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Earthquake Research

Parkfield Earthquake Experiment

Earthquake Team Seminars Series

3D Geologic and Seismic Velocity Model of SF Bay Region

Borehole Geophysics and Rock Mechanics

Crustal Deformation

Crustal Structure

Geology

Seismology

Strong Motion Seismology


Software for Download


External Research Program

Access to Earthquake Data

 
physics.jpg 3D Geologic and Seismic Velocity Model of the San Francisco Bay Region
A 3D model of faults and geologic rock units in the San Francisco Bay region is being used to construct a velocity model for seismic waves as they travel under the region. Seismic waves can be propagated through this velocity model to predict the shaking effects of future earthquake at various sites depending and to explore the dependence on soil conditions under given sites.
physics.jpg Borehole Geophysics and Rock Mechanics
Using borehole geophysical measurements in conjunction with laboratory studies, scientists study heat flow, stress, fluid pressure, and the mechanical behavior of fault-zone materials at seismogenic depths to yield improved models of the earthquake cycle.
deformation.jpg Crustal Deformation
Plate motion produces distortion or deformation in the surface of the earth near active faults. Several techniques are used to measure this deformation, including GPS, 2-color Electronic Distance Meters (EDMs), strain meters, magnetometers, tilt meters, and water level monitors.
structure.jpg Crustal Structure
Geophysicists use refraction and reflection techniques (usually involving explosion-generated seismic waves) to learn about the material structure of the Earth's crust (its density, wave propagation speeds, thickness, layering and faulting).
geology.jpg Geology
Geologists learn about future earthquakes by looking at evidence left behind by past earthquakes, such as fault traces (the "footprints" of fault motion at the Earth's surface), offset natural and man-made features (which mark relative movement across a fault), and the disruption of sedimentary layers (as revealed in trenches).
seismology.gif Seismology
The locations of earthquakes reveal where active faults are located and where faults may be "locked." Studies of the waves from these earthquakes help map the structure of the Earth's crust, the orientation of stresses in it, and the movement of the faults within it.
strongmo.gif Strong Motion Seismology
Near large earthquakes, seismic waves have large amplitudes. Studying this strong shaking requires specialized sensors and produces information used in developing building codes and in designing earthquake-resistant structures such as buildings, bridges, and highways.

Earthquake Hazards Program: Project Proposals
Current research activities supported by the USGS Earthquake Hazards Program.

External Research Program
The USGS invites research proposals that will assist in achieving the goals of the National Earthquake Hazards Reduction Program (NERHP)

Access to Earthquake Data
Links to numerous government agencies and non-government organizations that provide earthquake data.