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

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

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History of <strong>the</strong> Seismological Observatories in <strong>the</strong> British Isles 485A Milne-Shaw seismograph was installed in 1914 (no. 1) and an improved versionof <strong>the</strong> same instrument replaced it in 1924 (no. 32). The static magnification of<strong>the</strong>se instruments was 150. A second component was added in 1934. The stationceased recording in 1957.3.2. DurhamDurham University Seismological Observatory was set up in 1930, with <strong>the</strong> installationof a Milne-Shaw (N-S component) seismograph which started operationin January, 1931. A second Milne-Shaw (EW component) was added in January1938. The station ceased operation in July, 1939 and restarted in January, 1946.A vault was constructed in 1955 and a Wilson-Lamison vertical instrument wasinstalled, toge<strong>the</strong>r with <strong>the</strong> two Milne-Shaw seismographs, in October 1956. Thestation was still in operation in 1985.3.3. Dyce/AberdeenThe first seismological observatory to be established in <strong>the</strong> Aberdeen area was atParkhill House, Dyce. This observatory was founded by J. E. Crombie. Recordingwas begun in 1914 using two Mainka horizontal seismographs and an Agamennoneinstrument. The Mainkas had a free period of 10 seconds and a static magnificationof 150. In 1918 a Milne-Shaw seismograph was added. All <strong>the</strong>se instrumentsran until Crombie’s death in August 1932, when <strong>the</strong> Agamennone and one of <strong>the</strong>Mainkas was donated to <strong>the</strong> Science Museum. The Milne-Shaw, which was donatedto Aberdeen University, was set up for testing in <strong>the</strong> basement of King’s College,Aberdeen in 1932, and eventually became <strong>the</strong> EW component of <strong>the</strong> Aberdeen stationwhich operated continuously <strong>from</strong> December 1936 to June 1967. A Milne-ShawN-S component was added in 1938. The Milne-Shaw instruments ceased recordingin 1966 (Neilson, 1981).3.4. The Royal Observatory, EdinburghThe first instrument to operate in Edinburgh was a Darwin bifilar pendulum,which was originally installed in <strong>the</strong> Calton Hill Observatory in March 1894 andmoved to <strong>the</strong> Royal Observatory, Blackford Hill, in October 1895. Photographicregistration apparatus was added in August 1896 and a second pendulum was purchasedin May 1898. In 1900 a Milne pendulum was installed. New recording drumswere added in 1909, which gave a faster paper speed of 240 mm per hour.A Milne-Shaw seismograph (no. 3), formerly at Eskdalemuir, was moved toEdinburgh and began recording on July 4, 1919. The E-W component had a staticmagnification of 250.After World War 11, E. Tillotson took over <strong>the</strong> reading of <strong>the</strong> Edinburgh seismograms.During <strong>the</strong> period 1939-1940 various interruptions to recordings occurredowing to defects of <strong>the</strong> drum drive and to quarry blasting.The Milne-Shaw instrument ceased operation in April 1962, when it was transferredto <strong>the</strong> Royal Scottish Museum.

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