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Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

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MICROFILMINGHISTORICAL SEISMOGRAMS ATABUYAMA SEISMOLOGICAL OBSERVATORY,KYOTO UNIVERSITYYasuhiro Umeda and Katsuyoshi It0Abuyama Seismological Observatory, Kyoto University944 Nasahara Takatsuki, Osaka 569, Japan1. History of Seismological ObservationsAbuyama Seismological Observatory of <strong>the</strong> Faculty of Science, Kyoto University,was established in 1930. In <strong>the</strong> previous year, <strong>the</strong> experimental seismologicalobservations began with a two-component horizontal Wiechert seismograph. Continuousobservation with a three-component Wiechert seismograph began in 1932.The Wiechert seismograph is an excellent instrument which has a response of relativelylong-period and high-gain. In those days, many good records were obtained.However, for <strong>the</strong> moderate and large earthquakes occurring in and around Japan,<strong>the</strong> instrument is unstable because of its complex structure.In 1934, two types of strong-motion seismographs were designed and operated by<strong>the</strong> staff of our observatory. One of <strong>the</strong>m is a set of long-period (To = 24 - 27 sec),low-magnification (V = 1.1) two-component horizontal seismographs. The lengthof <strong>the</strong> pendulum is 1.7 m, and <strong>the</strong> recording stroke is about 30 cm. This instrumenthas recorded destructive earthquakes occurring near <strong>the</strong> Abuyama Observatoryand great earthquakes such as <strong>the</strong> 1960 Chile and <strong>the</strong> 1964 Alaska earthquakes.The o<strong>the</strong>r instrument is a set of short-period (To = 1.4 - 6.0 sec), strong-motion(V = 5 - 15) three-component seismographs. Those two sets of seismographs constitute<strong>the</strong> low-gain broad-band seismograph system.<strong>Historical</strong> seismograms have been obtained mainly using <strong>the</strong> above three kindsof seismographs. The Wiechert seismograms are recorded daily and saved, but <strong>the</strong>seismograms of <strong>the</strong> latter two sets of instruments are saved only when events arerecorded.2. Microfilming in <strong>the</strong> First StageIn response to <strong>the</strong> resolutions of <strong>the</strong> 1982 Tokyo Workshop on <strong>Historical</strong> <strong>Seismograms</strong>,we began preliminary work in preparation for microfilming. On one handwe applied for financial support, and on <strong>the</strong> o<strong>the</strong>r hand we arranged our archivedseismograms in chronological order and listed all missing records. In 1984, this microfilmingproject was supported by <strong>the</strong> Science Research Fund of <strong>the</strong> Ministry ofEducation of Japan. Because this support will continue until March 1987, we havemade a three-year plan for <strong>the</strong> microfilming project as shown in Figure 1.In <strong>the</strong> first fiscal year (<strong>from</strong> April 1984 to March 1985), 20,346 sheets of Wiechertseismograms were arranged and filmed on 30 rolls of microfilm. An average of 500frames are filmed on one roll 30.5 m long. The total number of frames is 14,196.3. Filming FormatEvery roll of film is kept in a small box. The roll number, <strong>the</strong> kind of instrument,and <strong>the</strong> dates of <strong>the</strong> records are given on <strong>the</strong> face of this box.<strong>Historical</strong> <strong>Seismograms</strong>and Earthquakes of <strong>the</strong> World439Copyright 0 198h by Academic Press, Inc.All rights of reproduction in any form reserved.

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