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Data from the Global Volcanism Program of the Smithsonian Institution
Details for: Nyiragongo
Nyiragongo is seen here from the S across Lake Kivu at Peyer Yard in Rwanda. It contained a lava lake in its deep summit crater that was active for half a century before draining suddenly in 1977. In contrast to the low profile of the nearby Nyamuragira shield volcano, Nyiragongo displays the steep slopes of a stratovolcano. About 100 smaller cones are located primarily along radial fissures east of the summit and along a NE-SW zone extending as far as Lake Kivu. Photo by B. Martinelli, 1994 (courtesy of Jack Lockwood, U.S. Geological Survey).
Volcano Number:
223030
Volcano Name:
Nyiragongo
Country:
DR Congo
Volcano Type:
Stratovolcano
Last Eruption:
2024 CE
Elevation:
3470m
Tectonic Setting:
Rift zone / Continental crust (> 25 km)
Pop. within 5km:
2416
Pop. within 10km:
31145
Pop. within 30km:
1006436
Pop. within 100km:
9087529
Latitude:
-1.52
Longitude:
29.25
Details
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The Nyiragongo stratovolcano contained a lava lake in its deep summit crater that was active for half a century before draining catastrophically through its outer flanks in 1977. The steep slopes contrast to the low profile of its neighboring shield volcano, Nyamuragira. Benches in the steep-walled, 1.2-km-wide summit crater mark levels of former lava lakes, which have been observed since the late-19th century. Two older stratovolcanoes, Baruta and Shaheru, are partially overlapped by Nyiragongo on the north and south. About 100 cones are located primarily along radial fissures south of Shaheru, east of the summit, and along a NE-SW zone extending as far as Lake Kivu. Many cones are buried by voluminous lava flows that extend long distances down the flanks, which is characterized by the eruption of foiditic rocks. The extremely fluid 1977 lava flows caused many fatalities, as did lava flows that inundated portions of the major city of Goma in January 2002.
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Eruption Data from the Global Volcanism Program of the Smithsonian Institution
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Emissions Data from the Global Volcanism Program of the Smithsonian Institution
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