by Brad Aagaard, USGS Research Geophysicist
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Ground shaking is the primary cause of earthquake damage to man-made structures. Many factors influence the strength of earthquake shaking at a site including the earthquake's magnitude, the site's proximity to the fault, the local geology, and the soil type.
More than 250 structures throughout the United States have been outfitted with seismic sensors by the USGS National Strong Motion Project (NSMP) to improve the overall understanding of earthquakes and their effects on the built environment.
The instrumentation and monitoring of structures by NSMP is only one part of USGS efforts to protect people’s lives and property from earthquake hazards in all of the Nation’s seismically active regions.
Learn more: Multidisciplinary Center for Earthquake Engineering Research
by Brad Aagaard, USGS Research Geophysicist
by Brad Aagaard, USGS Research Geophysicist
Building damanged by the February 2011 earthquake in Christchurch, New Zealand.
Building damanged by the February 2011 earthquake in Christchurch, New Zealand.
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.
Civilians on road alongside severely damaged residential buildings in Mianyang.
Civilians on road alongside severely damaged residential buildings in Mianyang.
A downtown building at the corner of Alice and 13th Streets lost part of its unreinforced facade and brick masonry.
A downtown building at the corner of Alice and 13th Streets lost part of its unreinforced facade and brick masonry.
by Brad Aagaard, USGS Research Geophysicist
by Brad Aagaard, USGS Research Geophysicist
Building damanged by the February 2011 earthquake in Christchurch, New Zealand.
Building damanged by the February 2011 earthquake in Christchurch, New Zealand.
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.
Civilians on road alongside severely damaged residential buildings in Mianyang.
Civilians on road alongside severely damaged residential buildings in Mianyang.
A downtown building at the corner of Alice and 13th Streets lost part of its unreinforced facade and brick masonry.
A downtown building at the corner of Alice and 13th Streets lost part of its unreinforced facade and brick masonry.