Abstract: Climate and geomorphy arc the main factors of the formation of forest bogs in Hingganling and changbaishan. The bogs are both multiple in types and widespread in distribution. There exist not only the type of lower bog, but also that of middle bog and raised bog. They are chiefly distributed in the alluvial flat or valley and in the watershed. The succession process of forest bog is generalized into two kinds: (1) The formation of forest bogs as a result of the natural succession of forest vegetation under the influence of natural conditions. (2) The formation of forest bogs as a result of the bogginess in the vicinity of forestland.