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.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
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 call
