4.6 Article

Sediment yield along the Andes: continental budget, regional variations, and comparisons with other basins from orogenic mountain belts

Journal

GEOMORPHOLOGY
Volume 216, Issue -, Pages 225-233

Publisher

ELSEVIER
DOI: 10.1016/j.geomorph.2014.04.007

Keywords

South America; Rivers; Andes Cordillera; Sediment yield; Sediment load; Continental budget

Funding

  1. Edward Larocque Tinker Foundation

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We assess the sediment yield at 119 gauging stations distributed from Colombia to Patagonia, covering the different morphotectonic and morphoclimatic settings of the Andes. The most productive areas are the Meta River basin within the northern Andes and the Bolivian and northern Argentina-Chaco systems, which produce an average of 3345, 4909 and 2654 t km(2) y(-1) of sediment, respectively. The rivers of the northern and central Andes (excluding the Pacific watersheds of Peru, northern Chile, and central Argentina) have a weighted mean sediment yield of 2045 t km(-2) y(-1) and produce 2.25 GTy(-1) of total sediment. A major constraint estimating the Andean continental budget of sediment yield lies in the lack of gauging data for the Peruvian region. Using the available gauge stations, the regional sediment yield appears underestimated. Assuming a higher value of sediment yield for the Peruvian Andes, the total budget for the whole central Andes could range between 2.57 GT y(-1) and 3.44 GT y(-1). A minimum of 055 GT y-1 and a probable maximum of similar to 1.74 GT y-1 of sediment are deposited in the intramontane and surrounding proximal sedimentary basins. The magnitude of sediment yield in the Andes is comparable to other rivers draining orogenic belts around the world. (C) 2014 Elsevier B.V. All rights reserved.

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