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 About the
Company
Jim Humphrey
Vice President
Mr. Humphrey is a founding principal and senior scientist at Lahontan
GeoScience. He specializes in environmental geology and seismic hazard assessment. Mr.
Humphrey received his Bachelor of Science Degree in Geology in 1980 from the University of
California at Davis. 1980, Mr. Humphrey joined Woodward-Clyde Consultants, an
internationally known engineering consulting firm. In 1989, Mr. Humphrey returned to
graduate school at the University of Nevada, Reno (UNR), to study site amplification
effects of large earthquakes. His research contributions include over 25 papers and
abstracts published in professional journals. Mr. Humphrey left UNR in 1994 to become a
founding principal at Lahontan GeoScience, Inc.
Mr. Humphrey has twenty years of professional experience in the
fields of engineering seismology and seismic hazard analysis. He specializes in seismic
data acquisition, regional and local seismicity evaluation, site-specific ground motion
estimation, and analysis of induced seismicity (both reservoir and mining induced). His
project experience typically involves integration of geologic and seismologic data to
assess seismic hazard and development of design ground motions for site-specific dynamic
analysis. Recently Lahontan GeoScience and William Lettis and Associates teamed to
evaluate seismic hazards for the Almanor and Butt Valley dams in the northern Sierra
Nevada for Pacific Gas & Electric. Mr.
Humphrey integrated the historical and instrumental earthquake data to compile a
seismicity catalog for the northern Sierra Nevada and northeastern Sacramento Valley, and
evaluated the occurrence, style and rate of seismic activity in the study region.
Mr. Humphrey has
extensively investigated the seismologic characteristics of large subduction zone
earthquakes including the 1985 M 8.1 Michoacan, Mexico, and the 1985 M 8 Valparaiso,
Chile, earthquakes to determine factors influencing site-specific seismic response.
Near-field ground motions were simulated using a stochastic, random vibration theory
based, finite-source model which incorporates the effects of dynamic and geometrical
properties of source rupture, crustal wave propagation, and site-specific response. These
projects provided a way to validate numerical models of earthquake source and seismic
energy propagation to enable estimation of ground motion from a postulated Cascadia
subduction zone earthquake in the seismic hazard evaluation for several critical
structures in Oregon, including the Trojan nuclear power plant.
Mr. Humphrey has been involved in several projects to evaluate
induced seismicity either due to reservoir loading or mining activities. These projects
usually involve data acquisition on site, analysis of seismic waveforms to differentiate
between tectonic and induced or triggered earthquakes, and determining the impact of a
maximum event.
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