Slow landslide building damage - Boyd County, Kentucky
Slow landslide building damage - Boyd County, KentuckyBuilding damage caused by a slow landslide in Boyd County, Kentucky. Previous repairs reveal that the landslide has moved in the past.
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Geologic Hazards Science Center images.
Building damage caused by a slow landslide in Boyd County, Kentucky. Previous repairs reveal that the landslide has moved in the past.
Building damage caused by a slow landslide in Boyd County, Kentucky. Previous repairs reveal that the landslide has moved in the past.
More signs for Fredericksburg Magnetic Observatory.
More signs for Fredericksburg Magnetic Observatory.
Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.
Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.
A landslide caused by heavy rainfall in April 2014 destroyed a building in Carroll County, KY.
A landslide caused by heavy rainfall in April 2014 destroyed a building in Carroll County, KY.
Aerial photograph of catastrophic landslide that occurred near Oso, Washington, March 22, 2014.
Aerial photograph of catastrophic landslide that occurred near Oso, Washington, March 22, 2014.
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 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.
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.
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
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
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.
Mt. Rainier with research boat in foreground on lake, Mt. Rainier NP
Mt. Rainier with research boat in foreground on lake, Mt. Rainier NP
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, 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.
Shumagin Magnetic Observatory sign.
Shumagin Magnetic Observatory sign.
Azimuth mark, Absolutes building and Coil building at 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.
The Boulder magnetic observatory. Variations and Proton Sensor buildings at the lower right.
Electronics building at Sitka magnetic observatory Alaska.
Electronics building at Sitka magnetic observatory Alaska.
Oblique photograph of Knife Ridge monitoring site showing approximate soil pit 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.
Zeiss Jena 010B Theodolite for making absolute measurements at Boulder magnetic observatory.
The Upper monitoring station at Chalk Cliffs, CO.
The Upper monitoring station at Chalk Cliffs, CO.
View of the west channel and Upper monitoring station (Station 1), Chalk Cliffs, CO.
View of the west channel and Upper monitoring station (Station 1), Chalk Cliffs, CO.