The Garnì (Armenia) large earthquake on 14 June 1679: a new analysis
The 1679 Garnì earthquake was one ofthe most destructive seismic events inArmenia, and one of the most widelydocumented directly by Armenian sources,considering this is an area where historical documentation is, on the whole,rather scarce. Moreover, this earthquakeappears in the literature as the re...
Gespeichert in:
Veröffentlicht in: | Journal of seismology 2003-07, Vol.7 (3), p.301-328 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 328 |
---|---|
container_issue | 3 |
container_start_page | 301 |
container_title | Journal of seismology |
container_volume | 7 |
creator | GUIDOBONI, E HAROUTIUNIAN, R KARAKHANIAN, A |
description | The 1679 Garnì earthquake was one ofthe most destructive seismic events inArmenia, and one of the most widelydocumented directly by Armenian sources,considering this is an area where historical documentation is, on the whole,rather scarce. Moreover, this earthquakeappears in the literature as the result ofvarious interpretative and research models,so there are contradictory assessments ofits impact and its parameters: itsmagnitude oscillated between 5.5 and 7, andepicentral intensity between VIII and Xdegree. Even its location varied by over40 km. This contribution aims to enhancethe acquired knowledge of this earthquakeby applying a methodology of analysis tothe available information that has alreadygiven positive results in historicalseismology in Europe. On the grounds of thenew sources and with a critical review ofpreviously known ones, the authors canprovide new and more accurate data on theearthquake, along with a detailed outlineof the characteristics of the buildingsaffected and the historical and demographicconditions under which the earthquakeoccurred. Moreover, the data has beensupplemented with a direct observationof the monuments still standing, thusrevealing some of the earthquake'spreviously unassessed damaging effects. Theauthors have clearly arranged the use ofdata pertaining to different typologies,maintaining the evidence of suchdiversities even in the evaluation of themacroseismic intensity. This methodologicalapproach has been adopted in order toevaluate the seismic effects in an areawith a low density of historicaldocumentation. As a result, the effects ofthis earthquake could be estimated at 34sites (of which 20 documented from coevalsources and 14 on the grounds of directobservations). For this event there isalso a good geological database regardingthe active fault of Garnì. Hence, thisstudy has also represented a test forcomparing the results of the historicalresearch with the known geological data.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1023/A:1024561622879 |
format | Article |
fullrecord | <record><control><sourceid>proquest_pasca</sourceid><recordid>TN_cdi_proquest_miscellaneous_28018172</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2145049891</sourcerecordid><originalsourceid>FETCH-LOGICAL-p241t-40fa8401d5c26bc31fefd75f8fa09a9f758c41bec81872051be255ad08626d823</originalsourceid><addsrcrecordid>eNpdjstKAzEYhYMoWKtrt0FQdDGaP_d0V0q9UXBTwd3wdyaxU6fTNukgfSffwhdzxK7cnO8sPg6HkHNgt8C4uBsOOkilQXNujTsgPVBGZF28HXZdWJFJLd0xOUlpwRhz1okeGU_nnj5gbL6_6PUwLn1T4Q2tMb576jFu55sWPzxdNRQkfW4bT0EbN6BIG_9JscF6l6p0So4C1smf7dknr_fj6egxm7w8PI2Gk2zNJWwzyQJayaBUBdezQkDwoTQq2IDMoQtG2ULCzBcWrOFMdZUrhSWzmuvSctEnV3-767jatD5t82WVCl_X2PhVm3JuGVgwv-LFP3GxamP3NuVGCcUZaNVJl3sJU4F1iNgUVcrXsVpi3OUgnVMMlPgB0KJknA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>753520165</pqid></control><display><type>article</type><title>The Garnì (Armenia) large earthquake on 14 June 1679: a new analysis</title><source>SpringerLink Journals - AutoHoldings</source><creator>GUIDOBONI, E ; HAROUTIUNIAN, R ; KARAKHANIAN, A</creator><creatorcontrib>GUIDOBONI, E ; HAROUTIUNIAN, R ; KARAKHANIAN, A</creatorcontrib><description>The 1679 Garnì earthquake was one ofthe most destructive seismic events inArmenia, and one of the most widelydocumented directly by Armenian sources,considering this is an area where historical documentation is, on the whole,rather scarce. Moreover, this earthquakeappears in the literature as the result ofvarious interpretative and research models,so there are contradictory assessments ofits impact and its parameters: itsmagnitude oscillated between 5.5 and 7, andepicentral intensity between VIII and Xdegree. Even its location varied by over40 km. This contribution aims to enhancethe acquired knowledge of this earthquakeby applying a methodology of analysis tothe available information that has alreadygiven positive results in historicalseismology in Europe. On the grounds of thenew sources and with a critical review ofpreviously known ones, the authors canprovide new and more accurate data on theearthquake, along with a detailed outlineof the characteristics of the buildingsaffected and the historical and demographicconditions under which the