Abstract
The basic mechanisms producing rough surfaces during geomorphological evolution are studied by carrying out model experiments and analyzing the results in terms of fractal scaling. We have been able to find an experimental evidence for kinetic roughening in our micromodel of mountain ranges. We have observed that during the watering of an initially smooth ridge made of a mixture of granular materials, the surface evolves into a shape analogous to actual mountain profiles with self-affine geometry. For the exponents describing respectively the spatial and the temporal scaling of the surface width, α=0.78±0.05 and β≈0.9 have been obtained. Our value for the static exponent α is in very good agreement with several earlier results for various mountains and we have calculated the estimate α=0.8±0.1 for a set of genuine transect profiles taken in the Dolomites, Italy. The results are interpreted in terms of “landslides” of widely scattered magnitudes.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
