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  2. 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 ...

  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. List of paleocontinents - Wikipedia

    en.wikipedia.org/wiki/List_of_paleocontinents

    Animation of the break-up of the supercontinent Pangaea and the subsequent drift of its constituents, from the Early Triassic to recent (250 Ma to 0).. This is a list of paleocontinents, significant landmasses that have been proposed to exist in the geological past.

  5. East African Orogeny - Wikipedia

    en.wikipedia.org/wiki/East_African_Orogeny

    The East African Orogeny (EAO) is the main stage in the Neoproterozoic assembly of East and West Gondwana (Australia–India–Antarctica and Africa–South America) along the Mozambique Belt. [ 2 ] Gondwana assembly

  6. Talk:Pannotia - Wikipedia

    en.wikipedia.org/wiki/Talk:Pannotia

    Outside of the V was a very large ancient ocean called the Panafrican Ocean that may have surrounded Pannotia, equivalent to the future Panthalassic Ocean. Pannotia was short-lived. The collisions that formed Pannotia were glancing collisions, and the continents composing Pannotia already had active rifting.

  7. Pan-African Ocean - Wikipedia

    en.wikipedia.org/wiki/Pan-African_Ocean

    The Pan-African Ocean is a hypothesized paleo-ocean whose closure created the supercontinent of Pannotia. [1] The ocean may have existed before the break-up of the supercontinent of Rodinia. The ocean closed before the beginning of the Phanerozoic Eon, when the Panthalassa ocean expanded, and was eventually replaced by it.

  8. Grenville orogeny - Wikipedia

    en.wikipedia.org/wiki/Grenville_orogeny

    It is important to separate local from large-scale tectonic history of the orogenic belt in order to understand the orogeny. For this purpose, the Grenville orogen is generally broken into four localities: the southern extent in Texas and Mexico, the Appalachians, the Adirondacks, and the Grenville Province. A portion of the orogen can be found ...

  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".