earthquakeoccurred. Moreover, the data has beensupplemented with a direct observationof the monuments still standing, thusrevealing some of the earthquake'spreviously unassessed damaging effects. Theauthors have clearly arranged the use ofdata pertaining to different typologies,maintaining the evidence of suchdiversities even in the evaluation of themacroseismic intensity. This methodologicalapproach has been adopted in order toevaluate the seismic effects in an areawith a low density of historicaldocumentation. As a result, the effects ofthis earthquake could be estimated at 34sites (of which 20 documented from coevalsources and 14 on the grounds of directobservations). For this event there isalso a good geological database regardingthe active fault of Garnì. Hence, thisstudy has also represented a test forcomparing the results of the historicalresearch with the known geological data.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 1383-4649</identifier><identifier>EISSN: 1573-157X</identifier><identifier>DOI: 10.1023/A:1024561622879</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Earth sciences ; Earth, ocean, space ; Earthquakes ; Earthquakes, seismology ; Engineering and environment geology. Geothermics ; Exact sciences and technology ; Internal geophysics ; Marine and continental quaternary ; Natural hazards: prediction, damages, etc ; Seismic activity ; Seismology ; Surficial geology</subject><ispartof>Journal of seismology, 2003-07, Vol.7 (3), p.301-328</ispartof><rights>2003 INIST-CNRS</rights><rights>Kluwer Academic Publishers 2003</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14995015$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>GUIDOBONI, E</creatorcontrib><creatorcontrib>HAROUTIUNIAN, R</creatorcontrib><creatorcontrib>KARAKHANIAN, A</creatorcontrib><title>The Garnì (Armenia) large earthquake on 14 June 1679: a new analysis</title><title>Journal of seismology</title><description>The 1679 Garnì earthquake was one ofthe most destructive seismic events inArmenia, and one of the most widelydocumented directly by Armenian sources,considering this is an area where historical documentation is, on the whole,rather scarce. Moreover, this earthquakeappears in the literature as the result ofvarious interpretative and research models,so there are contradictory assessments ofits impact and its parameters: itsmagnitude oscillated between 5.5 and 7, andepicentral intensity between VIII and Xdegree. Even its location varied by over40 km. This contribution aims to enhancethe acquired knowledge of this earthquakeby applying a methodology of analysis tothe available information that has alreadygiven positive results in historicalseismology in Europe. On the grounds of thenew sources and with a critical review ofpreviously known ones, the authors canprovide new and more accurate data on theearthquake, along with a detailed outlineof the characteristics of the buildingsaffected and the historical and demographicconditions under which the earthquakeoccurred. Moreover, the data has beensupplemented with a direct observationof the monuments still standing, thusrevealing some of the earthquake'spreviously unassessed damaging effects. Theauthors have clearly arranged the use ofdata pertaining to different typologies,maintaining the evidence of suchdiversities even in the evaluation of themacroseismic intensity. This methodologicalapproach has been adopted in order toevaluate the seismic effects in an areawith a low density of historicaldocumentation. As a result, the effects ofthis earthquake could be estimated at 34sites (of which 20 documented from coevalsources and 14 on the grounds of directobservations). For this event there isalso a good geological database regardingthe active fault of Garnì. Hence, thisstudy has also represented a test forcomparing the results of the historicalresearch with the known geological data.[PUBLICATION ABSTRACT]</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Internal geophysics</subject><subject>Marine and continental quaternary</subject><subject>Natural hazards: prediction, damages, etc</subject><subject>Seismic activity</subject><subject>Seismology</subject><subject>Surficial geology</subject><issn>1383-4649</issn><issn>1573-157X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpdjstKAzEYhYMoWKtrt0FQdDGaP_d0V0q9UXBTwd3wdyaxU6fTNukgfSffwhdzxK7cnO8sPg6HkHNgt8C4uBsOOkilQXNujTsgPVBGZF28HXZdWJFJLd0xOUlpwRhz1okeGU_nnj5gbL6_6PUwLn1T4Q2tMb576jFu55sWPzxdNRQkfW4bT0EbN6BIG_9JscF6l6p0So4C1smf7dknr_fj6egxm7w8PI2Gk2zNJWwzyQJayaBUBdezQkDwoTQq2IDMoQtG2ULCzBcWrOFMdZUrhSWzmuvSctEnV3-767jatD5t82WVCl_X2PhVm3JuGVgwv-LFP3GxamP3NuVGCcUZaNVJl3sJU4F1iNgUVcrXsVpi3OUgnVMMlPgB0KJknA</recordid><startdate>20030701</startdate><enddate>20030701</enddate><creator>GUIDOBONI, E</creator><creator>HAROUTIUNIAN, R</creator><creator>KARAKHANIAN, A</creator><general>Springer</general><general>Springer Nature