A fractal analysis is given of surface drainage networks obtained from
erosion plot data. Of particular interest is the comparison of the fr
actal dimension of micro-basins to that of major river systems. Fracta
l dimensions were estimated using Richardson's method and using a rela
tionship based on Horton's bifurcation and length ratios. The small-sc
ale fractal dimensions obtained in this study are generally in good ag
reement with reported values for large-scale river systems. In additio
n to these results, the article also derives the fractal dimension of
networks in a framework that allows differences in previously proposed
relationships to be delineated.