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http://hdl.handle.net/2122/3136
DC Field | Value | Language |
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dc.contributor.authorall | Crisci, G. M.; Department of Earth Sciences,University of Calabria, Arcavacata | en |
dc.contributor.authorall | Di Gregorio, S.; Department of Mathematics,University of Calabria, Arcavacata | en |
dc.contributor.authorall | Rongo, R.; Department of Earth Sciences,University of Calabria, Arcavacata, University of Calabria, Arcavacata | en |
dc.contributor.authorall | Scarpelli, M.; Department of Earth Sciences,University of Calabria, Arcavacata, University of Calabria, Arcavacata | en |
dc.contributor.authorall | Spataro, W.; Department of Mathematics,University of Calabria, Arcavacata, | en |
dc.contributor.authorall | Calvari, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.date.accessioned | 2007-12-12T15:34:51Z | en |
dc.date.available | 2007-12-12T15:34:51Z | en |
dc.date.issued | 2001-09 | en |
dc.identifier.uri | http://hdl.handle.net/2122/3136 | en |
dc.description.abstract | SCIARA (Smart Cellular Interactive Automata for modeling the Rheology of Aetnean lava flows, to be read as “shea’rah”), our first two-dimensional Cellular Automata model for the simulation of lava flows, was tested and validated with success on several lava events like the 1986/87 Etnean eruption and the last phase of the 1991/93 Etnean one. Real and simulated events are satisfying within limits to forecast the surface covered by the lava flow. Moreover, improved versions have been adopted in testing other real lava flows of Mount Etna and of Reunion Island (Indian Ocean). The model has been applied with success in the determination of risk zones in the inhabited areas of Nicolosi, Pedara, S. Alfio and Zafferana (Sicily). The main goal of the present work has been the verification of the effects, in volcanic risk terms, in the Etnean area from Nicolosi to Catania, of a eruptive crisis similar to the event that occurred in 1669, as if the episode would happen nowadays. Catania has been severely interested in some major Etnean events in history, the most famous one being, namely, the 1669 eruption, involving 1 km3 of lava during 130 days. The simulation of lava tubes and the usage of different histories within the experiments have been crucial in the determination of a new risk area for Catania. In fact, simulations carried out without the introduction of lava tubes, never involved the city, proving the fact that lava tubes, played a fundamental role in the 1669 Catania lava crisis. | en |
dc.language.iso | English | en |
dc.relation.ispartof | Annual Conference of the International Association for Mathematical Geology, IAMG 2001 | en |
dc.subject | Mount Etna | en |
dc.subject | cellular automata | en |
dc.title | The Catania 1669 lava eruptive crisis: simulation of a new possible eruption | en |
dc.type | Conference paper | en |
dc.description.status | Published | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk | en |
dc.description.ConferenceLocation | Cancún, Mexico | en |
dc.relation.references | [1] Toffoli, T., Cellular Automata as an alternative to (rather than an approximation of) differential equations in modeling physics, Physica 10D, 117-127 (1984). [2] Petitot, J., Centrato/acentrato, Enciclopedia Einaudi, Vol. II, pp 894-954, Ed. Einaudi, Torino, Italy (1977) [3] Burks, A. W., Essays on Cellular Automata, University of Illinois Press (1970). [4] S. Wolfram, Computation theory of Cellular Automata, Comm. Math. Phys. 96, 15-57 (1984). [5] Margolus, N., Toffoli, T., Vichniac, G., Cellular Automata supercomputers for fluid-dynamics modelling, Phys. Rev. Lett. 56 n. 10 ,1694-1696 (1986). [6] Vichniac, G., Simulating physics with cellular automata, Physica 10D, 96-115 (1984). [7] von Neumann, J., Theory of self reproducing automata, University of Illinois Press (1966). [8] Lindenmayer, A., Cellular Automata, formal languages and development systems, IV Int. Congress for Logic, Methodology and Philosophy of Science , Bucarest (1971). [9] Toffoli, T., Margolus, N., Cellular Automata Machines A new enviroment for modeling, MIT Press (1987). [10] Norman, M.G., Henderson, J.R., Main, G., Wallace, D.J., The use of the CAPE Environment in the simulation of rock fracturing, Concurrency: Practice and Experience, Vol. 3 (6), 687-698 (1991). [11] Barca, D., Crisci, G.M., Di Gregorio, S., Nicoletta F.P., Cellular Automata methods for modeling lava flow: simulation of the 1986-1987 etnean eruption, Chapt. twelve