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Earthquake weak motions and noise measurements unravel significant site amplification effects in the Val d’Agri basin (southern Italy)
Forward modelling of Bouguer anomalies along a transect of the Southern Apennines and the Southern Tyrrhenian Sea (Italy)
Structural investigation of background features and normal faults affecting the Calcari con Selce formation, Southern Apennines, Italy
Rift inheritance controls the switch from thin- to thick-skinned thrusting and basal décollement re-localization at the subduction-to-collision transition
Crystal Chemistry and Thermal Behavior of Fe-Carpholite from the Pollino Massif, Southern Italy
Self-constrained inversion of potential fields through a 3D depth weighting
Depositional processes and environmental settings in rock shelters: the case of the prehistoric Oscurusciuto site (Southern Italy)
Epistemic Uncertainties in Local Earthquake Locations and Implications for Managing Induced Seismicity
Naturally Occurring Asbestiform Minerals in Italian Western Alps and in Other Italian Sites
Latest Villafranchian climate and landscape reconstructions at Pirro Nord (southern Italy)
U-Pb detrital zircon ages and compositional features of Bifurto quartz-rich sandstones from Southern Apennines (Southern Italy): comparison with Numidian Flysch sandstones to infer source area
Different stacking patterns along an active fold-and-thrust belt—Acerenza Bay, Southern Apennines (Italy)
The equivalent pore aspect ratio as a tool for pore type prediction in carbonate reservoirs
Mass transport deposits overprinted by contractional tectonics: a case study from the southern Apennines of Italy
Assessing uncertainties in high-resolution, multifrequency receiver-function inversion: A comparison with borehole data
Ultrasonic wave velocity measurements for detecting decay in carbonate rocks
Abstract Small-size karst landforms may potentially provide very useful information to fully understand the behaviour of karst systems and their dynamics. In this chapter we demonstrate the need to pay attention to such features. ‘Inghiottitoio della Masseria Rotolo’, located in a remarkable karst area of southern Italy, has in recent years become the most controversial and discussed speleological site in Apulia. Even though it has been known for several decades, recently excavation work has allowed cavers to enter a huge karst system, eventually reaching the water table. The total depth of the cave is now 324 m, making it the deepest in the region. This chapter summarizes the history of discoveries at the site, starting from the description of the polje, also including information about the link between toponymy and karst. The works carried out at the swallet site are then described to emphasize the importance of the often neglected small-size karst features. In fact, when carefully observed and studied, these might be able to shed new light and greatly increase our knowledge about karst. The final part of the chapter deals with the cave system and provides an outline of the ongoing research.
Evaluating the susceptibility to anthropogenic sinkholes in Apulian calcarenites, southern Italy
Abstract Sinkholes are the main hazard related to underground voids of both natural and anthropogenic origin. Instabilities developing underground may propagate upwards in a dramatic manner and reach the surface in the form of a sinkhole. The Apulia region in southern Italy is an interesting case study due to the outcropping of soluble rocks throughout the region. These rocks are affected by karst processes and have a high number of anthropogenic cavities. The latter were excavated by humans at different times for a variety of purposes. The worrying recent increase in the number of sinkhole events registered in Apulia led us to collect information on natural and anthropogenic sinkholes in Apulia. We focused on anthropogenic cavities, mostly excavated in Plio-Pleistocene calcarenites, and characterized the rock masses before using two- and three-dimensional parametric numerical analyses to model the instability processes, with the aim of exploring the failure mechanisms that lead to the occurrence of sinkholes. The parametric studies allowed us to carry out a preliminary evaluation of the stability conditions through simple charts designed for use in the field.