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Dynamics and effects of the Vesuvius Pomici di Avellino Plinian eruption and related phenomena on the Bronze Age landscape of Campania region (Southern Italy)

机译:维苏威火山波密西迪阿韦利诺普林尼火山喷发及相关现象对坎帕尼亚地区(意大利南部)青铜时代景观的动力学和影响

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摘要

The Pomici di Avellino eruption is the Plinian event of Vesuvius with the highest territorial impact. It affected an area densely inhabited by Early Bronze Age human communities and resulted in the long term abandonment of an extensive zone surrounding the volcano. Traces of human life beneath the eruption products are very common throughout the Campania Region. A systematic review of the available archaeological data, the study of geological and archaeological sequences exposed in excavations, and the reconstruction of the volcanic phenomena affecting single sites has yielded an understanding of local effects and their duration. The archaeological and volcanological analyses have shown that the territory was rapidly abandoned before and during the eruption, with rare post-eruption attempts at resettlement of the same sites inhabited previously. The definition of the distribution and stratigraphy of alluvial deposits in many of the studied sequences leads us to hypothesise that the scarce presence of humans during phases 1 and 2 of the Middle Bronze Age in the wide area affected by the eruption was due to diffuse phenomena of remobilisation of the eruption products, generating long lasting alluvial processes. These were favoured by the deposition of loose fine pyroclastic material on the slopes of the volcano and the Apennines, and by climatic conditions. A significant resettlement of the territory occurred only hundreds of years after the Pomici di Avellino eruption, during phase 3 of the Middle Bronze Age. This study show the role of volcanic and related phenomena from a Plinian event in the settlement dynamics of a complex territory like Campania. (C) 2018 Elsevier Ltd and INQUA. All rights reserved.
机译:Pomici di Avellino喷发是维苏威火山的普林纪事件,对领土的影响最大。它影响了早期青铜时代人类社区密集居住的地区,并导致长期放弃了围绕火山的广阔地带。在整个坎帕尼亚地区,喷发产物下的人类生活痕迹非常普遍。对可用考古数据的系统回顾,对挖掘过程中暴露的地质和考古序列的研究以及对影响单个地点的火山现象的重建,已经使人们对局部影响及其持续时间有了了解。考古和火山学分析表明,在喷发前和喷发期间,该领土迅速被废弃,在喷发后极少尝试重新安置以前居住的相同地点。在许多研究序列中冲积沉积物的分布和地层的定义使我们得出这样的假设:在青铜器时代的第一和第二阶段,受喷发影响的广大地区人类稀少存在。喷发产品的移动,产生持久的冲积过程。火山和亚平宁山脉的山坡上散布着细小的火山碎屑物质,以及气候条件对这些形成了支持。在中古铜器时代的第3阶段,波米西迪·阿韦利诺火山喷发仅几百年后,该地区发生了大规模的重新安置。这项研究表明,来自普林尼事件的火山及其相关现象在像坎帕尼亚这样的复杂地区的定居动态中的作用。 (C)2018爱思唯尔有限公司和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2019年第ptab期|231-244|共14页
  • 作者单位

    Ist Nazl Geofis & Vulcanol, Sez Napoli Osservatorio Vesuviano, Via Diocleziano 328, Naples, Italy;

    MiBACT, Parco Archeol Campi Flegrei, Rome, Italy;

    Ist Nazl Geofis & Vulcanol, Sez Napoli Osservatorio Vesuviano, Via Diocleziano 328, Naples, Italy;

    Ist Nazl Geofis & Vulcanol, Sez Napoli Osservatorio Vesuviano, Via Diocleziano 328, Naples, Italy;

    Univ Pisa, Dipartimento Sci Terra, Via S Maria 53, I-56126 Pisa, Italy;

    MiBACT, Soprintendenza Archeol Belle Arti & Paesaggio Met, Rome, Italy;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Plinian eruption; Volcanoclastic mass flow; Vesuvius; Bronze Age; Eruption impact;

    机译:斜山喷发;火山碎屑物质流;维苏威;青铜时代;喷发影响;
  • 入库时间 2022-08-18 04:08:59

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