In this paper the hydrogeological setting of Rome is figured out. This setting has been strongly influenced by different factors as tectonic activity, volcanism and seal level variations. The conceptual model of the groundwater flow in the roman area is represented by four aquifers, three of which being overlappingones. These aquifers flow from peripheral sectors of the study area toward Tiber and Aniene Rivers and the Sea.

Mazza, R., Vigna, F.L., Capelli, G., Dimasi, M., Mancini, M., Mastrorillo, L. (2016). Hydrogeology of Rome. ACQUE SOTTERRANEE, 4(4/142), 19-30 [10.7343/AS-129-15-0156].

Hydrogeology of Rome

MAZZA, Roberto
;
CAPELLI, Giuseppe;MASTRORILLO, LUCIA
2016

Abstract

In this paper the hydrogeological setting of Rome is figured out. This setting has been strongly influenced by different factors as tectonic activity, volcanism and seal level variations. The conceptual model of the groundwater flow in the roman area is represented by four aquifers, three of which being overlappingones. These aquifers flow from peripheral sectors of the study area toward Tiber and Aniene Rivers and the Sea.
Mazza, R., Vigna, F.L., Capelli, G., Dimasi, M., Mancini, M., Mastrorillo, L. (2016). Hydrogeology of Rome. ACQUE SOTTERRANEE, 4(4/142), 19-30 [10.7343/AS-129-15-0156].
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/11590/291295
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