The Ribagorda sand gully (east-central Spain): Sediment yield and human-induced origin

• Published in: Geomorphology (Amsterdam, Netherlands) Netherlands), 2014-11, Vol.224, p.122-138
• Main Authors: Martín-Moreno, C., Fidalgo Hijano, C., Martín Duque, J.F., González Martín, J.A., Zapico Alonso, I., Laronne, J.B.
• Format: Article
• Language: English
• Subjects: Badlands; Check dams; Dams; Dynamics; Geomorphology; Gullies; Gully; Human land transformation; Origins; Rainfall; Sand; Sediment yield; Sediments; Upper Tagus Natural Park (Spain)
• ISSN: 0169-555X; 1872-695X
• DOI: 10.1016/j.geomorph.2014.07.013

Gullies are developed under different climatic conditions and lithologies; however, those formed on sands have been scarcely described. This paper reports the study of the Ribagorda sand gully, 2.57ha in area (east-central Spain). The main objectives were to characterize and quantify its geomorphic dynamics and to trace its origin. We described the landforms of the gully and measured the surface strength of the sand. We monitored, for six years, the filling of the storage areas of three check dams built downstream from the gully, and related it with rainfall characteristics. We also described the nature of the sediments trapped by the dams and estimated the amount of sediment eroded since the gully formation. Finally, we consulted historical records and maps to determine past land uses and transformations that may have affected the origin of the gully. The study shows a high diversity of landforms, denoting active processes, consistent with a measured mean annual sediment yield of 114Mgha−1yr−1. A statistically significant relationship exists between the mass of sediment (Mg) and: 1) the total rainfall (mm) (P=0.0007) or 2) the analysed rainfall intensities. Among five identified facies in the sedimentary wedge, the sandy ones are predominant. The total amount of sediment eroded by the Ribagorda gully since its origin was 962,800Mg. The results are unequivocal signs of an intense geomorphic activity within the gully, with an alluvial-fan type deposition in the dams. We interpret that the Ribagorda gully was initiated by deforestation after the 13th century, when forests began to be intensively logged, and before the 18th century, when the gully was first indirectly described in print. The age, origin, evolution and dynamics of this gully indicate that this landscape is currently evolving towards a new steady state, after human disturbances over centuries. Given the gully evolution and local extent, we suggest that no correction measures are needed for its management. •This article elucidates the origin, history and current dynamics of a sand gully.•Historical sources, and empirical data from a 6-year study, were used.•The characterization and monitoring show a high geomorphic activity in this gully.•Human-induced deforestation was the main cause to the gully's formation.•This study provides useful information for this gully's environmental management.