The distinctive properties of frozen soils compared to the Talys are their staining or deposition in them, which prevents the natural circulation of water, although pebble sediments are also found that are frozen to a considerable depth, in peat bogs there is a multi -layer permafrost on the outskirts of the valleys, consisting of interspersed peat and ice. Then there is the so -called dry permafrost in clay, sandy and indigenous rocks, where it is difficult to catch from ordinary melt soils.
