Hydrogeology of Rome

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Roberto Mazza *
Francesco La Vigna
Giuseppe Capelli
Michele Dimasi
Marco Mancini
Lucia Mastrorillo
(*) Corresponding Author:
Roberto Mazza | roberto.mazza@uniroma3.it

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.

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