This study has integrated a range of geoscientific evidence in order to constrain the spatial and temporal development of the reactivated catastrophic landslide at Eisenberg in North Bohemia.

The western part of the Bohemian Massif (Vogtland/West Bohemia region at the Czech-German border) is characterized by relatively frequent intraplate earthquake swarms and by other manifestations of current geodynamic activity, such as mofettes, mineral and ...