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首页> 外文期刊>Bollettino della Unione matematica italiana, B >Archaeoseismological evidence of a disruptive Late Antique earthquake at Alba Fucens (central Italy)
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Archaeoseismological evidence of a disruptive Late Antique earthquake at Alba Fucens (central Italy)

机译：阿尔巴·富森斯（意大利中部）破坏性的晚期古董地震的考古学证据

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摘要

Paleoseimological investigations in the 1990s identified a surface faulting event in the Fucino Plain (central Italy) related to the 5 century AD. This event originated along the same seismogenic source responsible for the 1915 earthquake (Mw 7.0) that caused damage over a vast region, including Rome. This earthquake was associated to the one that was responsible for damage to the Colosseum in Rome, just before 484 AD or 508 AD. Considering that this event was energetic enough to create surface faulting, significant effects would be expected on the settlements of the 5~(th)-6~(th) century AD. In modern archaeological publications, the destruction of Alba Fucens in the north-western sector of the Fucino area has been related to the effects of a destructive earthquake that occurred during the Late Antiquity. Archaeological evidence on the effects of the earthquake is mostly made up of collapsed layers including columns, statues, coins and other materials and layers formed by burnt remains (mainly parts of the wooden structures of the buildings). However, this Late Antique earthquake has been attributed to the 4~(th) century AD in archaeological literature. With this discrepancy in mind, we have carried out a study of the archaeological sources and have collected new archaeological data, in order to cast light on this chronological problem. The review of the published and unpublished archaeological information regarding the excavations carried out at Alba Fucens between 1949 and 1979, plus the data collected at new excavations that have been going on since 2004 at different sites in the Fucino basin, suggest that the destruction of A1ba Fucens and other towns and settlements of the region occurred later than assumed in archaeological literature. On the whole, the gathered data are consistent with the published paleoseismological information, and suggest that this destruction occurred during the 5~(th)-6~(th) century AD. Although the processing of the data concerning the archaeological investigations at A1ba Fucens in 2006-2008 is still ongoing, the current, most plausible hypothesis at present, is that the 484-508 AD earthquake was probably responsible for the destruction of Alba Fucens.
机译：在1990年代的古生物学调查中，发现了与5世纪AD有关的Fucino平原（意大利中部）的地表断层事件。该事件起源于与1915年地震（Mw 7.0）相同的震源，该地震在包括罗马在内的广大地区造成了破坏。这场地震与造成罗马罗马竞技场受损的那场地震有关，就在公元484年或508年之前。考虑到该事件的能量足以产生地表断层，因此预计对公元5世纪至6世纪的定居点将产生重大影响。在现代考古出版物中，Fucino地区西北部的Alba Fucens遭到破坏与上古晚期发生的破坏性地震的影响有关。关于地震影响的考古证据主要是由坍塌的层组成的，包括柱子，雕像，硬币和其他材料，以及由残骸形成的层（主要是建筑物木结构的一部分）。然而，这次晚期古董地震在考古文献中被归因于公元4世纪。考虑到这一差异，我们对考古资源进行了研究，并收集了新的考古数据，以期阐明这一年代问题。回顾了1949年至1979年在Alba Fucens进行的考古发掘的和未出版的考古学信息，以及2004年以来在Fucino盆地不同地点进行的新发掘中收集的数据，表明A1ba遭到破坏该地区的富森人和其他城镇和居民区发生的时间比考古文献中所假定的要晚。总体而言，收集到的数据与已发表的古地震学信息相一致，表明这种破坏发生在公元5至6世纪。尽管仍在进行有关2006-2008年A1ba Fucens考古调查数据的处理，但当前最合理的假设是，公元484-508年地震可能是Alba Fucens遭到破坏的原因。

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