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209:. In the neighborhood in northwestern direction is the Ehi Mousgau, a stratovolcano with the same elevation, 3,100 metres (10,200 ft) above sea level. Deposits from
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clouds are found 15 to 35 kilometres (9.3 to 21.7 mi) around the caldera. The mountain was constructed over a basement of
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is the largest in the
Tibesti Mountains, it is located about 5 kilometres (3.1 mi) west of the summit rim. The active
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The summit of the mountain is dominated by the 14-by-18-kilometre (8.7 mi × 11.2 mi) relatively flat
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flows lie on the northeastern side in a 180-degree arc and are a result of the high activity in the
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are visited by the people of the
Tibesti for medical purposes.
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190:. It is located in the western center of the
182:is a 3,100-metre (10,200 ft) high
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16:Stratovolcano in the Republic of Chad
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186:in the north of the Republic of
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49:3,100 m (10,200 ft)
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33:Tarso Voon seen from space
340:Stratovolcanoes of Africa
249:List of volcanoes in Chad
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330:Holocene stratovolcanoes
283:Global Volcanism Program
225:Soborom Solfataric field
288:Smithsonian Institution
73: /
39:Highest point
325:Volcanoes of Chad
320:Mountains of Chad
315:Tibesti Mountains
192:Tibesti Mountains
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144:Tibesti Mountains
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335:Calderas of Chad
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223:The well known
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77:20.92°N 17.28°E
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184:stratovolcano
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168:Last eruption
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161:Stratovolcano
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156:Mountain type
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291:. Retrieved
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278:"Tarso Voon"
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201:. Extensive
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138:Parent range
82:20.92; 17.28
237:hot springs
215:Precambrian
211:pyroclastic
80: /
55:Coordinates
309:Categories
293:18 January
255:References
207:Quaternary
180:Tarso Voon
118:Tarso Voon
22:Tarso Voon
229:fumaroles
93:Geography
45:Elevation
243:See also
203:basaltic
233:mudpots
218:schists
199:caldera
172:Unknown
150:Geology
68:17°17′E
65:20°55′N
295:2007
235:and
188:Chad
178:The
125:Chad
311::
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263:^
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297:.
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