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A. Scheidegger (1968)
Horton's Laws of Stream Lengths and Drainage AreasWater Resources Research, 4
R. Shreve (1969)
Stream Lengths and Basin Areas in Topologically Random Channel NetworksThe Journal of Geology, 77
Smart Smart (1969)
The topological properties of channel networksBull. Geol. Soc. Amer., 80
Ranalli Ranalli, Scheidegger Scheidegger (1968)
A test of the topological structure of river netsInt. Ass. Sci. Hydrol. Bull., 13
J. Smart (1969)
Topological Properties of Channel NetworksGeological Society of America Bulletin, 80
Morisawa Morisawa (1962)
Quantitative geomorphology of some watersheds in the Appalachian plateauBull. Geol. Soc. Amer., 73
Scheidegger Scheidegger (1967)
Random graph patterns of drainage basins, Hydrological aspects of the utilization of waterInt. Ass. Sci. Hydrol. Publ., 76
W. James, W. Krumbein (1969)
Frequency Distributions of Stream Link LengthsThe Journal of Geology, 77
J. Smart (1968)
MEAN STREAM NUMBERS AND BRANCHING RATIOS FOR TOPOLOGICALLY RANDOM CHANNEL NETWORKSHydrological Sciences Journal-journal Des Sciences Hydrologiques, 13
M. Melton (1957)
analysis of the relations among elements of climate, surface properties, and geomorphology
M. Morisawa (1962)
Quantitative Geomorphology of Some Watersheds in the Appalachian PlateauGeological Society of America Bulletin, 73
Smart Smart (1968)
Mean stream numbers and branching ratios for topologically random channel networksInt. Ass. Sci. Hydrol. Bull., 13
G. Ranalli, A. Scheidegger (1968)
A TEST OF THE TOPOLOGICAL STRUCTURE OF RIVER NETSHydrological Sciences Journal-journal Des Sciences Hydrologiques, 13
R. Shreve (1966)
Statistical Law of Stream NumbersThe Journal of Geology, 74
J. Smart (1968)
Statistical Properties of Stream LengthsWater Resources Research, 4
The Smart and Scheidegger stream length models are compared and shown to have similar concepts. Discrepancies in the general conclusions reached by the two authors arise from different methods of developing the models and of making comparisons with observation. The results of my analysis of Scheidegger's procedures and the results of tests designed to avoid some of the difficulties encountered there fail to lend any support to the suggestion that interior link lengths increase with stream order.
Water Resources Research – Wiley
Published: Dec 1, 1969
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