The phenomenon of «Deep water» influx from the Earth's interior and its role in the development of the earth

The phenomenon of extensive permanent influx of the «deep-water» to the hydrosphere of the Earth characterized by a high content of various chemical components, including mineral and toxic elements of deep origin is considered. Results of analysis of large amount of experimental data suggest that «deep-water» is a source of formation and permanent supplement of the ocean water with stable salinity, chemical and isotopic composition, and the formation of various mineralized water deposits. «Deep-water» can cause formation of sub-standard water clusters within the underground fresh water fields, affecting their ecological quality.