SEASONAL VARIATION OF RELATIVE DEPTH THAW ANTHROPOGENIC SUCCESSIONS CENTRAL YAKUTIA
The paper discusses two varieties of thaw depth variation through restoration stages of the disturbed permafrost landscapes that function on loamy and sandy deposits of the high terraces on the right and left banks of the Lena River. Qualitative changes in the dynamics of seasonal thaw depth were found to occur in definite intervals of successional stages: herb, shrub-birch, larch (pine) – birch, and larch (pine).