a different color. Bottom: The productivity parameter (a-value) and temporal decay parameter (p-value) for each global tectonic regime shown as a “+” with uncertainty shown by the line of matching color. Figures from Page et al. (2016).
fig5-aftershock.gif
fig5-aftershock.gif
fig5-aftershock.gif

Top: The global tectonic regions modified from García et al. (2012), with each region shown in a different color. Bottom: The productivity parameter (a-value) and temporal decay parameter (p-value) for each global tectonic regime shown as a “+” with uncertainty shown by the line of matching color. Figures from Page et al. (2016).

Top: The global tectonic regions modified from García et al. (2012), with each region shown in a different color. Bottom: The productivity parameter (a-value) and temporal decay parameter (p-value) for each global tectonic regime shown as a “+” with uncertainty shown by the line of matching color. Figures from Page et al. (2016).

Toe of the active Cleveland Corral landslide in 2011
Cleveland Corral landslide in 2011
Cleveland Corral landslide in 2011
Cleveland Corral landslide in 2011

Toe of the active Cleveland Corral landslide in 2011, perched above US Highway 50 in distance.  Movement typically only occurs during wet winter and spring months.

Toe of the active Cleveland Corral landslide in 2011, perched above US Highway 50 in distance.  Movement typically only occurs during wet winter and spring months.

Azimuth mark, Absolutes building and Coil building at Boulder magnetic observatory.
Boulder Magnetic Observatory
Boulder Magnetic Observatory
Boulder Magnetic Observatory

Azimuth mark, Absolutes building and Coil building at Boulder magnetic observatory.

The Boulder magnetic observatory. Variations and Proton Sensor buildings at the lower right.
Boulder Magnetic Observatory
Boulder Magnetic Observatory
Boulder Magnetic Observatory

The Boulder magnetic observatory. Variations and Proton Sensor buildings at the lower right.

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