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Charles
Richter, originally trained as a theoretical geophysicist, joined the
staff of the Seismo Lab in 1927. Beno Gutenberg, a renowned German geophysicist,
joined the geology division of Caltech in 1930, and became the Lab's first
director.
Richter
and Gutenberg’s collaboration led to several important studies,
of which the most well-known is the magnitude scale. The Richter Scale
was initially used by Richter and later expanded by Gutenberg.
In the early 1930s, two Caltech scientists—physicist Charles Richter and mathematician Beno Gutenberg—played a pivotal role in developing seismology into an international science of earthquake study and detection.
(to
the top)
Responsibility for the Seismo Lab, its programs, and most of its personnel was transferred to Caltech in 1937. Gutenberg and his colleagues—Hugo Benioff, John Buwalda, Richter, and others—led the Seismological Laboratory to worldwide prominence in the study of local earthquakes and, equally important, in the use of teleseismic recordings to study the Earth’s deep interior.
John
Buwalda came to Caltech in 1926 to organize the Division of Geological
Sciences. He assembled the staff, worked out the instruction and research
programs in geology, paleontology, and geophysics, and supervised the
design and construction of the Charles Arms and Seeley W. Mudd laboratories
on campus. In addition to teaching, he had a distinguished career as a
consulting geologist.
Frank Press, who later was to become the director of the Office of Science and Technology Policy in Washington as well as president of the National Academy of Sciences, became the Seismo Lab’s director in 1957. Press was largely responsible for developing innovative quantitative approaches to seismology and in making the laboratory heavily computer-based. In
1974, during the directorship of Don Anderson, the Seismo Lab moved from
its original location at Kresge to its current location on campus in South
Mudd. By this time, the lab’s seismic network included 30 stations.
At
the same time, the Seismo Lab and the United States Geological Survey
(USGS) began a cooperative program that developed into the Southern California
Seismic Network (SCSN).
The Seismological
Laboratory at Caltech has a long tradition in earthquake science and is
actively involved in the California Integrated Seismic Network (CISN)—one
of the most advanced seismographic networks in the world. The Lab today
continues to build on its tradition of geophysical study, and is a modern
geophysical observatory that emphasizes the acquisition, analysis, and modeling
of data pertaining to the structure and dynamics of the earth and other
planetary bodies. This data originates from many sources, including regional
and global seismic networks, inhouse analytic facilities (e.g., the Lindhurst
Laboratory of Experimental Geophysics ), oceanic research cruises, remote
sensing (e.g., GPS, interferometric radar, Landsat etc.), and geologic field
mapping. Current Seismo Lab research incorporates all aspects of geophysics
including, but not limited to, the structure, chemistry, and convective
flow of the earth's interior, the physics of earthquakes, oceanic and continental
tectonics, and lithospheric deformation. (to
the top)
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Modified:
14-Jan-2004
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