Intrusion of eccentric dikes: The case of the 2001 eruption and its role in the dynamics of Mt. Etna volcano
Language
English
Obiettivo Specifico
1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
1.4. TTC - Sorveglianza sismologica delle aree vulcaniche attive
1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
3.2. Tettonica attiva
3.6. Fisica del vulcanismo
4.3. TTC - Scenari di pericolosità vulcanica
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
/471 (2009)
Publisher
Elsevier
Pages (printed)
78–86
Date Issued
June 2009
Subjects
Abstract
The 2001 eruption represents one of the most studied events both from volcanological and geophysical point
of view on Mt. Etna. This eruption was a crucial event in the recent dynamics of the volcano, marking the
passage from a period (March 1993–June 2001) of moderate stability with slow, continuous flank sliding and
contemporaneous summit eruptions, to a period (July 2001 to present) of dramatically increased flank
deformations and flank eruptions. We show new GPS data and high precision relocation of seismicity in
order to demonstrate the role of the 2001 intrusive phase in this change of the dynamic regime of the
volcano. GPS data consist of two kinematic surveys carried out on 12 July, a few hours before the beginning of
the seismic swarm, and on 17 July, just after the onset of eruptive activity. A picture of the spatial distribution
of the sin-eruptive seismicity has been obtained using the HypoDD relocation algorithm based on the
double-difference (DD) technique. Modeling of GPS measurements reveals a southward motion of the upper
southern part of the volcano, driven by a NNW–SSE structure showing mainly left-lateral kinematics. Precise
hypocenter location evidences an aseismic zone at about sea level, where the magma upraise was
characterized by a much higher velocity and an abrupt westward shift, revealing the existence of a weakened
or ductile zone.
These results reveal how an intrusion of a dike can severely modify the shallow stress field, triggering
significant flank failure. In 2001, the intrusion was driven by a weakened surface, which might correspond to
a decollement plane of the portion of the volcano affected by flank instability, inducing an additional stress
testified by GPS measurements and seismic data, which led to an acceleration of the sliding flanks.
of view on Mt. Etna. This eruption was a crucial event in the recent dynamics of the volcano, marking the
passage from a period (March 1993–June 2001) of moderate stability with slow, continuous flank sliding and
contemporaneous summit eruptions, to a period (July 2001 to present) of dramatically increased flank
deformations and flank eruptions. We show new GPS data and high precision relocation of seismicity in
order to demonstrate the role of the 2001 intrusive phase in this change of the dynamic regime of the
volcano. GPS data consist of two kinematic surveys carried out on 12 July, a few hours before the beginning of
the seismic swarm, and on 17 July, just after the onset of eruptive activity. A picture of the spatial distribution
of the sin-eruptive seismicity has been obtained using the HypoDD relocation algorithm based on the
double-difference (DD) technique. Modeling of GPS measurements reveals a southward motion of the upper
southern part of the volcano, driven by a NNW–SSE structure showing mainly left-lateral kinematics. Precise
hypocenter location evidences an aseismic zone at about sea level, where the magma upraise was
characterized by a much higher velocity and an abrupt westward shift, revealing the existence of a weakened
or ductile zone.
These results reveal how an intrusion of a dike can severely modify the shallow stress field, triggering
significant flank failure. In 2001, the intrusion was driven by a weakened surface, which might correspond to
a decollement plane of the portion of the volcano affected by flank instability, inducing an additional stress
testified by GPS measurements and seismic data, which led to an acceleration of the sliding flanks.
Sponsors
This work was funded by the Istituto Nazionale di Geofisica e
Vulcanologia and by the Dipartimento per la Protezione Civile (Italy).
Vulcanologia and by the Dipartimento per la Protezione Civile (Italy).
References
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s00445-003-0280-3.
Acocella, V., Neri, M., 2005. Structural features of an active strike-slip fault on the sliding
flank of Mt. Etna (Italy). J. Struct. Geol. 27, 343–355. doi:10.1016/j.jsg.2004.07.006.
Acocella, V., Behncke, B., Neri, M., D, Amico, S., 2003. Link between major flank slip and
eruptions at Mt. Etna (Italy). J. Geophys. Res. 30, 2286. doi:10.1029/2003GL018642.
Allard, P., Behncke, B., D, Amico, S., Neri, M., Gambino, S., 2006. Mount Etna 1993–2005:
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insights into a complex plumbing system. Bull. Volcanol. 67, 314–330. doi:10.1007/
s00445-004-0372-8.
Behncke, B., Neri, M., 2003a. The July–August 2001 eruption of Mt. Etna (Sicily). Bull.
Volcanol. 65, 461–476.
