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Computer simulations of lava flow paths in the town of Goma, Nyiragongo volcano, Democratic Republic of Congo
Author(s)
Language
English
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Issue/vol(year)
/111 (2006)
Publisher
Agu
Pages (printed)
B06202
Issued date
2006
Abstract
The 17 January 2002 fissure eruption of Mount Nyiragongo, Democratic Republic of
Congo, produced lava flows which entered and devastated the densely inhabited town of
Goma. The 2002 and previous 1977 eruptions demonstrate the high level of volcanic
risk in the area. We present an analysis of the susceptibility to lava flow invasion in Goma,
by means of computer simulations based on the steepest descent path and probabilisticcomputed
flow spreading and obstacle overcoming. The DEM is obtained from a
topographic map of Goma by using the DEST algorithm. The numerical results show the
distribution of probable lava flow paths from possible vents in the investigated
topographic domain. Numerical simulations are validated through comparison with
the mapped paths of the 2002 lava flows in Goma. The subsequent investigation includes
the analysis of (1) hypothetical lava flow paths from ephemeral vents on the edge of the
2002 lava flows, (2) paths from venting along the hypothetical extension of the 2002
fissures, (3) paths in case of lava flow arrival in town from the north, and (4) changes
induced by the presence of the solidified 2002 lava field. The results show the
susceptibility of the different parts of the town of Goma to be invaded by future lava
flows, and reveal the existence of a large area in town with minimum susceptibility and
which can be invaded only in case of venting within it. The areas destroyed by the
2002 lava flows are predicted to be characterized by maximum susceptibility to lava flow invasion.
Congo, produced lava flows which entered and devastated the densely inhabited town of
Goma. The 2002 and previous 1977 eruptions demonstrate the high level of volcanic
risk in the area. We present an analysis of the susceptibility to lava flow invasion in Goma,
by means of computer simulations based on the steepest descent path and probabilisticcomputed
flow spreading and obstacle overcoming. The DEM is obtained from a
topographic map of Goma by using the DEST algorithm. The numerical results show the
distribution of probable lava flow paths from possible vents in the investigated
topographic domain. Numerical simulations are validated through comparison with
the mapped paths of the 2002 lava flows in Goma. The subsequent investigation includes
the analysis of (1) hypothetical lava flow paths from ephemeral vents on the edge of the
2002 lava flows, (2) paths from venting along the hypothetical extension of the 2002
fissures, (3) paths in case of lava flow arrival in town from the north, and (4) changes
induced by the presence of the solidified 2002 lava field. The results show the
susceptibility of the different parts of the town of Goma to be invaded by future lava
flows, and reveal the existence of a large area in town with minimum susceptibility and
which can be invaded only in case of venting within it. The areas destroyed by the
2002 lava flows are predicted to be characterized by maximum susceptibility to lava flow invasion.
References
Baxter, P., P. Allard, M. Halbwachs, J.-C. Komorowski, A. Woods, and
A. Ancia (2004), Human health and vulnerability in the Nyiragongo
volcano eruption and humanitarian crisis at Goma, Democratic Republic
of Congo, Acta Vulcanol., 14, 8 –14.
Calvari, S., and H. Pinkerton (1999), Lava tube morphology on Etna and
evidence for lava flow emplacement mechanisms, J. Volcanol. Geotherm.
Res., 90, 263– 280.
Capaccioni, B., O. Vaselli, A. P. Santo, and M. M. Yalire (2004),
Monogenic and polygenic volcanoes in the area between the Nyiragongo
summit crater and the Lake Kivu shoreline, Acta Vulcanol., 14, 1–8.
Costa, A., and G. Macedonio (2005), Numerical simulation of lava flows
based on depth-averaged equations, Geophys. Res. Lett., 32, L05304,
doi:10.1029/2004GL021817.
