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  2. Afar triple junction - Wikipedia

    en.wikipedia.org/wiki/Afar_Triple_Junction

    It has been argued that the current Ethiopian plateau is a result of the most recent uplift of 500 metres (1,600 ft) estimated to be an Oligocene–early Miocene event. But the most accepted argument of the plateau is the result of the Paleogene flood-basalts. The uplift associated with both domes has resulted in major structural features due ...

  3. Danakil Depression - Wikipedia

    en.wikipedia.org/wiki/Danakil_Depression

    Erta Ale erupting within the Danakil Depression Mount Ayalu, the westernmost and older of two volcanoes at the southern end of the Danakil Depression. The Danakil Depression is the northern part of the Afar Triangle or Afar Depression in Ethiopia and Eritrea, [1] [2] a geological depression that has resulted from the divergence of three tectonic plates in the Horn of Africa.

  4. 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 .

  5. East African Rift - Wikipedia

    en.wikipedia.org/wiki/East_African_Rift

    A map of East Africa showing some of the historically active volcanoes (as red triangles) and the Afar Triangle (shaded at the center), which is a so-called triple junction (or triple point) where three plates are pulling away from one another: the Arabian plate and two parts of the African plate—the Nubian and Somali—splitting along the East African Rift Zone Main rift faults, plates ...

  6. Erta Ale - Wikipedia

    en.wikipedia.org/wiki/Erta_Ale

    Erta Ale is located in the Afar triple junction where three tectonic plates split apart: the African plate, the Arabian plate and the Somali plate. Specifically, it lies almost at the end of the southern Red Sea rift , where tectonic extension (via normal faults ) proceeds in conjunction with igneous intrusions to generate a new oceanic crust ...

  7. Ethiopian Highlands - Wikipedia

    en.wikipedia.org/wiki/Ethiopian_Highlands

    The Ethiopian Highlands (also called the Abyssinian Highlands) [1] [2] is a rugged mass of mountains in Ethiopia in Northeast Africa. It forms the largest continuous area of its elevation in the continent, with little of its surface falling below 1,500 m (4,900 ft), while the summits reach heights of up to 4,550 m (14,930 ft).

  8. Sanetti Plateau - Wikipedia

    en.wikipedia.org/wiki/Sanetti_Plateau

    Sanetti Plateau in Ethiopia. Ethiopian wolf with Helichrysum citrispinum - both are endemic species. The Sanetti Plateau is a major plateau of the Ethiopian Highlands, in the Oromia Region of Ethiopia. The plateau is the highest part of the Bale Mountains, and is located within Bale Mountains National Park. [1]

  9. Gregory Rift - Wikipedia

    en.wikipedia.org/wiki/Gregory_Rift

    The Gregory rift is oriented NS, and in the past the minimum horizontal tectonic stress direction was EW, the direction of extension. The alignment of rows of small vents, cones, domes and collapse pits in the Suswa, Silali and Kinangop Plateau regions support this theory. However, data from oil and gas exploration wells in Kenya, vents in ...