Geomorphology and geochronology of sackung features (uphill-facing scarps) in the Central Spanish Pyrenees
scarps and their kinematics by means of the study of trough fills exposed in artificial trenches; and the temporal and causal relationships between the deglaciation of the valleys and the gravitational spreading phenomena.
of heated pore fluids. The latter process creates space for the intruding magma and initiates a hydrothermal system, which can explain the observed hydrothermal deposits around fault scarps on the basin floor.