A new method for analyzing the self-similarity and self-affinity of si
ngle-thread channels is proposed. It permits the determination of the
fractal scaling exponents, of the characteristic scales, and the evalu
ation of the degree of anisotropy for self-similar fractal lines. Base
d upon the application of this method to the Dniester and Pruth rivers
we established the self-similarity of the river pattern on small scal
es and the self-affinity on large scales. For these rivers we obtained
the fractal scaling exponents, the characteristic scales, and the ani
sotropy parameters. A computer model has been developed which simulate
s river patterns whose fractal properties are close to the properties
of natural objects. A generalized model of fractal behavior of natural
rivers is proposed. On the basis of self-affinity of natural and simu
lated rivers on large scales, a hypothesis has been formulated which e
xplains the violation of the dimension principle in the well-known rel
ation between the river length and the catchment area,