Behncke, B., Neri, M., 2003b. Cycles and trends in the recent eruptive behaviour of
Mount Etna (Italy). Can. J. Earth Sci. 40, 1405–1411. doi:10.1139/E03–052.
Behncke, B., Neri, M., Carniel, R., 2003. An exceptional case of lava dome growth
spawning pyroclastic avalanches at Mt. Etna (Italy): the 1999 Bocca Nuova
eruption. J. Volcanol. Geotherm. Res. 124 (1–2), 115–128.
Behncke, B., Neri, M., Nagay, A., 2005. Lava flow hazard at Mount Etna (Italy): new data
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of lava flows. Spec. Pap. Geol. Soc. Am., vol. 396-13, pp. 187–205. doi:10.1130/
2005.2396(13).
Behncke, B., Neri, M., Pecora, E., Zanon, V., 2006. The exceptional activity and growth of
the Southeast Crater, Mount Etna (Italy), between 1996 and 2001. Bull. Volcanol. 69,
149–173. doi:10.1007/s00445-006-0061-x.
Behncke, B., Calvari, S., Giammanco, S., Neri, M., Pinkerton, H., 2008. Volcaniclastic flows
resulting from interaction of basaltic magma with hydrothermally altered rock: an
example from the 2006 summit eruptions of Mount Etna (Italy). Bull. Volcanol.
doi:10.1007/s00445-008-0200-7.
Billi, A., Acocella, V., Funiciello, R., Giordano, G., Lanzafame, G., Neri, M., 2003.
Mechanisms for ground-surface fracturing and incipient slope failure associated to
the July–August 2001 eruption of Mt. Etna, Italy: analysis of ephemeral field data.
J. Volcanol. Geotherm. Res. 122, 281–294. doi:10.1016/S0377-0273(02)00507-3.
Bonaccorso, A., Aloisi, M., Mattia, M., 2002. Dike emplacement forerunning the Etna July
2001 eruption modeled through continuous tilt and GPS data. Geophys. Res. Lett.
29. doi:10.1029/2001GL014397.
Bonaccorso, A., D,Amico, S.,Mattia,M., Patanè, D., 2004. Intrusivemechanisms atMt. Etna
forerunning the July–August 2001 eruption from seismic and ground deformation
data. Pure Appl. Geophys. 161, 1469–1487. doi:10.1007/s00024-004-2515-4.
Bonaccorso, A., Bonforte, A., Guglielmino, F., Palano, M., Puglisi, G., 2006. Composite
ground deformation pattern forerunning the 2004–2005 Mount Etna eruption.
J. Geophys. Res. 111, B12207. doi:10.1029/2005JB004206.
Bonforte, A., Puglisi, G., 2003. Magma uprising and flank dynamics on Mt. Etna volcano,
studied by GPS data (1994–1995). J. Geophys. Res. 108 (B3), 2153–2162.
Bonforte, A., Puglisi, G., 2006. Dynamics of the eastern flank of Mt. Etna volcano (Italy)
investigated by a dense GPS network. J. Volcanol. Geotherm. Res. 153, 357–369.
doi:10.1016/j.jvolgeores.2005.12.005.
Bonforte, A., Guglielmino, F., Palano, M., Puglisi, G., 2004. A syn-eruptive ground
deformation episode measured by GPS, during the 2001 eruption on the upper
southern flank of Mt. Etna. Bull. Volcanol. 66, 336–341.
Bonforte, A., Branca, S., Palano, M., 2007a. Geometric and kinematic variations along the
active Pernicana fault: Implication for the dynamics of Mount Etna NE flank (Italy).
J. Volcanol. Geotherm. Res. doi:10.1016/j.jvolgeores.2006.08.009.
Bonforte, A., Carbone, D., Greco, F., Palano, M., 2007b. Intrusive mechanism of the 2002
NE-rift eruption at Mt. Etna (Italy) modelled using GPS and gravity data. Geophys.
J. Int. doi:10.1111/j.1365-246X.2006.03249.x.
Bonforte, A., Gambino, S., Guglielmino, F., Obrizzo, F., Palano, M., Puglisi, G., 2007c.
Ground deformation modeling of flank dynamics prior to the 2002 eruption of Mt.
Etna. Bull. Volcanol. doi:10.1007/s00445-006-0106-1.
Bonforte, A., Bonaccorso, A., Guglielmino, F., Palano, M., Puglisi, G., 2008. Feeding system
and magma storage beneath Mt. Etna as revealed by recent inflation/deflation
cycles. J. Geophys. Res. 113, B05406. doi:10.1029/2007JB005334.
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Carlo, P., Lanzafame, G., Lodato, L., Miraglia, L., Salerno, G., Spampinato, L., 2005.
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sequence and the opening of the Valle del Bove on Etna volcano (Italy). J. Volcanol.
