Abstract
The results of comprehensive studies of bottom sediments and coastal transects in the Sea of Azov, obtained in recent years, have been analyzed. The changes in natural conditions that took place in the sea basin over the last 20 000 years correlate with the chronology of fluctuations in the level of the World Ocean. The stages of increase in the sea level due to melting of the glacier shields are considered. In view of this, it is noted that the change in the level of the World Ocean has made a decisive impact on the formation conditions of the current water area of the Sea of Azov.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
