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Mount Nyiragongo
Mount Nyiragongo (/ˌnɪərəˈɡɒŋɡoʊ, -ˈɡɔːŋ-/ neer-ə-GONG-go) is an active stratovolcano with an elevation of 3,470 m (11,385 ft) in the Virunga Mountains associated with the Albertine Rift. It is located inside Virunga National Park, in the North Kivu province in the Democratic Republic of the Congo, about 12 km (7.5 mi) north of the town of Goma and Lake Kivu and just 9.8 km (6.1mi) west of the border with Rwanda. The main crater is about two kilometres (1 mi) wide and usually contains a lava lake. The crater presently has two distinct cooled lava benches within the crater walls – one at about 3,175 m (10,417 ft) and a lower one at about 2,975 m (9,760 ft).
Nyiragongo's lava lake has at times been the most voluminous known lava lake in most recent history. The depth of the lava lake varies considerably. A maximum elevation of the lava lake was recorded at about 3,250 m (10,660 ft) prior to the January 1977 eruption – a lake depth of about 600 m (2,000 ft). Following the January 2002 eruption, the lava lake was recorded at a low of about 2,600 m (8,500 ft), or 900 m (3,000 ft) below the rim. The level has gradually risen since then. Nyiragongo and nearby Nyamuragira are together responsible for 40% of Africa's historical volcanic eruptions.
The volcano partly overlaps with two older volcanoes, Baruta and Shaheru, and is also surrounded by hundreds of small volcanic cinder cones from flank eruptions.
Nyiragongo's cone consists of pyroclastics and lava flows. Nyiragongo's lavas are low-silica, alkali-rich, ultramafic extrusive rocks essentially free of feldspars. They range from olivine-rich melilitites through leucites to nephelinites, containing, in various proportions mainly the minerals nepheline, leucite, melilite, kalsilite, and clinopyroxene. This very low silica composition results in eruptions with unusually fluid flows. 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 100 km/h (60 mph).
Not much is known about how long the volcano has been erupting, but it has erupted at least 34 times since 1882, 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 existence of the lava lake had been suspected for some time but was not scientifically confirmed until 1948. At that time, it was measured at nearly 120,000 square metres (1.3×106 ft2). Subsequent expeditions showed that the lake fluctuated in size, depth, and temperature over time.
The lava lake activity is ongoing. As of 2020[update], the lake is mostly confined within a broad, steep-sided cinder cone (roughly 18 m (60 ft) high by 180 m (600 ft) wide) on the crater floor.
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 km/h (37 mph) on the upper slopes, the fastest lava flow recorded to date, overwhelming villages and killing at least 50 people in the villages of Kibati and Moniki, according to reports made at the time.
Within 30 minutes, the lava lake had emptied, fastly flowing fluid lava north, south, and west of the volcano. Nyiragongo's proximity to heavily populated areas increases its potential for causing a natural disaster. The 1977 eruption raised awareness of the unique dangers posed by Nyiragongo, and because of this, in 1991 it was designated a Decade Volcano, worthy of particular study.
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Mount Nyiragongo
Mount Nyiragongo (/ˌnɪərəˈɡɒŋɡoʊ, -ˈɡɔːŋ-/ neer-ə-GONG-go) is an active stratovolcano with an elevation of 3,470 m (11,385 ft) in the Virunga Mountains associated with the Albertine Rift. It is located inside Virunga National Park, in the North Kivu province in the Democratic Republic of the Congo, about 12 km (7.5 mi) north of the town of Goma and Lake Kivu and just 9.8 km (6.1mi) west of the border with Rwanda. The main crater is about two kilometres (1 mi) wide and usually contains a lava lake. The crater presently has two distinct cooled lava benches within the crater walls – one at about 3,175 m (10,417 ft) and a lower one at about 2,975 m (9,760 ft).
Nyiragongo's lava lake has at times been the most voluminous known lava lake in most recent history. The depth of the lava lake varies considerably. A maximum elevation of the lava lake was recorded at about 3,250 m (10,660 ft) prior to the January 1977 eruption – a lake depth of about 600 m (2,000 ft). Following the January 2002 eruption, the lava lake was recorded at a low of about 2,600 m (8,500 ft), or 900 m (3,000 ft) below the rim. The level has gradually risen since then. Nyiragongo and nearby Nyamuragira are together responsible for 40% of Africa's historical volcanic eruptions.
The volcano partly overlaps with two older volcanoes, Baruta and Shaheru, and is also surrounded by hundreds of small volcanic cinder cones from flank eruptions.
Nyiragongo's cone consists of pyroclastics and lava flows. Nyiragongo's lavas are low-silica, alkali-rich, ultramafic extrusive rocks essentially free of feldspars. They range from olivine-rich melilitites through leucites to nephelinites, containing, in various proportions mainly the minerals nepheline, leucite, melilite, kalsilite, and clinopyroxene. This very low silica composition results in eruptions with unusually fluid flows. 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 100 km/h (60 mph).
Not much is known about how long the volcano has been erupting, but it has erupted at least 34 times since 1882, 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 existence of the lava lake had been suspected for some time but was not scientifically confirmed until 1948. At that time, it was measured at nearly 120,000 square metres (1.3×106 ft2). Subsequent expeditions showed that the lake fluctuated in size, depth, and temperature over time.
The lava lake activity is ongoing. As of 2020[update], the lake is mostly confined within a broad, steep-sided cinder cone (roughly 18 m (60 ft) high by 180 m (600 ft) wide) on the crater floor.
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 km/h (37 mph) on the upper slopes, the fastest lava flow recorded to date, overwhelming villages and killing at least 50 people in the villages of Kibati and Moniki, according to reports made at the time.
Within 30 minutes, the lava lake had emptied, fastly flowing fluid lava north, south, and west of the volcano. Nyiragongo's proximity to heavily populated areas increases its potential for causing a natural disaster. The 1977 eruption raised awareness of the unique dangers posed by Nyiragongo, and because of this, in 1991 it was designated a Decade Volcano, worthy of particular study.