Articles | Volume 11, issue 2
https://doi.org/10.5194/tc-11-841-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/tc-11-841-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 Mar 2017
Research article |
| 30 Mar 2017
Internal structure of two alpine rock glaciers investigated by quasi-3-D electrical resistivity imaging
Adrian Emmert
CORRESPONDING AUTHOR
Institute of Geography and Geology, University of Würzburg, 97074, Germany
Christof Kneisel
Institute of Geography and Geology, University of Würzburg, 97074, Germany
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Cited
32 citations as recorded by crossref.
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- 4D quantification of alpine permafrost degradation in steep rock walls using a laboratory‐calibrated electrical resistivity tomography approach R. Scandroglio et al. 10.1002/nsg.12149
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- Failure of Frozen Sandstone under Uniaxial Compression with Interpretation of Pressure Melting of Pore Ice from Electrical Resistance T. Wang et al. 10.1061/JGGEFK.GTENG-11025
- Geophysical measurements of the southernmost microglacier in Europe suggest permafrost occurrence in the Pirin Mountains (Bulgaria) G. Georgieva et al. 10.5194/tc-16-4847-2022
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- Pressure melting of pore ice in frozen rock under compression T. Wang et al. 10.1016/j.coldregions.2023.103856
- Recent evolution of an ice‐cored moraine at the Gentianes Pass, Valais Alps, Switzerland L. Ravanel et al. 10.1002/ldr.3088
- Three-dimensional subsurface architecture and its influence on the spatiotemporal development of a retrogressive thaw slump in the Richardson Mountains, Northwest Territories, Canada J. Kunz et al. 10.1080/15230430.2023.2167358
- Rock glaciers and mountain hydrology: A review D. Jones et al. 10.1016/j.earscirev.2019.04.001
- Petrophysical Joint Inversion Applied to Alpine Permafrost Field Sites to Image Subsurface Ice, Water, Air, and Rock Contents C. Mollaret et al. 10.3389/feart.2020.00085
32 citations as recorded by crossref.
- Dynamics and internal structure of a rock glacier: Inferring relationships from the combined use of differential synthetic aperture radar interferometry, electrical resistivity tomography and ground‐penetrating radar S. Buchelt et al. 10.1002/esp.5993
- Contextualizing lobate debris aprons and glacier-like forms on Mars with debris-covered glaciers on Earth M. Koutnik & A. Pathare 10.1177/0309133320986902
- Identifying mountain permafrost degradation by repeating historical electrical resistivity tomography (ERT) measurements J. Buckel et al. 10.5194/tc-17-2919-2023
- 4D quantification of alpine permafrost degradation in steep rock walls using a laboratory‐calibrated electrical resistivity tomography approach R. Scandroglio et al. 10.1002/nsg.12149
- Factors influencing the ground thermal regime in a mid-latitude glacial cirque (Hoyo Empedrado, Cantabrian Mountains, 2006–2020) A. Melón-Nava et al. 10.1016/j.catena.2022.106110
- Failure of Frozen Sandstone under Uniaxial Compression with Interpretation of Pressure Melting of Pore Ice from Electrical Resistance T. Wang et al. 10.1061/JGGEFK.GTENG-11025
- Geophysical measurements of the southernmost microglacier in Europe suggest permafrost occurrence in the Pirin Mountains (Bulgaria) G. Georgieva et al. 10.5194/tc-16-4847-2022
- Deciphering Small-Scale Seasonal Surface Dynamics of Rock Glaciers in the Central European Alps Using DInSAR Time Series S. Buchelt et al. 10.3390/rs15122982
- Small is strong: Post-LIA resilience of Europe's Southernmost glaciers assessed by geophysical methods A. Onaca et al. 10.1016/j.catena.2022.106143
- Is that a relict rock glacier? R. Colucci et al. 10.1016/j.geomorph.2019.02.002
- Internal structure and recent dynamics of a moraine complex in an alpine glacier forefield revealed by geophysical surveying and Sentinel-1 InSAR time series J. Kunz et al. 10.1016/j.geomorph.2021.108052
