Reasons and mechanism for soil sliding processes in the Rebrnice area, Vipava valley, SW Slovenia
Geologija, 2007 A motorway Razdrto–Podnanos is being built across Rebrnice area in Vipava valley. There is limestone scree material deposed on flysch rocks.Limestones creeis unstable and gradually slides downslopes because of slope inclination, underground water and ...
Jernej Jež
doaj +1 more source
Rare, slow but impressive: > 43 ka of rockslide in river canyon incising crystalline rocks of the eastern Bohemian Massif [PDF]
, 2023 International audienceAbstract Despite significant progress in understanding the stability of rock slopes, little is known about the time scales of the evolution of slow-moving rockslides.
František Kuda +9 more
core +1 more source
Dinámica, Factores condicionantes y posibles causas de la formación de la tartera de Cambrils (Solsonès, Lleida) [PDF]
, 2022 Landslides and rockfalls are a common hazard in mountain areas like the Pyrenees. However, due to the difficulty of access and therefore of data acquisition, and the low density of population they are poorly studied.
Travé i Herrero, Anna +4 more
core +1 more source
, 2021 Landslide inventory mapping is vital for hazard vulnerability and mitigation in mountainous terrain. The present study seeks to tentatively identify large bedrock landslides and related features across the Gilgit area in the Gilgit-Baltistan Province of ...
Awan, Usman +2 more
core +1 more source
Glissements de terrain et évolution des versants
, 1984 The frequency of rotational and deep landslides on valley sides, entirely shaped in coherent rocks (granite, gneiss, calcarenite) reputed unfavourable to these mass movements when they are not weathered, is explained not only by the state of fracturation
Jeannine Raffy +3 more
core +2 more sources
Relation between land cover and landslide susceptibility in Val d'Aran, Pyrenees (Spain): historical aspects, present situation and forward prediction [PDF]
, 2019 The effects of land use and land cover (LULC) dynamics on landslide susceptibility are not fully understood. This study evaluates the influence of LULC on landslide susceptibility and assesses the historic and future LULC changes in a high mountain ...
Ma, Jinzhu +6 more
core +1 more source
Exposure of the settlements in the Republic of Dagestan to landslide processes
Наука. Инновации. ТехнологииThe object of the study is the landslide activity in the Republic of Dagestan. The paper considers the results of systematization and analysis of various sources containing information on the activity and danger of landslide processes in the settlements ...
V. V. Razumov +4 more
doaj +1 more source
The Age and Origin of Block Deposits in the Victorian Alps, Australia
Permafrost and Periglacial Processes, EarlyView.ABSTRACT Large periglacial block deposits are found in the mountains of southeastern Australia. Despite their widespread distribution, their mode of formation and age are poorly understood. These landforms hold considerable potential to shed light on the nature of cooling during glacial periods. In this paper we present a new study of block deposits in
Timothy T. Barrows +4 more
wiley +1 more source
Observations of coastal cliff landslide runout in southern California from 21 years of data
Earth Surface Processes and Landforms, Volume 51, Issue 6, June 2026.Runout distance from coastal cliff landslides along the coast of northern San Diego County, California USA between 2001 and 2023 were mapped and quantified. Results indicated cliff height influenced runout distance, and that 98% of maximum runout distances were less than half the cliff height.
Catriona F. Thompson, Adam P. Young
wiley +1 more source
Talus slopes above creek in Teocalli Mountains, Alaska, August 1914
, 1914 Talus, or scree, is the result of weathering of bedrock; the materials in talus are in the process of transforming from stable bedrock into clay. Talus is not a stable material, and landslides may easily occur on talus slopes.
core +3 more sources