ALLUVIUM OF PRIKAMYE
Alluvium is widely developed in nature and involves a lot of minerals, deposits, building materials, water, oil, etc. The area of the Quaternary alluvium in Kama region is very vast and of high quality. Large sand and gravel deposits are covered by reservoirs. The history of the Quaternary alluvium is associated with rewashing of intermediate collectors – conglomerates. Neotectonic movement, кarst, climate change also influenced the formation of the alluvium. Complex usage of alluvium within the area of reservoirs can result in obtaining a series of goods – gravel, concrete sand, small precious minerals – gold, zirconium, titanium, etc.