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Results 1 - 6 of 6 for debris slope (0.0029 seconds)
The Significance of Trees and Coarse Woody Debris in Shaping the Debris Flow Accumulation Zone (North Slope of the Babia Gora Massif, Poland) [100.00% 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 … The Significance of Trees and Coarse Woody Debris in Shaping the Debris Flow Accumulation Zone ( … the Babia Gora Massif, Poland) In August 2002 a debris flow with a total length of 760m occurred on the … . 1 The Significance of Trees and Coarse Woody Debris in Shaping the Debris Flow Accumulation Zone ( … . 80, iss. 1, pp. 83-102 | dendrogeomorphology, debris flow, CWD, slope evolution, timberline, Babia … The Significance of Trees and Coarse Woody Debris in Shaping the Debris Flow Accumulation Zone (
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Tendencies of debris slope evolution in the High Tatra Mountains [58.33% relevance]
Tendencies of debris slope evolution in the High Tatra Mountains An … Geographia 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, … 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
article/item/8080.html - 13.72 kB
Geomorphic activity of debris flows in the Tatra Mts and in other European mountains [50.00% relevance]
Geomorphic activity of debris flows in the Tatra Mts and in other European … mountains Debris flows constitute the dominant high-energy slope … (2007) vol. 80, iss. 2 Geomorphic activity of debris flows in the Tatra Mts and in other European … Polonica (2007) vol. 80, iss. 2, pp. 137-150 | debris flows, extreme rainfall events, Tatra Mountains … geomorphic hazards Geomorphic activity of debris flows in the Tatra Mts and in other European … Debris flows constitute the dominant high-energy slope processes in the high-mountainbelt of the Tatra
article/item/5727.html - 13.87 kB
Cylowa Zerwa landslide – debris flow forms on Mount Babia Góra (1725) and their development over the last ca. 150 years, Western Carpathians [50.00% relevance]
Cylowa Zerwa landslide – debris flow forms on Mount Babia Góra (1725) and their … , Western Carpathians Cylowa Zerwa landslide – debris flow located on the northern slope of Mt. Babia … (2023) vol. 96, iss. 1 Cylowa Zerwa landslide – debris flow forms on Mount Babia Góra (1725) and their … homoclinal ridge, structural relief, landslide, debris flow, damages in forest • disturbances in … movement, geotourism Cylowa Zerwa landslide – debris flow forms on Mount Babia Góra (1725) and their … landslide – debris flow located on the northern slope of Mt. Babia Góra (1725 m a.s.l.) within the 400
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Permafrost Degradation and Slope Instability in the Italian Alps [33.33% relevance]
Permafrost Degradation and Slope Instability in the Italian Alps The occurrence … 2008) vol. 81, iss. 1 Permafrost Degradation and Slope Instability in the Italian Alps Francesco Dramis … , Italian Alps. Permafrost Degradation and Slope Instability in the Italian Alps, Francesco … an important predisposing factorfor landslides. Debris flows are frequent on slopes overlying
article/item/7677.html - 13.59 kB
Are there geomorphic indicators of permafrost in the Tatra Mountains? [16.67% relevance]
| permafrost, high-mountains at mid latitudes, debris slope, periglacial landforms Are there … , high-mountains at mid latitudes, debris slope, periglacial landforms Are there geomorphic
article/item/6036.html - 13.59 kB