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		<title>Uralian orogeny - Revision history</title>
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		<updated>2026-07-03T06:15:46Z</updated>
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		<id>https://en.encyclopedia.kz/index.php?title=Uralian_orogeny&amp;diff=9640&amp;oldid=prev</id>
		<title>Moderator: 1 revision</title>
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				<updated>2026-05-16T20:04:43Z</updated>
		
		<summary type="html">&lt;p&gt;1 revision&lt;/p&gt;
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				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 20:04, 16 May 2026&lt;/td&gt;
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		<author><name>Moderator</name></author>	</entry>

	<entry>
		<id>https://en.encyclopedia.kz/index.php?title=Uralian_orogeny&amp;diff=9639&amp;oldid=prev</id>
		<title>GeoWriter: changed start of Late Carboniferous from &quot;318&quot; to &quot;323&quot;</title>
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				<updated>2016-12-21T21:29:24Z</updated>
		
		<summary type="html">&lt;p&gt;changed start of Late Carboniferous from &amp;quot;318&amp;quot; to &amp;quot;323&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;The '''Uralian orogeny''' refers to the long series of linear deformation and [[mountain building]] events that raised the [[Ural Mountains]], starting in the Late [[Carboniferous]] and [[Permian]] periods of the [[Palaeozoic]] Era, c. 323–299 and 299–251 Mya respectively, and ending with the last series of continental collisions in [[Triassic]] to early [[Jurassic]] times. In terms of [[plate tectonics]], the Uralian [[orogeny]] resulted from a southwestern movement of the [[Siberia (continent)|Siberian plate]], catching a smaller landmass, [[Kazakhstania]], between it and the nearly completely assembled supercontinent, [[Pangaea]]. The mountains of [[Eastern Europe]] on the paleocontinent [[Laurussia]], and those of Western [[Siberia]] both rose as the edge of Kazakhstania dove under the European plate. This event was the last stage in the assembly of [[Pangaea]].{{citation needed|date=August 2015}}&lt;br /&gt;
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The region affected by the orogeny, the ''Uralian orogenic belt,'' is usually thought of as the boundary between [[Europe]] and [[Asia]].  It extends from the [[Aral Sea]] to [[Novaya Zemlya]], and it includes in addition to the Ural Mountains, the [[Pay-Khoy|Pay-Khoy Ridge]] and the [[Mugodzhar Hills]] of northwest [[Kazakhstan]].  Its total length is about {{convert|3500|km|mi}}, of which the Ural Mountains are about {{convert|2500|km|mi|abbr=on}}.&amp;lt;ref&amp;gt;[http://www.geo.arizona.edu/geo5xx/geo527/Urals/geography.html J. Zavacky, ''The Urals, a Late Paleozoic Mountain Belt'']&amp;lt;/ref&amp;gt;&lt;br /&gt;
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==See also==&lt;br /&gt;
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* [[Main Uralian Fault]]&lt;br /&gt;
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==References==&lt;br /&gt;
{{Reflist}}&lt;br /&gt;
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==External links==&lt;br /&gt;
*[http://www.scotese.com/newpage5.htm  Late Permian Period map]&lt;br /&gt;
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{{Paleozoic  Footer}}&lt;br /&gt;
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{{Geology of Europe}}&lt;br /&gt;
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[[Category:Ural Mountains]]&lt;br /&gt;
[[Category:Carboniferous orogenies]]&lt;br /&gt;
[[Category:Permian orogenies]]&lt;br /&gt;
[[Category:Geology of European Russia]]&lt;br /&gt;
[[Category:Geology of Russia]]&lt;br /&gt;
[[Category:Carboniferous Europe]]&lt;br /&gt;
[[Category:Permian Europe]]&lt;br /&gt;
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{{tectonics-stub}}&lt;/div&gt;</summary>
		<author><name>GeoWriter</name></author>	</entry>

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