Slow landslide building damage - Boyd County, Kentucky
Slow landslide building damage - Boyd County, KentuckyBuilding damage caused by a slow landslide in Boyd County, Kentucky, 2017
An official website of the United States government
Here's how you know
Official websites use .gov
A .gov website belongs to an official government organization in the United States.
Secure .gov websites use HTTPS
A lock () or https:// means you’ve safely connected to the .gov website. Share sensitive information only on official, secure websites.
Geologic Hazards Science Center images.
Building damage caused by a slow landslide in Boyd County, Kentucky, 2017
Building damage caused by a slow landslide in Boyd County, Kentucky, 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.
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 caused by intense rainfall in February 2017 in King County, WA. The rapid landslide destroyed a garage and a large propane tank.
Landslide caused by intense rainfall in February 2017 in King County, WA. The rapid landslide destroyed a garage and a large propane tank.
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.
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.
Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.
Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.
More signs for Fredericksburg Magnetic Observatory.
More signs for Fredericksburg Magnetic Observatory.
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.