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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. List of orogenies - Wikipedia

    en.wikipedia.org/wiki/List_of_orogenies

    The following is a list of known orogenies organised by continent, starting with the oldest in each. The headings are present-day continents, which may differ from the geography contemporary to the orogenies.

  4. Pan-African orogeny - Wikipedia

    en.wikipedia.org/wiki/Pan-African_orogeny

    The Pan-African orogeny was a series of major Neoproterozoic orogenic events which related to the formation of the supercontinents Gondwana and Pannotia about 600 million years ago. [1] This orogeny is also known as the Pan-Gondwanan or Saldanian Orogeny . [ 2 ]

  5. East African Orogeny - Wikipedia

    en.wikipedia.org/wiki/East_African_Orogeny

    In another model, the assembly of East Gondwana c. was a multiphase process which included two main periods of orogenesis: the older EAO (c.) and the younger Kuunga Orogeny (c. 6] In the former scenario the Kuunga Orogeny of the latter scenario are two coeval events: the collisions between India and Australia-East Antarctica and Azania and India.

  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. Rodinia - Wikipedia

    en.wikipedia.org/wiki/Rodinia

    In contrast with Pannotia, little is known about Rodinia's configuration and geodynamic history. Paleomagnetic evidence provides some clues to the paleolatitude of individual pieces of the Earth's crust , but not to their longitude, which geologists have pieced together by comparing similar geologic features, often now widely dispersed.

  8. Timeline of Nigerian history - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_Nigerian_history

    A History of Nigeria. Cambridge University Press, 2008. ISBN 978-0-511-39712-7; Muslim Civic Cultures and Conflict Resolution: The Challenge of Democratic Federalism in Nigeria — John N. Paden; Oriji, John N. Political Organization in Nigeria Since the Late Stone Age: A History of the Igbo People. New York: Palgrave Macmillan (St. Martin's ...

  9. List of time periods - Wikipedia

    en.wikipedia.org/wiki/List_of_time_periods

    The period ends with the beginning of the Age of Revolutions. Contemporary historyHistory within living memory. It shifts forward with the generations, and today is the span of historic events from approximately 1945 that are immediately relevant to the present time.