SCSN - The Southern California Seismic Network

1921 through 1931 could be considered the “pre-history” of the Seismological Laboratory, which originally belonged to the Carnegie Institute and not Caltech. Instruments for recording of local earthquakes (such as the Wood-Anderson torsion seismometer and the Benioff short-period instruments) were designed, fabricated, and installed at a few sites ( Pasadena and Riverside, for example). In 1926, the Seismological Laboratory became affiliated with the new geology department at California Institute of Technology. By 1931, seismographic stations existed at six locations (PAS, RVR, SBC, TIN, HAI & LJC), which allowed the location of most earthquakes over 3.0 in most areas of Southern California.
"The Fathers of Seismology" Early photo of Caltech Seismo Lab scientists. L to R - Frank Press, Beno Gutenburg, Hugo Benioff, and Charles Richter Photo © 2004, California Institute of Technology Dr. Charles F. Richter Photo © 2004, California Institute of Technology	1932 through 1971 could be called the era of the Caltech Seismic Network. The number of instrumented stations increased slowly, with distinct growth spurts after the 1933 Long Beach earthquake (Mw6.4), 1952 Kern County earthquake (Mw7.5), and the 1971 San Fernando earthquake (Mw6.7). Most recording still occurred photographically, at the station. Data from some stations were telemetered to Caltech beginning in about 1966. 1972 through 1976 is the period when the cooperative network with the U.S. Geological Survey was formed. It could also be called the era of analog (via telephone land line) telemetry. 1977 through approximately 1990 is still the era of analog telemetry, but data were digitized upon their arrival at Caltech and processed by real-time computer systems (using the CEDAR and CUSP software). 1991 through 2000 was the beginning of the era of broadband seismometers and digital telemetry. Although most signals were still transmitted in their analog form (now by mostly by radio and/or microwave) and digitized on their was into the computers, some stations were replace or supplemented by modern equipment under the TriNet program. Data processing was still using the CUSP system. After 1992 there were no more photographically recorded signals. 2001 through present is the modern digital, broad-band network. The 96 analog stations that we still have are digitized by “earthworm hubs” either in the field or at Caltech, before processing by our real-time systems.

1921 through 1931 could be considered the “pre-history” of the Seismological Laboratory, which originally belonged to the Carnegie Institute and not Caltech. Instruments for recording of local earthquakes (such as the Wood-Anderson torsion seismometer and the Benioff short-period instruments) were designed, fabricated, and installed at a few sites ( Pasadena and Riverside, for example). In 1926, the Seismological Laboratory became affiliated with the new geology department at California Institute of Technology. By 1931, seismographic stations existed at six locations (PAS, RVR, SBC, TIN, HAI & LJC), which allowed the location of most earthquakes over 3.0 in most areas of Southern California.

"The Fathers of Seismology"

Early photo of Caltech Seismo Lab scientists. L to R - Frank Press, Beno Gutenburg, Hugo Benioff, and Charles Richter

Dr. Charles F. Richter

1932 through 1971 could be called the era of the Caltech Seismic Network. The number of instrumented stations increased slowly, with distinct growth spurts after the 1933 Long Beach earthquake (Mw6.4), 1952 Kern County earthquake (Mw7.5), and the 1971 San Fernando earthquake (Mw6.7). Most recording still occurred photographically, at the station. Data from some stations were telemetered to Caltech beginning in about 1966.

1972 through 1976 is the period when the cooperative network with the U.S. Geological Survey was formed. It could also be called the era of analog (via telephone land line) telemetry.

1977 through approximately 1990 is still the era of analog telemetry, but data were digitized upon their arrival at Caltech and processed by real-time computer systems (using the CEDAR and CUSP software).

1991 through 2000 was the beginning of the era of broadband seismometers and digital telemetry. Although most signals were still transmitted in their analog form (now by mostly by radio and/or microwave) and digitized on their was into the computers, some stations were replace or supplemented by modern equipment under the TriNet program. Data processing was still using the CUSP system. After 1992 there were no more photographically recorded signals.

2001 through present is the modern digital, broad-band network. The 96 analog stations that we still have are digitized by “earthworm hubs” either in the field or at Caltech, before processing by our real-time systems.


	Web www.scsn.org