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J. Flint (1980)
Tributary arrangements in fluvial systemsAmerican Journal of Science, 280
A. Abrahams (1980)
A Multivariate Analysis of Chain Lengths in Natural Channel NetworksThe Journal of Geology, 88
W. James, W. Krumbein (1969)
Frequency Distributions of Stream Link LengthsThe Journal of Geology, 77
W. Cochran (1952)
The $\chi^2$ Test of Goodness of FitAnnals of Mathematical Statistics, 23
A. D. Abrahams (1980a)
Divide angles and their relation to interior link lengths in natural channel networksGeographical Analysis, 12
S. Edition, N. Nie, K. Steinbrenner (1970)
Statistical Package for the Social Sciences
Analyses of three different areas indicate that chain curvature controls chain length indirectly through valley‐side plan form. It follows that, since concave chains on one side of a stream are usually matched by convex chains on the other side, tributary development and abstraction do not occur independently along either side of a stream, as has hitherto been assumed.
Earth Surface Processes and Landforms – Wiley
Published: Jan 1, 1982
Keywords: ;
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