View of a mud pool in the Salinelle of Vallone Salato, Etna. Fluids are emitted through marly clays of the foredeep sedimentary deposits (Image credits: Emanuela Bagnato).
Volcano: | Etna (see Etna at the Smithsonian Institution website in a new tab) |
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Type: | Soil Diffuse Emission |
Description: | Fluids emitted through marly clays of the foredeep sedimentary deposits are composed of a gas phase and hypersaline waters that often pond in pools that range in size from centimeters to meters in diameter. |
Point of contact for this site:
Salvatore Giammanco, salvatore.giammanco@ct.ingv.it (INGV, Catania)
Measurement | date (d/m/y) | Added by | Added on |
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Etna Salinelle Vallone Salato_072005 | None/7/2005 | Emanuela Bagnato | Dec. 2, 2013 |
Giammanco, S., Parello, F., Gambardella, B., Schifano, R., Pizzullo, S., Galante, G., 2007,Focused and diffuse effluxes of CO2 from mud volcanoes and mofettes south of Mt. Etna (Italy), Journal of Volcanology and Geothermal Research, vol.165, n.n.d., pp. 46-63, DOI: 10.1016/j.jvolgeores.2007.04.010