Traditional and modem concepts of the geography of arctic soils are an
alyzed, and recently obtained soil data are discussed. A new approach
to the interpretation of climatic and geogenic (parent materials and r
elief) factors of pedogenesis is elucidated. The new concept of the zo
nation of arctic soils is suggested. The same set of pedogenic process
es is observed throughout the whole territory of the Arctic; the clima
te of this region is generally humid. However, a sharp increase in mes
o-and microclimatic diversity at high latitudes dictated by geogenetic
factors leads to the substantial divergence of soils including the ap
pearance of arid phenomena. One of the possible integral zonal/subzona
l divisions of the polar territories is proposed.