首页> 外文OA文献 >Les crues brutales dans la plaine d'Argos (Grèce) : une contrainte à l'aménagement, de l'Antiquité à nos jours/Violent flood in the plain of Argos (Greece): developments under constraint from Antiquity down to present day
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Les crues brutales dans la plaine d'Argos (Grèce) : une contrainte à l'aménagement, de l'Antiquité à nos jours/Violent flood in the plain of Argos (Greece): developments under constraint from Antiquity down to present day

机译:阿尔戈斯平原(希腊)的野蛮洪水:从古代到今天对发展的制约/ 阿尔戈斯平原(希腊)的暴力洪水:从上古到现在的发展一天

摘要

Abstract Combining the geomorphological analysis with new historical and archaeological data, we have reconstructed the alluvial dynamics at work in the Argos plain from the Mycenian era onwards. We try to show that violent floods are a permanent risk, though nowadays rather neglected in the recent developments of the plain, as a Mycenian dam and levees dating back to the 4th and 5th centuries ВС show it. The violent floods have caused substantial alluvial reshaping, which is deeper in the West, where the deposits are up to 8 m deep, than in the East of the plain, where they are no deeper than 40 cm or 1 m. In the eastern part of the plain, the Venitian cadastre ofNauplia, made at the end of the eighteenth century, and contemporary flooding show it. The explanation of such a dissymetry is to be found in orographie and climatic factors, the highest mountains and rainfalls being situated on the western drainage basins.
机译:摘要我们将地貌分析与新的历史和考古数据相结合,从迈锡尼时代开始重建了阿尔戈斯平原上的冲积动力学。我们试图证明暴力洪水是永久性风险,尽管如今在平原的近期发展中已被忽略,正如迈锡尼大坝和堤防可追溯到4世纪和5世纪ВС。猛烈的洪水造成了大量冲积层的重塑,在沉积层深达8 m的西部比平原东部深达40 cm或1 m的深层。在平原的东部,纳普里亚的威尼斯地籍,建于18世纪末,现代洪水表明了这一点。对这种不对称性的解释可以从地形学和气候因素中找到,最高的山脉和降雨量位于西部流域。

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