Crisci, G. M., R. Rongo, S. Di Gregorio, and W. Spataro (2004), The
simulation model SCIARA: The 1991 and 2001 lava flows at Mt. Etna,
J. Volcanol. Geotherm. Res., 132, 253– 267.
Demant, A., P. Lestrade, T. L. Ruananza, A. B. Kampunzu, and J. Durieux
(1994), Volcanological and petrological evolution of Nyiragongo volcano,
Virunga volcanic field, Zaire, Bull. Volcanol., 56, 47– 61.
Durieux, J. (2004a), Nyiragongo: The January 10th 1977 eruption, Acta
Vulcanol., 14, 141– 143.
Durieux, J. (2004b), Volcano Nyiragongo (D. R. Congo): Evolution of the
crater and lava lakes from the discovery to the present, Acta Vulcanol.,
14, 133– 140.
Favalli, M., and M. T. Pareschi (2004), Digital elevation model construction
from structured topographic data: The DEST algorithm, J. Geophys. Res.,
109, F04004, doi:10.1029/2004JF000150.
Favalli, M., M. T. Pareschi, A. Neri, and I. Isola (2005), Forecasting lava
flow paths by a stochastic approach, Geophys. Res. Lett., 32, L03305,
doi:10.1029/2004GL021718.
Goma Volcano Observatory, (2002), Nyiragongo, Bull. Global Volcan.
Network, 10– 27.
Kasereka,M., J.-P. Bajope,M.Yalire, J.Durieux, D. Tedesco, and J. Lockwood
(2002), Nyiragongo, Bull. Global Volcan. Network, 27, 9–10.
Kavotha, K. S., T. Mavonga, J. Durieux, and K. Mukambilwa (2004),
Towards a more detailed seismic picture of the January 17th, 2002 Nyiragongo
eruption, Acta Vulcanol., 14, 15– 28.
Komorowski, J. C., et al. (2004), The January 2002 flank eruption of
Nyiragongo volcano (Democratic Republic of Congo): Chronology, evidence
for a tectonic rift trigger, and impact of lava flows on the city of
Goma, Acta Vulcanol., 14, 29– 64.
Landi, P., M. Polacci, and M. Pompilio (2004), Final stages of cooling and
crystallization in magmas feeding the January 2002 Nyiragongo eruption,
paper presented at the EGU 1st General Assembly, Nice, France, 25–
30 April.
Lockwood, J. P., and T. J. Casadevall (1994), Status of active volcanoes in
the Goma area, Eastern Zaire, and associated hazards to residents and
refugees, U.S. Geol. Surv. Open File Rep., 94-581, 18 pp.
Miyamoto, H., and S. Sasaki (1997), Simulating lava flows by an improved
cellular automata method, Comput. Geosci., 23, 283– 292.
Pareschi, M. T., L. Cavarra, M. Favalli, and F. Giannini (2000a), GIS and
Volcanic Risk management, Nat. Hazard, 21, 361– 379.
Pareschi, M. T., M. Favalli, F. Giannini, R. Sulpizio, G. Zanchetta, and
R. Santacroce (2000b), May 5, 1998, Debris flows in circumvesuvian
areas (southern Italy), insights for hazard assessment, Geology, 28(7),
639– 642.
Pinkerton, H., and R. S. J. Sparks (1976), The 1975 sub-terminal lavas,
Mount Etna: A case history of the formation of a compound lava field,
J. Volcanol. Geotherm. Res., 1, 167– 182.
Polacci, M., and P. Papale (1999), The development of compound lava
fields at Mount Etna, Phys. Chem. Earth, 24, 949– 952.
Santo, A. P., B. Capaccioni, D. Tedesco, and O. Vaselli (2004), Petrographic
and geochemical features of the 2002 Nyiragongo lava flows,
Acta Vulcanol., 14, 59– 61.
Tazieff, H. (1949), Premie`re exploration du crate`re du volcan Nyiragongo,
Bull. Soc. Belge Ge´ol., 58, 165– 172.
Tazieff, H. (1977), An exceptional eruption: Mt. Nyiragongo, January 10th,
1977, Bull. Volcanol., 40, 1– 12.
