Climatic factors are considered major causes and triggers of slope instability, but the
palaeoclimatic implications of landslides have not yet been systematically reviewed. As …

Rock slope failures are characteristic of mountainous environments. These mass
movements produce sediment, alter catchment behaviour and contribute to the dynamics …

The area of Prados del Cervunal (PC) is an intra-morainic topographic depression located at
1800 m asl in the divide or interfluve between Garganta de Gredos and Garganta del Pinar …

The recent launch of national-scale LiDAR-derived topographic data provides an
opportunity for (re) evaluating the geomorphic imprint of landslides in forested mountains. A …

Relict rock glaciers are well-preserved features of high-elevated valleys in the Western Tatra
Mts., Western Carpathians, but their chronology remained poorly constrained with numerical …

Rock slope failure (RSF) is now widely recognised as a significant contributor to the
denudation of mountain ranges. Its spatial incidence can consequently be a valuable …

The timing of glacier disappearance and rock glacier stabilization in the highest massifs of
the Carpathians is still poorly documented. In this paper, we establish the extent and …

The direct dating of pre-and postfaulting dislocated calcite speleothems afforded new insight
into slope failure in the Tatra Mountains in southern Poland. A multi-approach study of the …

The increasing availability of high-resolution LiDAR data reveals surprisingly strong
topographic evidence of late Quaternary faulting in some intraplate regions characterized by …

Schmidt-hammer exposure-age dating (SHD) was performed on blockfields and related
landforms on Blåhø, Southern Norway. By developing a linear high-precision age …