<?xml version="1.0"?>
<?xml-stylesheet type="text/css" href="https://en.encyclopedia.kz/skins/common/feed.css?303"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="en">
		<id>https://en.encyclopedia.kz/api.php?action=feedcontributions&amp;feedformat=atom&amp;user=Hike395</id>
		<title>Kazakhstan Encyclopedia - User contributions [en]</title>
		<link rel="self" type="application/atom+xml" href="https://en.encyclopedia.kz/api.php?action=feedcontributions&amp;feedformat=atom&amp;user=Hike395"/>
		<link rel="alternate" type="text/html" href="https://en.encyclopedia.kz/index.php/Special:Contributions/Hike395"/>
		<updated>2026-07-03T05:14:43Z</updated>
		<subtitle>User contributions</subtitle>
		<generator>MediaWiki 1.23.15</generator>

	<entry>
		<id>https://en.encyclopedia.kz/index.php/Kazakhstania</id>
		<title>Kazakhstania</title>
		<link rel="alternate" type="text/html" href="https://en.encyclopedia.kz/index.php/Kazakhstania"/>
				<updated>2015-10-04T06:57:58Z</updated>
		
		<summary type="html">&lt;p&gt;Hike395: /* External links */remove overused {{geological history}} template per discussion at WT:WikiProject Geology using AWB&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;{{Unreferenced|date=May 2012}}&lt;br /&gt;
'''Kazakhstania''', also known as the '''Kazakhstan Block''', is a small geological region in the interior of [[Asia]]. It consists of the area north and east of the [[Aral Sea]], south of the Siberian [[craton]] and west of the [[Altai Mountains]] and [[Lake Balkhash]]. Politically, it comprises most of [[Kazakhstan]] and has a total area of around 1.3 million km². The [[Junggar basin]] in [[Xinjiang]], [[China]] is also part of Kazakhstania, though sometimes referred to as the '''Junggar Block'''.&lt;br /&gt;
&lt;br /&gt;
It is believed that present-day Kazakhstania is chiefly a mélange of early [[Paleozoic]] [[volcanic]] [[island arc]]s and some small continental [[terrane]]s. These were joined together during the [[Ordovician]] to form what was at the time an isolated continent of its own. During the [[Carboniferous]] and [[Permian]], [[Siberia (continent)|Siberia]] collided with Kazakhstania to form the [[Altai Mountains]], later [[Baltica]] collided in the [[Ural orogeny]], creating the basis for most of present-day [[Eurasia]].&lt;br /&gt;
&lt;br /&gt;
Kazakhstania is mainly flat: only in the east near [[Karaganda]] are there mountains and these only rise to 1,565 metres (5,130 feet) in the [[Tarbagatai Mountains|Tarbagatay Range]]. Although most of Kazakhstania is arid and practically no water flows from the region to the oceans, there is extensive grazing of [[cattle]], [[sheep]] and [[Bactrian camel|camels]] on the grasslands which cover most of the region today. Kazakhstania was too dry for extensive [[glaciation]] during the [[Quaternary]]. Kazakhstania contains as much as a quarter of the world's proven [[uranium]] reserves and is also one of the world's major source of [[lead]], [[zinc]], and [[antimony]] ores. On the southern boundary in the [[Turan Depression]] are large deposits of [[natural gas]].&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
*[[List of shields and cratons]]&lt;br /&gt;
&lt;br /&gt;
==External links==&lt;br /&gt;
*[http://www.es.ucsc.edu/~paleomag/tectonics/chmap.html Map of the Kazakhstan Block and surrounding areas]&lt;br /&gt;
*[http://www.jpg.co.uk/ab_jul_03_4.htm Ordovician-Permian paleogeography of Central Eurasia]&lt;br /&gt;
&lt;br /&gt;
{{Continents of the world}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Geology of Kazakhstan]]&lt;br /&gt;
[[Category:Historical continents]]&lt;br /&gt;
[[Category:Paleozoic Asia]]&lt;br /&gt;
[[Category:Carboniferous geology]]&lt;br /&gt;
[[Category:Permian geology]]&lt;br /&gt;
[[Category:Geography of Kazakhstan]]&lt;br /&gt;
[[Category:Geography of Xinjiang]]&lt;br /&gt;
[[Category:Natural history of Asia]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
{{paleo-geo-stub}}&lt;/div&gt;</summary>
		<author><name>Hike395</name></author>	</entry>

	</feed>