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The region of the Prilenskoe Plateau is situated in the conditions of extreme continental climate, which is characterizing by the negative annual temperatures of the air (to -9.9°C) at their annual amplitudes to 100° C. The precipitation doesn’t exceed 250 mm. It is area of continuous permafrost by the thickness till 300-500 m. The karstic rocks of the territory researched are represented by the limestones and dolostones dated from Lower Cambrian.