Moosfluh, towards a rock slope failure?
Landslides and rockfalls are critical hazards to take into account in mountainous areas and understanding their mechanisms is crucial for mitigation purposes. Due to climate change, permafrost degradation and glacial retreat are becoming more and more relevant to consider in steep terrain. Indeed cr...
Main Author: | |
---|---|
Other Authors: | , , |
Language: | English |
Published: |
ETH Zurich
2018
|
Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/456801 https://doi.org/10.3929/ethz-b-000456801 |
id |
ftethz:oai:www.research-collection.ethz.ch:20.500.11850/456801 |
---|---|
record_format |
openpolar |
spelling |
ftethz:oai:www.research-collection.ethz.ch:20.500.11850/456801 2023-05-15T17:58:10+02:00 Moosfluh, towards a rock slope failure? Galletti, Maud Manconi, Andrea Glueer, Franziska Picozzi, Matteo 2018 application/application/pdf https://hdl.handle.net/20.500.11850/456801 https://doi.org/10.3929/ethz-b-000456801 en eng ETH Zurich http://hdl.handle.net/20.500.11850/456801 doi:10.3929/ethz-b-000456801 info:eu-repo/semantics/openAccess http://rightsstatements.org/page/InC-NC/1.0/ In Copyright - Non-Commercial Use Permitted 2018 ftethz https://doi.org/20.500.11850/456801 https://doi.org/10.3929/ethz-b-000456801 2022-04-25T14:17:58Z Landslides and rockfalls are critical hazards to take into account in mountainous areas and understanding their mechanisms is crucial for mitigation purposes. Due to climate change, permafrost degradation and glacial retreat are becoming more and more relevant to consider in steep terrain. Indeed critically stressed slopes might react to these rapid changes and generate an increasing number of rock failure events. In the Great Aletsch region (Switzerland) glacial retreat has been considerable in the last decade and the adjacent southern slope (Moosfluh) has suffered progressive debuttressing, as well as increased deep-seated gravitational slope deformation (DSGSD) and enhanced rock failure phenomena. In this study, we investigate rockfall events occurring in the lower portions of the Moosfluh DSGSD in the 2017 summer season. We used a local network of three low-cost seismometers (raspberry shakes), webcam photos and field data to detect rockfalls and generate an event’s catalogue. Rockfall parameters as duration, amplitude, volume, runout, energy, as well as their spatial and temporal distribution, provided insights into the mechanisms driving the slope deformation. An increase in rockfall activity was detected at the beginning of August, corresponding to 3 days of heavy rainfalls. The weeks later followed a change in the displacement rate of the entire DSGSD. We also found that the majority of rockfalls occurred during night, pointing out a potential effect of daily surface temperature changes leading to rock contraction and eventually failure events. The peculiar spatial pattern of rockfall suggested temporally and spatially dependent activity for displacement in different domains of the moving mass. Finally, we calibrated a magnitude frequency relationship, which provides hints for mitigation strategies in Moosfluh as well as in other similar alpine areas. Other/Unknown Material permafrost ETH Zürich Research Collection |
institution |
Open Polar |
collection |
ETH Zürich Research Collection |
op_collection_id |
ftethz |
language |
English |
description |
Landslides and rockfalls are critical hazards to take into account in mountainous areas and understanding their mechanisms is crucial for mitigation purposes. Due to climate change, permafrost degradation and glacial retreat are becoming more and more relevant to consider in steep terrain. Indeed critically stressed slopes might react to these rapid changes and generate an increasing number of rock failure events. In the Great Aletsch region (Switzerland) glacial retreat has been considerable in the last decade and the adjacent southern slope (Moosfluh) has suffered progressive debuttressing, as well as increased deep-seated gravitational slope deformation (DSGSD) and enhanced rock failure phenomena. In this study, we investigate rockfall events occurring in the lower portions of the Moosfluh DSGSD in the 2017 summer season. We used a local network of three low-cost seismometers (raspberry shakes), webcam photos and field data to detect rockfalls and generate an event’s catalogue. Rockfall parameters as duration, amplitude, volume, runout, energy, as well as their spatial and temporal distribution, provided insights into the mechanisms driving the slope deformation. An increase in rockfall activity was detected at the beginning of August, corresponding to 3 days of heavy rainfalls. The weeks later followed a change in the displacement rate of the entire DSGSD. We also found that the majority of rockfalls occurred during night, pointing out a potential effect of daily surface temperature changes leading to rock contraction and eventually failure events. The peculiar spatial pattern of rockfall suggested temporally and spatially dependent activity for displacement in different domains of the moving mass. Finally, we calibrated a magnitude frequency relationship, which provides hints for mitigation strategies in Moosfluh as well as in other similar alpine areas. |
author2 |
Manconi, Andrea Glueer, Franziska Picozzi, Matteo |
author |
Galletti, Maud |
spellingShingle |
Galletti, Maud Moosfluh, towards a rock slope failure? |
author_facet |
Galletti, Maud |
author_sort |
Galletti, Maud |
title |
Moosfluh, towards a rock slope failure? |
title_short |
Moosfluh, towards a rock slope failure? |
title_full |
Moosfluh, towards a rock slope failure? |
title_fullStr |
Moosfluh, towards a rock slope failure? |
title_full_unstemmed |
Moosfluh, towards a rock slope failure? |
title_sort |
moosfluh, towards a rock slope failure? |
publisher |
ETH Zurich |
publishDate |
2018 |
url |
https://hdl.handle.net/20.500.11850/456801 https://doi.org/10.3929/ethz-b-000456801 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
http://hdl.handle.net/20.500.11850/456801 doi:10.3929/ethz-b-000456801 |
op_rights |
info:eu-repo/semantics/openAccess http://rightsstatements.org/page/InC-NC/1.0/ In Copyright - Non-Commercial Use Permitted |
op_doi |
https://doi.org/20.500.11850/456801 https://doi.org/10.3929/ethz-b-000456801 |
_version_ |
1766166720793280512 |