In the discovered sills among the sedimentary-terrigenous complex on the shore of the Baydaratskaya Bay of the Kara Sea (YNAO), minerals of PGM were discovered and studied. The compositions of minerals differ from known Ural deposits. The discovery of the minerals of the PGM is the first on the Torasoveiskaya area of the Polar Urals and one of the most northerly within the Ural fold belt.