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  2. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [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.

  3. Pan-African orogeny - Wikipedia

    en.wikipedia.org/wiki/Pan-African_orogeny

    The term Pan-African was coined by Kennedy 1964 for a tectono-thermal event at about 500 Ma when a series of mobile belts in Africa formed between much older African cratons. At the time, other terms were used for similar orogenic events on other continents, i.e. Brasiliano in South America; Adelaidean in Australia; and Beardmore in Antarctica.

  4. East African Orogeny - Wikipedia

    en.wikipedia.org/wiki/East_African_Orogeny

    The notion that Gondwana was assembled during the Late Precambrian from two older fragments along the Pan-African Mozambique Belt was first proposed in the early 1980s. [3] A decade later this continental collision was named the East African Orogeny, but it was also realised that this was not the simple bringing together of two halves.

  5. 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.

  6. Pannotia - Wikipedia

    en.wikipedia.org/wiki/Pannotia

    Pannotia was centred on the South Pole, hence its name. Pannotia (from Greek: pan-, "all", -nótos, "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, was a relatively short-lived Neoproterozoic supercontinent that formed at the end of the Precambrian during the Pan-African orogeny (650–500 Ma), during the ...

  7. Great Escarpment, Southern Africa - Wikipedia

    en.wikipedia.org/wiki/Great_Escarpment,_Southern...

    About 180 million years ago, a mantle plume under southern Gondwana caused bulging of the continental crust in the area that would later become southern Africa. [2] Within 10–20 million years, rift valleys formed on either side of the central bulge and flooded to become the proto-Atlantic Ocean and proto-Indian Ocean more or less along the present southern African coastline and separating ...

  8. History of East Africa - Wikipedia

    en.wikipedia.org/wiki/History_of_East_Africa

    The history of East Africa has been divided into its prehistory, the major polities flourishing, the colonial period, and the post-colonial period, in which the current nations were formed. East Africa is the eastern region of Africa , bordered by North Africa , Central Africa , Southern Africa , the Indian Ocean , and the Sahara Desert .

  9. List of kingdoms and empires in African history - Wikipedia

    en.wikipedia.org/wiki/List_of_kingdoms_and...

    There were many kingdoms and empires in all regions of the continent of Africa throughout history. A kingdom is a state with a king or queen as its head. [1] An empire is a political unit made up of several territories, military outposts, and peoples, "usually created by conquest, and divided between a dominant centre and subordinate peripheries".