The Iceland hotspot has a pronounced effect on the appearance and structure of the plate
boundary between the North America and Eurasia Plates that crosses the island. The thick …

Iceland is one of the few places on Earth where a divergent plate boundary can be observed
on land. Direct observations of crustal deformation for the whole country are available for the …

The largest earthquakes in Iceland occur in the South Iceland seismic zone (SISZ) and the
Tjörnes fracture zone in the northeast. With the latter being primarily offshore, the seismic …

Since the end of 1993, the digital, automatic seismic system, known as the SIL-system, has
acted as the national seismic network in Iceland. The number of stations in the network has …

We analyze data spanning up to 5 years from 18 continuous GPS stations in Iceland,
computing daily positions of the stations with three different high‐level geodetic processing …

Abstract From May to September 2013, 21 seismic stations were deployed around the
Snæfellsjökull volcano, Iceland. We cross-correlate the five months of seismic noise and …

We use data from GPS campaign and continuous measurements from 1992 to 2004 in SW
Iceland to map the surface velocity field from the Reykjanes Peninsula to the Eastern …

We have developed a method to measure finite-frequency amplitude and traveltime
anomalies of teleseismic P waves. We use a matched filtering approach that models the first …

Iceland is located on the Mid-Atlantic ridge, at a divergent plate boundary separating the
North America and the Eurasia plates. It is therefore one of the few places on Earth where …

We use high‐resolution simulations to analyze fluid flow, pore pressure, and fault
permeability evolution in the seismically active Tjörnes Fracture Zone (TFZ), a major …