| |
| | Nyiragongo Volcano |
 | | Nyiragongo was first studied for its permanent lava lake. |
 | | Nyiragongo was difficult for volcanologists to reach because of bureaucratic reasons, and political situations (Tazieff, 1994). |
 | | Nyiragongo poses many potential hazards other than lava flows, such as Mazukus (“evil winds” in Swahili), which are low-lying locations with dry CO2 vents, volcanic ash, phreatomagmatic eruptions from the high water table, earthquakes, and the possibility of the degassing of Lake Kivu (Lockwood, 1994). |
| www.geo.arizona.edu /geo5xx/geos577/projects/kayzar/html/nyiragongo_volcano.html (329 words) |
|