The mid-Atlantic plate boundary in Iceland is expressed by a series of seismic and volcanic
zones. The structure of the plate boundary is strongly influenced by the Iceland hot spot. The …

We have determined the three‐dimensional P wave velocity structure within the area of the
Hengill‐Grensdalur central volcano complex, southwest Iceland, from the tomographic …

Field observations and geodetic data indicate that dike intrusion in volcanic rift zones
typically generates normal faulting and graben subsidence at the Earth's surface. Elastic …

Magnetotelluric measurements have revealed a crustal thickness of 8–10 km in the axial rift
zone of NE Iceland and above the proposed hot spot in central east and north Iceland. The …

We analysed temporal variations of trace element concentrations in groundwater from a 101
m-deep borehole (HA01) in northern Iceland during 2010–2018 and compared them with …

On the 20th September 2012, a large debris slide occurred in the Móafellshyrna Mountain in
the Tröllaskagi peninsula, central north Iceland. Our work describes and discusses the …

Integration of knowledge of subglacial topogra-Phy, earthquake activity and jökulhlaups has
contributed to more precise locations ofthe volcanic systems beneath Vatnajökull …

Iceland is an oceanic plateau produced by channeled flow from the Iceland hotspot. The
Icelandic rift system moves WNW relative to the hotspot. About magnetic anomaly 7 time the …

Observations of eroded volcanic rift zones indicate that dikes in Iceland are typically several
times thicker than those in Hawaii. Geodetic and seismic observations of active rifts …

Lithostratigraphy, magnetostratigraphy, and new K/Ar ages from the region between
Eyjafjördur and Skjálfandi, north central Iceland, reflect tectonic reorganization of crustal …