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

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286 Tatsuo Usami1897lntenrLFigure 6. Isoseismals for four earthquakes occurring off the coast of northeasternJapan. Comparison should be tried with intensity in Figure 5. Numbers in parenthesesindicate earthquake magnitude. The 1896 event was formerly considered to be magnitude8.5, but was recently revised to 6.8.
Study of Historical Earthquakes in Japan 287Table 2. Comparison of Large Earthquakes Off the Coast of Northeastern JapanType Date d M Number of felt aftershocks Rem.year.mo.da (OE) (ON) Tokyo Ha Mo Mi S F 0 N H Hn A(a,) (b.12 1896.06.15 144 393 6.8 (1) 0 62 95 (1)4 1897.02.20 141.9 38.1 7.4 0 (2)4 1897.08.05 143.3 38.1 7.6 2+(1) 1+(3)4 1915.11.01 142.9 38.3 7.5 1+(1) (4) (2)3 1933.03.03 144.7 39.1 8.3 1 0 29 17 3 14 3 (3)5 1938.05.23 141.4 36.7 7.1 1 3 6 5 12 5 21 23 (4)5 1938.11.05 141.7 37.1 7.7 12 8 16 26 29 77 164 91 (5)1793.02.17 142.4 38.3 7.1 2 70 ? 69 170 184 (6)(a.) = within 7 days after the main shock; (b.) = 8 to 30 days after the main shock.Ha = Hachinohe; Mo = Morioka; Mi = Miyako; S = Sendai; F = Fukushima; 0 = Onahams;N = Nakamura; H = Hazama-machi; Hn = Hanamaki; A = Aomori.Parentheses in columns (a.) and (b.) indicate epicenter is not certain, but consideredas aftershock by the present author.Remarks: (1) = felt aftershock in June; (2) = felt earthquake in November; (3) = all feltearthquakes in March; (4) = all felt earthquakes in May and June; (5) = felt earthquakein November; (6) = felt earthquake within one week after the main shock.Table 3. Comparison Between 1793 Kansei Earthquake and Other TypicalEarthquakes Occurring off the Coast of Northeastern JapanType Typical earthquake referred Tsunami Distribution Number ofof intensity aftershocksEdo General1 Off Tokachi earthquake X X X 0(1677, 1763, 1856)2 Off Sanriku earthquake(reverse type, 1896)0 Q' X 03 Off Sanriku earthquake 0 0 X X(normal type, 1933)4 Off Miyagi Pref. earthquake X 0 X X(1897-1, 1897-2, 1915)5 Off F'ukushima Pref.earthquake (1938)X (> X 0Type = classification due to epicentral area and fault movement. Edo = former namefor Tokyo. Similarity to 1793 Kansei earthquake: 0 = good; C, = moderate; X = bad.(*) = isoseismal is aimilar, but the value of intensity is different.from Table 4 that reverse type earthquakes take place 30-40 years after a type 1event, therefore the next reverse fault type earthquake may take place circa theyear 2000. The interval between earthquakes is longer when the energy release bythe previous earthquake is large, and is average (about 100 years), when the energyrelease by the previous one is average. So, the prediction of the year for the nextoff-Sanriku earthquake of reverse type depends upon the estimation of the releasedenergy by the 1896 earthquake.
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Historical SeismogramsandEarthquake
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ToJames F. Landerfor his leadership
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viContentsThe Status, Importance, a
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...VlllEarthquake History of Califo
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XMicrofilming of Historical Seismog
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PrefaceA symposium on Historical Se
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I. Introduction
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4 W. H. K. Lee, H. Meyers, and K. S
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6 W. H. K. Lee, H. Meyers, and K. S
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8 W. H. h‘. Lee, H. Meyers, and K
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10 W. H. K. Lee, IT. Meyers, and K.
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12 W. H. K. Lee, H. Meyers, and K.
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14 W. H. K. Lee, H. Meyers, and K.
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IMPORTANCE OF HISTORICAL SEISMOGRAM
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18 Hiroo KanamoriTable Ib. Some Lar
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-60'1 1904-1985-M, >8.01II\I'.iPlus
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22 Hiroo Kanamorievents often have
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~~~24 Hiroo KanamoriThatcher et al.
