Damage to a village house. Longmenxiang.
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Damage to a village house. Longmenxiang.
Damage to a village house. Longmenxiang.
Damage to a village house. Longmenxiang.
Damage to a village house. Longmenxiang.
Damage to a village house. Longmenxiang.
Damage to a village house. Longmenxiang.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Damage to local stores in downtown Lushan.
Life in a tent. Two kids singing and playing among the tents.
Life in a tent. Two kids singing and playing among the tents.
Oilfield waste arrives by tanker truck at a wastewater disposal facility near Platteville, Colo. After removal of solids and oil, the wastewater is injected into a deep well for permanent storage underground. This disposal process has the potential to trigger earthquakes, but very few wastewater disposal wells produce earthquakes.
Oilfield waste arrives by tanker truck at a wastewater disposal facility near Platteville, Colo. After removal of solids and oil, the wastewater is injected into a deep well for permanent storage underground. This disposal process has the potential to trigger earthquakes, but very few wastewater disposal wells produce earthquakes.
Oilfield waste arrives by tanker truck at a wastewater disposal facility near Platteville, Colo. After removal of solids and oil, the wastewater is injected into a deep well for permanent storage underground. This disposal process has the potential to trigger earthquakes, but very few wastewater disposal wells produce earthquakes.
Oilfield waste arrives by tanker truck at a wastewater disposal facility near Platteville, Colo. After removal of solids and oil, the wastewater is injected into a deep well for permanent storage underground. This disposal process has the potential to trigger earthquakes, but very few wastewater disposal wells produce earthquakes.
USGS geophysicist Steve Snyder is measuring gravity, for information on geology beneath the surface, and the GPS location of this measurement in the earthquake area.
USGS geophysicist Steve Snyder is measuring gravity, for information on geology beneath the surface, and the GPS location of this measurement in the earthquake area.
USGS geoscientists Wright Horton, Richard Harrison, and Anjana Shah (left to right) are studying an exploratory trench for possible earthquake-related deformation.
USGS geoscientists Wright Horton, Richard Harrison, and Anjana Shah (left to right) are studying an exploratory trench for possible earthquake-related deformation.
House damage in central Oklahoma from the magnitude 5.6 earthquake on Nov. 6, 2011. Research conducted by USGS geophysicist Elizabeth Cochran and her university-based colleagues suggests that this earthquake was induced by injection into deep disposal wells in the Wilzetta North field.
House damage in central Oklahoma from the magnitude 5.6 earthquake on Nov. 6, 2011. Research conducted by USGS geophysicist Elizabeth Cochran and her university-based colleagues suggests that this earthquake was induced by injection into deep disposal wells in the Wilzetta North field.
USGS geologist Ed Harp photographing a small rock fall from a road cut along the Blue Ridge Parkway north of Roanoke, Virginia. This is part of a study documenting landslides triggered from the 2011 magnitude 5.8 earthquake in Virginia. Green grass beneath the rock fragments indicates that the rock fall is fresh and probably was triggered by the earthquake
USGS geologist Ed Harp photographing a small rock fall from a road cut along the Blue Ridge Parkway north of Roanoke, Virginia. This is part of a study documenting landslides triggered from the 2011 magnitude 5.8 earthquake in Virginia. Green grass beneath the rock fragments indicates that the rock fall is fresh and probably was triggered by the earthquake
Photo of chimney damage at a house in Louisa County, Virginia. This was a result from a magnitude 5.8 earthquake in Virginia on August 23, 2011.
Photo of chimney damage at a house in Louisa County, Virginia. This was a result from a magnitude 5.8 earthquake in Virginia on August 23, 2011.
Scientists from the USGS and the University of Rhode Island examine coastal sediment on Simeonof Island for evidence of sudden land-level change caused by earthquakes on the Aleutian megathrust.
Scientists from the USGS and the University of Rhode Island examine coastal sediment on Simeonof Island for evidence of sudden land-level change caused by earthquakes on the Aleutian megathrust.
Scientists from the USGS, University of Rhode Island, and the Alaska Dept of Geological and Geophysical Surveys dig into coastal bluffs of Simeonof Island in search of evidence for ancient beach deposits and tectonically uplifted shorelines.
Scientists from the USGS, University of Rhode Island, and the Alaska Dept of Geological and Geophysical Surveys dig into coastal bluffs of Simeonof Island in search of evidence for ancient beach deposits and tectonically uplifted shorelines.
Scientists from the USGS, University of Rhode Island, and the Alaska Dept of Geological and Geophysical Surveys use a hand-driven corer to sample soils and marsh sediment on Simeonof Island as part of an investigation to investigate evidence for earthquakes and tsunamis in the Shumagin Islands.
Scientists from the USGS, University of Rhode Island, and the Alaska Dept of Geological and Geophysical Surveys use a hand-driven corer to sample soils and marsh sediment on Simeonof Island as part of an investigation to investigate evidence for earthquakes and tsunamis in the Shumagin Islands.
Starting around July 10, 2013, an airplane operating under contract to the USGS will be making low-level flights over a 1400-square-mile area in the New Madrid Seismic Zone. This airplane is a Cessna-180, specially modified for low-altitude geophysical surveys.
Starting around July 10, 2013, an airplane operating under contract to the USGS will be making low-level flights over a 1400-square-mile area in the New Madrid Seismic Zone. This airplane is a Cessna-180, specially modified for low-altitude geophysical surveys.
Fractures along Superstition Hills Fault formed in response to the 2010 El Mayor-Cucapah earthquake. Black arrows mark matches across en echelon fractures. Centimeter rule for scale.
Fractures along Superstition Hills Fault formed in response to the 2010 El Mayor-Cucapah earthquake. Black arrows mark matches across en echelon fractures. Centimeter rule for scale.
Damage to structures in downtown Concepcion, Chile, due to the February 27, 2010 magnitude 8.8 earthquake.
Damage to structures in downtown Concepcion, Chile, due to the February 27, 2010 magnitude 8.8 earthquake.