[HTML][HTML] Structurally controlled rock slope deformation in northern Norway
Gravitational forcing of oversteepened rock mass leads to progressive failure, including
rupture, cree**, sliding and eventual avalanching of the unstable mass. As the point of …
rupture, cree**, sliding and eventual avalanching of the unstable mass. As the point of …
Detailed rockslide map** in northern Norway with small baseline and persistent scatterer interferometric SAR time series methods
Rockslides have a high socioeconomic and environmental importance in many countries.
Norway is particularly susceptible to large rockslides due to its many fjords and steep …
Norway is particularly susceptible to large rockslides due to its many fjords and steep …
[HTML][HTML] Permafrost in monitored unstable rock slopes in Norway–new insights from temperature and surface velocity measurements, geophysical surveying, and …
The warming and subsequent degradation of mountain permafrost within alpine areas
represent an important process influencing the stability of steep slopes and rock faces. The …
represent an important process influencing the stability of steep slopes and rock faces. The …
Analyses of past and present rock slope instabilities in a fjord valley: Implications for hazard estimations
For quantitative hazard assessment it is necessary to define the magnitude–frequency
distribution and a temporal model of the landslide frequency. This is often complicated for …
distribution and a temporal model of the landslide frequency. This is often complicated for …
Analyzing complex rock slope deformation at Stampa, western Norway, by integrating geomorphology, kinematics and numerical modeling
The unstable rock slope, Stampa, above the village of Flåm, Norway, shows signs of both
active and postglacial gravitational deformation over an area of 11km2. Detailed structural …
active and postglacial gravitational deformation over an area of 11km2. Detailed structural …
Inheritance of ductile and brittle structures in the development of large rock slope instabilities: examples from western Norway
A Saintot, IHC Henderson… - Geological Society, London …, 2011 - lyellcollection.org
The high density of slope failures in western Norway is due to the steep relief and to the
concentration of various structures that followed protracted ductile and brittle tectonics. On …
concentration of various structures that followed protracted ductile and brittle tectonics. On …
Systematic map** of large unstable rock slopes in Norway
Historically, large rock slope failures impacting into a fjord and causing a several tens of
metre high displacement wave have been one of the natural hazards in Norway claiming …
metre high displacement wave have been one of the natural hazards in Norway claiming …
Paraglacial rock-slope failure following deglaciation in western Norway
AM Curry - Landscapes and Landforms of Norway, 2021 - Springer
The paraglacial framework describes the geomorphological response to glaciation and
deglaciation, whereby non-renewable, metastable, glacially conditioned sediment sources …
deglaciation, whereby non-renewable, metastable, glacially conditioned sediment sources …
Modern Methods of Rock Mass Characterisation and Rockfall Monitoring: A Review
Modern methods to characterise rock masses and monitor rockfalls and rock slope stability
are evolving incredibly fast during the last decade. The rapid increase in new techniques …
are evolving incredibly fast during the last decade. The rapid increase in new techniques …
Large landslides induced by fluvial incision in the Cenozoic Duero Basin (Spain)
The Pleistocene opening of the endorheic Duero River drainage basin (northwestern Spain
and central Portugal) has led to river incision, creation of steep valley sides, and …
and central Portugal) has led to river incision, creation of steep valley sides, and …