Earthquakes in medieval Sicily. A historical revision (7th-13th century)
The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of...
Ausführliche Beschreibung
Autor*in: |
G. Traina [verfasserIn] E. Guidoboni [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
1996 |
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Übergeordnetes Werk: |
In: Annals of Geophysics - Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010, 39(1996), 6 |
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Übergeordnetes Werk: |
volume:39 ; year:1996 ; number:6 |
Links: |
Link aufrufen |
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DOI / URN: |
10.4401/ag-4048 |
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Katalog-ID: |
DOAJ03589394X |
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10.4401/ag-4048 doi (DE-627)DOAJ03589394X (DE-599)DOAJe0c1417517004ce1bb41342e042db654 DE-627 ger DE-627 rakwb eng QC851-999 QC801-809 G. Traina verfasserin aut Earthquakes in medieval Sicily. A historical revision (7th-13th century) 1996 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. Historical earthquakes Sicily Messina Syracuse Trapani Meteorology. Climatology Geophysics. Cosmic physics E. Guidoboni verfasserin aut In Annals of Geophysics Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010 39(1996), 6 (DE-627)559075804 (DE-600)2410939-3 2037416X nnns volume:39 year:1996 number:6 https://doi.org/10.4401/ag-4048 kostenfrei https://doaj.org/article/e0c1417517004ce1bb41342e042db654 kostenfrei http://www.annalsofgeophysics.eu/index.php/annals/article/view/4048 kostenfrei https://doaj.org/toc/1593-5213 Journal toc kostenfrei https://doaj.org/toc/2037-416X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 39 1996 6 |
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10.4401/ag-4048 doi (DE-627)DOAJ03589394X (DE-599)DOAJe0c1417517004ce1bb41342e042db654 DE-627 ger DE-627 rakwb eng QC851-999 QC801-809 G. Traina verfasserin aut Earthquakes in medieval Sicily. A historical revision (7th-13th century) 1996 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. Historical earthquakes Sicily Messina Syracuse Trapani Meteorology. Climatology Geophysics. Cosmic physics E. Guidoboni verfasserin aut In Annals of Geophysics Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010 39(1996), 6 (DE-627)559075804 (DE-600)2410939-3 2037416X nnns volume:39 year:1996 number:6 https://doi.org/10.4401/ag-4048 kostenfrei https://doaj.org/article/e0c1417517004ce1bb41342e042db654 kostenfrei http://www.annalsofgeophysics.eu/index.php/annals/article/view/4048 kostenfrei https://doaj.org/toc/1593-5213 Journal toc kostenfrei https://doaj.org/toc/2037-416X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 39 1996 6 |
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10.4401/ag-4048 doi (DE-627)DOAJ03589394X (DE-599)DOAJe0c1417517004ce1bb41342e042db654 DE-627 ger DE-627 rakwb eng QC851-999 QC801-809 G. Traina verfasserin aut Earthquakes in medieval Sicily. A historical revision (7th-13th century) 1996 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. Historical earthquakes Sicily Messina Syracuse Trapani Meteorology. Climatology Geophysics. Cosmic physics E. Guidoboni verfasserin aut In Annals of Geophysics Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010 39(1996), 6 (DE-627)559075804 (DE-600)2410939-3 2037416X nnns volume:39 year:1996 number:6 https://doi.org/10.4401/ag-4048 kostenfrei https://doaj.org/article/e0c1417517004ce1bb41342e042db654 kostenfrei http://www.annalsofgeophysics.eu/index.php/annals/article/view/4048 kostenfrei https://doaj.org/toc/1593-5213 Journal toc kostenfrei https://doaj.org/toc/2037-416X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 39 1996 6 |
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10.4401/ag-4048 doi (DE-627)DOAJ03589394X (DE-599)DOAJe0c1417517004ce1bb41342e042db654 DE-627 ger DE-627 rakwb eng QC851-999 QC801-809 G. Traina verfasserin aut Earthquakes in medieval Sicily. A historical revision (7th-13th century) 1996 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. Historical earthquakes Sicily Messina Syracuse Trapani Meteorology. Climatology Geophysics. Cosmic physics E. Guidoboni verfasserin aut In Annals of Geophysics Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010 39(1996), 6 (DE-627)559075804 (DE-600)2410939-3 2037416X nnns volume:39 year:1996 number:6 https://doi.org/10.4401/ag-4048 kostenfrei https://doaj.org/article/e0c1417517004ce1bb41342e042db654 kostenfrei http://www.annalsofgeophysics.eu/index.php/annals/article/view/4048 kostenfrei https://doaj.org/toc/1593-5213 Journal toc kostenfrei https://doaj.org/toc/2037-416X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 39 1996 6 |
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abstract |
The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. |
abstractGer |
The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. |
abstract_unstemmed |
The need to understand the activity of the main seismogenetic structures, to calculate the recurrence periods of major earthquakes and to identify their main epicentral areas, requires wide-ranging research in the field of historical seismology. The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA. |
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The present research was conducted in the framework of the projects of the Istituto Nazionale di Geofisica (1991-1995). The presence of different populations and ruling élites, and hence of languages and cultures, has in many cases confused the historical context of the medieval Sicilian sources. However, by going beyond the local sources, and analysing the events in a wider European and Mediterranean context, taking due account of the Byzantine, Latin and Arab sources, it has been possible to identify five seismic events that do not exist in the Italian catalogues or whose dates are very difficult to establish. Six spurious events have been deleted thanks to the revision (659, 785, 796, 963, 1069, 1259); the date of an event has been corrected (1140 into 1125) and five unknown events have been discovered: 853, 1172, 1203-1204, 1255-1256 and 1295-1296. The data on which these findings are based are in many cases dispersed and unused within the many specialised sectors of historical research; in some cases they are unknown even to historians. An example of textual analysis of the sources is also presented to show by what a roundabout route the chronological parameter for the 1125 earthquake was reached. The new events confirm the high seismicity of the eastern area of Sicily; nevertheless, the newly identified series does not seem to show any seismic event comparable to the one that struck the Messina Strait, in 1908 (I0 = XI MCS, M = 7.2): this historical element can provide information regarding the return times of such great event; a hypothesis is formulated by the authors: it will have to be carefully examinated by archaeology research. The criteria used in this research are explained, as well as the problems tackled in accordance with the method for the revision of the historical earthquakes adopted by ING-SGA.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Historical earthquakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sicily</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Messina</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Syracuse</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trapani</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Meteorology. Climatology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geophysics. Cosmic physics</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">E. 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