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  2. Danakil Depression - Wikipedia

    en.wikipedia.org/wiki/Danakil_Depression

    The Danakil Depression is a plain approximately 200 by 50 km (124 by 31 mi), lying in the north of the Afar Region of Ethiopia, near the border with Eritrea. It is about 125 m (410 ft) below sea level and is bordered to the west by the Ethiopian Plateau and to the east by the Danakil Alps , beyond which is the Red Sea.

  3. Blue Nile Basin - Wikipedia

    en.wikipedia.org/wiki/Blue_Nile_Basin

    The Blue Nile Basin is a major geological structure in the northwestern Ethiopian Plateau formed in the Mesozoic Era during a period of crustal extension associated with the break-up of Gondwana, and filled with sedimentary deposits. The modern Blue Nile river cuts across part of the sedimentary basin. [1]

  4. Geology of Ethiopia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Ethiopia

    The geology of Ethiopia includes rocks of the Neoproterozoic East African Orogeny, Jurassic marine sediments and Quaternary rift-related volcanism. Events that greatly shaped Ethiopian geology is the assembly and break-up of Gondwana and the present-day rifting of Africa.

  5. Afar Triangle - Wikipedia

    en.wikipedia.org/wiki/Afar_Triangle

    The Depression overlaps the borders of Eritrea, Djibouti and the entire Afar Region of Ethiopia; and it contains the lowest point in Africa, Lake Assal, Djibouti, at 155 m (509 ft) below sea level. The Awash River is the main waterflow into the region, but it runs dry during the annual dry season, and ends as a chain of saline lakes .

  6. Plate reconstruction - Wikipedia

    en.wikipedia.org/wiki/Plate_reconstruction

    This article describes techniques; for a history of the movement of tectonic plates, see Geological history of Earth.. Plate reconstruction is the process of reconstructing the positions of tectonic plates relative to each other (relative motion) or to other reference frames, such as the Earth's magnetic field or groups of hotspots, in the geological past.

  7. Gregory Rift - Wikipedia

    en.wikipedia.org/wiki/Gregory_Rift

    Volcanic activity started in the central Ethiopian plateau around 30 million years ago, long before rifting began. The first period of activity deposited flood basalts and rhyolites from 500 metres (1,600 ft) to 2,000 metres (6,600 ft) thick. Uplift of the Ethiopian plateau began around this time or soon after.

  8. Geography of Ethiopia - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Ethiopia

    The Bale Mountains are separated from the larger part of the Ethiopian highlands by the Great Rift Valley, one of the longest and most profound chasms in Ethiopia. The highest peaks of that range include Tullu Demtu , the second-highest mountain in Ethiopia (4,377 m or 14,360 ft), Batu (4,307 m or 14,131 ft), Chilalo (4,036 m or 13,241 ft) and ...

  9. Foreign relations of Ethiopia - Wikipedia

    en.wikipedia.org/wiki/Foreign_relations_of_Ethiopia

    The foreign relations of Ethiopia refers to overall diplomatic relationship of Ethiopia. The Ministry of Foreign Affairs oversees foreign relations and diplomatic missions of the country. Ethiopia is one of few early African countries admitted to the League of Nations, becoming a member on 28 September 1923, and was one of the founding members ...