Hostname: page-component-78c5997874-lj6df Total loading time: 0 Render date: 2024-11-02T22:05:03.706Z Has data issue: false hasContentIssue false

The volcanic history of the southwestern part of the city of Naples

Published online by Cambridge University Press:  01 May 2009

Paul D. Cole
Affiliation:
Dipartimento di Geofisica e Vulcanologia, Università di Napoli ‘Federico II’, Largo San Marcellino 10, 1-80138 Napoli, Italy
Annamaria Perrotta
Affiliation:
Dipartimento di Geofisica e Vulcanologia, Università di Napoli ‘Federico II’, Largo San Marcellino 10, 1-80138 Napoli, Italy
Claudio Scarpati
Affiliation:
Dipartimento di Geofisica e Vulcanologia, Università di Napoli ‘Federico II’, Largo San Marcellino 10, 1-80138 Napoli, Italy

Abstract

The southwestern part of Naples was the site of small volume volcanic activity prior to 12000 y B.P. Lava domes and possibly a lava flow were erupted during the earliest period. Explosive activity followed and produced pyroclastic sequences that are the proximal deposits of tuff cones within the city and at its southwestern extreme. The explosive activity was complex but predominantly phreatomagmatic. As the volcanic activity more than 12000 y B.P. in western Campi Flegrei shows a similar evolution from effusive to explosive, it is suggested that a large volcanic field ‘Paleoflegrei’, encompassing the western part of the city of Naples, existed prior to emplacement of the Neapolitan Yellow Tuff. The Neapolitan Yellow Tuff eruption about 12000 y B.P., from a vent in Campi Flegrei, produced widespread deposits up to 150 m thick that blanketed the area of the city of Naples, although the present day topography is strongly influenced by the pre-Neapolitan Yellow Tuff centres. Following the Neapolitan Yellow Tuff a small explosive eruption occurred in the bay of Chiaia, immediately south of the city, and results in the possibility of future eruptions within the city of Naples, outside the confines of Campi Flegrei and Vesuvius.

