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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.
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 ...
Blank political world map with blue oceans, fit to replace File:A large blank world map with oceans marked in blue.PNG. Date: 25 July 2006: Source: World Map Blank.svg: Author: Petr Dlouhý: Other versions: Derivative works of this file: Carte Coffea robusta arabic.svg; Hantaviren weltweit.svg; OttomanEmpireIn1683.png
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.
Paleomap – Map of continents and mountain ranges in the past based on plate reconstructions; Seamount – Mountain rising from the ocean seafloor that does not reach to the water's surface; Slab (geology) – The portion of a tectonic plate that is being subducted; Slab gap hypothesis – Theory in plate tectonics
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)