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

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HISTORICAL SEISMOGRAMS FROM AUSTRALI<strong>AD</strong>avid DenhamBureau of Mineral Resources, Geology and GeophysicsP.O. Boz 378, Canberra City 2601, AustraliaABSTRACTPermanent seismographs were established on <strong>the</strong> Australian continentshortly after <strong>the</strong> turn of <strong>the</strong> century. Milne instruments were set up inPerth (1901), Melbourne (1902), Sydney (1906), and Adelaide (1909) anda Weichert was installed at Riverview (Sydney) in 1909. The magnificationof <strong>the</strong> early Milne instruments was very low (M 6), however, and itwas not until Milne-Shaw instruments were installed in <strong>the</strong> 1920’s that auseful network of four stations was established.Most of <strong>the</strong> seismograms for <strong>the</strong>se four stations are available <strong>from</strong> <strong>the</strong>1920’s onward. The records are still stored in <strong>the</strong>ir original photographicformat, however, and a significant number of <strong>the</strong> early seismograms havedeteriorated. Expert conservation will be required if information on <strong>the</strong>early seismograms is to be preserved.1. IntroductionThe historical record in Australia goes back only about 200 years. Since Australiawas first settled by Europeans, however, reports of earthquakes and <strong>the</strong>ir effects havebeen common. The first reported earthquake was felt at Port Jackson (Sydney) inJune 1788, when “The 22nd of this month (June) we had a slight shock of anearthquake; it did not last more than 2 or 3 seconds. I felt <strong>the</strong> ground shake underme, and heard a noise that came <strong>from</strong> <strong>the</strong> southward, which I at first took for <strong>the</strong>report of guns fired at a great distance” (Phillip, 1788).In 1837 <strong>the</strong> first settlers in South Australia were made aware of <strong>the</strong> existence ofearthquakes when, “<strong>the</strong>re was a loud rumbling noise that lasted 20 seconds. Theearth shook and trembled. It was an earthquake” (Blackett, 1907). Similarly, in<strong>the</strong> early histories of Melbourne (1841; Underwood, 1972) and Perth (1849; McCue,1973) earthquakes were felt. Fortunately, <strong>the</strong>re is no record of anybody being killedby an earthquake in Australia and <strong>the</strong> total damage to buildings and installationssince 1950 has amounted to a modest 50 million in 1985 dollar values.Although <strong>the</strong> level of Australian seismicity is comparatively low, <strong>the</strong> Australiancontinent forms an excellent platform for studies of global seismicity and earthstructure. Active seismic zones range in distance <strong>from</strong> 5” to 180” <strong>from</strong> <strong>the</strong> continent,and <strong>the</strong> locations of earthquakes in <strong>the</strong> southwest Pacific and in sou<strong>the</strong>ast Asia areconstrained by seismic observations <strong>from</strong> Australia.2. Early Seismological StationsIn spite of Australia’s global seismological importance, it is somewhat ironic that<strong>the</strong> first seismic instruments were set up <strong>the</strong>re to record local earthquakes. Theseinstruments were constructed in Launceston, Tasmania, by Biggs (1885) to record<strong>the</strong> larger earthquakes <strong>from</strong> <strong>the</strong> swarm of over 2,000 events that occurred off <strong>the</strong><strong>Historical</strong> <strong>Seismograms</strong>and Earthquakes of <strong>the</strong> World45 1 Copyright 3 1988 by Academic Press, Inc.All rights of reproduction in an) form reserved.

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