Tazieff, H. (1979), Nyiragongo, the Forbidden Volcano, 287 pp., Barron’s
Educ. Ser., Inc.,Woodbury, N.Y. (Translated from French by J. F. Barnard,
Nyiragongo: Le volcan interdit, Flamarion, Paris, 1975.).
Tazieff, H. (1984), Mt. Nyiragongo: Renewed activity of the lava lake,
J. Volcanol. Geotherm. Res., 20, 267–280.
Tedesco, D. (2004), 1995 Nyiragongo and Nyamulagira activity in the
Virunga National Park: A volcanic crisis, Acta Vulcanol., 14, 149– 156.
Tedesco, D., P. Papale, O. Vaselli, and J. Durieux (2002), The January 17th,
2002 eruption of Nyiragongo, Democratic Republic of Congo, final report,
17 pp., UN Off. for the Coord. of Humanit. Affairs, Geneva.
Thonnard, R. L. G., M. E. Denaeyer, and P. Antun (1965), Carte volcanologique
des Virunga, Afrique Centrale, Feuille 1, 1:50,000 scale, Cent.
Natl. de Volcanol., Belgique, Missions Ge´ol. et Ge´ophys. aux Virunga,
Minist.e de l’Educ. et de la Culture, Brussels.
Von Go¨tzen, A. (1896), Durch Afrika von Ost nach West, Dietrich Reimer,
Berlin.
Wadge, G., P. A. V. Young, and I. J. McKendrick (1994), Mapping lava
flow hazards using computer simulation, J. Geophys. Res., 99, 489– 504.
A. Ancia (2004), Human health and vulnerability in the Nyiragongo
volcano eruption and humanitarian crisis at Goma, Democratic Republic
of Congo, Acta Vulcanol., 14, 8 –14.
Calvari, S., and H. Pinkerton (1999), Lava tube morphology on Etna and
evidence for lava flow emplacement mechanisms, J. Volcanol. Geotherm.
Res., 90, 263– 280.
Capaccioni, B., O. Vaselli, A. P. Santo, and M. M. Yalire (2004),
Monogenic and polygenic volcanoes in the area between the Nyiragongo
summit crater and the Lake Kivu shoreline, Acta Vulcanol., 14, 1–8.
Costa, A., and G. Macedonio (2005), Numerical simulation of lava flows
based on depth-averaged equations, Geophys. Res. Lett., 32, L05304,
doi:10.1029/2004GL021817.
Crisci, G. M., R. Rongo, S. Di Gregorio, and W. Spataro (2004), The
simulation model SCIARA: The 1991 and 2001 lava flows at Mt. Etna,
J. Volcanol. Geotherm. Res., 132, 253– 267.
Demant, A., P. Lestrade, T. L. Ruananza, A. B. Kampunzu, and J. Durieux
(1994), Volcanological and petrological evolution of Nyiragongo volcano,
Virunga volcanic field, Zaire, Bull. Volcanol., 56, 47– 61.
Durieux, J. (2004a), Nyiragongo: The January 10th 1977 eruption, Acta
Vulcanol., 14, 141– 143.
Durieux, J. (2004b), Volcano Nyiragongo (D. R. Congo): Evolution of the
crater and lava lakes from the discovery to the present, Acta Vulcanol.,
14, 133– 140.
Favalli, M., and M. T. Pareschi (2004), Digital elevation model construction
from structured topographic data: The DEST algorithm, J. Geophys. Res.,
109, F04004, doi:10.1029/2004JF000150.
Favalli, M., M. T. Pareschi, A. Neri, and I. Isola (2005), Forecasting lava
flow paths by a stochastic approach, Geophys. Res. Lett., 32, L03305,
doi:10.1029/2004GL021718.
Goma Volcano Observatory, (2002), Nyiragongo, Bull. Global Volcan.
Network, 10– 27.
Kasereka,M., J.-P. Bajope,M.Yalire, J.Durieux, D. Tedesco, and J. Lockwood
(2002), Nyiragongo, Bull. Global Volcan. Network, 27, 9–10.
