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

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472 J. RafaCl Goberna, S. J.S.1 <strong>Seismograms</strong>On account of <strong>the</strong> station being dismantled at <strong>the</strong> end of 1940, <strong>the</strong> instrumentsbeing transferred to a new site, and <strong>the</strong> new place being prepared, <strong>the</strong> installation of<strong>the</strong> seismographs was delayed until April 1942, when <strong>the</strong> new photographic verticalcomponent began operation. Therefore, no seismic records exist for <strong>the</strong>se two years.The operation of <strong>the</strong> Benioff seismograph was somewhat irregular during <strong>the</strong> yearbecause it was difficult to get photographic paper during <strong>the</strong> war. For some months<strong>the</strong> paper available was only 23.5 cm in width, which did not last <strong>the</strong> 24 hours, and<strong>the</strong>refore, some seismic events were missed. This condition lasted for several months,and even at <strong>the</strong> end of 1942, it was impossible to get any kind of photographic paper.The problem was solved by March, 1943.The Wiechert seismograph was reinstalled on July of 1943 and its normal operationcontinued until <strong>the</strong> end of this period. Its recording paper was quite thin,but <strong>the</strong> seismograms are well preserved. The smoke coating was at times too thickso that <strong>the</strong> seismograms are difficult to read or copy. Often <strong>the</strong> time marks weremissing, but <strong>the</strong> seismogram readings can be made <strong>from</strong> <strong>the</strong> photographic records;<strong>the</strong> clock used was <strong>the</strong> same for both instruments. The time correction was automaticallymarked on <strong>the</strong> seismogram by radio signals received <strong>from</strong> <strong>the</strong> Annapolisstation (U.S.A.) or <strong>from</strong> Panama.Since July 1947, <strong>the</strong> records of <strong>the</strong> horizontal Sprengne<strong>the</strong>r seismograph are alsopreserved, and <strong>the</strong>refore, <strong>the</strong> amount of <strong>the</strong> photographic records was greatly increased.During <strong>the</strong> early years <strong>the</strong> drum was kept running at <strong>the</strong> rate of 1 mm/secand at 5 mm of spacing between <strong>the</strong> lines. In this way <strong>the</strong> photographic paper didnot last for 24 hours, and sometimes seismic events were missed. This problem wasnot solved until 1950, when <strong>the</strong> rotation speed of <strong>the</strong> recorder was changed to 0.5mm/sec, but <strong>the</strong> vertical component was kept running at 1 mm/sec.The amount of seismograms for this period is not exactly known as yet, but<strong>from</strong> <strong>the</strong> time period and <strong>the</strong> daily papers used, a minimum of records can becalculated. The minimum amount of photographic records may be about 15,000,and <strong>the</strong> amount of smoked records may be about 6,000.3.2. AnalysisDuring this second period, <strong>the</strong> analysis of <strong>the</strong> seismograms were made every day,and <strong>the</strong> data of all seismic events were published in <strong>the</strong> Institute Seismic Bulletinsand sent to several o<strong>the</strong>r institutions, some of which usually published <strong>the</strong>m in <strong>the</strong>irseismic bulletins or used <strong>the</strong>m for determining <strong>the</strong> parameters of <strong>the</strong> seismic events.Thus, <strong>the</strong>y were published in <strong>the</strong> Mensuel Bulletin of <strong>the</strong> B.C.I.S. and in I.S.S. since1943. The first seismic data published by <strong>the</strong> Instituto Geofisico were those of Juneand July 1942, and after a few months of interruption <strong>the</strong>y resumed publication onApril 1943, until <strong>the</strong> end of this period.4. 0 <strong>the</strong>r Colombian StationsWhen <strong>the</strong> seismic station of Bogotd became well established and its permanentoperation secured, its Director tried to find funds for establishing some o<strong>the</strong>r seismicstations so that with <strong>the</strong>ir data one could determine <strong>the</strong> parameters of Colombianearthquakes. Two trading and financial institutions, <strong>the</strong> National Federation of

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