Articles | Volume 15, issue 1
https://doi.org/10.5194/tc-15-303-2021
© Author(s) 2021. 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-15-303-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
22 Jan 2021
Research article |
| 22 Jan 2021
| 22 Jan 2021
Full crystallographic orientation (c and a axes) of warm, coarse-grained ice in a shear-dominated setting: a case study, Storglaciären, Sweden
Morgan E. Monz
CORRESPONDING AUTHOR
Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN, USA
Peter J. Hudleston
Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN, USA
David J. Prior
Department of Geology, University of Otago, Dunedin, New Zealand
Zachary Michels
Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN, USA
Sheng Fan
Department of Geology, University of Otago, Dunedin, New Zealand
Marianne Negrini
Department of Geology, University of Otago, Dunedin, New Zealand
Pat J. Langhorne
Department of Geology, University of Otago, Dunedin, New Zealand
Key Laboratory of Earth and Planetary Physics, Chinese Academy of Sciences, Beijing, China
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Cited
26 citations as recorded by crossref.
- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- Progresses in studies on crystallographic preferred orientations in experimentally deformed ice Q. WANG & C. QI 10.3724/j.issn.1007-2802.20240103
- Evolution of crystallographic preferred orientations of ice sheared to high strains by equal-channel angular pressing Q. Wang et al. 10.5194/tc-19-827-2025
- Effects of impurities on the ice microstructure of Monte Perdido Glacier, Central Pyrenees, NE Spain N. González-Santacruz et al. 10.1017/aog.2023.66
- Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
- Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica H. Still et al. 10.3389/feart.2022.828313
- Thrust faulting in glaciers? Re‐examination of debris bands near the margin of Storglaciären, Sweden M. Monz et al. 10.1111/bor.12549
- Acoustic velocity measurements for detecting the crystal orientation fabrics of a temperate ice core S. Hellmann et al. 10.5194/tc-15-3507-2021
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Kinking facilitates grain nucleation and modifies crystallographic preferred orientations during high-stress ice deformation S. Fan et al. 10.1016/j.epsl.2021.117136
- Freezing and Thawing of D2O/Sand Mixtures Investigated by Neutron Diffraction L. Kalvoda et al. 10.3390/cryst11080961
- On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
- Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps S. Hellmann et al. 10.5194/tc-15-677-2021
- Microstructures in a shear margin: Jarvis Glacier, Alaska C. Gerbi et al. 10.1017/jog.2021.62
- Grain growth of natural and synthetic ice at 0 °C S. Fan et al. 10.5194/tc-17-3443-2023
- An initial study of interference coloration for quantifying the texture and fabric of ice C. Owen & H. Hendrikse 10.1016/j.coldregions.2022.103735
- Crystallographic preferred orientation (CPO) patterns in uniaxially compressed deuterated ice: quantitative analysis of historical data N. Hunter et al. 10.1017/jog.2022.95
- Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica F. Lutz et al. 10.5194/tc-16-3313-2022
- A magnetic fabric study of the origin of englacial debris bands at Fláajökull, Southeast Iceland W. Jacobson 10.1016/j.coldregions.2023.104051
- Linear-viscous flow of temperate ice C. Schohn et al. 10.1126/science.adp7708
- A borehole trajectory inversion scheme to adjust the measurement geometry for 3D travel-time tomography on glaciers S. Hellmann et al. 10.5194/se-14-805-2023
- Structures and Deformation in Glaciers and Ice Sheets S. Jennings & M. Hambrey 10.1029/2021RG000743
- Elastic wave propagation in anisotropic polycrystals: inferring physical properties of glacier ice N. Rathmann et al. 10.1098/rspa.2022.0574
- Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica R. Thomas et al. 10.3389/feart.2021.702213
- Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C S. Fan et al. 10.5194/tc-14-3875-2020
- Constraining Ice Shelf Anisotropy Using Shear Wave Splitting Measurements from Active‐Source Borehole Seismics F. Lutz et al. 10.1029/2020JF005707
24 citations as recorded by crossref.
- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- Progresses in studies on crystallographic preferred orientations in experimentally deformed ice Q. WANG & C. QI 10.3724/j.issn.1007-2802.20240103
- Evolution of crystallographic preferred orientations of ice sheared to high strains by equal-channel angular pressing Q. Wang et al. 10.5194/tc-19-827-2025
- Effects of impurities on the ice microstructure of Monte Perdido Glacier, Central Pyrenees, NE Spain N. González-Santacruz et al. 10.1017/aog.2023.66
- Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
- Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica H. Still et al. 10.3389/feart.2022.828313
- Thrust faulting in glaciers? Re‐examination of debris bands near the margin of Storglaciären, Sweden M. Monz et al. 10.1111/bor.12549
- Acoustic velocity measurements for detecting the crystal orientation fabrics of a temperate ice core S. Hellmann et al. 10.5194/tc-15-3507-2021
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Kinking facilitates grain nucleation and modifies crystallographic preferred orientations during high-stress ice deformation S. Fan et al. 10.1016/j.epsl.2021.117136
- Freezing and Thawing of D2O/Sand Mixtures Investigated by Neutron Diffraction L. Kalvoda et al. 10.3390/cryst11080961
- On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
- Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps S. Hellmann et al. 10.5194/tc-15-677-2021
- Microstructures in a shear margin: Jarvis Glacier, Alaska C. Gerbi et al. 10.1017/jog.2021.62
- Grain growth of natural and synthetic ice at 0 °C S. Fan et al. 10.5194/tc-17-3443-2023
- An initial study of interference coloration for quantifying the texture and fabric of ice C. Owen & H. Hendrikse 10.1016/j.coldregions.2022.103735
- Crystallographic preferred orientation (CPO) patterns in uniaxially compressed deuterated ice: quantitative analysis of historical data N. Hunter et al. 10.1017/jog.2022.95
- Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica F. Lutz et al. 10.5194/tc-16-3313-2022
- A magnetic fabric study of the origin of englacial debris bands at Fláajökull, Southeast Iceland W. Jacobson 10.1016/j.coldregions.2023.104051
- Linear-viscous flow of temperate ice C. Schohn et al. 10.1126/science.adp7708
- A borehole trajectory inversion scheme to adjust the measurement geometry for 3D travel-time tomography on glaciers S. Hellmann et al. 10.5194/se-14-805-2023
- Structures and Deformation in Glaciers and Ice Sheets S. Jennings & M. Hambrey 10.1029/2021RG000743
- Elastic wave propagation in anisotropic polycrystals: inferring physical properties of glacier ice N. Rathmann et al. 10.1098/rspa.2022.0574
- Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica R. Thomas et al. 10.3389/feart.2021.702213
2 citations as recorded by crossref.
- Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C S. Fan et al. 10.5194/tc-14-3875-2020
- Constraining Ice Shelf Anisotropy Using Shear Wave Splitting Measurements from Active‐Source Borehole Seismics F. Lutz et al. 10.1029/2020JF005707
Latest update: 11 May 2025
Short summary
We present full crystallographic orientations of warm, coarse-grained ice deformed in a shear setting, enabling better characterization of how crystals in glacial ice preferentially align as ice flows. A commonly noted c-axis pattern, with several favored orientations, may result from bias due to overcounting large crystals with complex 3D shapes. A new sample preparation method effectively increases the sample size and reduces bias, resulting in a simpler pattern consistent with the ice flow.
We present full crystallographic orientations of warm, coarse-grained ice deformed in a shear...