- Identification of Groundwater Using Geoelectrical Method VES (Vertical Electrical Sounding) in Karimunjawa City, Central Java M. Bahari et al. 10.1088/1742-6596/2392/1/012003
- Three‐dimensional investigation of an open‐ and a closed‐system Pingo in northwestern Canada J. Kunz & C. Kneisel 10.1002/ppp.2115
- Occurrence, evolution and ice content of ice‐debris complexes in the Ak‐Shiirak, Central Tien Shan revealed by geophysical and remotely‐sensed investigations T. Bolch et al. 10.1002/esp.4487
- Internal structure of a large, complex rock glacier and its significance in hydrological and dynamic behavior: A case study in the semi‐arid Andes of Argentina C. Villarroel et al. 10.1002/ppp.2132
- Glacier–Permafrost Interaction at a Thrust Moraine Complex in the Glacier Forefield Muragl, Swiss Alps J. Kunz & C. Kneisel 10.3390/geosciences10060205
- Improved estimation of ice and water contents in alpine permafrost through constrained petrophysical joint inversion: The Hoher Sonnblick case study M. Steiner et al. 10.1190/geo2020-0592.1
- Insights into a remote cryosphere: a multi-method approach to assess permafrost occurrence at the Qugaqie basin, western Nyainqêntanglha Range, Tibetan Plateau J. Buckel et al. 10.5194/tc-15-149-2021
- Rock glaciers of the semi-arid northwestern Himalayas: distribution, characteristics, and hydrological significance P. Pandey et al. 10.1016/j.catena.2024.107845
- Active layer and permafrost thickness in rock glaciers derived from geophysical methods in the semiarid Andes of Argentina C. Villarroel et al. 10.1016/j.geomorph.2020.107249
- Rock glaciers and the geomorphological evolution of deglacierizing mountains J. Knight et al. 10.1016/j.geomorph.2018.09.020
- Multi‐temporal 3D point cloud‐based quantification and analysis of geomorphological activity at an alpine rock glacier using airborne and terrestrial LiDAR V. Zahs et al. 10.1002/ppp.2004
- Quantification of permafrost creep provides kinematic evidence for classifying a puzzling periglacial landform Y. Hu et al. 10.1002/esp.5039
- Internal structure and palsa development at Orravatnsrústir Palsa Site (Central Iceland), investigated by means of integrated resistivity and ground‐penetrating radar methods A. Emmert & C. Kneisel 10.1002/ppp.2106
- Assessment of rock glaciers and their water storage in Guokalariju, Tibetan Plateau M. Li et al. 10.5194/tc-18-1-2024
- Numerical Analysis of Putative Rock Glaciers on Mount Sharp, Gale Crater, Mars J. Williams et al. 10.3390/rs14081887
- Mountain glacier-to-rock glacier transition D. Jones et al. 10.1016/j.gloplacha.2019.102999
- Pressure melting of pore ice in frozen rock under compression T. Wang et al. 10.1016/j.coldregions.2023.103856
- Recent evolution of an ice‐cored moraine at the Gentianes Pass, Valais Alps, Switzerland L. Ravanel et al. 10.1002/ldr.3088
- Three-dimensional subsurface architecture and its influence on the spatiotemporal development of a retrogressive thaw slump in the Richardson Mountains, Northwest Territories, Canada J. Kunz et al. 10.1080/15230430.2023.2167358
- Rock glaciers and mountain hydrology: A review D. Jones et al. 10.1016/j.earscirev.2019.04.001
- Petrophysical Joint Inversion Applied to Alpine Permafrost Field Sites to Image Subsurface Ice, Water, Air, and Rock Contents C. Mollaret et al. 10.3389/feart.2020.00085
Latest update: 14 Dec 2024
Short summary
We investigated the internal structure of two alpine rock glaciers to derive information on their development. Through a 3-D mapping of the electrical resistivity distribution of the subsurface, we could detect variations of ice content and delimit frozen and unfrozen structures. Our study shows that the development of the investigated rock glaciers is influenced by not only creep processes and remnant ice from past glaciations but also recently buried ice patches and refreezing meltwater.
We investigated the internal structure of two alpine rock glaciers to derive information on...
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