G. Papadopoulos, I. Triantafyllou, Andromachi Vassilopoulou
{"title":"公元6世纪中期希腊中部神秘的大地震和海啸:地震构造、考古学和历史的重新审视","authors":"G. Papadopoulos, I. Triantafyllou, Andromachi Vassilopoulou","doi":"10.1177/09596836221138330","DOIUrl":null,"url":null,"abstract":"In AD 552 the area around the Gulf of Corinth, Central Greece, was reportedly hit by large destructive earthquakes. At the same time a tsunami supposedly hit Maliac Bay. The case calls for a realistic interpretation since earthquake scenarios failed to explain rationally the narration of the contemporary Byzantine historian Procopius, the only literary source. Scholars have some doubts about Procopius’ reliability since he frequently copied classical authors. We found impressive similarities between the texts of Procopius and those by classic authors regarding the 426 BC central Greece tsunamigenic earthquake. Very likely the AD 552 Maliac Bay tsunami is a fake event in mimic of the 426 BC one. Sixth-century seismic disasters in southern Greece, reported away from the Gulf of Corinth have been attributed as a deus ex machina to the AD 552 earthquake(s) due to the lack of supporting literary sources. After critical examination of the Procopius’ narration and of relevant geological, seismotectonic, and archeological evidence, we concluded with a scenario comprising two strong (magnitude ~6.5) earthquakes but without tsunami generation. The first earthquake perhaps happened in Boeotia, NE Corinth Gulf, as palaeoseismological evidence also indicates. The second earthquake, in Patras-Naupactus area, western Corinth Gulf, is supported by convincing archeological findings. However, seismic destruction horizons in southern Greece are interpreted by distinct sixth-century earthquakes independent from the Procopius’ ones.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"267 - 280"},"PeriodicalIF":1.6000,"publicationDate":"2022-12-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"The mid-6th century AD enigmatic mega earthquake and tsunami in central Greece: a seismotectonic, archeological, and historical reexamination\",\"authors\":\"G. Papadopoulos, I. Triantafyllou, Andromachi Vassilopoulou\",\"doi\":\"10.1177/09596836221138330\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In AD 552 the area around the Gulf of Corinth, Central Greece, was reportedly hit by large destructive earthquakes. At the same time a tsunami supposedly hit Maliac Bay. The case calls for a realistic interpretation since earthquake scenarios failed to explain rationally the narration of the contemporary Byzantine historian Procopius, the only literary source. Scholars have some doubts about Procopius’ reliability since he frequently copied classical authors. We found impressive similarities between the texts of Procopius and those by classic authors regarding the 426 BC central Greece tsunamigenic earthquake. Very likely the AD 552 Maliac Bay tsunami is a fake event in mimic of the 426 BC one. Sixth-century seismic disasters in southern Greece, reported away from the Gulf of Corinth have been attributed as a deus ex machina to the AD 552 earthquake(s) due to the lack of supporting literary sources. After critical examination of the Procopius’ narration and of relevant geological, seismotectonic, and archeological evidence, we concluded with a scenario comprising two strong (magnitude ~6.5) earthquakes but without tsunami generation. The first earthquake perhaps happened in Boeotia, NE Corinth Gulf, as palaeoseismological evidence also indicates. The second earthquake, in Patras-Naupactus area, western Corinth Gulf, is supported by convincing archeological findings. However, seismic destruction horizons in southern Greece are interpreted by distinct sixth-century earthquakes independent from the Procopius’ ones.\",\"PeriodicalId\":50402,\"journal\":{\"name\":\"Holocene\",\"volume\":\"33 1\",\"pages\":\"267 - 280\"},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2022-12-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Holocene\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1177/09596836221138330\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Holocene","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1177/09596836221138330","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
The mid-6th century AD enigmatic mega earthquake and tsunami in central Greece: a seismotectonic, archeological, and historical reexamination
In AD 552 the area around the Gulf of Corinth, Central Greece, was reportedly hit by large destructive earthquakes. At the same time a tsunami supposedly hit Maliac Bay. The case calls for a realistic interpretation since earthquake scenarios failed to explain rationally the narration of the contemporary Byzantine historian Procopius, the only literary source. Scholars have some doubts about Procopius’ reliability since he frequently copied classical authors. We found impressive similarities between the texts of Procopius and those by classic authors regarding the 426 BC central Greece tsunamigenic earthquake. Very likely the AD 552 Maliac Bay tsunami is a fake event in mimic of the 426 BC one. Sixth-century seismic disasters in southern Greece, reported away from the Gulf of Corinth have been attributed as a deus ex machina to the AD 552 earthquake(s) due to the lack of supporting literary sources. After critical examination of the Procopius’ narration and of relevant geological, seismotectonic, and archeological evidence, we concluded with a scenario comprising two strong (magnitude ~6.5) earthquakes but without tsunami generation. The first earthquake perhaps happened in Boeotia, NE Corinth Gulf, as palaeoseismological evidence also indicates. The second earthquake, in Patras-Naupactus area, western Corinth Gulf, is supported by convincing archeological findings. However, seismic destruction horizons in southern Greece are interpreted by distinct sixth-century earthquakes independent from the Procopius’ ones.
期刊介绍:
The Holocene is a high impact, peer-reviewed journal dedicated to fundamental scientific research at the interface between the long Quaternary record and the natural and human-induced environmental processes operating at the Earth''s surface today. The Holocene emphasizes environmental change over the last ca 11 700 years.