Crustal Deformation

Monitoring crustal deformation in Parkfield, CA.

As a consequence of continental plate movement, the Earth's surface near active faults deforms before, during and after earthquakes. Similarly, the ground surface near active volcanoes also deforms as a consequence of eruptions and volcano evolution. Crustal deformation can be observed as relative movement of points on the Earth's surface, ground tilt, ground strain, and fault slip (creep). We routinely measure these and other parameters that reflect this deformation.