Glaciation and deglaciation, along with their associated climatic and non-climatic processes,
modify slope stresses and influence slope stability. Paraglacial slope failures are those that …

Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …

In the following sections we define first the term “seismic array” and show examples of
seismic arrays installed around the world. We then describe the theoretical basics of the …

The increasing density of geodetic measurements makes it possible to map surface strain
rate in many zones of active tectonics with unprecedented spatial resolution. Here we show …

In order to estimate well-constrained seismic hazard and risk on local scales, the knowledge
of site amplification factors is one of several important requirements. Seismic hazard studies …

Submarine mass failures (which include submarine slides or submarine landslides) occur
widely on open continental margins. Understanding their cause is of great importance in …

We investigate the influence of the glacial isostatic adjustment (GIA) on the deformation at
the surface and at seismogenic depths in Fennoscandia. The surface strain rate field …

In the French north‐western Alps, several lakes of glacial origin, such as Aiguebelette and
La Thuile, present some mass‐transport deposits within their sedimentary sequences …

In this study, we modify and extend a data analysis technique to determine the stress
orientations between data clusters by adding an additional constraint governing the …

The strandflat as a geomorphological element was defined by Reusch (1894). The timing
and mechanism of its formation have been discussed at great length over the last century …