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

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SEISMOLOGICAL MEASUREMENT IN HONG KONG1. IntroductionH. K. LamRoyal ObservatoryNathan Road, Kowloon, Hong KongSeismological measurements in Hong Kong began in 1921 by <strong>the</strong> Royal Observatory,Hong Kong. Apart <strong>from</strong> <strong>the</strong> period 1941-1950, continuous recordings havebeen made.2. SeismographsTable 1 shows <strong>the</strong> seismological instrumentation used since 1921. Before WorldWar TI, <strong>the</strong> instrumentation consisted of two horizontal-component Milne-Shaw seismometerseach having a natural period of 12 seconds. The recording was made photographicallyusing a galvanometer of similar period, <strong>the</strong> exact values of which areno longer on record. The seismometers were located on a pillar in a double-walledcellar about 6 meters below <strong>the</strong> Royal Observatory grounds. These instruments wereremoved during <strong>the</strong> war, and so no records are available for <strong>the</strong> period 1941-1950.Seismological recordings resumed in 1951 with <strong>the</strong> acquisition of two horizontalcomponentand one vertical-component Sprengne<strong>the</strong>r seismometers. The naturalperiod of <strong>the</strong> horizontal seismometers was 14.5 seconds, and that of <strong>the</strong> verticalseismometer was 1.5 seconds. Recordings were made photographically using mirrorgalvanometers having periods of 18.0 seconds and 1.5 seconds, respectively; for <strong>the</strong>horizontal and vertical components. The operation of this set of seismographs wasterminated in 1976 due to frequent seismometer and galvanometer faults.As part of <strong>the</strong> programs for <strong>the</strong> International Geophysical Year, a set of threecomponentlong-period seismographs with 15-second Press-Ewing seismometers and105-second galvanometers was set up in 1958 in a cooperative experiment with<strong>the</strong> Lamont-Doherty Geological Observatory of Columbia University. It operateduntil 1976 when <strong>the</strong> supply of spares and consumables <strong>from</strong> Lamont ceased. TheRoyal Observatory later acquired electronic recording equipment for <strong>the</strong> Lamontseismometers. Pen-and-ink recordings resumed in 1979.In 1963, a set of three-component long-period seismographs with 15-second Sprengne<strong>the</strong>rseismometers and 100-second galvanometers and ano<strong>the</strong>r set of three-componentshort-period seismographs with 1-second Benioff seismometers and 0.75-second galvanometers were installed as part of <strong>the</strong> U.S. Worldwide StandardizedSeismograph Network (WWSSN). These sets are currently operational.In recent years, <strong>the</strong>re has been increased interest in local seismology in connectionwith <strong>the</strong> design of many extensive engineering projects that might be subject to <strong>the</strong>earthquake hazards. This interest was heightened by <strong>the</strong> occurrences of disastrousearthquakes in China, such as <strong>the</strong> Tangshan earthquake in 1976, and by earthquakepredictions made at various times. Despite such interests, <strong>the</strong> Royal Observatorysite was increasingly affected by ground noise <strong>from</strong> urban development.In order to monitor in more detail <strong>the</strong> location and magnitude of earthquakesin <strong>the</strong> vicinity of Hong Kong, a three-station network of short-period seismographswas installed in 1979. The stations, each equipped with a Teledyne Geotech S-13<strong>Historical</strong> <strong>Seismograms</strong>and Earthquakes of <strong>the</strong> World476Copyright 0 I988 by Academic Press, Inc.All rights of reproduction in any form reserved.

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