Electrical resistivity tomography (ERT) is a minimally invasive geophysical method that
produces a model of subsurface resistivity from a large number of electrical resistance …

Observations in the European Alps show a long-term rise in rock glacier velocities, which is
often associated with increased air and ground temperatures and, more recently, water …

The degradation of mountain permafrost is well documented at many Alpine sites.
Geophysical techniques have been intensively used to monitor these sites, since permafrost …

Frozen layers within the subsurface of rock glaciers are generally assumed to act as
aquicludes or aquitards. So far, this behavior has been mainly defined by analyzing the …

Rock slope instabilities and failures from permafrost are among the most significant alpine
hazards in a changing climate and represent considerable threats to high-alpine …

Rock slope instabilities and failures from permafrost rocks are among the most significant
alpine hazards in a changing climate and represent considerable threats to high-alpine …

Degrading permafrost in rock glaciers has been reported from several sites in the European
Alps. Changes in ground temperature and ice content are expected to affect the …

While recent permafrost degradation in Alpine peri-and paraglacial slopes has been
documented in several studies, only restricted information is available on the respective …

Seismic refraction tomography is a commonly used technique to characterise rock glaciers,
as the boundary between unfrozen and ice-bearing layers represents a strong impedance …

Electrical resistivity tomography (ERT) is widely used to map, characterize, and monitor the
ground in alpine and periglacial environments, where coarse blocky surfaces are often …