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• W2166560808 startingPage "320" @default.
• W2166560808 abstract "Abstract. Formation of mountain ranges results from complex coupling between lithospheric deformation, mechanisms linked to subduction and surface processes: weathering, erosion, and climate. Today, erosion of the eastern Andean cordillera and sub-Andean foothills supplies over 99% of the sediment load passing through the Amazon Basin. Denudation rates in the upper Ucayali basin are rapid, favoured by a marked seasonality in this region and extreme precipitation cells above sedimentary strata, uplifted during Neogene times by a still active sub-Andean tectonic thrust. Around 40% of those sediments are trapped in the Ucayali retro-foreland basin system. Recent advances in remote sensing for Amazonian large rivers now allow us to complete the ground hydrological data. In this work, we propose a first estimation of the erosion and sedimentation budget of the Ucayali River catchment, based on spatial and conventional HYBAM Observatory network." @default.
• W2166560808 created "2016-06-24" @default.
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• W2166560808 date "2015-03-03" @default.
• W2166560808 modified "2023-10-18" @default.
• W2166560808 title "Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River" @default.
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• W2166560808 doi "https://doi.org/10.5194/piahs-367-320-2015" @default.
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