Linking the Mediterranean MIS 5 tephra markers to Campi Flegrei (southern Italy) 109–92 ka explosive activity and refining the chronology of MIS 5c-d millennial-scale climate variability

Autor: Monaco, L., Palladino, D.M., Albert, P.G., Arienzo, I., Conticelli, S., Di Vito, M., Fabbrizio, A., D'Antonio, M., Isaia, R., Manning, C.J., Nomade, S., Pereira, A., Petrosino, P., Sottili, G., Sulpizio, R., Zanchetta, G., Giaccio, B.

Publikováno v: In Global and Planetary Change April 2022 211

Analysis of tourism in Campania as a tool for the development of high-quality cultural services for sightseers: The 'Reale Osservatorio Vesuviano' case history

Autor: Simonetti, B., Fuccio, N., Nunziata, C., Antolini, F., González- Rodríguez, M. R., Díaz-Fernández, M. C., Avvisati, G., Marotta, E., Peluso, R., Sangianantoni, A., De Natale, G., De Vita, S., Di Vito, M., Marfè, B., Pinto, S., Tulino, S., Trimarchi, E., Ghilardi, M.

Publikováno v: Tourism and Hospitality International Journal ; Vol. 5 No. 1 (2015): September 2015 [10th Edition]; 64-87
Tourism and Hospitality International Journal ; Vol. 5 Núm. 1 (2015): Septiembre 2015 [10ª Edición]; 64-87
Tourism and Hospitality International Journal ; Vol. 5 N.º 1 (2015): Setembro 2015 [10ª Edição]; 64-87

The purpose of this work is to identify the guidelines for the development and diversification of the cultural touristic offer achievable at the Reale Osservatorio Vesuviano (ROV). Founded in 1841, it is the oldest volcano observatory in the world an

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cf99c284e56e334db5adc57c94f46f2f
https://revistas.rcaap.pt/thij/article/view/30297

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Rheological investigations of fluidised volcanic rocks and implication for the dynamic of pyroclastic density currents

Autor: Rucco, I., Dioguardi, F., Di Vito, M., Sarocchi, D., Ocone, R.

Publikováno v: XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)

Dense pyroclastic density currents are granular mass flows consisting of a mixture of solid particles and gas, denser than the surrounding atmosphere, which flow down the slopes of a volcano edifice under the action of gravity.They are one of the mos

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef69d59ed9bb00fb6109256ef18a7177

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