Geodetic observations at Campi Flegrei caldera were initiated in 1905. Historical observations and the few measurements made before 1970 suggested a deflationary trend. Since 1969, the ground started to inflate during two major uplift episodes in 1969-72 and 1982-1985. We collected and reanalyzed all available punctual observations of vertical ground displacement taken in the period 1905-2009 with special attention to the period before 1969, to reconstruct in greater detail the deformation history of the caldera. We make use of the many photographs of the sea level in a roman ruin (the Serapeum Market) taken during the period between 1905 and 1969 to infer with more accuracy its relative height with respect to the sea level. We identify a p...
Campi Flegrei caldera has been in a state of unrest since 1950. Between 1950-1984 the centre of the ...
Campi Flegrei caldera, which includes the highly urbanized city of Naples, is the most dangerous vol...
Hazard assessment and risk mitigation at restless calderas is only possible with adequate geophysica...
Geodetic observations at Campi Flegrei caldera were initiated in 1905. Historical observations and t...
Geodetic observations at Campi Flegrei caldera were initiated in 1905. Historical observations and t...
After some centuries of subsidence, following the AD 1538 Monte Nuovo last eruption, the Campi Flegr...
Campi Flegrei (Italy) caldera has experienced episodes of ground deformation throughout its geologic...
The Campi Flegrei caldera (Italy) is an active volcanic system characterized by significant long- an...
Volcanic risk in the explosive Campi Flegrei (CF) caldera is extremely high, because of its location...
Campi Flegrei caldera is located just west of the city of Naples, within the central-southern sector...
Ground deformations are among the main volcanic phenomena occurring within the caldera system and pr...
The Campi Flegrei caldera (Italy) is an active volcanic system characterized by significant long- a...
Campi Flegrei caldera has been in a state of unrest since 1950. Between 1950-1984 the centre of the ...
Campi Flegrei caldera, which includes the highly urbanized city of Naples, is the most dangerous vol...
Hazard assessment and risk mitigation at restless calderas is only possible with adequate geophysica...
Geodetic observations at Campi Flegrei caldera were initiated in 1905. Historical observations and t...
Geodetic observations at Campi Flegrei caldera were initiated in 1905. Historical observations and t...
After some centuries of subsidence, following the AD 1538 Monte Nuovo last eruption, the Campi Flegr...
Campi Flegrei (Italy) caldera has experienced episodes of ground deformation throughout its geologic...
The Campi Flegrei caldera (Italy) is an active volcanic system characterized by significant long- an...
Volcanic risk in the explosive Campi Flegrei (CF) caldera is extremely high, because of its location...
Campi Flegrei caldera is located just west of the city of Naples, within the central-southern sector...
Ground deformations are among the main volcanic phenomena occurring within the caldera system and pr...
The Campi Flegrei caldera (Italy) is an active volcanic system characterized by significant long- a...
Campi Flegrei caldera has been in a state of unrest since 1950. Between 1950-1984 the centre of the ...
Campi Flegrei caldera, which includes the highly urbanized city of Naples, is the most dangerous vol...
Hazard assessment and risk mitigation at restless calderas is only possible with adequate geophysica...