Abstract

A paleochannel and paleotributary of the Ashamba River at the bottom of the Blue Bay in Black Sea near the city of Gelendzhik were discovered and studied using broadband seismoacoustic profiling. A basic description of the geomorphology of the Blue Bay bottom is presented. The technology for studying bottom paleostructures of the coastal sea zone by means of broadband seismoacoustic profiling with a different directional diagram and GPS navigation is presented. The composition and main characteristics of the equipment used are presented. The results of profiling and transverse profiles of the paleochannel and paleotributary of the Ashamba River are presented, as well as their geomorphological analysis. Gas flares accompanying the paleochannel of the Ashamba River were discovered. A detailed map of the river paleostructures of the Blue Bay bottom and the discovered gas flares has been compiled.

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