We conducted geophysical-geochemical measurements on a similar to 2 km N-S profile cutting across the Pernicana Fault, one of the most active tectonic features on the NE flank of Mt. Etna. The profile passes from the unstable E flank of the volcano (to the south) to the stable N flank and significant fluctuations in electrical resistivity, self-potential, and soil gas emissions (CO(2), Rn and Th) are found. The detailed multidisciplinary analysis reveals a complex interplay between the structural setting, uprising hydrothermal fluids, meteoric fluids percolating downwards, ground permeability, and surface topography. In particular, the recovered fluid circulation model highlights that the southern sector is heavily fractured and faulted, al...
The shallow vertical temperature profile has been measured in the proximity of an eruptive fissure f...
Two strong flank eruptions occurred in July–August 2001 and from late October 2002 to late January 2...
Mount Etna is characterized by a complex regional tectonics with a N-S compression related to the Af...
We conducted geophysical-geochemical measurements on a similar to 2 km N-S profile cutting across th...
A multidisciplinary approach integrating self-potential, soil temperature, heat flux, CO2 efflux and...
Monitoring of hydrothermal fluid emissions can provide detailed information about convective upwelli...
This paper presents a magnetotelluric (MT) survey of the unstable eastern flank of Mt. Etna. We tak...
Flank instability and collapse are observed at many volcanoes. Among these, Mt. Etna is characterize...
Monitoring of hydrothermal fluid emissions can provide detailed information about convective upwelli...
Mount Etna in Sicily (973 km2), the most active European volcano, is known as one of the largest con...
We investigated the relationship between the occurrence of earthquakes along the main volcano-tecton...
Phreatic and hydrothermal eruptions are small energetic explosive events that generally have few to...
This paper presents a magnetotelluric (MT) survey of the unstable eastern flank of Mt Etna. We take ...
On March 15th 2007 a paroxysmal explosion occurred at the Stromboli volcano. This event generated a ...
The shallow vertical temperature profile has been measured in the proximity of an eruptive fissure f...
Two strong flank eruptions occurred in July–August 2001 and from late October 2002 to late January 2...
Mount Etna is characterized by a complex regional tectonics with a N-S compression related to the Af...
We conducted geophysical-geochemical measurements on a similar to 2 km N-S profile cutting across th...
A multidisciplinary approach integrating self-potential, soil temperature, heat flux, CO2 efflux and...
Monitoring of hydrothermal fluid emissions can provide detailed information about convective upwelli...
This paper presents a magnetotelluric (MT) survey of the unstable eastern flank of Mt. Etna. We tak...
Flank instability and collapse are observed at many volcanoes. Among these, Mt. Etna is characterize...
Monitoring of hydrothermal fluid emissions can provide detailed information about convective upwelli...
Mount Etna in Sicily (973 km2), the most active European volcano, is known as one of the largest con...
We investigated the relationship between the occurrence of earthquakes along the main volcano-tecton...
Phreatic and hydrothermal eruptions are small energetic explosive events that generally have few to...
This paper presents a magnetotelluric (MT) survey of the unstable eastern flank of Mt Etna. We take ...
On March 15th 2007 a paroxysmal explosion occurred at the Stromboli volcano. This event generated a ...
The shallow vertical temperature profile has been measured in the proximity of an eruptive fissure f...
Two strong flank eruptions occurred in July–August 2001 and from late October 2002 to late January 2...
Mount Etna is characterized by a complex regional tectonics with a N-S compression related to the Af...