Evaluation of cliff recession in the Valle dei Templi in Agrigento (Sicily)

The sacral complex of the Valle dei Templi in Agrigento, added in the UNESCO Heritage Site List, stands over the crest of a rigid calcarenite cuesta, which overlies a layer of partially saturated (S=6–12%) carbonate sand. In turn, the sand stratum lies on a thick stratum of clays. The environment is...

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Bibliographic Details
Published inEngineering geology Vol. 192; pp. 129 - 138
Main Authors Ercoli, Laura, Zimbardo, Margherita, Nocilla, Nicola, Nocilla, Alessandra, Ponzoni, Elisa
Format Journal Article
LanguageEnglish
Published Elsevier B.V 18.06.2015
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