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  2. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Pangaea or Pangea (/ p æ n ˈ dʒ iː ə / pan-JEE-ə) [1] was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. [2] It assembled from the earlier continental units of Gondwana , Euramerica and Siberia during the Carboniferous approximately 335 million years ago, and began to break apart about 200 million years ...

  3. Indian plate - Wikipedia

    en.wikipedia.org/wiki/Indian_Plate

    In the late Cretaceous approximately , and subsequent to the splitting from Gondwana of conjoined Madagascar and India, the Indian plate split from Madagascar and formed Insular India. It began moving north, at about 20 cm (7.9 in) per year, [ 9 ] and is believed to have begun colliding with Asia as early as 55 million years ago , [ 11 ] in the ...

  4. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    Pangaea's supercontinent cycle is a good example of the efficiency of using the presence or lack of these entities to record the development, tenure, and break-up of supercontinents. There is a sharp decrease in passive margins between 500 and 350 Ma during the timing of Pangaea's assembly.

  5. 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.

  6. Insular India - Wikipedia

    en.wikipedia.org/wiki/Insular_India

    Insular India was an isolated landmass which became the Indian subcontinent.Across the latter stages of the Cretaceous and most of the Paleocene, following the breakup of Gondwana, the Indian subcontinent remained an isolated landmass as the Indian Plate drifted across the Tethys Ocean, forming the Indian Ocean.

  7. Madagascar plate - Wikipedia

    en.wikipedia.org/wiki/Madagascar_Plate

    The Madagascar plate or Madagascar block is a tectonic plate holding the island of Madagascar. It was once attached to the Gondwana supercontinent and later the Indo-Australian plate . Rifting in the Somali Basin began at the end of the Carboniferous 300 million years ago, as a part of the Karoo rift system .

  8. Category:Maps of Asia - Wikipedia

    en.wikipedia.org/wiki/Category:Maps_of_Asia

    Maps are also available as part of the Wikimedia Atlas of the World project in the Atlas of Asia Wikimedia Commons has media related to Maps of Asia . Subcategories

  9. Geography of Asia - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Asia

    These varying definitions are not generally reflected in the map of Asia as a whole; for example, Egypt is typically included in the Middle East, but not in Asia, even though the bulk of the Middle East is in Asia. The demarcation between Asia and Africa is the Suez Canal, the Gulf of Suez, the Red Sea, and the Bab-el-Mandeb.