ФРАКТАЛЫ В ЭРОЗИОННОМ РАСЧЛЕНЕНИИ ПОВЕРХНОСТИ И АВТОКОЛЕБАНИЯ В ДИНАМИКЕ ГЕОМОРФОСИСТЕМ

A methodology for modeling a fractal scale-invariant set is put forward. The set characterizes the stages of formation of dissected erosional relief. The fractal nature of the process of erosion dissecting may cause self-oscillations in geomorphosystems and motion of the geosystems to the dynamic equilibrium. An algorithm of relief formation as a result of interaction between  F-  and  D- flows of matter.