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Devil Landforms as Resources for Geotourism Development: An Example from Southern Apulia (Italy)

机译：魔鬼地形作为地质旅游开发的资源：以南部普利亚（意大利）为例

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摘要

The landscape of Murge Tarantine limestone ridge (southern Apulia, Italy) is marked by the presence of an isolated relief showing a singular shape and name, the Monte del Diavolo (i.e., the Devil’s Mount). The Monte del Diavolo is located in a very interesting area from a geological point of view since it shows an E–W trending high-fault scarp, the morphological effect of the right-lateral transtensive North Salento Fault Zone. The Monte del Diavolo is a small isolated conical relief reaching at its top 115 m above m.s.l.; it elevates about 20 m from the surrounding plain surface, stretching at about 95 m altitude. Its evolution has been influenced by the occurrence of strongly cemented breccia deposits, most likely due to cave roof collapse and calcite precipitation, which are more resistant to the karst denudation process than surrounding limestones. This paper would be the first step towards the cultural promotion of the Monte del Diavolo area, which is marked by geological and geomorphological peculiar features and by a relevant archaeological and natural heritage as well.
机译：Murge Tarantine石灰岩山脊（意大利阿普利亚南部）的景观以一个孤立的浮雕为标志，该浮雕显示出一个奇异的形状和名称，Monte del Diavolo（即魔鬼山）。从地质学的角度来看，Monte del Diavolo位于一个非常有趣的区域，因为它显示出一条E-W趋势的高断层陡坡，这是右侧萨兰托北部断裂带的形态学效应。 Monte del Diavolo是一个小的孤立的圆锥形浮雕，延伸到比m.s.l.高115 m的顶部;它从周围的平原表面升起约20 m，在约95 m的高度上伸展。其演化受到强烈胶结角砾岩沉积物的影响，最可能的原因是山洞顶塌陷和方解石沉淀，与周围的石灰石相比，它们对岩溶剥蚀过程的抵抗力更大。本文将是朝着蒙特·迪亚沃洛地区（Monte del Diavolo）地区进行文化推广的第一步，该地区的特征是地质和地貌特有的特征以及相关的考古和自然遗产。

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