Understanding and constraining the source of geodetic deformation in volcanic areas is an
important component of hazard assessment. Here, we analyse deformation and seismicity …

The stress field controls patterns of crustal deformation, including which faults are likeliest to
cause earthquakes or transmit fluids. Since the 1950s, maps of maximum horizontal stress …

Large volume effusive eruptions with relatively minor observed precursory signals are at
odds with widely used models to interpret volcano deformation. Here we propose a new …

Over 2 weeks in August 2014, magma propagated 48 km laterally from Bárðarbunga
volcano before erupting at Holuhraun for 6 months, accompanied by collapse of the caldera …

Understanding the mechanical conditions for dike arrest and associated surface deformation
or, alternatively, dike propagation to the surface to supply magma to an eruption, is of …

Abstract Between August 2014 and February 2015, a caldera collapse process in
Bárðarbunga volcano accompanied a fissure eruption at the Holuhraun lava field after …

The intrusion of magma into Kīlauea's lower East Rift Zone in May 2018 led to the largest
eruption along this segment of the volcano in over 200 years. As magma drained from the rift …

Understanding the extensional processes in tectonic context at the transition from
continental to oceanic spreading is fundamental to obtain new insights about formations of …

The Icelandic crust is a product of its unique tectonic setting, where the interaction of an
ascending mantle plume and the Mid‐Atlantic Ridge has caused elevated mantle melting …

Aseismic deformation has been suggested as a mechanism to release the accumulated
strain in rifts. However, the fraction and the spatial distribution of the aseismic strain are …