Abstract
The analysis of special-temporal distribution of eolian sands surrounding highlands with humid climate reveals a connection between active deflation-accumulation processes and the level of receiving basins - seas and lakes. Accumulation of eolian sands in the sea coastal zone in the Far East corresponds to Early and Late Wurm regressions and even to small regression in Holocene. The conditions most favorable for eolian processes took place during regressions in the mouths of large rivers with the vast areas of sandy ground without mantle of submersed plants. Such conditions existed in Late Pleistocene and Holocene in different climates but in similar situations - regression of basins.
Sign-in/Register to access full text options 
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.
