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Sinkhole evolution in the Apulian karst of southern Italy: a case study, with some considerations on sinkhole hazard

机译:意大利南部阿普利亚岩溶的污水坑演化:一个案例研究,并考虑了污水坑的危害

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摘要

Sinkholes are the main karst landforms characterizing the Salento Peninsula, which is the southernmost part of the Apulia region of southern Italy. They occur both as evolving recent phenomena and old or relict features testifying to ancient phases of karst processes acting in the area. Most of the sinkholes were formed by karst processes that may be reactivated, a risk to the anthropogenic structures nearby. To highlight such\uda subtle hazard, an area located a few kilometers from Lecce, the main town in Salento, was the subject of geological, morphological, and geophysical investigations. Historical\udanalysis of multi-year aerial photographs, in particular, allowed identification of several phases in the recent evolution of a particular sinkhole, and demonstrated the need to carefully evaluate the likely evolution of similar features in Salento.
机译:污水坑是代表意大利南部普利亚地区最南端的萨伦托半岛的主要喀斯特地貌。它们既发生在不断发展的新现象中,又表现出古老或遗迹的特征,证明了该地区岩溶作用的古代阶段。大部分的下陷都是由可能重新活化的岩溶过程形成的,这对附近的人为结构构成了风险。为了突出这种微妙的危害,距离萨伦托主要城镇莱切几公里的地区是地质,形态和地球物理研究的主题。特别是对多年航拍照片的历史\分析,可以确定特定污水坑近期演化中的几个阶段,并表明需要仔细评估萨伦托类似特征的可能演化。

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