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

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482 G. Neilson and P. W. BurtonAfter Milne’s death in 1913 <strong>the</strong> headquarters of this organization, now known as<strong>the</strong> International Seismological Summary (ISS), moved to Oxford under <strong>the</strong> directionof Professor H. H. Turner.British stations formed a vital part of <strong>the</strong> new worldwide network set up byMilne. Research was performed on site noise, microseisms, etc., by comparing <strong>the</strong>seismograms written at <strong>the</strong> various stations in Britain, and applying <strong>the</strong> results toall British Association stations.The scientific results <strong>from</strong> <strong>the</strong> worldwide organizations were of enormous importanceto seismology because <strong>the</strong>y covered topics as diverse as deep-focus earthquakes,submarine disturbances caused by earthquakes, seismicity studies and epicenter-determinationmethods, and o<strong>the</strong>rs.Seismology in Britain was considerably disrupted by World War I, although mostof <strong>the</strong> stations managed to continue operating throughout <strong>the</strong> war. After 1918 <strong>the</strong>situation became normal again fairly quickly. The period between World Wars Iand I1 saw a great advance in seismology in Britain, <strong>the</strong> most significant contributionpossibly being <strong>the</strong> production of <strong>the</strong> Jeffreys-Bullen traveltime tables (Jeffreys,1939), but only two new observatories were established, Jersey and Durham.By <strong>the</strong> end of World War I1 few British observatories were operating purely in<strong>the</strong> interests of seismology. Jersey, under <strong>the</strong> German occupation, had great difficultyfinding materials to continue recording. Edinburgh and Durham had ceasedanalysing <strong>the</strong> records for <strong>the</strong> duration of <strong>the</strong> war, although <strong>the</strong> seismographs atEdinburgh were kept in operation throughout.After World War 11, <strong>the</strong> stations in <strong>the</strong> British Isles were equipped with obsoleteequipment, efficiency at <strong>the</strong> stations had declined, and a few stations had closedaltoge<strong>the</strong>r. In 1960, only Kew, Durham, Jersey, and Aberdeen were operating andKew and Aberdeen closed within a few years.The Geneva Test Ban negotiations, <strong>from</strong> 1958 onwards, led to a re-awakeningof interest in seismology and provided <strong>the</strong> catalyst necessary for <strong>the</strong> renovationof instrumental seismology. In Britain this led to <strong>the</strong> establishment of <strong>the</strong> WorldWide Standard Station at Eskdalemuir and of a large array station nearby (Truscott,1964). In Ireland a World Wide Standard Station was set up at Valentia. Edinburghwas re-equipped with modern instruments recording on magnetic tape (Willmoreand Connell, 1963). An array station was set up at Rookhope, near Durham, andmany modern stations have been deployed over all <strong>the</strong> British Isles in <strong>the</strong> yearssince 1960 (Crampin and o<strong>the</strong>rs, 1970; Browitt and o<strong>the</strong>rs, 1985).This report deals with <strong>the</strong> period beginning with <strong>the</strong> return of Milne <strong>from</strong> Japanand ends with <strong>the</strong> renaissance of instrumental seismology in Britain, which beganin <strong>the</strong> 1960’s.2. The History of <strong>the</strong> Establishment of Seismological Observatories in<strong>the</strong> British IslesThe principal observatories established in Britain and Ireland during 1896- 1960are shown in Figure 1 and listed in Table 1. The first observatory in Britain equippedwith a seismograph was Milne’s at Shide, Isle of Wight, set up in 1895. Milne alsoinstalled a temporary station at Carisbrooke Castle to compare records. Withintwo or three years o<strong>the</strong>r stations such as Edinburgh, Kew, Paisley and Bidston wereestablished. All <strong>the</strong>se places had astronomical and/or meteorological observatoriesto provide an accurate source of timing for seismographic recording.

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