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264:. It is nearly circular, 13 kilometers long and 11 kilometers wide. During the dry season it can completely run dry.
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260:, which forks seven kilometers southwest of the lake. The lake is about 100 kilometers north of the border with the
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256:. It is fed in the summer and autumn months from the eastern arm of the
316:, Journal of African Earth Sciences, Volume 93, May 2014, Pages 57–175.
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It has been suspected that the depression is the remains of an
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330:http://www.geonames.org/2431230/lac-iro.html
302:POSSIBLE IMPACT STRUCTURES IN CENTRAL AFRICA
248:) is a cyclically occurring lake in the
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314:Impact structures in Africa: A review
283:– a confirmed impact crater in Africa
312:W. Reimold & C. Koeberl (2014).
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201:110 km (42 sq mi)
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209:386 m (1,266 ft)
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300:James B. Garvin (1986).
262:Central African Republic
193:11 km (6.8 mi)
185:13 km (8.1 mi)
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250:Moyen-Chari Region
88:Moyen-Chari Region
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206:Surface elevation
121:10.100°N 19.417°E
16:(Redirected from
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252:in southeastern
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153:Primary outflows
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75:Location in Chad
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139:Primary inflows
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345:Lakes of Chad
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258:Bahr Salamat
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198:Surface area
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145:Bahr Salamat
44:image (2021)
228:Settlements
182:Max. length
160:evaporation
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99:Coordinates
288:References
231:Boum Kabir
190:Max. width
42:Sentinel-2
339:Category
275:See also
238:Iro Lake
84:Location
69:Lake Iro
30:Lake Iro
18:Lake Iro
246:Lac Iro
219:Islands
112:19°25′E
109:10°06′N
242:French
168:Basin
254:Chad
173:Chad
92:Chad
341::
271:.
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223:no
90:;
240:(
20:)
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