RT Journal Article
T1 El Deslizamiento de Güevéjar (provincia de Granada): un caso de inestabilidad de laderas inducida por sismos
T1 The Güevéjar Landslide: a case study of slope instability triggered by earthquakes
A1 Jiménez Pintor, J.
A1 Azor, A.
AB Drawing on historical documents and a detailed field study, we have been able to characterize the Güevéjarlandslide as a complex landmass movement with a dominant multi-rotational component. The landslidebody is made up of very heterogeneous rocks, while the basal surface is located on lignite-bearing marls.The main triggering factor responsible for this landslide is thought to be the dynamic effect of high magnitudeearthquakes with the focus located at very long distances (tens to hundreds of km) from Güevéjar. Somepieces of evidence point to local-scale amplification of seismic waves (site effect) as causing reactivation ofthe landslide
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8597
UL http://hdl.handle.net/10272/8597
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026