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26 Hiroo Kanamo riIf relatively com
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28 Hiroo Kanamori9. Difficulties in
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30 Hiroo KanamoriNagamune, T. (1971
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32 Hiroo KanamoriI I I I I1000100z
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11. Analysis of Historical Seismogr
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38 Kat su y uki A beaddition to thi
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42 Katsuyuki Abe20:oow19:302-I--Ia
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44 Katsuyuki AbeIn the present stud
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46 Katsuyuki AbeTable 3. Sinkiang E
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~48 Katsuyuki AbeSieh (1978) and ot
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50 Katsuyuki AbeREFERENCESAbe, K. (
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52 E. Hurtig and G. KowalleFRG'.L.-
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54 E. Hurtig and G. Kowalle2.2 Reco
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56 E. Hurtig and G. KowalleREFERENC
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58 N. V. Kondorskaya and Yu. F. Kop
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THE STATUS, IMPORTANCE, AND USE OFH
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66 Ota Kulhdnek1 8 35lo. r 1s ' 20
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68 Ota Kulhdnek1 UPP EW SEP 9 1954
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ANALYSIS OF HISTORICAL SEISMOGRAMS
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72 S. K. Singhfrom Uppsala. We also
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74S. K. SinghN1 1Oaxaca-X .-x x- x
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76S. K. SinghESKUPPWIECHERT ELPZ A-
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78 S. K. SinghJdFJ-22 Feb 1943Ms=7.
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80 S. K. SinghDE BlLT (DBN) Z$I = 3
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82 S. K. Singh7. The Great Jalisco,
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84 S. K. SinghREFERENCESAbe, K. (19
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86 S. Stein, E. A. Okal and D. A. W
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94S. Stein, E. A. Okal and D. A. Wi
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96S. Stein, E. A. Okal and D. A. Wi
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100 S. Stein, E. A. Okal and D. A.
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RECENT ACTIVITIES AT THE INTERNATIO
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S.S. Felt and Damaging EarthquakesI
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In t e r na tio n a1 Se is mo logic
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1. IntroductionCatalogue of Chinese
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Catalogue of Chinese Earthquakes (M
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Catalogue of Chinese Earthquakes (A
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Catalogue of Chinese Earthquakes (A
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DATA BASES ON HISTORICAL SEISMICITY
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Data Bases on Historical Seismicity
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COMPILATION AND PROCESSING OF HISTO
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Compilation and Processing of Histo
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The U. S. Geological Survey’s Dat
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The U. S. Geological Survey's Datab
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~ ~The U. 5‘. Geological Survey
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The U. S. Geological Survey’s Dat
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Catalog of Large and Damaging Earth
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YCatalog of Large and Damaging Eart
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YM D h m1918 2 9 20 461918 2 13 6 7
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His to ric al Mate ria Is of Chine
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Historic a1 Mate rials of Chinese E
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Historical Materials of Chinere Ear
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His t o r ical Mate rials of Chin e
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IV. Individual Historical Earthquak
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174 N. N. Ambraseys and C. F. Finke
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182 N. N. Arnbraseys and C. P. Melv
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184 N. N. Ambraseys and C. P. Melvi
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188 N. N. Arnbraseys and C. P. Melv
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202G. E. Fiedler B.FI1 IFigure 1. T
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204 G. E. Fiedler B.Figure 3. The S
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206 G. E. Fiedler B.Origin time Epi
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EVALUATION OF DAMAGE AND SOURCE PAR
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2 10 D. Muiioz and A. Udias3. Evalu
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212 D. Muiioz and A. Udias3 wFigure
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2 14 D. Mun"oz and A. Udiasgiven by
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216 D. Muioz and A. UdiasTable 2. D
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218 D. Munot and A. UdiasGentil, P.
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220 D. Muiioz and A. UdiasArchivo M
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V. Earthquake History
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226 M. DeBecker and T. CamelbeeckAt
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~~228 M. DeBecker and T. Camelbeeck
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230 M. DeBecker and T. Camelbeeek10
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DOCUMENTING NEW ZEALAND EARTHQUAKES
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234 G. A. EabyFrom a seismic point
Page 250 and 251: 236 G. A. EibyImmediate practical p
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Page 254 and 255: 240 G. A. Eibywith near-earthquake
Page 256 and 257: 242 Pao Hua Lee120 121 122 123Figur
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Page 260 and 261: Pa0 Hua LeeTable 2. Major Earthquak
Page 262 and 263: 248 Pao Hua LeeTable 2. (Continued
Page 264 and 265: 250 Pao Hua Lee‘. . . an earthqua
Page 266 and 267: 252 Pao Hua LeeREFERENCESCentral We
Page 268 and 269: 254 S. Prac h ua b21I151 O0IFigure
Page 270 and 271: 256 S. PrachuabTable 1. 12 Seismic
Page 272 and 273: 258 S. Prac h u a bTable 2. (Contin
Page 274 and 275: 260S. Prachuab94" 96" 98" 1 ooo2ac2
Page 276 and 277: 262 S. Prachuab.17 MAY 1955EMrliCUA
Page 278 and 279: :;13264 S. Prachuab0 .me.0 . .eeee0
Page 280 and 281: 266 S. Prac hua b005 6 7MAGNITUDEFi
Page 282 and 283: 268 T. R. Toppozada, C. R. Real, an
Page 286 and 287: 2 72 T. R. Toppozada, C. R. Real, a
Page 290 and 291: STUDY OF HISTORICAL EARTHQUAKES IN
Page 292 and 293: 278 Tatsuo Usarni(3) Documents publ
Page 294 and 295: 280 Tatsuo Usarnin5nlob0D KyotoKama
Page 296 and 297: 282 Tatsuo Usami:.:.., ........ L,/
Page 298 and 299: 284 Tatsuo Usami(2) A tsunami attac
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Page 304 and 305: 290 R. G. Valenzuela and L. C. Garc
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Page 308 and 309: ~ ~~294 R. G. Valenzuela and L. C.
