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- Geology_of_Chad abstract "The terrain of Chad in central Africa is dominated by the low-lying Chad Basin (elevation about 250 m / 820 ft), which rises gradually to mountains and plateaus on the north, east, and south. In the east heights of more than 900 metres (3,000 ft) are attained in the Ennedi and Ouaddaï plateaus. The greatest elevations are reached in the Tibesti massif in the north, with a maximum height of 3,415 metres (11,204 ft) at Emi Koussi. The northern half of the republic lies in the Sahara. The Bodélé Depression is a low region in the southern Sahara that is surrounded by basalt mountain ridges. Winds flow through this region and lift dust. The dust from this region supplies over half of the dust to Amazon rainforests.The only important rivers, the Logone and Chari, are located in the southwest and flow into Lake Chad. The lake doubles in size during the rainy season.".
- Geology_of_Chad thumbnail Cd-map.png?width=300.
- Geology_of_Chad wikiPageID "6450294".
- Geology_of_Chad wikiPageRevisionID "586125610".
- Geology_of_Chad hasPhotoCollection Geology_of_Chad.
- Geology_of_Chad subject Category:Geography_of_Chad.
- Geology_of_Chad subject Category:Geology_by_country.
- Geology_of_Chad subject Category:Geology_of_Chad.
- Geology_of_Chad comment "The terrain of Chad in central Africa is dominated by the low-lying Chad Basin (elevation about 250 m / 820 ft), which rises gradually to mountains and plateaus on the north, east, and south. In the east heights of more than 900 metres (3,000 ft) are attained in the Ennedi and Ouaddaï plateaus. The greatest elevations are reached in the Tibesti massif in the north, with a maximum height of 3,415 metres (11,204 ft) at Emi Koussi. The northern half of the republic lies in the Sahara.".
- Geology_of_Chad label "Geology of Chad".
- Geology_of_Chad sameAs Q5535344.
- Geology_of_Chad sameAs Q5535344.
- Geology_of_Chad wasDerivedFrom Geology_of_Chad?oldid=586125610.
- Geology_of_Chad depiction Cd-map.png.
- Geology_of_Chad isPrimaryTopicOf Geology_of_Chad.
