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  • developed to estimate erosion rates with exposed roots; (b) shows new advances through case studies; and finally, (c) discusses future lines of research to reduce methodological uncertainties and for making dendrogeomorphology more widely applicable.
  • if the material is smectite-rich or smectite-poor can help in prediction of processes and the erosion rates. Precipitation characteristics will determine the rate of weathering on smectite-rich surfaces. Smectite-poor materials appear to be more resistant
  • drivers. More attention should be paid in the future to investigating the evolution of these landforms over time, mostly through modelling studies. Although some badland areas determine on- and off-site environmental issues, others are spots of landscape
  • to find possible solutions and ways forward to render the preservation of the biancana landscape and its biodiversity more efficient.