Abstract:<p>Within the extensive periglacial belt of the dry Andean high mountain range (17&#176;30&#8217;S to 35&#176;S), the most visible expression of creeping mountain permafrost is the occurrence of rock glaciers, which have been studied systematically in the last decades (e.g. Schrott, 1996; Trombotto et al., 1999; Halla et al. 2021). Active, inactive and relict rock glaciers are included in regional and national inventories (e.g. IANIGLA-CONICET 2018), whereas the spatial di… Show more
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