of Active Lavas, Kilburn C. and Luongo G. Eds., 283-301, UCL Press London (1993). [12] Barca, D., Crisci, G.M., Di Gregorio, S., Nicoletta F.P., Cellular Automata for simulating lava flows: a method and examples of the Etnean eruptions, Transport Theory and Statistical Physics, 23 (1-3), pp. 195-232 (1994). [13] Di Gregorio, S., Rongo, R., Spataro, W., Spezzano, G., Talia, D., A Parallel Cellular Tool for Interactive Modeling and Simulation, IEEE Computational Science & Engineering, vol. 3, no. 3, pp. 33-43 (1996). [14] Crisci, G.M., Di Gregorio, S., Ranieri, G., A cellular space model of basaltic lava flow. Proc. Int. Conf. “Applied Modelling and Simulation 82”, Paris -France, Vol. 11, pp. 65-67 (1982). [15] Crisci, G.M., Di Gregorio, S., Pindaro, O., Ranieri, G. Lava flow simulation by a discrete cellular model: first implementation. Int. Journal of Modelling and Simulation, Vol. 6 pp. 137-140 (1986). [16] Barca, D., Crisci, G.M., Di Gregorio, S., Nicoletta,, F.P.,: Lava flow simulation by cellular automata: Pantelleria’ s examples. - Proc. AMS Int. Conf. “Modeling and Simulation”, Cairo, Vol. 4 A, pp. 9-15 (1987). [17] Barca, D., Crisci, G.M., Di Gregorio, S., Marabini, S., Nicoletta, F.P., Nuovo modello cellulare per flussi lavici : colate di Pantelleria. - Bollettino GNV, 4, pp. 41-51 (1988). [18] Barca, D., Crisci, G.M., Di Gregorio, S., Marabini, S., Nicoletta, F.P., Lava flow simulation by Cellular Automata and Pantelleria’s example - Proc. Kagoshima Int. Conf. on Volcanoes pp. 475-478 (1988). [19] Barca, D., Crisci, G.M., Di Gregorio, S., Nicoletta, F.P., Cellular Automata methods for modeling lava flow: simulation of the 1986-1987 etnean eruption. - Chapt. Twelve of Active Lavas - Kilburn C. and Luongo G. Eds. - UCL Press London (1993), pp 283-301 (1993). [20] Barca, D, Crisci, G.M., Di Gregorio, S., Nicoletta, F.P., Cellular Automata for simulating lava flows: a method and examples of the Etnean eruptions - Transport Theory and Statistical Physics, 23 (1-3), pp. 195-232 (1994). [21] Ishihara, K., Iguchi, M. and Kamo, K., Numerical simulation of lava flows at Sakurajima. Proc. Kagoshima Int. Conf. on Volcanoes pp. 479-482 (1988). [22] Ishihara, K., Iguchi, M. and Kamo, K., Numerical simulation of lava flows on some volcanoes in Japan. IAVCEI Proc. in Volcanology, Vol. 2 Ed. by J. Fink Springer-Verlag (1989). [23] Young, P. and Wadge, G., Flowfront: simulation of a lava flow. Computer & Geosciences Vol. 16, N. 8, pp. 1171-1191 (1990). [24] Crisci, G.M., Di Francia, A., Di Gregorio, S., Nicoletta, F., Rongo, R., Spataro, W., Sciara.2: A Cellular Automata Model for Lava Flow Simulation. Proc. IAMG97, Vera Pawlowsky Glahn (Ed.), Addendum, pp. 11-16 (1997). | en |
dc.description.obiettivoSpecifico | 4.3. TTC - Scenari di pericolosità vulcanica | en |
dc.description.fulltext | open | en |
dc.contributor.author | Crisci, G. M. | en |
dc.contributor.author | Di Gregorio, S. | en |
dc.contributor.author | Rongo, R. | en |
dc.contributor.author | Scarpelli, M. | en |
dc.contributor.author | Spataro, W. | en |
dc.contributor.author | Calvari, S. | en |
dc.contributor.department | Department of Earth Sciences,University of Calabria, Arcavacata | en |
dc.contributor.department | Department of Mathematics,University of Calabria, Arcavacata | en |
dc.contributor.department | Department of Earth Sciences,University of Calabria, Arcavacata, University of Calabria, Arcavacata | en |
dc.contributor.department | Department of Earth Sciences,University of Calabria, Arcavacata, University of Calabria, Arcavacata | en |
dc.contributor.department | Department of Mathematics,University of Calabria, Arcavacata, | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
item.openairetype | Conference paper | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Università della Calabria, Dipartimento di Scienze della Terra, Arcavacata di Rende (Cosenza), Italy | - |
crisitem.author.dept | Department of Mathematics, University of Calabria, 87036 Rende, Italy | - |
crisitem.author.dept | Università della Calabria, Dipartimento di Scienze della Terra, Arcavacata di Rende (Cosenza), Italy | - |
crisitem.author.dept | Department of Earth Sciences, University of Calabria, Arcavacata | - |
crisitem.author.dept | High Performance Computing Centre, University of Calabria, 87036 Rende, Italy | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.orcid | 0000-0001-8189-5499 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Conference materials |
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