Glacially-induced scaling relations in mountain drainage basins

River networks define specific scaling relations in the landscape. Accordingly, contributing area scales with local slope gradient controlling geomorphic process domains hence rates of erosion; and channel-reach hydraulic geometry and morphology. In currently glaciated environments ice flows possess peculiar geomorphic erosion and transport laws which likely disturb pre-glacial landscape structure and superimpose "glacial" scaling dependences. On such premise, it is hypothesized that formerly glaciated environments currently exhibit transient scaling dependences that deviate significantly from those documented in unglaciated analogs. Study sites are drawn from the Coast Mountains of British Columbia. Results show direct spatial scale linkages and generalized departure from unglaciated scaling relations at all levels. Glacial macro-forms, by imposing local channel gradient and degree of colluvial-alluvial coupling, affect the spatial distribution of process domains, which in turn control channel-reach morphology and hydraulic geometry. In particular, morphometric characteristics of relict glacial troughs introduce a peculiar colluvial-alluvial transition trend in the area-slope space. Hanging valleys, which enclose purely alluvial riffle-pool reaches separate strongly-coupled colluvial reaches located both up- and down-stream. Transitions across process domains tend to reset downstream trends of channel width, depth, and D95. Exponents of area-width and area-depth relations deviate significantly from 0.5 and 0.33. Specifically, colluvial channels exhibit higher downstream channel widening, while fluvial reaches denote negative (downstream narrowing) or nearly null exponents. To model channel width, a Manning-based expression, which expresses roughness as a function of D95, is applied. Complex channel-width trends that were measured in the field are described reasonably well. Channel width in colluvial reaches is consistently underestimated. The stepped topography of