 The Paleozoic Weathering Crust of the Kursk Magnetic Anomaly, KMA, is developed along the interior schists of the ferriginous-solicious formation of the Kursk series. In the Bandit Iron Formations, the Weathering Crust is represented by high-grade iron ores forming a series of deposits with bauxites. These deposits are confined to the ridges of Bandit Iron Formations, which tower up in the relief of the Precambrian and are overlained by a thick layer of sediments. Recently obtained rock material studied with the use of precision methods enabled a significant refinement and adjustment of the existing ideas about KMA bauxites. Based on their texture, structure, and mineral composition, five main types were singled out. One finely porous substantially beymite, two macro porous berthyrin beymite, three stony hydrohematite berthyrin beymite, four massive berthyrin kaolinite beymite, five pseudo-beam substantially gipsite, and this article was authored by A. D. Safko and M. U. of Chinakova. We are article.tv. Links in the description below.