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

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STUDY OF HISTORICAL EARTHQUAKES IN JAPAN (2)Tatsuo UsarniFaculty of EngineeringShinshu University, Nagano, JapanABSTRACTIn Japan, a project on historical earthquakes (i.e., <strong>the</strong> collection andpublication of old materials describing historical earthquakes) is acceleratedrecently, The purpose of this article is to introduce <strong>the</strong> project andsome of <strong>the</strong> scientific works based on <strong>the</strong>se materials and to show thathistorical documents can aid modern scientific studies, such as seismotectonicsand long-range prediction of large earthquakes.We define “historical earthquake” as before 1873. Studies on historicalearthquakes carried out before 1970 are summarized in Section 1. Thesestudies begin with collection and publication of historical materials relatingto old earthquakes. The first and second phases of <strong>the</strong> project areintroduced in Section 2, and <strong>the</strong> status of <strong>the</strong> third phase being carriedout by <strong>the</strong> present author and collaborators is given in Section 4.Among studies based on <strong>the</strong>se historical materials, <strong>the</strong> following threetopics were carried out by <strong>the</strong> present author:(1) Change of seismicity of destructive earthquakes in Japan is documentedin Section 3. Materials for destructive earthquakes are more reliableand more uniform than for non-destructive earthquakes.(2) The 1858 Omati earthquake is studied employing recently collectedmaterials (Section 5). O<strong>the</strong>r historical earthquakes occurring in valleysconnecting Itoigawa-MatumoteIida-Toyokawa cities are also considered.It is shown that <strong>the</strong> damaged area of each earthquake contacts each o<strong>the</strong>r,covering valleys with almost no gaps.(3) The 1793 Kansei earthquake is studied in Section 5. Comparison withrecent earthquakes suggests that <strong>the</strong> Kansei event is quite similar to <strong>the</strong>1896 off-Sanriku event of reverse type. Comparison of this result witho<strong>the</strong>r large earthquakes off <strong>the</strong> Sanriku coast of Japan, provides a clue for<strong>the</strong> occurrence time of <strong>the</strong> next off-Sanriku earthquake of reverse type.1. IntroductionAlthough this is <strong>the</strong> second paper of <strong>the</strong> same title, <strong>the</strong> introductory parts of <strong>the</strong>first paper (Usami, 1979) are reproduced. In this article, we consider earthquakeswhich took place in and near Japan, that is, Hokkaido including <strong>the</strong> sou<strong>the</strong>rn Kurile,Nonshu, Shikoku, Kyushu and Ryukyu <strong>Islands</strong> (Figure 1). In this article, <strong>the</strong> word“historical” refers to <strong>the</strong> time period before 1873. The year 1873 was chosen as <strong>the</strong>year of division for <strong>the</strong> following reasons:(1) In this year, instrumental observations of earthquakes started.(2) At <strong>the</strong> end of this year, <strong>the</strong> Gregorian calendar replaced <strong>the</strong> Japanese lunarcalendar. On 9 November of <strong>the</strong> fifth year of <strong>the</strong> Meiji era, 1 January 1873, <strong>the</strong>Gregorian calendar was first put into general use.<strong>Historical</strong> <strong>Seismograms</strong>and Earthquakes of <strong>the</strong> World2 76Copyright 0 I 9RX by Academic Prers, Inc.All rights of reproduction in any form reserved.

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