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Kozhukhovskaya metro line is under construction in the southeast of Moscow now. The geological cross-section at the construction site shows Carboniferous limestone at a depth of 30-65 m, overlain by Jurassic and Quaternary clay, loam, sand and sandy loam. The principle geohazards originate from the presence of the thick horizon of water-saturated sandy and sandy-loamy deposits. These deposits serve as an enclosing medium for the future metro tunnel. The deposits along the route were typified according to their res...