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  2. Great Rift Valley - Wikipedia

    en.wikipedia.org/wiki/Great_Rift_Valley

    Great Rift Valley. The Great Rift Valley ( Swahili: Bonde la ufa) is a series of contiguous geographic trenches, approximately 7,000 kilometres (4,300 mi) in total length, that runs from Lebanon in Asia to Mozambique in Southeast Africa. [1] While the name continues in some usages, it is rarely used in geology as it is considered an imprecise ...

  3. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    The second major phase in the break-up of Pangaea began in the Early Cretaceous (150–140 Ma), when Gondwana separated into multiple continents (Africa, South America, India, Antarctica, and Australia). The subduction at Tethyan Trench probably caused Africa, India and Australia to move northward, causing the opening of a "South Indian Ocean".

  4. 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 ...

  5. A New Ocean Could Split Africa Into Two Continents ... - AOL

    www.aol.com/lifestyle/ocean-could-split-africa...

    A massive rift in Ethiopia separated continental plates by 400 feet and is part of a rift network that may flood enough to create a new ocean in 2 million years.

  6. Midcontinent Rift System - Wikipedia

    en.wikipedia.org/wiki/Midcontinent_Rift_System

    Midcontinent Rift System. The Midcontinent Rift System (MRS) or Keweenawan Rift is a 2,000 km (1,200 mi) long geological rift in the center of the North American continent and south-central part of the North American plate. It formed when the continent's core, the North American craton, began to split apart during the Mesoproterozoic era of the ...

  7. Laurasia - Wikipedia

    en.wikipedia.org/wiki/Laurasia

    Laurasia (/ l ɔː ˈ r eɪ ʒ ə,-ʃ i ə /) was the more northern of two large landmasses that formed part of the Pangaea supercontinent from around ), the other being Gondwana.It separated from Gondwana (beginning in the late Triassic period) during the breakup of Pangaea, drifting farther north after the split and finally broke apart with the opening of the North Atlantic Ocean c. 56 Mya.

  8. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana ( / ɡɒndˈwɑːnə /) [1] was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian Subcontinent .

  9. Geography of Africa - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Africa

    Geography of Africa. Africa is a continent comprising 63 political territories, representing the largest of the great southward projections from the main mass of Earth 's surface. [1] Within its regular outline, it comprises an area of 30,368,609 km 2 (11,725,385 sq mi), excluding adjacent islands.

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