Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-977-2016
© Author(s) 2016. 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-10-977-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
12 May 2016
Research article |
| 12 May 2016
Frozen debris lobe morphology and movement: an overview of eight dynamic features, southern Brooks Range, Alaska
Margaret M. Darrow
CORRESPONDING AUTHOR
Department of Mining and Geological Engineering, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA
Nora L. Gyswyt
Department of Mining and Geological Engineering, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA
Jocelyn M. Simpson
Department of Mining and Geological Engineering, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA
Ronald P. Daanen
Alaska Division of Geological & Geophysical Surveys, Fairbanks, Alaska 99709, USA
Trent D. Hubbard
Alaska Division of Geological & Geophysical Surveys, Fairbanks, Alaska 99709, USA
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Cited
16 citations as recorded by crossref.
- The Ac-5 (Fejokoo) quadrangle of Ceres: Geologic map and geomorphological evidence for ground ice mediated surface processes K. Hughson et al. 10.1016/j.icarus.2017.09.035
- Permafrost thaw‐related slope failures in Alaska’s Arctic National Parks, c. 1980–2019 D. Swanson 10.1002/ppp.2098
- Effect of grain dissolution on sloping ground M. Cha & J. Santamarina 10.1038/s41598-022-26620-1
- Predicting movement using internal deformation dynamics of a landslide in permafrost M. Darrow et al. 10.1016/j.coldregions.2017.09.002
- Long-term analysis of cryoseismic events and associated ground thermal stress in Adventdalen, Svalbard R. Romeyn et al. 10.5194/tc-16-2025-2022
- Incorporating InSAR kinematics into rock glacier inventories: insights from 11 regions worldwide A. Bertone et al. 10.5194/tc-16-2769-2022
- Freeze-thaw induced landslides on grasslands in cold regions J. Yang et al. 10.1016/j.catena.2022.106650
- Mitigating embankment frost heave with nano-ZnO in the Arctic M. Zhang et al. 10.1016/j.jclepro.2023.136073
- The triggering factors of the Móafellshyrna debris slide in northern Iceland: Intense precipitation, earthquake activity and thawing of mountain permafrost Þ. Sæmundsson et al. 10.1016/j.scitotenv.2017.10.111
- Glacier–permafrost relations in a high-mountain environment: 5 decades of kinematic monitoring at the Gruben site, Swiss Alps I. Gärtner-Roer et al. 10.5194/tc-16-2083-2022
- Detection and Assessment of a Large and Potentially Tsunamigenic Periglacial Landslide in Barry Arm, Alaska C. Dai et al. 10.1029/2020GL089800
- Reconstructing movement history of frozen debris lobes in northern Alaska using satellite radar interferometry W. Gong et al. 10.1016/j.rse.2018.12.014
- Field investigation on the influence of periglacial processes on pile foundations on the Qinghai–Tibet plateau L. Guo et al. 10.1002/ppp.2092
- Disturbances in North American boreal forest and Arctic tundra: impacts, interactions, and responses A. Foster et al. 10.1088/1748-9326/ac98d7
- Recent Acceleration of a Rock Glacier Complex, Ádjet, Norway, Documented by 62 Years of Remote Sensing Observations H. Eriksen et al. 10.1029/2018GL077605
- Documenting the Collision of a Landslide in Permafrost with a Highway Embankment M. Darrow et al. 10.21663/EEG-D-23-00080
16 citations as recorded by crossref.
- The Ac-5 (Fejokoo) quadrangle of Ceres: Geologic map and geomorphological evidence for ground ice mediated surface processes K. Hughson et al. 10.1016/j.icarus.2017.09.035
- Permafrost thaw‐related slope failures in Alaska’s Arctic National Parks, c. 1980–2019 D. Swanson 10.1002/ppp.2098
- Effect of grain dissolution on sloping ground M. Cha & J. Santamarina 10.1038/s41598-022-26620-1
- Predicting movement using internal deformation dynamics of a landslide in permafrost M. Darrow et al. 10.1016/j.coldregions.2017.09.002
- Long-term analysis of cryoseismic events and associated ground thermal stress in Adventdalen, Svalbard R. Romeyn et al. 10.5194/tc-16-2025-2022
- Incorporating InSAR kinematics into rock glacier inventories: insights from 11 regions worldwide A. Bertone et al. 10.5194/tc-16-2769-2022
- Freeze-thaw induced landslides on grasslands in cold regions J. Yang et al. 10.1016/j.catena.2022.106650
- Mitigating embankment frost heave with nano-ZnO in the Arctic M. Zhang et al. 10.1016/j.jclepro.2023.136073
- The triggering factors of the Móafellshyrna debris slide in northern Iceland: Intense precipitation, earthquake activity and thawing of mountain permafrost Þ. Sæmundsson et al. 10.1016/j.scitotenv.2017.10.111
- Glacier–permafrost relations in a high-mountain environment: 5 decades of kinematic monitoring at the Gruben site, Swiss Alps I. Gärtner-Roer et al. 10.5194/tc-16-2083-2022
- Detection and Assessment of a Large and Potentially Tsunamigenic Periglacial Landslide in Barry Arm, Alaska C. Dai et al. 10.1029/2020GL089800
- Reconstructing movement history of frozen debris lobes in northern Alaska using satellite radar interferometry W. Gong et al. 10.1016/j.rse.2018.12.014
- Field investigation on the influence of periglacial processes on pile foundations on the Qinghai–Tibet plateau L. Guo et al. 10.1002/ppp.2092
- Disturbances in North American boreal forest and Arctic tundra: impacts, interactions, and responses A. Foster et al. 10.1088/1748-9326/ac98d7
- Recent Acceleration of a Rock Glacier Complex, Ádjet, Norway, Documented by 62 Years of Remote Sensing Observations H. Eriksen et al. 10.1029/2018GL077605
- Documenting the Collision of a Landslide in Permafrost with a Highway Embankment M. Darrow et al. 10.21663/EEG-D-23-00080
Saved (preprint)
Discussed (final revised paper)
Latest update: 21 Nov 2024
Short summary
Frozen debris lobes (FDLs) are slow-moving landslides in permafrost. Several FDLs are located adjacent to the Dalton Highway in Alaska's Brooks Range, and may pose a risk to adjacent infrastructure as their rates of movement increase. Through a comprehensive overview of eight FDLs, we found that FDL movement is asynchronous, surface features suggest that increased movement rates correlate to general instability, and the closest FDL will reach the current Dalton Highway alignment by 2023.
Frozen debris lobes (FDLs) are slow-moving landslides in permafrost. Several FDLs are located...
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