Most of the land surface of the earth is formed by valley slopes. At a given point on the ground surface it is normally possible to follow the line of maximum slope downwards until a drainage channel is reached; moreover a causal relation between the slope and the channel is apparent. This feature has been little remarked upon, possibly because it is so widespread as to seem part of the natural order. It is nevertheless a fundamental and remarkable feature of the earth’s surface form. <...>

Slope profile analysis: the system of best units by A. young Hillslope process-response models based on the continuity equation by
M. J.KIRKBY
An application of the concept of threshold slopes to the Laramie Mountains, Wyoming by m. a. carson
State, environment and attribute in scree-slope studies by j. в. thornes
Micro-erosion processes and factors affecting slope development in the Lower Swansea Valley by e.m. bridges and d.m. harding
Slope form and geomorphological process: an Australian example by
R.R. ARNETT
The role of snow avalanches in the evolution of alpine talus slopes by B.H.LUCKMAN
Landsliding on the Jurassic escarpment near Rockingham, Northamptonshire by R.J. CHANDLER
Some examples of mudflow and rockfall activity in north-east Ireland by
D.B. PRIOR, N. STEPHENS and G.R. DOUGLAS
Relationships between slope form and soil properties developed over Chalk parent materials by p.a.furley
The relationship between soil patterns and slope form in the Ettrick Association, south-east Scotland by w. a. d. Whitfield and
P. A. FURLEY
The British Geomorphological Research Group The Institute of British Geographers Publications in print

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