Studying the Significance of Subaqueous Slides in Lake Hallstatt. (UNESCO World Heritage Cultural Landscape, Austria). S4LIDE - Hallstatt最新文献

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Studying the Significance of Subaqueous Slides in Lake Hallstatt. (UNESCO World Heritage Cultural Landscape, Austria). S4LIDE - Hallstatt - PROJECT REPORT 研究哈尔施塔特湖水下滑坡的意义。(联合国教科文组织世界遗产文化景观，奥地利)。S4LIDE -哈尔施塔特-项目报告

Studying the Significance of Subaqueous Slides in Lake Hallstatt. (UNESCO World Heritage Cultural Landscape, Austria). S4LIDE - Hallstatt

Pub Date : 1900-01-01 DOI: 10.1553/ess-igcp-s4lide-hallstatts1

The Bronze to Iron Age underground salt mining complex of Hallstatt (Austria) is widely recognised for its cultural importance and wealth of archaeological artefacts. However, while the daily life in the salt mines is archaeologically well documented and environmental effects of the mining activity have been investigated recently, the impact of natural hazards on the prehistoric mining community is still poorly understood. For instance, while it is well established that the prehistoric underground mines have repeatedly been destroyed by large‐scale mass movements, only little is known about the characteristics and extent of these events as well as about mass‐movement recurrence during more recent times. To shed light on past mass‐movement activity in the vicinity of the Hallstatt salt mines, we investigated sediment cores from adjacent Lake Hallstatt. Within the regular lake sediments we identified three large‐scale event deposits, which are interpreted to originate from spontaneous or seismically induced mass movements in the mid‐19th and late 9th century CE and the mid‐4th century BCE. While the age of the latter event is in good agreement with the abandonment of the famous Iron Age cemetery at Hallstatt, the younger events indicate that large‐scale mass movements also occurred repeatedly during the Common Era. © 2022 The Authors. Journal of Quaternary Science Published by John Wiley & Sons Ltd.

哈尔施塔特(奥地利)的青铜至铁器时代地下盐矿因其文化重要性和丰富的考古文物而被广泛认可。然而，虽然盐矿的日常生活在考古学上有很好的记录，最近也对采矿活动的环境影响进行了调查，但自然灾害对史前采矿社区的影响仍然知之甚少。例如，虽然已经确定史前地下矿山多次被大规模的群体运动破坏，但对这些事件的特征和程度以及最近时期的群体运动复发知之甚少。为了阐明哈尔施塔特盐矿附近过去的群众运动活动，我们调查了邻近的哈尔施塔特湖的沉积物岩心。在正常的湖泊沉积物中，我们发现了三个大型事件沉积物，它们被解释为起源于19世纪中叶和9世纪晚期以及公元前4世纪中叶的自发或地震诱发的物质运动。虽然后一事件发生的时间与哈尔施塔特著名的铁器时代墓地的废弃时间很吻合，但较年轻的事件表明，大规模的群众运动在公元期间也多次发生。©2022作者。《第四纪科学杂志》，John Wiley & Sons Ltd.出版。

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