Volcanic edifices, such as Mt. Etna (Italy), are commonly subject to repeated cycles of stress
over time due to the combination of magma emplacement from deep reservoirs to shallow …

Combining SO2 plume emissions from Mt. Etna in 1975–1995 with the magma S content
suggests that between 3.5 and 5.9 km³ of basalt were degassed for sulfur over two decades …

Repeating earthquakes, or repeaters, affecting overlap** rupture patches with a similar
focal mechanism, have important implications to track fault slip rates, aseismic deformation …

After a period of deflation during the 1991–1993 flank eruption, Mount Etna underwent a
rapid inflation. Seismicity and ground deformation show that since 1994, a huge volume of …

Recognition of active faults and assessment of their kinematics constrain thedeformative
model of an area. Thus, observations on coseismic faulting at Etna can provideeffective …

Volcano deformation may occur under different conditions. To understand how a volcano
deforms, as well as relations with magmatic activity, we studied Mt. Etna in detail using …

Since the second half of the 1990s, the eruptive activity of Mount Etna has provided
evidence that both explosive and effusive eruptions display periodic variations in discharge …

Satellite radar interferometry of Mt. Etna volcano, Sicily, Italy, reveals a sequence of
deformation characterized by deflation during the end of the 1993 eruption, inflation from …

Over the last 30 years Mt. Etna has had a high rate of eruptive events and therefore
constitutes an important natural laboratory for the understanding of eruptive processes and …

Abstract 3D earthquake locations, focal mechanisms and stress tensor distribution in a 16‐
month interval covering the 2018 Mt. Etna flank eruption, enabled us to investigate the …