In the Central Caucasus region. the intense process of deglaciation is identified as caused by cryoconite formation and accumulation. The fine earth materials were collected on the surfaces of Skhelda and Garabashi glaciers as well as from zonal soils of Baksan Gorge and were studied in terms of chemical. particle-size. https://spencertifieders.shop/product-category/recorders-cassette-players/