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Mount Nyiragongo
*** Shopping-Tip: Mount Nyiragongo
{{Mtnbox start|Name=Mount Nyiragongo|Photo=Nyiragongo lava lake.jpg|
Caption=Lava lake in the crater of Mount Nyiragongo|Elevation=3,470 metres (11,384 feet)|
Location=
Democratic Republic of the Congo|Range=
Virunga Mountains}}
{{Mtnbox coor dms|1|31|0|S|29|15|0|E|type:mountain_region:Central_Africa}}
{{Mtnbox volcano|Type=
Stratovolcano|Age=|Last eruption=
2002 (continuing)}}
{{Mtnbox finish}}
'''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 19km north of the town of
Goma and the
Lake Kivu and just
west of the border with
Rwanda. The main crater is 250m deep, 2km wide and sometimes contains a lava lake. Nyiragongo and nearby
Mount Nyamuragira 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 1883, it has erupted at least 15 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 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
hotspot (geology) 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 (97 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.
1977 eruption
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 Volcanoes 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
Image:Nyiragongo 2002 eruption.jpg thumb|250px|left|Satellite image of the eruption plume from Nyiragongo in July 2004
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
seismology seismic and
fumarole fumarolic activity. An 18 km
fissure opened in the south flank of the volcano, spreading in a few hours from 2800 m to 1550 m elevation.
The fissure emitted three streams of lava, one of which flowed through the city of
Goma. 400,000 people were evacuated from the city during the eruption. Lava also destroyed Goma Airport, and reached nearby
Lake Kivu. 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, but property damage was extensive. At least 15% of Goma was destroyed, leaving about 120,000 people
homeless. The eruption was the most destructive effusive eruption in modern history.
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.
External links
-
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
-
Expeditions to Nyiragongo
-
Stromboli Online's expedition to Nyiragongo in May, 2005
-
Alkali Basalt Association of the Continents - Nyiragongo's unusual petrology is mentioned in there.
-
Volcanological and petrological evolution of Nyiragongo volcano, Virunga volcanic field, Zaire (''now
Democratic Republic of the Congo'')
References
* 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
Category:Active volcanoes Nyiragongo
Category:Decade Volcanoes Nyiragongo
Category:Mountains of the Democratic Republic of the Congo Nyiragongo
Category:Stratovolcanoes Nyiragongo, Mount
Category:Virunga Mountains Nyiragongo
Category:Volcanoes of the Democratic Republic of the Congo Nyiragongo
de:Nyiragongo
fr:Nyiragongo
nl:Nyiragongo
*** Shopping-Tip: Mount Nyiragongo