Due to a lapse in appropriations, the majority of USGS websites may not be up to date and may not reflect current conditions. Websites displaying real-time data, such as Earthquake and Water and information needed for public health and safety will be updated with limited support. Additionally, USGS will not be able to respond to inquiries until appropriations are enacted. For more information, please see www.doi.gov/shutdown
EarthWord – Induced Seismicity
The occurrence or frequency of earthquakes for which the origin is attributable to human activities.
EarthWords is an on-going series in which we shed some light on the complicated, often difficult-to-pronounce language of science. Think of us as your terminology tour-guides, and meet us back here every week for a new word!
- The occurrence or frequency of earthquakes for which the origin is attributable to human activities.
- Seismos – comes from the Greek for “earthquake”; and induce – to cause (something) to happen or exist.
Use/Significance in the Earth Science Community:
- Induced seismicity refers to non-tectonic (i.e., non-natural) earthquakes that result from human activities that alter the stresses and strains on the Earth’s crust. There are many activities that can cause induced earthquakes including: wastewater disposal, mining, development of artificial lakes, extraction of fossil fuels, extraction of groundwater, development of geothermal energy, hydraulic fracturing, and subsurface storage of CO2.
- The USGS studies induced seismicity to assess earthquake hazards. A particular focus has been the central and eastern U.S., where the number of earthquakes has increased dramatically since 2008. Recent studies have shown that the seismicity in many of these locations is induced by the deep injection of fluids from nearby oil and gas operations. Because USGS periodically issues earthquake hazard assessments for the Nation, our assessments must include this increasingly significant induced hazard. Additionally, USGS is conducting research to determine why some waste water injection sites are susceptible to induced earthquakes, while the vast majority of sites are not. Research aimed at understanding the processes that control the location, rate, and size of induced seismicity will allow humans to mitigate the occurrence of induced earthquakes in the future.
Next EarthWord: This EarthWord shows where water goes after it goes to ground.
Hungry for some science, but you don’t have time for a full-course research plate? Then check out USGS Science Snippets, our snack-sized science series that focuses on the fun, weird, and fascinating stories of USGS science.