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The archaeologic site from Basarabi is digged into a lithological generated hill, consisting of chalks and chalky marnes, where Senonian occurs continuously over the Baremiene limestone from the valley Carasu flank, or over the Aptiene gravels. The limestone from Basarabi is compact, with variable thickness from 42 m to 95 m, and below them there are marl and limestone. It is white with flint nodule with 91% CaCO3. From geological and technical point of view, could be identified semi-hard rocks (limestone, limesto...