Scree Slopes
Scree Slopes is a geomorphological landform characterized by an accumulation of loose, coarse rock fragments at the base of cliffs or steep rocky slopes, differentiated from other colluvial deposits by its origin through physical weathering and its typically unstable, conical profile shaped by gravity-driven particle movement.
99
Publications
4.5K
Citations
274
Authors
151
Institutions
Publications per year
2017–2026
12
Variants
Talus
Parents
99
Permafrost creep and rock glacier dynamics
Wilfried Haeberli, B. Hallet, Lukas U. Arenson et al. · Permafrost and Periglacial Processes · 2006 · 632 citations
Reynald Delaloye, Christophe Lambiel · Norsk Geografisk Tidsskrift - Norwegian Journal of Geography · 2005 · 156 citations
Ian Statham · Earth Surface Processes · 1976 · 141 citations
1–5 of 99
274
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University of Chemistry and Technology, Prague, Czechia
3 publications · 112 citations
3
h-index
1–5 of 274
151
University of Pavol Jozef Šafárik
Košice, Slovakia
6 h-index
17 publications
392 citations
ETH Zurich
Zurich, Switzerland
5 h-index
12 publications
909 citations
Slovak Academy of Sciences
Bratislava, Slovakia
4 h-index
4 publications
75 citations
Université du Québec à Rimouski
Rimouski, Canada
4 h-index
4 publications
297 citations
Institute of Entomology
České Budějovice, Czechia
3 h-index
3 publications
112 citations
Institute of Parasitology of the Slovak Academy of Sciences
Košice, Slovakia
3 h-index
3 publications
64 citations
University of Pavia
Pavia, Italy
3 h-index
4 publications
186 citations

University of Calgary
Calgary, Canada
3 h-index
4 publications
109 citations
1–8 of 151
6 publications · 800 citations
6
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4 publications · 82 citations
4
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3 publications · 144 citations
3
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3 publications · 159 citations
3
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3 publications · 87 citations
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