Rock glaciers—ice-rich cree** landforms typical of permafrost mountain ranges—can
develop an anomalous landslide-like behaviour called destabilisation. This behaviour is …

Relict rockglaciers are distinctive indicators of past permafrost occurrence. Their lower limit
is attributed to a former mean annual air temperature (MAAT) of below− 2° C. This study …

Abstract In the Nepalese Himalaya, there is little information on the number, spatial
distribution and morphometric characteristics of rock glaciers, and this information is …

The ongoing acceleration in rock glacier velocities concurrent with increasing air
temperatures, and the widespread onset of rock glacier destabilization have reinforced the …

Rock glaciers are an important geomorphic element of glaciated mountain landscapes, but
our understanding of their distribution and ages, controls on their development, and their …

This paper aims to evaluate sources of uncertainty and variability associated with rock
glacier inventories compiled from remotely sensed imagery. To this end, we ran three …

Rock glaciers are cree** bodies of ice and rock that account for an important part of the
mountain cryosphere. In this study, we investigated long‐term changes of the Laurichard …

Little information about the number, spatial distribution, and characteristics of rock glaciers in
Himachal Himalaya is available. This information is crucial to assess the hydrological …

Viscous-flow features in perennially frozen talus/debris called rock glaciers are being
systematically inventoried as part of the global climate-related monitoring of mountain …

Alpine permafrost occurrence in maritime climates has received little attention, despite
suggestions that permafrost may occur at lower elevations than in continental climates. To …