Page 310 and 311: 296 R. G. Valenzuela and L. C. Garc
Page 312 and 313: 298 R. Muir Wood, G. Woo, and H. Bu
Page 323 and 324: MAGNITUDE-FAULT LENGTH RELATIONSHIP
Page 325 and 326: APPLICATIONS OF FUZZY MATHEMATICSIN
Page 327 and 328: Applications of Fuzzy Mathematics 3
Page 333 and 334: Applications of Fuzzy hluthematics
Page 335 and 336: ON THE SEISMICITY OF THE MIDDLEASTS
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Page 339 and 340: On the Seismicity of the Middle Eas
Page 347 and 348: On the Seismicity oj the Middle Eas
Page 349 and 350: HISTORICAL SEISMICITY AND EARTHQUAK
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Historical Seismic it y and Earthqu
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fIistorica1 Seismicity and Earthquu
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Historical Seismicity and Earthquak
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PATTERN ANALYSIS OF SMALL EARTHQUAK
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Pattern Analysis of Small Earthquak
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Earthquakes and Deep Fracture Zones
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--_-Earthquakes and Deep Fracture Z
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HISTORICAL SEISMOGRAM FILMING PROJE
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~~Historical Seismogram Filming Pro
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Historical Seismogram Filming Proje
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Historical Seismogram Filming Proje
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Filming Seismograms and Related Mat
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Digitization and Processing of J.M.
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SOME REMARKS ON HISTORICAL SEISMOGR
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Historical Seismograms and the Micr
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~~~~Historical Seismograms and the
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His torical Se is mogru ms and the
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Historical Sezs mogra ms and the Ma
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H1s t o rical Seismograms a nd the
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Historical Seismograms in China 42
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424 Kezin Qua History of Chinese Se
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428 Kexin Qu8. Plans for the Near F
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430 0. Ye. Starovoita station, its
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DAT ANDTHE STANDARDIZATION OF SEISM
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434 Y. Tamura, H. Sasaki, M. Ooe, a
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~ So.i436 Y. Tarnura, H. Sasaki, M.
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438 Y. Tarnura, H. Sasaki, M. Ooe,
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440 Yasuhiro Umeda and Katsuyoshi I
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442 Yasuhiro Umeda and Katsuyoshi I
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HISTORICAL SEISMOGRAMS IN ITALYR. C
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Historical Seismograms in Italy 449
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HISTORICAL SEISMOGRAMS FROM AUSTRAL
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His to rical Se is mog ra ms From A
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SEISMOGRAMS MADE BEFORE 1963 AT STA
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2. New ZealandSeismograms Before 19
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Seismograms Before 1963 in the Sout
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Seismograms Before 1963 in the Sout
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Historical Seismograms Recorded in
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Hist orieal Se is mograms Reeo rded
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THE HISTORICAL SEISMOGRAMS OF COLOM
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The Historical Seismograms of Colom
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Helwan Historical Seismograms 475Al
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Se is mo log ic a1 Mea s use me n t
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Seismological Measurement an Hong K
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A BRIEF HISTORY OF THE SEISMOLOGICA
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History of the Seismological Observ
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~~ ~ ~ ~~ ~ ~~Historical Seismogram
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494 Sergio S. Su, S. J.Figure S. Se
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496 Sergao S. Su, S. J.Figure 7. Ce
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498 K. L. SuendsenDominican Republi
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INDEXAAbuyama Seismological Observa
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Index 503China, see also Taiwan466
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Indez505HIHalin seismograph, 421Haw
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Index 507Karuizawa, 417Kobe, 117, 1
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Index 509PPacific Ocean1943 Malpelo
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Index 511Sri Lanka, Colombo station
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Index 513Wood-Anderson seismographW
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