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  5. Continuous record of the gravity changes at Mt. Vesuvius
 
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Continuous record of the gravity changes at Mt. Vesuvius

Author(s)
Berrino, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Corrado, G,  
Dipartimento di Geofisica e Vulcanologia, Università di Napoli «Federico II», Napoli, Italy  
Magliulo, R.  
Dipartimento di Geofisica e Vulcanologia, Università di Napoli «Federico II», Napoli, Italy  
Riccardi, U.  
Dipartimento di Geofisica e Vulcanologia, Università di Napoli «Federico II», Napoli, Italy  
Date Issued
October 1997
Issue/vol(year)
5/40 (1997)
Language
English
Subjects
04. Solid Earth::04.03. Geodesy::04.03.05. Gravity variations  
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring  
URI
https://www.earth-prints.org/handle/2122/1544
Subjects

Earth tide

amplification factor

gravity residual

volcanic activity

Abstract
High precision relative and absolute gravity measurements are periodically carried out at Mt. Vesuvius (Southern Italy) to monitor the changes in the gravity field caused by the internal dynamics of the volcano. Moreover, a recording gravity station is also operating at the Osservatorio Vesuviano (Old Building) aimed at measuring in continuous mode the time variations of the gravity and the tidal parameters, possibly due to changes in the physical state of the volcano. The analysis carried out on an hourly data set spanning the 1994-1996 time interval and a comparison of the results with those previously obtained, exhibit a change in the tidal parameters which occurred between 1991 and 1994. A gravity decrease of about 60 µGal was observed during the same time interval in the same area. Consistent with relative and absolute gravity observations, no significant variations have been detected since 1994 in the tidal parameters and gravity residuals.
Type
article
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