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  2. File:Pangaea continents.svg - Wikipedia

    en.wikipedia.org/wiki/File:Pangaea_continents.svg

    Printable version; Page information; ... Pangea map, with names of the continents. Image of pangaea made by en:User:Kieff. ... Geological history of North America;

  3. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    The South Atlantic did not open until the Cretaceous when Laurasia started to rotate clockwise and moved northward with North America to the north, and Eurasia to the south. The clockwise motion of Laurasia led much later to the closing of the Tethys Ocean and the widening of the "Sinus Borealis", which later became the Arctic Ocean .

  4. File:Pangea continents and oceans.svg - Wikipedia

    en.wikipedia.org/wiki/File:Pangea_continents_and...

    This image is a derivative work of the following images: File:Pangaea continents.svg licensed with Cc-by-sa-3.0-migrated, GFDL 2009-10-21T17:07:11Z Justass 815x960 (57091 Bytes) {{Information |Description=Pangea map, with names of the continents.

  5. Central Pangean Mountains - Wikipedia

    en.wikipedia.org/wiki/Central_Pangean_Mountains

    Map of Earth during the Early Permian, around 285 million years ago, showing Central Pangean mountain range at equator. The Central Pangean Mountains were formed during the collision of Euramerica and northern Gondwana as part of the Variscan and Alleghanian orogenies, which began during the Carboniferous approximately 340 million years ago, and complete by the beginning of the Permian around ...

  6. 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.

  7. 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.

  8. Template:Continents of Earth - Wikipedia

    en.wikipedia.org/wiki/Template:Continents_of_Earth

    This template's initial visibility currently defaults to autocollapse, meaning that if there is another collapsible item on the page (a navbox, sidebar, or table with the collapsible attribute), it is hidden apart from its title bar; if not, it is fully visible.

  9. List of orogenies - Wikipedia

    en.wikipedia.org/wiki/List_of_orogenies

    South America Guriense orogeny: 2.8 2.7 South America Sunsás orogeny: 1.4 1.1 South America Cariri Velhos orogeny.54 South America Brasiliano-Pan African orogeny.54 South America Pampean orogeny.53 .48 South America Chonide orogeny.25 .20 South America Terra Australis Orogen.54 .23 South America Famatinian orogeny.49 .46 South America