Central Pyrenees
Analysis of the ground vibration generated by debris flows and other torrential processes at the Rebaixader monitoring site (Central Pyrenees, Spain)
... Abstract. Monitoring of debris flows using ground vibration sensors has increased in the last two decades. However, the correct interpretation of the signals still presents ambiguity. In the Rebaixader monitoring site ...
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Rockfall travel distance analysis by using empirical models (Sol`a (d’Andorra la Vella, Central Pyrenees)
... The purpose of this paper is (i) to propose a method to pre- dict travel distance of small rockfalls (<100 m 3 ) by using ba- sic empirical models (both reach and shadow angle models), (ii) to verify empirical results ...
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Besiberris glacigenic rock glacier (Central Pyrenees, Spain) : mapping surface horizontal and vertical movement (1993-2003)
... the Pyrenees, but they are mainly relict, showing in most cases no signs of present-day activity (Chueca, 1991, ...the Central Pyrenees was made by Chueca (1992), who identified 170 rock glaciers in ...
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Long-term entrenchment and consequences for present flood hazard in the Garona River (Val d’Aran, Central Pyrenees, Spain)
... of Central Pyrenees due to the isostatic compensation, with an estimated uplift rate between ...the Pyrenees crest zone where the largest sediment volumes are ...
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Mapping and monitoring geomorphological processes in mountainous areas using PSI data: Central Pyrenees case study
... Abstract. In this paper the Stable Point Network technique, an established Persistent Scatterer InSAR (PSI) technique, (SPN), has been applied for the first time to the analysis of several geomorphological processes ...
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Sediment yield and transport in badlands located in the Inner Depression (Araguás Basin, Central Pyrenees)
... ABSTRACT. This study shows the analyses of suspended sediment transport from badland areas developed in the Inner Depression (Central Pyrenees). The impor- tance of these morphologies is related to its ...
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Volumetric budget and grain size fractionation of a geological sediment routing system: Eocene Escanilla Formation, south central Pyrenees
... which >75% was deposited in the Jaca Basin (Fig. 10C). This total sediment volume is an underestimate due to erosion at the base Oligo- cene boundary, which would have recycled a volume from time interval 3 into the ...
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Factors in peak flows generation in an experimental catchment of the Central Pyrenees, Spain
... Total de crecidas: 39 Crecidas en estación fría: 24 Crecidas en estación cálida: 15 V1: Precipitación total mm V2: Precipitación máxima en 30 minutos V3: Precipitación máxima en 60 minut[r] ...
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Scenarios, timing and paleo-environmental indicators for the identification of Anthropocene in the vegetal landscape of the Central Pyrenees (NE Iberia)
... Este escenario de ritmo acelerado, coincidió con el crecimiento demográfico, que en general, alcanzó en el Pirineo Central sus cifras más elevadas a mediados del siglo XIX. La consecuencia más destacada fue la ...
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History of fire and vegetation in a Holocene sequence of the Central Pyrenees: the Basa de la Mora lake
... fire activity. Studying the relationship between long-term fire ecology, ecosystems and climate allows us to understand how vegetation responds to this perturbation and to define the thresholds triggering irreversible ...
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Cartography of probable avalanche starting zones in the Alto Gállego Valley (Spanish Central Pyrenees) using Geographical Information System
... RESUMEN. En el presente trabajo se realiza una cartografía de zonas proba- bles de salida de aludes en el valle del Alto Gállego (Pirineo Central aragonés) a partir del empleo de Sistemas de Información Geográfica ...
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Influence of reservoirs on river flow regimes in the Central Pyrenees
... Signo de la diferencia entre las salidas y las entradas de agua a los embalses Embalse Yesa pie de presa+canal Yesa pie de presa Lanuza Bubal La Peña Mediano El Grado pie de presa+canal [r] ...
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Seasonal differencesin a small farmland abandoned catchment, Central Pyrenees
... Este trabajo muestra que las relaciones entre precipitación y escorrentía a escala de crecida en una pequeña cuenca de campos abandonados no son lineales y que la respuesta hidrológica s[r] ...
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Installation and use of a snow pillow to monitor the snowpack. izas experimental basin (central pyrenees)
... (Pirineo Central) y desde entonces ha proporcionado información de la evolución de la densidad de nieve y el equiva- lente del manto de nieve en agua (SWE) durante tres ...
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Historical geomorphological processes and its relationship to the human activity in central pyrenees (spain)
... En la actualidad son bien visibles las huellas de esta actividad humana: en el piso subalpino movimientos en masa superficiales y densas redes de rills han provocado la pét•dida de gran [r] ...
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On the Usefulness of the Modern Analog Approach to Interpret High Resolution Records: The Case of Varved Sediments from Lake Montcortès (Central Pyrenees)
... combination of pollen data from traps, varved lake sediments and modern. meteorological data may produce long, high-resolution ecological time series by[r] ...
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Sedimentologic approximation to reservoir situation and erosion in mountain basins: the barsona reservoir and the esera-isábena catchment (central pyrenees, huesca)
... Los procesos sedimentarios más importantes que suceden en el embalse durante los periodos de exposición subaérea son los siguientes: 1 formación autigénica de yesos; 2 agrietamiento de l[r] ...
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Hydrological functions of a small mountain cathment with badland morphologies in the Central Pyrenees
... Según la Encyclopedia of Geomorphology (Goudie, 2004) los badlands son “paisajes erosivos profundamente disectados formados en rocas blandas, por lo general, en regiones semiáridas aunque no exclusivamente” (Harvey, ...
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Identifying erosive periods by using RUSLE factors in mountain fields of the Central Spanish Pyrenees
... This work aims to identify different erosive periods in rela- tion to temporal changes in rainfall characteristics (erosivity, maximum intensity and number of erosive events), soil prop- erties (soil erodibility in ...
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The water balance of different soils on abandoned fields along a transect from the High Pyrenees to the Central Ebro Basin
... The second test area (Arnas) is located in the Central Pyrenees, in the montane alti- tude zone, 1000 m a.s.l. Geologically the area is dominated by Eocene clay-, marl- and sandstone of the Sierras ...
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