Journal Article10.1016/J.GEOMORPH.2008.09.009
Longitudinal ridges in mass movement deposits
Anja Dufresne,Tim Davies +1 more
188
TL;DR: In this article, the formation of elongate ridges (and their expressions as flowbands, aligned hummocks, or distal lobes and digits) in both laboratory and field environments suggests they represent an intrinsic tendency of granular flows in a wide range of situations.
read more
About: This article is published in Geomorphology. The article was published on 15 Apr 2009. The article focuses on the topics: Debris & Volcanic rock.
read more
Chat with Paper
AI Agents for this Paper
Find similar papers on Google Scholar, PubMed and Arxiv
Write a critical review of this paper
Analyze citations of this paper to find unaddressed research gaps
Citations
Quantitative reconstruction of late Holocene surface evolution on an alpine debris-flow fan
Peter Schürch,Alexander L. Densmore,Susan Ivy-Ochs,Nick Rosser,Florian Kober,Fritz Schlunegger,Brian W. McArdell,Vasili Alfimov +7 more
TL;DR: In this article, the authors used terrain analysis, radiocarbon dating of sediment fill in the Illgraben catchment, and cosmogenic 10Be and 36Cl exposure dating of debris-flow deposits on the fan to constrain the temporal evolution of the sediment routing system in the catchment and on the fans during the past 3200 years.
Glacially moulded landslide runout debris in the Scottish Highlands.
TL;DR: A tongue of hummocky terrain ∼1 km long and ∼400m wide extends downslope from the source area of a rock-slope failure that formed the summit arete of Sgurr nan Ceathreamhnan in the NW Highlands.
Influence of intergranular friction weakening on rock avalanche dynamics
TL;DR: In this article , the authors investigated the significance of intergranular friction weakening on the dynamics of the Jiweishan rock avalanche and compared the results from the numerical models with and without granular friction strengthening to investigate its influence on the dynamic of the rock avalanche.
The largest rock avalanche in China at Iymek, Eastern Pamir, and its spectacular emplacement landscape
TL;DR: Wang et al. as discussed by the authors conducted a comprehensive investigation on the gigantic Iymek rock avalanche (IRA) in eastern Pamir, China, which exhibited characteristic undulating features, including trimlines, longitudinal ridges, hummocks, raised distal edge, and raised lateral levees.
The glacial and periglacial evolution of Coprates Chasma (Valles Marineris, Mars)
Fabio Vittorio De Blasio,Giovanni B. Crosta,Davide Fusetti,Elena Valbuzzi +3 more
References
Large volcanic debris avalanches: Characteristics of source areas, deposits, and associated eruptions
TL;DR: In this paper, the authors show that large volcanic debris avalanches, often exceeding a cubic kilometer in volume, create massive amphitheater-shaped reentrants into the volcanic edifice that differ in morphology and origin from normal collapse calderas.
724
Entrainment of debris in rock avalanches: An analysis of a long run-out mechanism
Oldrich Hungr,Stephen G. Evans +1 more
TL;DR: In this paper, the authors describe two recent cases from British Columbia, Canada, where rockslides entrained substrate on a very large scale, influencing the character of the events.
536
Influence of particle characteristics on granular friction
TL;DR: In this paper, the authors report on laboratory experiments designed to illuminate grain-scale deformation mechanisms within granular fault gouge and compare results from shear between smooth boundaries, where they hypothesize that grain boundary sliding is the dominant deformation mechanism, and roughened surfaces, where rolling and granular dilation contribute to shear deformation.
Rockslide-debris avalanche of May 18, 1980, Mount St. Helens Volcano, Washington
Harry Glicken
- 01 Jan 1996
TL;DR: In this paper, the authors present a survey of the state-of-the-art tools and techniques used in the development of the HOGA algorithm and its application in the field of artificial intelligence.
Fingering in granular flows
TL;DR: In this paper, the authors describe an instability that occurs when a front of granular material propagates down a rough inclined plane, which is initially uniform in cross-section, rapidly breaks up into fingers.
241