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		<title>WikiDwarf at 06:52, 29 May 2022</title>
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		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{short description|Tectonic plate which includes most of the continent of Eurasia}}&lt;br /&gt;
{{More citations needed|date=March 2011}}&lt;br /&gt;
{{Infobox tectonic plate&lt;br /&gt;
| image = File:EurasianPlate.png&lt;br /&gt;
| image_alt = The Eurasian Plate&lt;br /&gt;
| caption = The Eurasian Plate.&lt;br /&gt;
| type = [[List of tectonic plates#Major plates|Major]]&lt;br /&gt;
| area = {{convert|67,800,000|km2|sqmi|abbr=on}}&amp;lt;ref&amp;gt;{{cite web|url=http://geology.about.com/library/bl/blplate_size_table.htm |title=Sizes of Tectonic or Lithospheric Plates |publisher=Geology.about.com |date=2014-03-05 |access-date=2015-12-26}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
| move_direction = south&lt;br /&gt;
| move_speed = {{convert|7|-|14|mm|in|abbr=on}}/year&lt;br /&gt;
| geo_features = [[Europe]], [[Asia]], [[Atlantic Ocean]], [[Arctic Ocean]]&lt;br /&gt;
}}&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Eurasian Plate&amp;#039;&amp;#039;&amp;#039; is a [[tectonic plate]] which includes most of the continent of [[Eurasia]] (a landmass consisting of the traditional [[continent]]s of [[Europe]] and [[Asia]]), with the notable exceptions of the [[Indian subcontinent]], the [[Arabian Plate|Arabian subcontinent]], and the area east of the [[Chersky Range]] in East [[Siberia]]. It also includes [[oceanic crust]] extending westward to the [[Mid-Atlantic Ridge]] and northward to the [[Gakkel Ridge]].&lt;br /&gt;
&lt;br /&gt;
The eastern side is a boundary with the [[North American Plate]] to the north and a boundary with the [[Philippine Sea Plate]] to the south and possibly with the [[Okhotsk Plate]] and the [[Amurian Plate]]. The southerly side is a boundary with the [[African Plate]] to the west, the [[Arabian Plate]] in the middle and the [[Indo-Australian Plate]] to the east. The westerly side is a [[divergent boundary]] with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge, which is straddled by [[Iceland]]. All volcanic eruptions in Iceland, such as the 1973 eruption of [[Eldfell]], the 1783 eruption of [[Laki]], and the 2010 eruption of [[Eyjafjallajökull]], are caused by the North American and the Eurasian Plates moving apart, which is a result of [[divergent boundary|divergent]] plate boundary forces. The Himalayan mountain range and Tibetan plateau have formed as a result of the collision between the Indian Plate and Eurasian Plate, which began 50 million years ago and continues today.&lt;br /&gt;
&lt;br /&gt;
[[File:Eurasian &amp;amp; Anatolian Plate.jpg|thumb|Eurasian &amp;amp; Anatolian Plates]]&lt;br /&gt;
&lt;br /&gt;
The geodynamics of central Asia is dominated by the interaction between the Eurasian and [[Indian Plate]]s. In this area, many subplates or crust blocks have been recognized, which form the [[Central Asian]] and the [[East Asian]] transit zones.&amp;lt;ref&amp;gt;&amp;quot;Up-to-Date Geodynamics and Seismicity of Central Asia&amp;quot; by Y. Gatinsky, D. Rundquist, G. Vladova, T. Prokhodova&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
* [[Sunda Plate]]&lt;br /&gt;
* [[Anatolian Plate]]&lt;br /&gt;
* [[Aegean Sea Plate]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
&lt;br /&gt;
{{Tectonic plates}}&lt;br /&gt;
{{Geology of Europe}}&lt;br /&gt;
{{Indochina plates}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Tectonic plates]]&lt;br /&gt;
[[Category:Geology of Asia]]&lt;br /&gt;
[[Category:Geology of Europe]]&lt;br /&gt;
[[Category:Geology of Iceland]]&lt;br /&gt;
[[Category:Geology of the Pacific Ocean]]&lt;br /&gt;
[[Category:Geology of the Atlantic Ocean]]&lt;/div&gt;</summary>
		<author><name>WikiDwarf</name></author>
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