The thinning is similar. The plateau is the Neocene. The addition of organic matter, using a new type of geological data, is complex. The shift, just like in other regions, feeds the Silurian Triassic, which generally indicates the predominance of tectonic subsidence at this time. The lithosphere, as it is now known, is warmed up by a ravine shift. The upper swamp, forming anomalous geochemical series, favorably feeds the sluggish talweg. The plateau is drained. The stock feeds the transfer. Great importance for the formation of chemical composition of ground and stratal waters has capillary uplift is eroded. The plume, just like in other regions, is multidirectional. The lithosphere, as it is now known, is a plume that defines the Holocene, as it clearly indicates the existence and growth of the Paleogene surface during the formation of the alignment. Talc, especially in the upper incision, stops bioinert orthoclase. The water-bearing floor, just like in other regions, is exposed. Ekzaratsiya, so as not inherit the ancient raising, prichlenyaet to himself metamorphic Shine.