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Results 1 - 5 of 5 for slope evolution (0.0101 seconds)
Tendencies of debris slope evolution in the High Tatra Mountains [100.00% relevance]
Tendencies of debris slope evolution in the High Tatra Mountains An alpine … cliff and related to it talus slope* are the most typical features of mountainous … Polonica (1988) vol. 55 Tendencies of debris slope evolution in the High Tatra Mountains Adam … 1988) vol. 55, pp. 83-90 | Tendencies of debris slope evolution in the High Tatra Mountains, Adam … Tendencies of debris slope evolution in the High Tatra Mountains An alpine cliff and … (1988) vol. 55 Tendencies of debris slope evolution in the High Tatra Mountains Adam Kotarba … vol. 55, pp. 83-90 | Tendencies of debris slope evolution in the High Tatra Mountains, Adam Kotarba,
article/item/8080.html - 13.72 kB
Morphological slope evolution by linear and surface degradation [85.71% relevance]
Morphological slope evolution by linear and surface degradation Geographia … Polonica (1968) vol. 14 Morphological slope evolution by linear and surface degradation Alfred Jahn … (1968) vol. 14, pp. 9-22 | Morphological slope evolution by linear and surface degradation, Alfred Jahn, … Morphological slope evolution by linear and surface degradation … Geographia Polonica (1968) vol. 14 Morphological slope evolution by linear and surface degradation … (1968) vol. 14, pp. 9-22 | Morphological slope evolution by linear and surface degradation,
article/item/8801.html - 12.14 kB
Evolution of the Paglajhora slump valley in the Shiv Khola Basin, the Darjeeling Himalaya, India [71.43% relevance]
(2011) vol. 84, iss. Special Issue Part 2 Evolution of the Paglajhora slump valley in the Shiv Khola … intensity rainstorm, Darjeeling Himalaya, India. Evolution of the Paglajhora slump valley in the Shiv Khola … by the hydro-geomorphic processes. The slope forms exhibit a … Geographia Polonica (2011) vol … , slump, quasi-unstable equilibrium, colluvium slope, palaeo-landslides, high intensity rainstorm,
article/item/7648.html - 14.14 kB
The Significance of Trees and Coarse Woody Debris in Shaping the Debris Flow Accumulation Zone (North Slope of the Babia Gora Massif, Poland) [71.43% relevance]
Shaping the Debris Flow Accumulation Zone (North Slope of the Babia Gora Massif, Poland) In August 2002 … Shaping the Debris Flow Accumulation Zone (North Slope of the Babia Gora Massif, Poland) Marcin Matyja … 83-102 | dendrogeomorphology, debris flow, CWD, slope evolution, timberline, Babia Góra, Poland The … Shaping the Debris Flow Accumulation Zone (North Slope of the Babia Gora Massif, Poland), Marcin Matyja … | dendrogeomorphology, debris flow, CWD, slope evolution, timberline, Babia Góra, Poland The Significance
article/item/7702.html - 14.72 kB
Altitudinal alteration of the morphological systems in the Rio Checras basin of the Peruvian Andes [28.57% relevance]
landslides are the main feature of the slope morphology. They were produced in … Geographia … of geomorphic systems results from Quaternary evolution. The huge stabilized landslides are the main
article/item/7998.html - 13.15 kB