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Geologic Hazards Science Center images.

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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.

Electronics building at Sitka magnetic observatory Alaska.
Geomagnetism Sitka
Geomagnetism Sitka
Geomagnetism Sitka

Electronics building at Sitka magnetic observatory Alaska.

Image of the hillside and where each station is set up there at Knife Ridge
Knife Ridge station locations
Knife Ridge station locations
Knife Ridge station locations

Oblique photograph of Knife Ridge monitoring site showing approximate soil pit locations.

Zeiss Jena 010B Theodolite for making absolute measurements at Boulder magnetic observatory.
Boulder Magnetic Observatory
Boulder Magnetic Observatory
Boulder Magnetic Observatory

Zeiss Jena 010B Theodolite for making absolute measurements at Boulder magnetic observatory.

Set up of Station 1 in Chalk Cliffs with view up-channel
Station 1
Station 1
Station 1

The Upper monitoring station at Chalk Cliffs, CO.

The Upper monitoring station at Chalk Cliffs, CO.

Chalk Cliffs in the background showing view from video camera towards station 1.
Chalk Cliffs view of Station 1
Chalk Cliffs view of Station 1
Chalk Cliffs view of Station 1

View of the west channel and Upper monitoring station (Station 1), Chalk Cliffs, CO.

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