Skip to main content
Log in

Focal parameters of seismic sources during the 1981 and 1983 eruption at Mt. Etna volcano (Sicily, Italy)

  • Original Article
  • Published:
Environmental Geology

Abstract

In this study 50 seismic events, preceding and accompanying the eruptions occurring in 1981 and 1983, have been considered. Seismic moments, fault radii, stress drops and seismic energies have been calculated using Brune’s model (J Geophys Res 75:4997–5009, 1970; J Geophys Res 76:5002, 1971); site, anelastic attenuation along the propagation path, geometrical spreading and interaction with the free surface effects are taken into account. For each event we have also estimated the equivalent Wood–Anderson magnitude (MWAeq) (Scherbaum and Stoll in Bull Seism Soc Am 73:1321–1343, 1983); relations among all these source parameters have been determined. Furthermore, the hypothesis of self-similarity (Aki in J Geophys Res 72:1217–1231, 1967) is not verified for events with seismic moments <1012 N-m: in fact the relationship between log-stress drop and log-moment is linear up to a moment of 1012 N-m (events of 1981 eruption), while for higher moments (events of 1983 eruption) the slope of the regression line is not significantly different from zero. We suppose that such a behaviour is related to a heterogeneous medium with barriers on the faults. Finally, the main conclusion is that eruptions of 1981 and 1983 differ from one another both in eruptive and seismic aspects; analysis of seismic energies indicates an increase in Mt. Etna’s activity, confirmed by studies performed on the following lateral eruption of 1991–1993 (Patanè et al. in Bull Volcanol 47:941–952, 1995), occurring on the same structural trend.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Aki K (1967) Scaling law of seismic spectrum. J Geophys Res 72:1217–1231

    Article  Google Scholar 

  • Aki K (1984) Asperities, barriers, characteristic earthquakes and strong motion prediction. J Geophys Res 89-B7:5867–5872

    Article  Google Scholar 

  • Aki K (1987) Magnitude–Frequency relation for small earthquakes: a clue to the origin of fmax of large earthquakes. J Geophys Res 92-B2:1349–1355

    Article  Google Scholar 

  • Aki K, Richards PG (1980a) Quantitative seismology: theory and methods, vol I. W.H. Freeman, San Francisco

    Google Scholar 

  • Aki K, Richards PG (1980b) Quantitative seismology: theory and methods, vol II. W.H. Freeman, San Francisco

    Google Scholar 

  • Barberi F, Gasparini P, Innocenti F, Villari L (1974) Volcanism of the southern Tyrrhenian Sea and geodynamic implications. J Geophys Res 78:5221–5232

    Article  Google Scholar 

  • Brune JN (1970) Tectonic stress and the spectra of seismic shear waves from Earthquake. J Geophys Res 75:4997–5009

    Article  Google Scholar 

  • Brune JN (1971) Correction. J Geophys Res 76:5002

    Article  Google Scholar 

  • Centamore C, Montalto A, Patanè G (1997) Self-similarity and scaling relations for microearthquakes at Mt. Etna volcano (Italy). Phys Earth Planet Inter 103:165–177

    Article  Google Scholar 

  • Cosentino M, Cristofolini R, Ferri M et al. (1981) L’eruzione dell’Etna del 17–23 Marzo 1981: Rapporto preliminare. Rend Soc Geol Ital 4:249–252

    Google Scholar 

  • Cristofolini R, Imposa N, Patanè G (1984) Etna 1983: Cronaca minore di un evento storico, vol 1. Tringale ed., Catania, pp 116

    Google Scholar 

  • Del Pezzo E, Gresta S, Patanè G, Patanè D, Scarcella G (1987) Attenuation of short period seismic waves at Etna as compared to other volcanic areas, Pageoph 125:1039–1050

    Article  Google Scholar 

  • Dysart PS, Snoke JA, Sacks IS (1988) Source parameters and scaling relations for small earthquakes in the Matsushiro region, southwest Honshu, Japan. Bull Seism Soc Am 78:571–589

    Google Scholar 

  • Feignier B (1991) How geology can influence scaling relations. Tectonophysics 197:41–53

