关于l’hydrogéomorphologie anthropisation密集型城市空间的网站:Nı̂my更新世(Languedoc)法国大于古代;撞击后

Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science Pub Date : 2001-10-31 DOI:10.1016/S1251-8050(01)01664-0

Guilhem Fabre , Martial Monteil

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引用次数: 3

摘要

对非常城市化的纽梅地区进行的水文地形学、考古学和地质历史综合研究证明，自古更新世末期开始挖掘维斯特河谷以来，山前斜坡和急流冲积扇就已经存在。城市化位于一个主要的更新世-全新世冲积扇的顶部。这扇扇子存在于上古时期，并在大帝国时期因人格化而被广泛截断。这个扇与其他小扇相连，形成了一个与现在的维斯特河冲积平原相连的集体冲积扇地貌。它现在仍在运作，就像在最近的1988年10月3日山洪灾害期间一样。

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Sur l'hydrogéomorphologie d'un espace à forte anthropisation urbaine : le site de Nı̂mes (Languedoc, France) du Pléistocène supérieur à l'Antiquité ; impacts postérieurs

Hydrogeomorphological, archaeological and geohistorical integrated studies of the very urbanised Nı̂mes area attest of piedmont slopes and torrential alluvial fan existence from the beginning of digging of the Vistre valley since the end of the ancient Pleistocene. The urbanisation is situated on top of a major superior Pleistocene–Holocene alluvial fan. This fan existed during the old Antiquity, and has been widely truncated by the anthropisation during the High Empire. This fan is connected to other little ones, and becomes a colluvial–alluvial fan landform connected to the present flood plain of the Vistre River. It is still functioning now, as during the recent flash flood disaster of 3 October 1988.

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Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science

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