Geotherm. Res. 87 (1–4), 193–209. doi:10.1016/S0377-0273(98)00089-4.
Calvari, S., Neri, M., Pinkerton, H., 2003. Effusion rate estimation during the 1999 summit
eruption onMt. Etna, and growth of two distinct lava flowfields. J.Volcanol. Geotherm.
Res. 119 (1–4), 107–123.
Clocchiatti, R., Condomines, M., Guénot, N., Tanguy, J.-C., 2004. Magma changes at Mount
Etna: the 2001 and 2002–2003 eruptions. Earth Planet. Sci. Lett. 226, 397–414.
doi:10.1016/j.epsl.2004.07.039.
Cocina, O., Neri, G., Privitera, E., Spampinato, S., 1997. Stress tensor computations in the
Mount Etna area (Southern Sicily) and tectonic implications. J. Geodyn. 23,109–127.
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inferred from petrologic monitoring. Geophys. Res. Lett. 32, L13302. doi:10.1029/
2005GL022347.
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s00445-003-0280-3.
Acocella, V., Neri, M., 2005. Structural features of an active strike-slip fault on the sliding
flank of Mt. Etna (Italy). J. Struct. Geol. 27, 343–355. doi:10.1016/j.jsg.2004.07.006.
Acocella, V., Behncke, B., Neri, M., D, Amico, S., 2003. Link between major flank slip and
eruptions at Mt. Etna (Italy). J. Geophys. Res. 30, 2286. doi:10.1029/2003GL018642.
Allard, P., Behncke, B., D, Amico, S., Neri, M., Gambino, S., 2006. Mount Etna 1993–2005:
anatomy of an evolving eruptive cycle. Earth-Sci. Rev. 78, 85–114. doi:10.1016/j.
earscirev.2006.04.002.
Andronico, D., Branca, S., Calvari, S., Burton, M., Caltabiano, T., Corsaro, R.A., Del Carlo, P.,
Garfì, G., Lodato, L., Miraglia, L., Murè, F., Neri, M., Pecora, E., Pompilio, M., Salerno,
G., Spampinato, L., 2005. A multi-disciplinary study of the 2002–03 Etna eruption:
insights into a complex plumbing system. Bull. Volcanol. 67, 314–330. doi:10.1007/
s00445-004-0372-8.
Behncke, B., Neri, M., 2003a. The July–August 2001 eruption of Mt. Etna (Sicily). Bull.
Volcanol. 65, 461–476.
Behncke, B., Neri, M., 2003b. Cycles and trends in the recent eruptive behaviour of
Mount Etna (Italy). Can. J. Earth Sci. 40, 1405–1411. doi:10.1139/E03–052.
Behncke, B., Neri, M., Carniel, R., 2003. An exceptional case of lava dome growth
spawning pyroclastic avalanches at Mt. Etna (Italy): the 1999 Bocca Nuova
eruption. J. Volcanol. Geotherm. Res. 124 (1–2), 115–128.
Behncke, B., Neri, M., Nagay, A., 2005. Lava flow hazard at Mount Etna (Italy): new data
from a GIS-based study. In: Manga, M., Ventura, G. (Eds.), Kinematics and dynamics
of lava flows. Spec. Pap. Geol. Soc. Am., vol. 396-13, pp. 187–205. doi:10.1130/
2005.2396(13).
Behncke, B., Neri, M., Pecora, E., Zanon, V., 2006. The exceptional activity and growth of
the Southeast Crater, Mount Etna (Italy), between 1996 and 2001. Bull. Volcanol. 69,
149–173. doi:10.1007/s00445-006-0061-x.
Behncke, B., Calvari, S., Giammanco, S., Neri, M., Pinkerton, H., 2008. Volcaniclastic flows
resulting from interaction of basaltic magma with hydrothermally altered rock: an
example from the 2006 summit eruptions of Mount Etna (Italy). Bull. Volcanol.
doi:10.1007/s00445-008-0200-7.
Billi, A., Acocella, V., Funiciello, R., Giordano, G., Lanzafame, G., Neri, M., 2003.
Mechanisms for ground-surface fracturing and incipient slope failure associated to
the July–August 2001 eruption of Mt. Etna, Italy: analysis of ephemeral field data.
J. Volcanol. Geotherm. Res. 122, 281–294. doi:10.1016/S0377-0273(02)00507-3.
Bonaccorso, A., Aloisi, M., Mattia, M., 2002. Dike emplacement forerunning the Etna July
2001 eruption modeled through continuous tilt and GPS data. Geophys. Res. Lett.
29. doi:10.1029/2001GL014397.
