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The Wilson cycle theory is based upon the idea of an ongoing cycle of ocean closure, continental collision, and a formation of new ocean on the former suture zone.The Wilson Cycle can be described in six phases of tectonic plate motion: the separation of a continent (continental rift), formation of a young ocean at the seafloor, formation of ocean basins during continental drift, initiation of ...
John Tuzo Wilson (October 24, 1908 – April 15, 1993) was a Canadian geophysicist and geologist who achieved worldwide acclaim for his contributions to the theory of plate tectonics. He added the concept of hot spots , a volcanic region hotter than the surrounding mantle (as in the Hawaii hotspot ).
[[Category:Timeline templates]] to the <includeonly> section at the bottom of that page. Otherwise, add <noinclude>[[Category:Timeline templates]]</noinclude> to the end of the template code, making sure it starts on the same line as the code's last character.
The second timeline shows an expanded view of the most recent eon. In a similar way, the most recent era is expanded in the third timeline, the most recent period is expanded in the fourth timeline, and the most recent epoch is expanded in the fifth timeline.
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The Wilson cycle describes the cyclicity in plate tectonics by forming supercontinents (Rodinia, Pangaea) and its breakup in hundreds of millions of years. It is named after the canadian geologist John Tuzo Wilson (1908-1993). Date: 1 November 2010, 01:00 (UTC) Source: File:Wilson-cycle hg.png: Author: Hannes Grobe 08:34, 21 January 2007 (UTC)
Template parameters [Edit template data] Parameter Description Type Status Page page Page in the source that supports the content; displays after 'p.' String optional Pages pages Pages in the source that support the content (not an indication of the number of pages in the source); displays after 'pp.' String optional No pp nopp Set to 'y' to suppress the 'p.' or 'pp.' display with 'page' or ...
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