JPL
Careers
Education
Science & Technology
JPL Logo
JPL Logo
Image

Computer Model Estimates Permanent Ground Motions from the Aug. 23, 2011 Magnitude 5.8 Virginia Earthquake

Jet Propulsion Laboratory https://www.jpl.nasa.gov/ Aug. 24, 2011
A magnitude 5.8 earthquake in Mineral, Va. was widely felt up and down the East Coast of the United States. This computer model is a QuakeSim model image overlaid on a Google Earth image.

The Aug. 23, 2011, magnitude 5.8 earthquake in Mineral, Va., was widely felt up and down the East Coast of the United States. Earthquakes are caused when a fault -- a fracture in a volume of rock in Earth's crust -- breaks and its two sides slip past each other in opposite directions. This sudden slip produces shaking that can be widely felt. However, that slip also causes permanent ground movements that can be measured as motion of Earth's surface. GPS and radar technology can be used to measure these motions if they are greater than about 1/16 to 1/8 inch. The Aug. 23 earthquake was not observed by GPS or Interferometric Synthetic Aperture Radar (InSAR), but computer models can predict the permanent ground displacements that are likely to occur from such an earthquake. The earthquake was widely felt in Washington, D.C. and resulted in the evacuation of numerous buildings; however, the total permanent movement of the city from this earthquake is estimated to be only about 0.02 inches to the northwest and downwards. The area near Mineral, Va., probably moved closer to a maximum of 2.8 inches northwest and upward in a dome extending out from the quake's epicenter about 10 miles northeasterly across and 5 miles wide. Both GPS and InSAR require data to be collected both before and after an earthquake. GPS measures exact positions of points on the ground. InSAR produces an image of deformation across a region. The computer model was generated under NASA's QuakeSim project, a computational framework for modeling and understanding earthquake and tectonic processes. QuakeSim focuses on deformation of Earth's crust, which can be measured using airborne and spaceborne technologies. The models and data can be used to better understand earthquake hazard, stress transfer between faults, and ground disturbance following earthquakes.

QuakeSim, a collaboration of JPL-Caltech, USC, UC Davis, UC Irvine, Indiana University, and NASA Ames, is sponsored by NASA's Advanced Information Systems Technology Program through the Earth Science Technology Office.

Download JPG
Download TIFF
Target
  • Earth
Credit
NASA/JPL-Caltech/Google

Keep Exploring

About JPL
Who We Are
Directors
Careers
Internships
The JPL Story
JPL Achievements
Documentary Series
JPL Annual Report
Executive Council
Missions
Current
Past
Future
All
News
All
Earth
Solar System
Stars and Galaxies
Eyes on the News
Subscribe to JPL News
Galleries
Images
Videos
Audio
Podcasts
Apps
Visions of the Future
Slice of History
Robotics at JPL
Events
Lecture Series
Speakers Bureau
Calendar
Visit
Public Tours
Virtual Tour
Directions and Maps
Topics
JPL Life
Solar System
Mars
Earth
Climate Change
Exoplanets
Stars and Galaxies
Robotics
More
Asteroid Watch
NASA's Eyes Visualizations
Universe - Internal Newsletter
Social Media
Accessibility at NASA
Contact Us
Get the Latest from JPL
Follow Us

JPL is a federally funded research and development center managed for NASA by Caltech.

More from JPL
Careers
Education
Science & Technology
Acquisition
JPL Store
Careers
Education
Science & Technology
Acquisition
JPL Store
Related NASA Sites
Basics of Spaceflight
NASA Kids Science - Earth
Earth / Global Climate Change
Exoplanet Exploration
Mars Exploration
Solar System Exploration
Space Place
NASA's Eyes Visualization Project
Voyager Interstellar Mission
NASA
Caltech
Privacy
Image Policy
FAQ
Feedback
Version: v3.1.3 - 5e83a9a
Site Managers:Emilee Richardson, Alicia Cermak
Site Editors:Naomi Hartono, Steve Carney
CL#:21-0018