Zobrazeno 1 - 10
of 57
pro vyhledávání: '"Marco Camarda"'
Autor:
Antonio Caracausi, Marco Camarda, Lauro Chiaraluce, Sofia De Gregorio, Rocco Favara, Antonino Pisciotta
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Static and dynamic stress, along with earthquakes, can trigger the emission and migration of crustal fluids, as frequently observed on the surface and within the upper crust of tectonically active areas such as the northern Apennines of Italy. To inv
Externí odkaz:
https://doaj.org/article/ffe4c443ad4e4aa59c814eb5d8c12c28
Publikováno v:
Geosciences, Vol 13, Iss 9, p 266 (2023)
The La Fossa volcano is near the inhabited zone of the island of Vulcano and is a suitable case for studying gas sources of different geological origins. Since the last eruption, fumarolic-solfataric activity has interested this area with fumarolic e
Externí odkaz:
https://doaj.org/article/9bc8feb0aa9e402ea77916881c12df11
Autor:
Cinzia Federico, Ornella Cocina, Salvatore Gambino, Antonio Paonita, Stefano Branca, Mauro Coltelli, Francesco Italiano, Valentina Bruno, Tommaso Caltabiano, Marco Camarda, Giorgio Capasso, Sofia De Gregorio, Iole Serena Diliberto, Roberto Maria Rosario Di Martino, Susanna Falsaperla, Filippo Greco, Giovannella Pecoraino, Giuseppe Salerno, Mariangela Sciotto, Sergio Bellomo, Giuseppe Di Grazia, Ferruccio Ferrari, Alessandro Gattuso, Leonardo La Pica, Mario Mattia, Antonino Fabio Pisciotta, Lucia Pruiti, Francesco Sortino
Publikováno v:
Remote Sensing, Vol 15, Iss 5, p 1405 (2023)
In September 2021, the La Fossa crater at Vulcano, in Italy, entered a new phase of unrest. We discuss a set of monitoring parameters included in the INGV surveillance network, which closely tracked the sequence of effects related to the crisis. The
Externí odkaz:
https://doaj.org/article/09b1333c4d08479fbc757c14b5a116ad
Water-gas interaction is an ordinary process occurring in volcanic areas because of gases released from magma reservoir at depth interact and dissolve in groundwater and/or are discharged from the soils or fumaroles. At the island of Vulcano (Aeolian
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bfb18b9ab4010706fff9e68eb8a03872
https://doi.org/10.5194/egusphere-egu23-12305
https://doi.org/10.5194/egusphere-egu23-12305
Among extreme geological events, people feel the effects of volcanic eruptions through fear and wonder. Several volcanoes erupt across the world with sheer physical power, but a large part of them is either dormant or quiescent. Risks for explosions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::586a9d016bf4f8741ffbe4725638af8f
https://doi.org/10.5194/egusphere-egu23-16440
https://doi.org/10.5194/egusphere-egu23-16440
Periodic surveys for the measurement of the soil CO2 flux are regularly performed in three peripheral areas of the Mt Etna (Paternò, Zafferana-S. Venerina and Vena-Presa) for a whole of 140 measurement sites. It is widely demonstrated that anomalous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::254d5b0d9ca54092dd62a0621ff93c82
https://doi.org/10.5194/egusphere-egu23-16282
https://doi.org/10.5194/egusphere-egu23-16282
Publikováno v:
Journal of Geophysical Research: Solid Earth. 127
Publikováno v:
Italian Journal of Geosciences. 140:79-94
The geochemistry of volcanic gases has been fruitfully applied to identify important changes in the volcanic activity. This study reviews the dataset of the volcanic gas survey performed during 2009 and 2010 at Stromboli (Aeolian Islands - Italy). Dr
Publikováno v:
Annals of Geophysics, Vol 57, Iss 3 (2014)
Herein, we present and discuss the result of 148 measurements of soil CO2 flux performed for the first time in Linosa island (Sicily Channel, Italy), a Plio-Pleistocene volcanic complex no longer active but still of interest owing to its location wit
Externí odkaz:
https://doaj.org/article/038f772738d04f3b8523e93b55025e54
Autor:
Manfredi Longo, Fabio Vita, Antonio Paonita, Sergio Gurrieri, Francesco Italiano, Iole Serena Diliberto, Marco Camarda, V. Francofonte, Roberto M. R. Di Martino
The La Fossa volcano lies nearby the settled zone of the Island of Vulcano and its last eruption occurred in 1888-1890. Since then, the fumarolic-solfataric degassing accounted for both sulfur and carbon dioxide emissions at Vulcano Porto zone. Long
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56c2a8a54a67496c9ec3b90b620da7d2
https://doi.org/10.5194/egusphere-egu21-8422
https://doi.org/10.5194/egusphere-egu21-8422