Bonaccorso, A., D,Amico, S.,Mattia,M., Patanè, D., 2004. Intrusivemechanisms atMt. Etna
forerunning the July–August 2001 eruption from seismic and ground deformation
data. Pure Appl. Geophys. 161, 1469–1487. doi:10.1007/s00024-004-2515-4.
Bonaccorso, A., Bonforte, A., Guglielmino, F., Palano, M., Puglisi, G., 2006. Composite
ground deformation pattern forerunning the 2004–2005 Mount Etna eruption.
J. Geophys. Res. 111, B12207. doi:10.1029/2005JB004206.
Bonforte, A., Puglisi, G., 2003. Magma uprising and flank dynamics on Mt. Etna volcano,
studied by GPS data (1994–1995). J. Geophys. Res. 108 (B3), 2153–2162.
Bonforte, A., Puglisi, G., 2006. Dynamics of the eastern flank of Mt. Etna volcano (Italy)
investigated by a dense GPS network. J. Volcanol. Geotherm. Res. 153, 357–369.
doi:10.1016/j.jvolgeores.2005.12.005.
Bonforte, A., Guglielmino, F., Palano, M., Puglisi, G., 2004. A syn-eruptive ground
deformation episode measured by GPS, during the 2001 eruption on the upper
southern flank of Mt. Etna. Bull. Volcanol. 66, 336–341.
Bonforte, A., Branca, S., Palano, M., 2007a. Geometric and kinematic variations along the
active Pernicana fault: Implication for the dynamics of Mount Etna NE flank (Italy).
J. Volcanol. Geotherm. Res. doi:10.1016/j.jvolgeores.2006.08.009.
Bonforte, A., Carbone, D., Greco, F., Palano, M., 2007b. Intrusive mechanism of the 2002
NE-rift eruption at Mt. Etna (Italy) modelled using GPS and gravity data. Geophys.
J. Int. doi:10.1111/j.1365-246X.2006.03249.x.
Bonforte, A., Gambino, S., Guglielmino, F., Obrizzo, F., Palano, M., Puglisi, G., 2007c.
Ground deformation modeling of flank dynamics prior to the 2002 eruption of Mt.
Etna. Bull. Volcanol. doi:10.1007/s00445-006-0106-1.
Bonforte, A., Bonaccorso, A., Guglielmino, F., Palano, M., Puglisi, G., 2008. Feeding system
and magma storage beneath Mt. Etna as revealed by recent inflation/deflation
cycles. J. Geophys. Res. 113, B05406. doi:10.1029/2007JB005334.
Borgia, A., Ferrari, L., Pasquarè, G., 1992. Importance of gravitational spreading in the
tectonic and volcanic evolution of Mt. Etna. Nature 357, 231–235.
Burton, M., Neri, M., Andronico, D., Branca, S., Caltabiano, T., Calvari, S., Corsaro, R.A., Del
Carlo, P., Lanzafame, G., Lodato, L., Miraglia, L., Salerno, G., Spampinato, L., 2005.
Etna 2004–2005: an archetype for geodynamically-controlled effusive eruptions.
Geophys. Res. Lett. 32, L09303. doi:10.1029/2005GL022527.
Calvari, S., Tanner, L.H., Groppelli, G., 1998. Debris-avalanche deposits of the Milo Lahar
sequence and the opening of the Valle del Bove on Etna volcano (Italy). J. Volcanol.
Geotherm. Res. 87 (1–4), 193–209. doi:10.1016/S0377-0273(98)00089-4.
Calvari, S., Neri, M., Pinkerton, H., 2003. Effusion rate estimation during the 1999 summit
eruption onMt. Etna, and growth of two distinct lava flowfields. J.Volcanol. Geotherm.
Res. 119 (1–4), 107–123.
Clocchiatti, R., Condomines, M., Guénot, N., Tanguy, J.-C., 2004. Magma changes at Mount
Etna: the 2001 and 2002–2003 eruptions. Earth Planet. Sci. Lett. 226, 397–414.
doi:10.1016/j.epsl.2004.07.039.
Cocina, O., Neri, G., Privitera, E., Spampinato, S., 1997. Stress tensor computations in the
Mount Etna area (Southern Sicily) and tectonic implications. J. Geodyn. 23,109–127.
Corsaro, R.A., Miraglia, L., 2005. Dynamics of 2004–2005 Mt. Etna effusive eruption as
inferred from petrologic monitoring. Geophys. Res. Lett. 32, L13302. doi:10.1029/
2005GL022347.
Froger, J., Merle, O., Briole, P., 2001. Active spreading and regional extension at Mount
Etna imaged by SAR interferometry. Earth Planet. Sci. Lett. 187, 245–258.
Gambino, S., 2004. Continuous dynamic response along a pre-existing structural
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