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Rockfall both is a major process in shaping steep topography and a hazard in mountainous regions. Besides increasing thread due to thawing permafrost-stabilization in high-elevation areas, there are abundant permafrost-free over-steepened rockwalls r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5873c2f98a1961737ec4bbfa0f86f49
https://doi.org/10.5194/egusphere-egu22-1866
https://doi.org/10.5194/egusphere-egu22-1866
