The analysis deals with the scaling properties of infinite topological
ly random channel networks (ITRNs) first introduced by Shreve (1967, J
. Geol., 75: 179-186) to model the branching structure of rivers as a
random process. The expected configuration of ITRNs displays scaling b
ehaviour only asymptotically, when the ruler (or 'yardstick') length i
s reduced to a very small extent. The random model can also reproduce
scaling behaviour at larger ruler lengths if network magnitude and dia
meter are functionally related according to a reported deterministic r
ule. This indicates that subsets of ITRNs can be scaling and, although
ITRNs are asymptotically plane-filling due to the law of large number
s, scaling ITRNs can also display fractional dimension.