Abstract
Almost maximal diversity of genetic landform types was provided in the Far East by peculiarity and changeability of external conditions of relief formation and confined set of agents. The specific interaction between processes of relief formation leads to diversity and high intensity of links in the geomorphosystem “mountain ridge joint”, securing its capacity to self-regulating and self-development. Catastrophic processes are widely distributed. Fluvial process is working towards the grading of relief and at the same time towards its dissection.
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