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278 BERBERIAN AND TCHALENKOecontinued)Village Earthquake Damage RemarksPatehvirPayajukSadaghianSailabSaramerikSarmanava$arnaqSavran~en.jiShekar YaziSheydanSheytanavaShivehShiveh DarrohShurgelShurikSiavanSidanSoltan AhmedSowfiabadSutunrashTamarUlehUrbanVardanYavshanluYengijehZaviehjukZindashtZola113 destroyed,churches including130 destroyed,churchincluding1050 completely destroyed600 partly destroyed960 completely destroyed170 partly destroyed180 village destroyed;churchlapsedmostly col626 completel destroyed;including 2 churches120 completely destroyed960 little damaged90 about 80% destroyed0not damagednot damaged330 about 30% collapsedmoderately damagedlightly damagednot damaged1200 about 20% of tim housescollapsed60 destroyed0660 complete.ly destroyed1200 completely destroyed390? ~noderately damaged480 destroyed420 moderately damaged,many houses standing110 completely destroyed240 destroyed; 1 churchunda~nagedlightly damaged70 destroyed116O1828181512l0111521202501810many slept out(ST, AZ)most slept out(ST)about 50~o sleptoutmost slept outmost slept inmost slept inmost slept outmost slept out(ST)most slept outmost slept inmost slept innot inh,~bitcd1930inmost sleptmost sleptoutoutnot inhabited1930inmost slept outmost slept outmost slept inmost slept outmost sleptoutabout 50% slop1out
1930 SALMAS EARTHQUAKE 279there were seven formidable shocks and more than one thousand weaker ones" (Zayia,1930b).3.3. Casualties and destructionIn 1973 over 60 villages of the epicentral region were studied in the field, andin most of them survivors of the earthquake could be found and irtterviewed. A limitedamount of information was also compiled from existing contemporary accounts andnewspaper reports. The results of this investigation are summarized in figure 3 andTables 1 and 2, and are described in more detail below.Fig. 4.S.Stephanos near Julfa. Located over 100km to the northeast of the epicentral region, theeastern wall of this 16th century church developed a vertical fissure from apex to ground level,probably as a result of uneven foundation settlement.
Page 1 and 2: Geol. Surv. Iran, 39, 271-342, 1976
Page 3 and 4: U S S R~ ’~; ~J.U LFAS. Stephanos
Page 5 and 6: I3a252635
Page 7 and 8: 1930SALMAS EARTHQUAKE 275about 40 c
Page 9: 1930 SALMAS EARTHQUAKE 277’contin
Page 13 and 14: 1930 SALMAS EARTGQUAKE 281Approx.di
Page 15 and 16: 1930 SALMAS EARTGQUAKE 283Approx.di
Page 17 and 18: 1930SALMAS EARTHQUAKE 285the usual
Page 19 and 20: 1930SALMAS EARTHQUAKE 287slept indo
Page 21 and 22: 1930SALMAS EARTHQUAKE 289relatively
Page 23 and 24: 1930 SALMAS EARTHQUAKE 291saw them
Page 25 and 26: 1930SALMAS EAR.THQUAKE 293watched t
Page 27 and 28: 1930 SALMAS EARTHQUAKE 295to the we
Page 29 and 30: 1930 SALMAS EATHQUAKE 297indoors. H
Page 31 and 32: 1930 SALMAS EARTHQUAKE 299Zaviehjuk
Page 33 and 34: 1930SALMAS EARTHQUAKE 301Gevork was
Page 35 and 36: 1930 SALMAS EARTHQUAKE 303cracks ne
Page 37 and 38: Eig. 25a. Unique photograph illustr
Page 39 and 40: 1930 SALMAS EARTHQUAKE 307of descri
Page 41 and 42: 1930SALMAS EARTHQUAKE3O9and had a h
Page 43 and 44: 1930 SALMAS EARTHQUAKE 311to the di
Page 45 and 46: 1930SALMAS EARTHQUAKE 313region, 85
Page 47 and 48: BERBERIAN AND TCHALENKO 315for the
Page 49 and 50: 1930 SALMAS EARTHQUAKE 317as the Ak
Page 51 and 52: 1930 SALMAS EARTHQUAKE 319a stream
Page 53 and 54: 1930SALMAS EARTHQUAKE 321for measur
Page 55 and 56: 1930 SALMAS EARTHQUAKE 323West of t
Page 57 and 58: 1930SALMAS EARTHQUAKE 325fields and
Page 59 and 60: 1930 SALMAS EARTHQUAKE 327for medic
Page 61 and 62:
1930SALMAS EARTHQUAKE 329down) (Fig
Page 63 and 64:
1930SALMAS EARTHQUAKE 331The entire
Page 65 and 66:
1930. SALMAS EARTHQUAKE3335. NON-TE
Page 67 and 68:
1930 SALMAS EARTHQUAKE 3356. AFTERS
Page 69 and 70:
1930SALMAS EARTHQUAKE 3377. CONCLUS
Page 71 and 72:
1930SALMAS EARTHQUAKE 339APPENDIX 1
Page 73 and 74:
1930 SALMAS EARTHQUAKE 341APPENDIX
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