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

The south-western part of the White Carpathians (Czech Republic, Slovakia) is known for its
exceptional grassland diversity and occurrence of many species with disjunct distribution …

One of the largest long-runout landslides in the modern history of the Czech Republic
originated on the southern slopes of the Girová Mountain (Outer Western Carpathians) at the …

Complex flow-like landslides (CFLLs) are important geomorphic agents of Late Quaternary
mountain evolution in the Flysch Belt of the Outer Western Carpathians. The CFLLs are …

Abstract In the Tibetan Plateau, active tectonic deformation triggers frequent earthquakes,
and giant landslides associated with active faults produce serious consequences. A study of …

A good understanding of seismic giant landslides could provide favourable guidance for
seismic stability evaluation of nearby slopes. Here, an excellent example of a catastrophic …

Historical documentary sources from two regions with contrasting historical and social
development were examined for information about landslide occurrence and characteristics …

Calcareous tufas are great archives of geochemical information for the reconstruction of past
climate. Their importance increases in the regions where other proxies are rare, such as …

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 …

It is a widely accepted idea that hydrologically triggered deep-seated landslides are initiated
by an increase in pore-water pressure on potential slip surface induced by rising …