    Article  Google Scholar 

  • Fletcher JB, Haar LC, Vernon FL, Brune JN, Hanks TC, Berger J (1986) The effects of attenuation on the scaling of source parameters for earthquakes at Anza, California. In: Das J, Boatwright J, Scholtz CH (eds) Earthquake source mechanics. Geophysical monographs. Am Geophys Union 57:331–338

  • Frankel A (1982) The effects of attenuation and site response on the spectra of microearthquakes in the north-eastern Carribeans. Bull Seism Soc Am 72:1379–1402

    Google Scholar 

  • Glot JP, Gresta S, Patanè G, Poupinet G (1984) Earthquake activity during the 1983 Etna eruption. Bull Volcanol 47:953–963

    Article  Google Scholar 

  • Gvirtzman Z, Nur A (1999) The formation of Mount Etna as the consequence of slab rollback. Nat vol 401:782–785

    Article  Google Scholar 

  • Hanks TC (1982) fmax. Bull Seism Soc Am 72:1867–1879

    Google Scholar 

  • Hirn A, Nercessian A, Sapin M, Ferrucci F, Wittlinger G (1991) Seismic heterogeneity of Mt. Etna: structure and activity. Geophys J Int 105:139–153

    Article  Google Scholar 

  • La Delfa S, Patanè G, Clocchiatti R, Joron JL, Tanguy JC (2001) Activity of Mount Etna preceding the February 1999 fissure eruption: inferred mechanism from seismological and geochemical data. J Volcanol Geotherm Res 105:121–139

    Article  Google Scholar 

  • Lee WHK, Lahr JC (1975) Hypo71 (revised): a computer program for determining hypocenter, magnitude, and first motion pattern of local earthquakes. Geol Surv Open File Rep (US) 75-311:1–116

    Google Scholar 

  • Malin PE, Waller JA (1985) Preliminary results from vertical seismic profiling of Oroville microearthquake S-waves. Geophys Res Lett 12:137–140

    Article  Google Scholar 

  • Papageorgiou AS, Aki K (1983) A specific barrier model for the earthquake quantitative description of inhomogeneous faulting and the prediction of strong ground motion. I. Description of the model. Bull Seism Soc Am 73:693–722

    Google Scholar 

  • Patanè G, Gresta S, Imposa S (1984) Seismic activity preceding the 1983 eruption of Mt. Etna. Bull Volcanol 47:941–952

    Article  Google Scholar 

  • Patanè G, Coco G, Corrao M, Imposa S, Montalto A (1995) Source parameters of seismic events at Mount Etna Volcano, Italy, during the outburst of the 1991–1993 eruption. Phys Earth Planet Inter 89:149–162

    Article  Google Scholar 

  • Romano R, Vaccaro C (1986) The recent eruptive activity on Mt. Etna, Sicily: 1981–1985. Per Mineral 55:91–111

    Google Scholar 

  • Scherbaum F, Stoll D (1983) Source parameters and scaling laws of the 1978 Swabian Jura (Southwest Germany) afterschocks. Bull Seism Soc Am 73:1321–1343

    Google Scholar 

  • Schiano P, Clocchiatti R, Ottolini L, Busà T (2001) Transition of Mount Etna lavas from a mantle-plume to an island-arc magmatic source. Nature 412:900–904

    Article  Google Scholar 

  • SEAN Bulletin, 1981. 6:2–5, 60–61

  • SEAN Bulletin, 1983. 8, 5:6–7

  • Tanguy JC, Condomines M, Kieffer G (1997) Evolution of the Mount Etna magma: constraints on the present feeding system and eruptive mechanism. J Volcanol Geotherm Res 75:221–250

    Article  Google Scholar 

Download references

Acknowledgments

S. Imposa was supported by grants (Fondi di Ateneo—2005) from the University of Catania.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Sebastiano Imposa.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Imposa, S. Focal parameters of seismic sources during the 1981 and 1983 eruption at Mt. Etna volcano (Sicily, Italy). Environ Geol 55, 1061–1073 (2008). https://doi.org/10.1007/s00254-007-1055-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00254-007-1055-5

Keywords

Navigation