B.V</general><scope>IQODW</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7SM</scope></search><sort><creationdate>20030701</creationdate><title>The Garnì (Armenia) large earthquake on 14 June 1679: a new analysis</title><author>GUIDOBONI, E ; HAROUTIUNIAN, R ; KARAKHANIAN, A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p241t-40fa8401d5c26bc31fefd75f8fa09a9f758c41bec81872051be255ad08626d823</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Earthquakes</topic><topic>Earthquakes, seismology</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Exact sciences and technology</topic><topic>Internal geophysics</topic><topic>Marine and continental quaternary</topic><topic>Natural hazards: prediction, damages, etc</topic><topic>Seismic activity</topic><topic>Seismology</topic><topic>Surficial geology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>GUIDOBONI, E</creatorcontrib><creatorcontrib>HAROUTIUNIAN, R</creatorcontrib><creatorcontrib>KARAKHANIAN, A</creatorcontrib><collection>Pascal-Francis</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>Earthquake Engineering Abstracts</collection><jtitle>Journal of seismology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>GUIDOBONI, E</au><au>HAROUTIUNIAN, R</au><au>KARAKHANIAN, A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Garnì (Armenia) large earthquake on 14 June 1679: a new analysis</atitle><jtitle>Journal of seismology</jtitle><date>2003-07-01</date><risdate>2003</risdate><volume>7</volume><issue>3</issue><spage>301</spage><epage>328</epage><pages>301-328</pages><issn>1383-4649</issn><eissn>1573-157X</eissn><abstract>The 1679 Garnì earthquake was one ofthe most destructive seismic events inArmenia, and one of the most widelydocumented directly by Armenian sources,considering this is an area where historical documentation is, on the whole,rather scarce. Moreover, this earthquakeappears in the literature as the result ofvarious interpretative and research models,so there are contradictory assessments ofits impact and its parameters: itsmagnitude oscillated between 5.5 and 7, andepicentral intensity between VIII and Xdegree. Even its location varied by over40 km. This contribution aims to enhancethe acquired knowledge of this earthquakeby applying a methodology of analysis tothe available information that has alreadygiven positive results in historicalseismology in Europe. On the grounds of thenew sources and with a critical review ofpreviously known ones, the authors canprovide new and more accurate data on theearthquake, along with a detailed outlineof the characteristics of the buildingsaffected and the historical and demographicconditions under which the earthquakeoccurred. Moreover, the data has beensupplemented with a direct observationof the monuments still standing, thusrevealing some of the earthquake'spreviously unassessed damaging effects. Theauthors have clearly arranged the use ofdata pertaining to different typologies,maintaining the evidence of suchdiversities even in the evaluation of themacroseismic intensity. This methodologicalapproach has been adopted in order toevaluate the seismic effects in an areawith a low density of historicaldocumentation. As a result, the effects ofthis earthquake could be estimated at 34sites (of which 20 documented from coevalsources and 14 on the grounds of directobservations). For this event there isalso a good geological database regardingthe active fault of Garnì. Hence, thisstudy has also represented a test forcomparing the results of the historicalresearch with the known geological data.[PUBLICATION ABSTRACT]</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1023/A:1024561622879</doi><tpages>28</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1383-4649 |
ispartof | Journal of seismology, 2003-07, Vol.7 (3), p.301-328 |
issn | 1383-4649 1573-157X |
language | eng |
recordid | cdi_proquest_miscellaneous_28018172 |
source | SpringerLink Journals - AutoHoldings |
subjects | Earth sciences Earth, ocean, space Earthquakes Earthquakes, seismology Engineering and environment geology. Geothermics Exact sciences and technology Internal geophysics Marine and continental quaternary Natural hazards: prediction, damages, etc Seismic activity Seismology Surficial geology |
title | The Garnì (Armenia) large earthquake on 14 June 1679: a new analysis |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-01T20%3A31%3A42IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_pasca&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20Garn%C3%AC%20(Armenia)%20large%20earthquake%20on%2014%20June%201679:%20a%20new%20analysis&rft.jtitle=Journal%20of%20seismology&rft.au=GUIDOBONI,%20E&rft.date=2003-07-01&rft.volume=7&rft.issue=3&rft.spage=301&rft.epage=328&rft.pages=301-328&rft.issn=1383-4649&rft.eissn=1573-157X&rft_id=info:doi/10.1023/A:1024561622879&rft_dat=%3Cproquest_pasca%3E2145049891%3C/proquest_pasca%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=753520165&rft_id=info:pmid/&rfr_iscdi=true |