Abstract
The dispersed sedimentary material in the snow–ice cover near the North Pole was analyzed directly for the first time. The composition of sediments in the snow–ice cover and vertical fluxes of the material from the ice water layer were studied at the maximal distance for the Northern Hemisphere from the continents. The data were obtained by sedimentation traps (for water) and in large volumes of melt water (for snow and ice). It has been revealed that the dispersed sedimentary material of aeolian genesis plays the leading role in snow and sea ice.
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.
