Information for "Japan Trench"

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Display title	Japan Trench
Default sort key	Japan Trench
Page length (in bytes)	3,211
Page ID	3671
Page content language	en - English
Page content model	wikitext
Indexing by robots	Allowed
Number of redirects to this page	0
Counted as a content page	Yes
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Page creator	The King of the Monsters (talk \| contribs)
Date of page creation	21:04, 27 January 2016
Latest editor	Koopa (talk \| contribs)
Date of latest edit	13:02, 6 November 2022
Total number of edits	17
Total number of distinct authors	7
Recent number of edits (within past 90 days)	0
Recent number of distinct authors	0

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Description	Content
Article description: (`description`) This attribute controls the content of the `description` and `og:description` elements.	The Japan Trench (日本海溝, Nihon Kaikō) is an oceanic trench, and part of the Pacific Ring of Fire. It extends from the Kuril Islands to the Ogasawara Islands and is 9,000 meters (30,000 ft) at its deepest. It is an extension of the Kuril-Kamchatka Trench to its north and the Izu-Ogasawara Trench to its south. This trench is created when the Oceanic Pacific Plate subducts beneath the Continental Eurasian Plate. The subduction process, together with the friction created, 'drags' the oceanic plate underneath the continental plate which Japan sits on, causing a deep-sea trench to be formed. The interactions of the tectonic plates at the Japan Trench is one of the reasons why tsunamis and earthquakes in Japan are relatively frequent.

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