Ice-rich syncryogenic (termed “Ice Complex”) deposits are common in northern East Siberia and constitute the most important feature of the Quaternary geology of the region. The Ice Complex formed throughout the Late Pleistocene and not only contains an archive of paleoenvironmental proxies such as Pleistocene faunal remains. but also comprises a record of human habitation spanning ∼50... https://thehookahlabes.shop/product-category/water-coloring/