Articles | Volume 18, issue 4
https://doi.org/10.5194/tc-18-1669-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-18-1669-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Discriminating viscous-creep features (rock glaciers) in mountain permafrost from debris-covered glaciers – a commented test at the Gruben and Yerba Loca sites, Swiss Alps and Chilean Andes
Wilfried Haeberli
CORRESPONDING AUTHOR
Department of Geography, University of Zurich, 8057 Zurich, Switzerland
Lukas U. Arenson
BGC Engineering, Suite 500 – 980 Howe Street, Vancouver, BC V6Z 0C8, Canada
Julie Wee
Department of Geosciences, University of Fribourg, 1700 Fribourg, Switzerland
Christian Hauck
Department of Geosciences, University of Fribourg, 1700 Fribourg, Switzerland
Nico Mölg
ENVEO, Fürstenweg 176, 6020 Innsbruck, Austria
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Cited
15 citations as recorded by crossref.
- The Identification and Diagnosis of ‘Hidden Ice’ in the Mountain Domain B. Whalley 10.3390/glacies2030008
- Glacial to periglacial transition at the end of the last ice age in the subtropical semiarid Andes J. García et al. 10.1016/j.geomorph.2024.109379
- Multisource Synthesized Inventory of CRitical Infrastructure and HUman-Impacted Areas in AlaSka (SIRIUS) S. Kaiser et al. 10.5194/essd-16-3719-2024
- Combining facts and physics-based concepts with objective treatment of landsystem relations for documenting viscous flow features (rock glaciers) in mountain permafrost: examples from Nuristan/Hindu Kush, Galena Creek (Absaroka Mountains) and Gruben (Swiss Alps) W. Haeberli et al. 10.1080/04353676.2025.2452760
- Seasonal ice storage changes and meltwater generation at Murtèl rock glacier (Engadine, eastern Swiss Alps): estimates from measurements and energy budgets in the coarse blocky active layer D. Amschwand et al. 10.5194/hess-29-2219-2025
- Characterizing ground ice content and origin to better understand the seasonal surface dynamics of the Gruben rock glacier and the adjacent Gruben debris-covered glacier (southern Swiss Alps) J. Wee et al. 10.5194/tc-18-5939-2024
- Derebaşı (Kaçkar Dağı) Kaya Buzulunun Jeomorfolojisi Ve Kinematik Özellikleri S. Yeşilyurt 10.46453/jader.1633480
- Inventorying rock glaciers in the Western Himalaya, India, and assessing their hydrological significance I. Bhat et al. 10.1016/j.geomorph.2024.109514
- Divergent Responses of Alpine Rock Glaciers to Climate Change: A Review of Ecological and Abiotic Dynamics S. Piccinelli & N. Cannone 10.1002/ppp.2278
- RGIK guidelines for compiling consistent rock glacier inventories F. Brardinoni et al. 10.1016/j.geomorph.2025.110050
- Creeping permafrost in Mexico: environmental status of “Nevado” Rock Glacier, Nevado de Toluca volcano V. Soto et al. 10.1007/s11629-025-9767-0
- The last years of Infiernos Glacier and its transition to a new paraglacial stage J. Revuelto et al. 10.1017/jog.2025.22
- Sub-surface processes and heat fluxes at coarse blocky Murtèl rock glacier (Engadine, eastern Swiss Alps): seasonal ice and convective cooling render rock glaciers climate-robust D. Amschwand et al. 10.5194/esurf-13-365-2025
- Will landscape responses reduce glacier sensitivity to climate change in High Mountain Asia? S. Harrison et al. 10.5194/tc-19-4113-2025
- Acceleration and interannual variability of creep rates in mountain permafrost landforms (rock glacier velocities) in the European Alps in 1995–2022 A. Kellerer-Pirklbauer et al. 10.1088/1748-9326/ad25a4
14 citations as recorded by crossref.
- The Identification and Diagnosis of ‘Hidden Ice’ in the Mountain Domain B. Whalley 10.3390/glacies2030008
- Glacial to periglacial transition at the end of the last ice age in the subtropical semiarid Andes J. García et al. 10.1016/j.geomorph.2024.109379
- Multisource Synthesized Inventory of CRitical Infrastructure and HUman-Impacted Areas in AlaSka (SIRIUS) S. Kaiser et al. 10.5194/essd-16-3719-2024
- Combining facts and physics-based concepts with objective treatment of landsystem relations for documenting viscous flow features (rock glaciers) in mountain permafrost: examples from Nuristan/Hindu Kush, Galena Creek (Absaroka Mountains) and Gruben (Swiss Alps) W. Haeberli et al. 10.1080/04353676.2025.2452760
- Seasonal ice storage changes and meltwater generation at Murtèl rock glacier (Engadine, eastern Swiss Alps): estimates from measurements and energy budgets in the coarse blocky active layer D. Amschwand et al. 10.5194/hess-29-2219-2025
- Characterizing ground ice content and origin to better understand the seasonal surface dynamics of the Gruben rock glacier and the adjacent Gruben debris-covered glacier (southern Swiss Alps) J. Wee et al. 10.5194/tc-18-5939-2024
- Derebaşı (Kaçkar Dağı) Kaya Buzulunun Jeomorfolojisi Ve Kinematik Özellikleri S. Yeşilyurt 10.46453/jader.1633480
- Inventorying rock glaciers in the Western Himalaya, India, and assessing their hydrological significance I. Bhat et al. 10.1016/j.geomorph.2024.109514
- Divergent Responses of Alpine Rock Glaciers to Climate Change: A Review of Ecological and Abiotic Dynamics S. Piccinelli & N. Cannone 10.1002/ppp.2278
- RGIK guidelines for compiling consistent rock glacier inventories F. Brardinoni et al. 10.1016/j.geomorph.2025.110050
- Creeping permafrost in Mexico: environmental status of “Nevado” Rock Glacier, Nevado de Toluca volcano V. Soto et al. 10.1007/s11629-025-9767-0
- The last years of Infiernos Glacier and its transition to a new paraglacial stage J. Revuelto et al. 10.1017/jog.2025.22
- Sub-surface processes and heat fluxes at coarse blocky Murtèl rock glacier (Engadine, eastern Swiss Alps): seasonal ice and convective cooling render rock glaciers climate-robust D. Amschwand et al. 10.5194/esurf-13-365-2025
- Will landscape responses reduce glacier sensitivity to climate change in High Mountain Asia? S. Harrison et al. 10.5194/tc-19-4113-2025
Latest update: 27 Oct 2025
Short summary
Rock glaciers in ice-rich permafrost can be discriminated from debris-covered glaciers. The key physical phenomenon relates to the tight mechanical coupling between the moving frozen body at depth and the surface layer of debris in the case of rock glaciers, as opposed to the virtually inexistent coupling in the case of surface ice with a debris cover. Contact zones of surface ice with subsurface ice in permafrost constitute diffuse landforms beyond either–or-type landform classification.
Rock glaciers in ice-rich permafrost can be discriminated from debris-covered glaciers. The key...