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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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Philippine His to rical Earthquakes 291Table 1. Destructive Philippine Earthquakes, 1589-19831.2.3.4.5.6.7.8.9.10.11.12.13.14.15.16.17.18.19.20.21.22.23.24.25.26.27.28.29.30.31.32.33.34.35.36.37.38.39.40.Date Time (LST) Lat. Long. Magnitude I0ON OE MS (MI)1599 Jun 211619 Nov 301743 Jan 121787 Jul 131796 Nov 051852 Sep 161863 Jun 031869 Aug 161869 Oct 011873 Nov 141880 Jul 181885 Jul 231889 May 261892 Mar 161893 Jun 211897 Sep 211897 Oct 191902 Aug 211907 Nov 241911 Jul 121913 Mar 141917 Jan 311918 Aug 151924 Apr 151924 Aug 301925 Nov 131929 Jun 131931 Mar 191937 Aug 201948 Jan 251954 JulO21955 Apr 011968 Aug 021970 Apr 071973 Mar 171976 Aug 171977 Mar 191981 Nov 221982 Jan 111983 Aug 171O:OO a.m.12:OO p.m.5:OO-6:00 p.m.6:45 a.m.2:OO p.m.6:30 p.m.7:20 p.m.3:OO p.m.11:15 a.m.5:30 p.m.12:40 p.m.10:45 a.m.2:23 a.m.9:Ol p.m.3:30 p.m.1:15 p.m.7:52 p.m.7:17 p.m.9:59 p.m.12:09 p.m.4:47 p.m.12:02 p.m.820 p.m.12:22 a.m.11:07 a.m.8:16 p.m.5:26 p.m.2:26 p.m.7:59 p.m.1:46 a.m.10:46 a.m.2:17 a.m.4:19 a.m.1:34 p.m.4:31 p.m.12:ll a.m.5:43 a.m.11:06 p.m.2:11 p.m.8:18 p.m.14.6018.1714.0010.7016.0513.9514.6312.1714.8213.1116.008.4313.5916.066.887.1 112.408.1013.109 .oo4.505.605.506.508.5013.008.5018.3014.2010.9013.008.0016.5015.8013.417.3016.7018.7114 .OO18.33121.00121.60121.60122.55120.30120.40121.04123.69120.82122.98121.85123.60121.19120.42125.83122.11125.00124.25123.40126.00126.50124.80123.00126.50126.50125.00127.00120.20122.10122.10124.00124.00122.30121.70122.87123.60122.31120.65124.50120.878.7 *8.1 *7.7 *7.9 (PAS)8.3 *8.3 *7.3 (PAS)7.3 (PAS)7.2 (PAS)6.9 (PAS)7.5 *8.3 *6.75 (PAS)7.5 (PAS)7.3 *7.3 (NEIS)7.0 (NEIS)7.9 (NEIS)7.0 (NEIS)6.7 (NEIS)7.1 (NEIS)6.5 (NEIS)VIIIXXXXIXXIXIXVIIIXXVIIIIXXIXIXXXXIXIXXIXIXVIIIXVIIIVIIIIXIXXIXIXXIXVIIIVIIIVIIIVIII* Lomnitz (1974)accuracy of <strong>the</strong> assessment of many of <strong>the</strong> earthquakes may not have been uniformconsidering <strong>the</strong> variance in <strong>the</strong> degree of subjectivity different observers have inevaluating intensities of earthquakes. (c) Limitation of <strong>the</strong> spatial distribution ofearthquake effects observations - in many cases, reports are confined to a region ofone intensity level. For cases like <strong>the</strong>se, isoseismal maps were not drawn.

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