Type
Articles
Copyright
Copyright © Cambridge University Press 1994

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Capaldi, G., Civetta, L., & Gillot, P.-Y., 1985. Geochronology of Plio-Pleistocene volcanic rocks from southern Italy. Rendiconti delta Società Italiana di Mineralogia e Petrografia 40, 2544.Google Scholar
Capaldi, G., Civetta, L., Di Girolamo, P., Lanzara, R., Orsi, G., & Scarpati, C., 1987. Volcanological and geochemical constraints on the genesis of the deposits of Yellow Tuff in the Neapolitan-Phlegrean area. Rendiconti dell' Accademia delle Scienze Fisiche e Matematiche, Special Issue, 2540.Google Scholar
Cas, R. A. F., & Wright, J. V., 1987. Volcanic Successions. London: Allen & Unwin, 528 pp.CrossRefGoogle Scholar
D'Erasmo, G., 1931. Studio geologico dei pozzi Profundi della Campania. Bolletino della Società dei Naturatisti 43, 15130.Google Scholar
Dell'Erba, L., 1893. L'andesite pirosseno-micacea di Posillipo. Atti dell' Accademia Pontaniana 23, 115.Google Scholar
Di Girolamo, P., Ghiara, M. R., Lirer, L., Munno, R., Rolandi, G., & Stanzione, D., 1984. Vulcanologia e petrologia dei Campi Flegrei. Bollettino della Società Geologica Italiana 103, 349413.Google Scholar
Di Vito, M., Lirer, L., Mastrolorenzo, G., Rolandi, G., & Scandone, R., 1985. Volcanological map of Campi Flegrei. Università degli Studi di Napoli.Google Scholar
Fisher, R. V., Orsi, G., Ort, M., & Heiken, G., 1993. Mobility of a large volume pyroclastic flow-emplacement of the Campanian Ignimbrite, Italy. Journal of Volcanology and Geothermal Research 56, 205–20.CrossRefGoogle Scholar
Freda, G., 1889. Sulle masse trachitiche rinvenute nei recenti trafori delle colline di Napoli. Rendiconti della Reale Accademia della Scienze Fisiche e Matematiche 3, 3846.Google Scholar
Gleijeses, V., 1978. La storia di Napoli. Napoli: Soc. Ed. Napoletana, 939 pp.Google Scholar
Guadagno, M., 1926. La galleria della direttissima. Atti della Reale Istituto d'Incoraggiamenlo 78, 175.Google Scholar
Heiken, G. H., 1971. Tuff rings: examples from Fort rock-Christmas Lake valley basin, south central Oregon. Journal of Geophysical Research 16, 5615–26.CrossRefGoogle Scholar
Henry, C. D., & Wolf, J. A., 1992. Distinguishing strongly rheomorphic tuffs from extensive silicic lavas. Bulletin of Volcanology 54, 171–86.CrossRefGoogle Scholar
Johnston-Lavis, H. J., 1888. Report of the committee appointed for the investigation of the volcanic phenomena of Vesuvius and its neighbourhood, pp. 17. London.Google Scholar
Johnston-Lavis, H. J., 1889 a. Report of the committee appointed for the investigation of the volcanic phenomena of Vesuvius and its neighbourhood, pp. 812. London.Google Scholar
Johnston-Lavis, H. J., 1889 b. On a remarkable sodalite trachyte lately discovered in Naples, Italy. Geological Magazine 6, 74–7.CrossRefGoogle Scholar
Kokelaar, B. P., 1983. The mechanism of Surtseyan volcanism. Journal of the Geological Society, London 140, 939–44.CrossRefGoogle Scholar
Nicotera, P., 1950. Osservazioni geologiche sulla collina di Posillipo e sulla zona urbana occidentale di Napoli. Bollettino delta Società Geologica Italiana 69, 335–62.Google Scholar
Parascandola, A., 1936. I vulcani occidentali di Napoli. Bollettino delta Società dei Naturalisti 48, 3958.Google Scholar
Perrotta, A., & Scarpati, C., 1994. The dynamics of the Breccia Museo eruption (Campi Flegrei, Italy) and the significance of spatter clasts associated with lithic breccias. Journal of Volcanolology and Geothermal Research 59, 335–55.CrossRefGoogle Scholar
Rosi, M., & SBRANA, A., (eds) 1987. The Phlegrean Fields. CNR Quaderni de “La Ricerca Scientifica” no. 114 (8). 175 pp.Google Scholar
Santacroce, R., 1987. Somma Vesuvius. CNR Quaderni de “La Ricerca Scientifica” no. 114 (9).Google Scholar
Scarpati, C., Cole, P. D., & Perrotta, A., 1993. The Neapolitan Yellow Tuff—a large volume multi-phase eruption from Campi Flegrei, southern Italy. Bulletin of Volcanology 55, 343–56.CrossRefGoogle Scholar
Scherillo, A., 1953. Sulla revisione del foglio ‘Napoli’ della Carta Geologica d'ltalia. Bollettino del Servizio Geologico d'ltalia 75, 808–26.Google Scholar
Scherillo, A., 1957. I ‘tufi antichi’ tra S. Maria Apparente e via Parco Grifeo in Napoli. Bollettino della Società dei Naturalisti 66, 6989.Google Scholar
Scherillo, A., & Franco, E., 1960. Rilevamento stratigrafico del territorio communale di Napoli. Bollettino della Società dei Naturalisti 69, 255–62.Google Scholar
Scherillo, A., & Franco, E., 1967. Introduzione alia carta stratigrafica del suolo di Napoli. Atti dell' Accademia Pontaniana 16, 515.Google Scholar
Scherillo, A., & Scherillo, M., 1990. I Campi Flegrei e la stratigrafia napoletana. Accademia Pontaniana, 138 pp.Google Scholar
Sohn, Y. K., & Chough, S. K., 1992. The llchulbong tuff cone, Cheju Island, South Korea: depositional process and evolution of an emergent, Surtsian-type cone. Sedimentology 39, 523–44.CrossRefGoogle Scholar
Vighi, L., 1950. Rilevamento geologico della zona a sud del parallelo di Baia e della zona di Nisida, Coroglio e Trentaremi, nei Campi Flegrei. Bollettino della Società Geologica Italiana 69, 179209.Google Scholar