2022
DOI: 10.1080/17445647.2022.2144497
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Hydrological features of Matese Karst Massif, focused on endorheic areas, dolines and hydroelectric exploitation

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Cited by 6 publications
(2 citation statements)
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“…The second tunnel, in the Campania region, is fed by Biferno Springs on the Adriatic side of the Matese massif in Molise and by Torano and Maretto springs on the Tyrrhenian side of the same massif. The Matese karst massif is composed of limestone, dolomite, and marl carbonate platform and scarp deposits from the Triassic to Miocene [131,132]. The minimum and maximum discharge recorded around Caserta and Naples by the Acquedotto Campano was 2.1 m 3 /s and 5.3 m 3 /s, respectively.…”
Section: Contemporary Usesmentioning
confidence: 99%
“…The second tunnel, in the Campania region, is fed by Biferno Springs on the Adriatic side of the Matese massif in Molise and by Torano and Maretto springs on the Tyrrhenian side of the same massif. The Matese karst massif is composed of limestone, dolomite, and marl carbonate platform and scarp deposits from the Triassic to Miocene [131,132]. The minimum and maximum discharge recorded around Caserta and Naples by the Acquedotto Campano was 2.1 m 3 /s and 5.3 m 3 /s, respectively.…”
Section: Contemporary Usesmentioning
confidence: 99%
“…In this context, we note that the examination of sinkholes in the karst regions is significant not only from a morphometric point of view but also because most of the precipitation reaching the surface in these areas infiltrates into the depth through the dolines, which makes these landforms extremely important from a hydrological point of view. The sinkholes therefore play a significant role in the preservation of the caves, as well as in the protection of the karst water resources [58,59].…”
Section: Introductionmentioning
confidence: 99%