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The distribution and cryolitological structure of the Ice Complex deposits (IC) in mountain regions of North-Eastern Russia is studied very poor. These ice-rich syngenetic deposits with wide ice-wedges are known in river valleys around gold minings, but they have not been practically studied. In the summer of 2018, field studies of the IC in the open-cut minings in the Debin and Susuman river valleys were conducted. That rivers are the left tributaries of the Kolyma River. IC was traced in the upstream of riv. Debin for about 40 km along it’s valley. In the Susuman river valley IC studied in the area of creeks Lukich and Ambardakh.