Kavotha, K. S., T. Mavonga, J. Durieux, and K. Mukambilwa (2004),
Towards a more detailed seismic picture of the January 17th, 2002 Nyiragongo
eruption, Acta Vulcanol., 14, 15– 28.
Komorowski, J. C., et al. (2004), The January 2002 flank eruption of
Nyiragongo volcano (Democratic Republic of Congo): Chronology, evidence
for a tectonic rift trigger, and impact of lava flows on the city of
Goma, Acta Vulcanol., 14, 29– 64.
Landi, P., M. Polacci, and M. Pompilio (2004), Final stages of cooling and
crystallization in magmas feeding the January 2002 Nyiragongo eruption,
paper presented at the EGU 1st General Assembly, Nice, France, 25–
30 April.
Lockwood, J. P., and T. J. Casadevall (1994), Status of active volcanoes in
the Goma area, Eastern Zaire, and associated hazards to residents and
refugees, U.S. Geol. Surv. Open File Rep., 94-581, 18 pp.
Miyamoto, H., and S. Sasaki (1997), Simulating lava flows by an improved
cellular automata method, Comput. Geosci., 23, 283– 292.
Pareschi, M. T., L. Cavarra, M. Favalli, and F. Giannini (2000a), GIS and
Volcanic Risk management, Nat. Hazard, 21, 361– 379.
Pareschi, M. T., M. Favalli, F. Giannini, R. Sulpizio, G. Zanchetta, and
R. Santacroce (2000b), May 5, 1998, Debris flows in circumvesuvian
areas (southern Italy), insights for hazard assessment, Geology, 28(7),
639– 642.
Pinkerton, H., and R. S. J. Sparks (1976), The 1975 sub-terminal lavas,
Mount Etna: A case history of the formation of a compound lava field,
J. Volcanol. Geotherm. Res., 1, 167– 182.
Polacci, M., and P. Papale (1999), The development of compound lava
fields at Mount Etna, Phys. Chem. Earth, 24, 949– 952.
Santo, A. P., B. Capaccioni, D. Tedesco, and O. Vaselli (2004), Petrographic
and geochemical features of the 2002 Nyiragongo lava flows,
Acta Vulcanol., 14, 59– 61.
Tazieff, H. (1949), Premie`re exploration du crate`re du volcan Nyiragongo,
Bull. Soc. Belge Ge´ol., 58, 165– 172.
Tazieff, H. (1977), An exceptional eruption: Mt. Nyiragongo, January 10th,
1977, Bull. Volcanol., 40, 1– 12.
Tazieff, H. (1979), Nyiragongo, the Forbidden Volcano, 287 pp., Barron’s
Educ. Ser., Inc.,Woodbury, N.Y. (Translated from French by J. F. Barnard,
Nyiragongo: Le volcan interdit, Flamarion, Paris, 1975.).
Tazieff, H. (1984), Mt. Nyiragongo: Renewed activity of the lava lake,
J. Volcanol. Geotherm. Res., 20, 267–280.
Tedesco, D. (2004), 1995 Nyiragongo and Nyamulagira activity in the
Virunga National Park: A volcanic crisis, Acta Vulcanol., 14, 149– 156.
Tedesco, D., P. Papale, O. Vaselli, and J. Durieux (2002), The January 17th,
2002 eruption of Nyiragongo, Democratic Republic of Congo, final report,
17 pp., UN Off. for the Coord. of Humanit. Affairs, Geneva.
Thonnard, R. L. G., M. E. Denaeyer, and P. Antun (1965), Carte volcanologique
des Virunga, Afrique Centrale, Feuille 1, 1:50,000 scale, Cent.
Natl. de Volcanol., Belgique, Missions Ge´ol. et Ge´ophys. aux Virunga,
Minist.e de l’Educ. et de la Culture, Brussels.
Von Go¨tzen, A. (1896), Durch Afrika von Ost nach West, Dietrich Reimer,
Berlin.
Wadge, G., P. A. V. Young, and I. J. McKendrick (1994), Mapping lava
flow hazards using computer simulation, J. Geophys. Res., 99, 489– 504.
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