Stress magnitudes for the East Flank derived from measurements in wells

Active Tectonics at UC Berkeley

Frontiers A multi-proxy approach to detect the pore pressure and

Frontiers Stability Analysis of a Landslide Scarp by Means of

Determination of stress orientation and magnitude in deep wells

Characterization of in-situ stresses and its implications for

A) Location of the sites of structural measurements performed

Stephen HICKMAN, Research Geophysicist, PhD, United States Geological Survey, Colorado, USGS, Earthquake Science Center, Moffett Field CA

Determination of stress orientation and magnitude in deep wells

Stress magnitudes for the East Flank derived from measurements in

Characterization of in-situ stresses and its implications for

Extensive freshened groundwater resources emplaced during the