Mount Nyiragongo

Mount Nyiragongo
Lava lake in the crater of Mount Nyiragongo.
Elevation	3,470 metres (11,384 feet)
Location	Democratic Republic of the Congo
Range	Virunga Mountains
Coordinates	1°31′0″S, 29°15′0″E
Type	Stratovolcano
Last eruption	2007 (continuing)

Mount Nyiragongo is a volcano in the Virunga Mountains associated with the Great Rift Valley. It is located in the Democratic Republic of the Congo, about 19 km north of the town of Goma and Lake Kivu and just west of the border with Rwanda. The main crater is 250 m deep, two km wide and sometimes contains a lava lake. Nyiragongo and nearby Nyamuragira are together responsible for 40% of Africa's historical volcanic eruptions.

Geology

Not much is known about how long the volcano has been erupting, but since 1882, it has erupted at least 34 times, including many periods where activity was continuous for years at a time, often in the form of a churning lava lake in the crater. The volcano partly overlaps with two older volcanoes, Baratu and Shaheru, and is also surrounded by hundreds of small volcanic cinder cones from flank eruptions.

Volcanism at Nyiragongo is caused by the rifting of the Earth's crust where two parts of the African Plate are breaking apart. A hot spot is probably also partly responsible for the great activity at Nyiragongo and Nyamuragira.

The lava emitted in eruptions at Nyiragongo is often unusually fluid. Nyiragongo's lavas are made of melilite nephelinite, an alkali-rich type of volcanic rock whose unusual chemical composition may be a factor in the unusual fluidity of the lavas there. Whereas most lava flows move rather slowly and rarely pose a danger to human life, Nyiragongo's lava flows may race downhill at up to 60 miles per hour (up to 100 km/h). This is because of the extremely low silica content (the lava is mafic). Hawaiian volcanic eruptions are also characterised by lavas with low silica content, but the Hawaiian volcanoes are broad, shallow-sloped shield volcanoes in contrast to the steep-sided cone of Nyiragongo, and the silica content is high enough to slow most flows to walking pace.

Nyiragongo is most famous for its semi permanent lava lake, which was discovered by French vulcanologist Haroun Tazieff.

1977 eruption

Mount Nyiragongo

Between 1894 and 1977 the crater contained an active lava lake. On 10 January 1977, the crater walls fractured, and the lava lake drained in less than an hour. The lava flowed down the flanks of the volcano at speeds of up to 60 miles per hour on the upper slopes, overwhelming villages and killing at least 70 people. Some reports quote much higher figures of up to several thousand people. The hazards posed by eruptions like this are unique to Nyiragongo. Nowhere else in the world does such a steep-sided stratovolcano contain a lava lake containing such fluid lavas. Nyiragongo's proximity to heavily populated areas increases its potential for causing natural disasters. The 1977 eruption raised awareness of the unique dangers posed by Nyiragongo, and because of this it was designated a Decade Volcano, worthy of particular study, in 1991.

The 1977 eruption was preceded by the creation of a new small volcano, Murara, a short distance away on the slopes of Mount Nyamuragira.

2002 eruption

Another view of Nyiragongo's lava lake

Lava lakes reformed in the crater in eruptions in 1982-1983 and 1994. Another major eruption of the volcano began on January 17, 2002, after several months of increased seismic and fumarolic activity. A 13 km fissure opened in the south flank of the volcano, spreading in a few hours from 2800 m to 1550 m elevation, reaching the outskirts of the city of Goma the provincial capital on the northern shore of Lake Kivu. Lava streamed from three spatter cones at the end of the fissure and flowed in a stream 200 to 1000 m wide and up to 2 m deep through Goma. Warnings had been given and 400,000 people were evacuated from the city across the Rwandan border into neighbouring Gisenyi during the eruption. Lava covered the northern end of the runway at Goma International Airport, leaving the southern two-thirds usable, and reached Lake Kivu.^[1] This raised fears that the lava might cause gas-saturated waters deep in the lake to suddenly rise to the surface, releasing lethally large amounts of carbon dioxide and methane - a similar event to the disaster at Lake Nyos in Cameroon in 1986. This did not happen, but volcanologists continue to monitor the area closely.

About 45 people died in the eruption from asphyxiation by carbon dioxide and buildings collapsing due to the lava and earthquakes.^[1] At least 15% of Goma comprising 4500 buildings were destroyed, leaving about 120,000 people homeless. The eruption was the most destructive effusive eruption in modern history.^{[citation needed]}

Immediately after the eruption stopped, a large number of earthquakes were felt around Goma and Gisenyi. This swarm activity continued for about three months and caused the collapse of more buildings.^[1]

Six months after the start of the 2002 eruption, Nyamuragira volcano also erupted. Activity at Nyiragongo is ongoing, but currently confined to the crater, where another lava lake has formed about 250 metres below the level of the 1994 lava lake.

Tourist death

Satellite image of the eruption plume from Nyiragongo in July 2004

On Friday, July 6th 2007, 34 years-old Cecelia Cheng Siu-yan (Traditional chinese: 鄭兆茵), a Hong Kong Chinese female tourist on a guided tour up the volcano, slipped and fell 140 meters down into the crater. She landed on a small ledge and apparently survived the fall. Rescue workers were not able to get the woman back to safety that day, and she later died. Rescue attempts included a UN helicopter, but the attempt failed due to bad weather conditions. Indian peacekeepers and French vulcanologist Jacques Durieux will climb down to attempt to retrieve the body.

References

General references

• Tazieff, Haroun (1979). Nyiragongo: The Forbidden Volcano. Barron's Educational Series, 288 pp. ISBN 0-8120-5296-X. 
• Allard P., Baxter P., Halbwachs M., Kasareka M., Komorowski J.C., Joron J.L. (2003), The most destructive effusive eruption in modern history: Nyiragongo 2003, Geophysical Research Abstracts, v. 5, 11970
• Demant A., Lestrade P., Lubala R.T., Kampunzu A.B., Durieux J. (1994), Volcanological and petrological evolution of Nyiragongo volcano, Virunga volcanic field, Zaire, Bulletin of Volcanology, v. 56, p. 47-60 [1]
• Ekstrabaldet.dk (2007), Kvinde overlevede fald på 100 meter [2] in Danish
• "Chinese woman dies after falling into Congo volcano" Reuters 7 July 2007

External links

• Global Volcanism Program: Nyiragongo
• Volcano World Nyiragongo page
• BBC News pictures of the 2002 eruption
• PBS Nova: "Volcano under the City"
• Recent photos from Nyiragongo and its lava lake
• Stromboli Online's expedition to Nyiragongo in May, 2005
• Alkali Basalt Association of the Continents
• Climbing the Nyiragongo (Wildlife Conservation Society article)

Coordinates: 1°31′0″S, 29°15′0″E

Donate to Wikimedia