During the July^August 2001 eruption of Mt. Etna development of extensional fractures/faults and grabens accompanied magma intrusion and subsequent volcanic activity. During the first days of the eruption, we performed an analysis of attitude, displacement and propagation of fractures and faults exposed on the ground surface in two sites, Torre del Filosofo and Valle del Leone, located along the same fracture system in the region surrounding the Valle del Bove depression on the eastern flank of Mt. Etna. Fractures and faults formed as the consequence of a shallow intruding dyke system that fed the several volcanic centres developed along the fracture system. The investigated sites differ in slope attitude and in geometrical relationsh...
Volcanic edifices are often unable to support their own load, triggering the instability of their fl...
Flank instability and collapse are observed at many volcanoes. Among these, Mt. Etna is characterize...
The intrusive process of the 2001 Mt. Etna eruption was accompanied by marked ground deformation and...
Mount Etna produced two significant eruptions in 2001 and 2002-2003, which we have analysed using ge...
Mount Etna produced two significant eruptions in 2001 and 2002–2003, which we have analysed using ge...
The development of the 2004–2005 eruption at Etna (Italy) is investigated by means of field surveys ...
The 1928 CE volcanic activity on eastern Etna, Italy, produced wide surface deformation and high eff...
Mount Etna produces frequent eruptions from its summit craters and from fissures on its flanks. The ...
Mount Etna (Italy) produced two important flank eruptions in 2001 and 2002-2003, which were peculia...
We merge volcanological, structural, and volcanic tremor data to shed light on a fissure system open...
Fracture Reactivation and Magma Intrusion: The Case of the 1989 Fissure System at Mt Etna, Italy ...
We describe the evolution of the volcanic activity and deformation patterns observed at Mount Etna d...
Abstract: We describe the evolution of the volcanic activity and deformation patterns observed at Mo...
Mount Etna (Italy) produced two important flank eruptions in 2001 and 2002-2003, which were peculia...
The 2002–2003 Mount Etna eruption and the associated deformation provide a unique possibility to stu...
Volcanic edifices are often unable to support their own load, triggering the instability of their fl...
Flank instability and collapse are observed at many volcanoes. Among these, Mt. Etna is characterize...
The intrusive process of the 2001 Mt. Etna eruption was accompanied by marked ground deformation and...
Mount Etna produced two significant eruptions in 2001 and 2002-2003, which we have analysed using ge...
Mount Etna produced two significant eruptions in 2001 and 2002–2003, which we have analysed using ge...
The development of the 2004–2005 eruption at Etna (Italy) is investigated by means of field surveys ...
The 1928 CE volcanic activity on eastern Etna, Italy, produced wide surface deformation and high eff...
Mount Etna produces frequent eruptions from its summit craters and from fissures on its flanks. The ...
Mount Etna (Italy) produced two important flank eruptions in 2001 and 2002-2003, which were peculia...
We merge volcanological, structural, and volcanic tremor data to shed light on a fissure system open...
Fracture Reactivation and Magma Intrusion: The Case of the 1989 Fissure System at Mt Etna, Italy ...
We describe the evolution of the volcanic activity and deformation patterns observed at Mount Etna d...
Abstract: We describe the evolution of the volcanic activity and deformation patterns observed at Mo...
Mount Etna (Italy) produced two important flank eruptions in 2001 and 2002-2003, which were peculia...
The 2002–2003 Mount Etna eruption and the associated deformation provide a unique possibility to stu...
Volcanic edifices are often unable to support their own load, triggering the instability of their fl...
Flank instability and collapse are observed at many volcanoes. Among these, Mt. Etna is characterize...
The intrusive process of the 2001 Mt. Etna eruption was accompanied by marked ground deformation and...