Volume 88, Issue 16 p. 177-181
Free Access

Cooperation on Congo volcanic and environmental risks

D. Tedesco

D. Tedesco

Department of Environmental Sciences, University of Napoli 2, Caserta, Italy

CNR-IGAG P.zale Aldo Moro, Rome

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L. Badiali

L. Badiali

Istituto Nazionale di Geofisica eVulcanologia, Rome

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E. Boschi

E. Boschi

Istituto Nazionale di Geofisica eVulcanologia, Rome

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P. Papale

P. Papale

Istituto Nazionale di Geofisica eVulcanologia, Pisa, Italy

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F. Tassi

F. Tassi

Department of Earth Sciences, University of Firenze, Florence, Italy

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O. Vaselli

O. Vaselli

Department of Earth Sciences, University of Firenze, Florence, Italy

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C. Kasereka

C. Kasereka

Goma Volcano Observatory, Goma, Democratic Republic of Congo

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J. Durieux

J. Durieux

Goma Volcano Observatory, Goma, Democratic Republic of Congo

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G. DeNatale

G. DeNatale

Osservatorio Vesuviano, Istituto Nazionale di Geofisica e Vulcanologia, Naples, Italy

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A. Amato

A. Amato

Istituto Nazionale di Geofisica eVulcanologia, Rome

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M. Cattaneo

M. Cattaneo

Istituto Nazionale di Geofisica eVulcanologia, Rome

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H. Ciraba

H. Ciraba

Goma Volcano Observatory

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G. D. Chirico

G. D. Chirico

Istituto Nazionale di Geofisica eVulcanologia, Pisa

Department of Earth Sciences and Environmental Geology, University of Bologna, Italy

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A. Delladio

A. Delladio

Istituto Nazionale di Geofisica eVulcanologia, Rome

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M. Demartin

M. Demartin

Istituto Nazionale di Geofisica eVulcanologia, Rome

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G. Favalli

G. Favalli

Istituto Nazionale di Geofisica eVulcanologia, Pisa, Italy

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D. Franceschi

D. Franceschi

Istituto Nazionale di Geofisica eVulcanologia, Rome

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V. Lauciani

V. Lauciani

Istituto Nazionale di Geofisica eVulcanologia, Rome

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G. Mavonga

G. Mavonga

Goma Volcano Observatory

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G. Monachesi

G. Monachesi

Istituto Nazionale di Geofisica eVulcanologia, Rome

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N.M. Pagliuca

N.M. Pagliuca

Istituto Nazionale di Geofisica eVulcanologia, Rome

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D. Sorrentino

D. Sorrentino

Istituto Nazionale di Geofisica eVulcanologia, Rome

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M. Yalire

M. Yalire

Goma Volcano Observatory

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First published: 26 June 2007
Citations: 6

Abstract

On 17 January 2002, the Nyiragongo volcano (1.52°S, 29.25°E, 3469 meters above sea level), located about 18 kilometers north of Lake Kivu in the Democratic Republic of Congo, erupted, releasing a volume of 14–34 million cubic meters of lava. Lava flows originated from north-south oriented fractures that rapidly developed along the southern flank of the volcano. Two lava flows divided the nearby city of Goma (∼500,000 people) into two parts, forcing a rapid exodus of the population into Rwanda. One of these lava flows ran into Lake Kivu, encroaching 60 meters below lake level with a submerged lava volume of 1 million cubic meters. About 15% of the town was directly affected, leaving approximately 120,000 people homeless. At least 170 people died as a direct consequence of the eruption.