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  2. The Continents Are Secretly Rising Because of Hidden ... - AOL

    www.aol.com/continents-secretly-rising-because...

    Now, scientists have discovered that resulting “deep mantle waves” from these tectonic separations likely caused the interiors of continents to rise, forming plateaus.

  3. Plateau - Wikipedia

    en.wikipedia.org/wiki/Plateau

    Satellite image of the Tibetan Plateau between the Himalayan mountains to the south and the Taklamakan Desert to the north. In geology and physical geography, a plateau (/ p l ə ˈ t oʊ, p l æ ˈ t oʊ, ˈ p l æ t oʊ /; French:; pl.: plateaus or plateaux), [1] [2] also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the ...

  4. List of tectonic plates - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plates

    Map showing Earth's principal tectonic plates and their boundaries in detail. These plates comprise the bulk of the continents and the Pacific Ocean.For purposes of this list, a major plate is any plate with an area greater than 20 million km 2 (7.7 million sq mi)

  5. Continental divide - Wikipedia

    en.wikipedia.org/wiki/Continental_divide

    Major continental divides, showing drainage into the major oceans and seas of the world. Grey areas are endorheic basins that do not drain to the ocean.. A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, not ...

  6. Outline of plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Outline_of_plate_tectonics

    Kerguelen Plateau – Oceanic plateau in the southern Indian Ocean; Laramidia – Island continent that existed until the end of the Late Cretaceous period; Laurentia – Craton forming the geological core of North America; Mauritia (microcontinent) – A Precambrian microcontinent that broke away as India and Madagascar separated

  7. Passive margin - Wikipedia

    en.wikipedia.org/wiki/Passive_margin

    Continental rifting forms new ocean basins. Eventually the continental rift forms a mid-ocean ridge and the locus of extension moves away from the continent-ocean boundary. The transition between the continental and oceanic lithosphere that was originally formed by rifting is known as a passive margin.

  8. Category:Plateaus by continent - Wikipedia

    en.wikipedia.org/wiki/Category:Plateaus_by_continent

    Plateaus of North America (3 C, 2 P) O. Plateaus of Oceania (2 C, 5 P) S. Plateaus of South America (5 C, 2 P) This page was last edited on 21 January 2024, at ...

  9. Australian plate - Wikipedia

    en.wikipedia.org/wiki/Australian_Plate

    The continental crust also includes northwestern New Zealand, New Caledonia and Fiji. The oceanic crust includes the southeast Indian Ocean , the Tasman Sea , and the Timor Sea . The Australian plate is bordered (clockwise) by the Eurasian plate , the Philippine plate , the Pacific plate , the Antarctic plate , the African plate and the Indian ...