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Pangaea or Pangea (/ p æ n ˈ dʒ iː. 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 ago, at the ...
Summary. Pangea map, with names of the continents. Image of pangaea made by en:User:Kieff. File: Pangaea continents.svg has 10 translations. The SVG code is valid. This vector image was created with Inkscape. This file is translated using SVG switch elements: all translations are stored in the same file.
File:Pangea continents and oceans.svg. Size of this PNG preview of this SVG file: 639 × 600 pixels. Other resolutions: 256 × 240 pixels | 512 × 480 pixels | 819 × 768 pixels | 1,091 × 1,024 pixels | 2,183 × 2,048 pixels | 1,021 × 958 pixels. Original file (SVG file, nominally 1,021 × 958 pixels, file size: 47 KB) This is a file from ...
In geology, a supercontinent is the assembly of most or all of Earth 's continental blocks or cratons to form a single large landmass. [1][2][3] However, some geologists use a different definition, "a grouping of formerly dispersed continents", which leaves room for interpretation and is easier to apply to Precambrian times. [4]
The newer model has Australia and Antarctica between South America and southeast Asia, south of the Medi-Pangaean Sea. Pangaea Proxima (also called Pangaea Ultima, Neopangaea, and Pangaea II) is a possible future supercontinent configuration. Consistent with the supercontinent cycle, Pangaea Proxima could form within the next 250 million years.
Formed from three cratonic fragments - the Baltic Shield, Sarmatia and Volgo–Uralia. Formed part of Columbia, then Rodinia and Pannotia. Collided with Laurentia and Avalonia to form Laurussia. [1][4][2][10] Cathaysia. 1800. Continent. Fused with the Yangtze block to form the South China Craton during the Early Paleozoic.
Map of Pangaea with modern continental outlines. The supercontinent cycle is the quasi-periodic aggregation and dispersal of Earth's continental crust.There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth's crust is constantly being reconfigured.
The Central Pangean Mountains were an extensive northeast–southwest trending mountain range in the central portion of the supercontinent Pangaea during the Carboniferous, Permian and Triassic periods. They were formed as a result of collision between the large landmasses of Euramerica (also known as Laurussia) and Gondwana during the ...