Slope-Channel Coupling as a Factor in the Evolution of Mountains

Nominated as an outstanding Ph. D. thesis by the University of Silesia in Katowice, Poland Dendrochronological record of lateral slope-channel (landsliding-erosion) coupling - the work presents results of an original approach, the first such comparative study until now Results of coupling in valley morphology are documented by numerous photos, schemes and maps Includes a scheme of mid-mountain landscape evolution based on observations of slope-channel coupling New dendrochronological tool for analyses of landslide activity was used - examples of spatial-temporal analyses (presentations of landslide dynamics) are provided Includes supplementary material: sn.pub/extras

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