RT Journal Article
T1 Consecuencias geomorfológicas derivadas de un proceso de captura fluvial
T1 Geomorphic features developed after a fluvial piracy process
A1 Calvache Quesada, María Luisa
A1 Viseras, César
AB The recent capture of the drainage of the ancient endohreic Guadix-Baza basin is favoured by a process of uplift implyng northwestward tilting and shift of the ancient axial master drainage system.Since the capture onwards a dendritic drainage pattern (western sector) and a centripetal one (eastern sector) are developed impiyng associated phenomena of fluvial superimposition. Flow inversion in some reaches of the trunk stream carries on the appearance of a barbed drainage pattern showing boat hook bends. The new equilibrium profile created after the piracy is responsible for the inestability of the infilling of the ancient basin. So, rapid erosion started giving way to a badlands landscape in which the development of badlands and piping has a control in the stratigraphic architecture of the alluval sediments being eroded away
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13466
UL http://hdl.handle.net/10272/13466
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026