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	<title>Sidoarjo mud flow - Revision history</title>
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	<updated>2026-04-25T14:17:15Z</updated>
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		<id>https://wikimd.org/index.php?title=Sidoarjo_mud_flow&amp;diff=5817817&amp;oldid=prev</id>
		<title>Prab: CSV import</title>
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		<updated>2024-05-24T17:37:46Z</updated>

		<summary type="html">&lt;p&gt;CSV import&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Pre-Sidoarjo_Mud_Flow.jpg|thumb|Pre-Sidoarjo Mud Flow]] {{clear}}== Sidoarjo Mud Flow ==&lt;br /&gt;
&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Sidoarjo mud flow&amp;#039;&amp;#039;&amp;#039;, also known as &amp;#039;&amp;#039;&amp;#039;Lusi&amp;#039;&amp;#039;&amp;#039;, is a [[mud volcano]] in the subdistrict of [[Porong, Sidoarjo]], in [[East Java]], [[Indonesia]]. The eruption of the mud volcano began in May 2006 and has continued since, causing significant environmental, social, and economic impacts.&lt;br /&gt;
&lt;br /&gt;
=== History ===&lt;br /&gt;
The mud flow started on May 29, 2006, in the village of [[Siring, Porong]], following a drilling accident by the company [[Lapindo Brantas]]. The drilling was part of an exploration for natural gas. The eruption has been attributed to a combination of drilling activities and natural geological conditions.&lt;br /&gt;
&lt;br /&gt;
=== Geology ===&lt;br /&gt;
The Sidoarjo mud flow is characterized by the continuous eruption of mud, water, and gas. The mud is primarily composed of [[clay]], [[silt]], and [[sand]], with traces of [[hydrocarbons]]. The source of the mud is believed to be a deep underground reservoir, which is under high pressure.&lt;br /&gt;
&lt;br /&gt;
=== Impact ===&lt;br /&gt;
The mud flow has submerged several villages, displacing thousands of residents. The affected areas include [[Renokenongo]], [[Jatirejo]], and [[Siring]]. The disaster has also damaged infrastructure, including roads, railways, and industrial facilities.&lt;br /&gt;
&lt;br /&gt;
==== Environmental Impact ====&lt;br /&gt;
The continuous flow of mud has led to the destruction of agricultural land and the contamination of water sources. The mud has also created a large, unstable area that poses ongoing risks of subsidence and further eruptions.&lt;br /&gt;
&lt;br /&gt;
==== Social Impact ====&lt;br /&gt;
Thousands of people have been displaced from their homes, leading to significant social and economic challenges. The government and various organizations have provided temporary housing and financial assistance, but many residents continue to face hardships.&lt;br /&gt;
&lt;br /&gt;
==== Economic Impact ====&lt;br /&gt;
The disaster has had a substantial economic impact, with losses estimated in the billions of dollars. The affected area was an important industrial and agricultural region, and the destruction has led to job losses and economic instability.&lt;br /&gt;
&lt;br /&gt;
=== Response ===&lt;br /&gt;
The Indonesian government has taken various measures to mitigate the impact of the mud flow, including the construction of levees and the relocation of affected residents. The company responsible for the drilling, Lapindo Brantas, has also been involved in compensation and mitigation efforts.&lt;br /&gt;
&lt;br /&gt;
=== Controversy ===&lt;br /&gt;
The cause of the mud flow has been a subject of controversy. Some experts argue that the drilling activities by Lapindo Brantas triggered the eruption, while others believe that natural geological processes were the primary cause. Legal and scientific debates continue regarding responsibility and accountability.&lt;br /&gt;
&lt;br /&gt;
=== See Also ===&lt;br /&gt;
* [[Mud volcano]]&lt;br /&gt;
* [[Porong, Sidoarjo]]&lt;br /&gt;
* [[East Java]]&lt;br /&gt;
* [[Lapindo Brantas]]&lt;br /&gt;
&lt;br /&gt;
=== References ===&lt;br /&gt;
{{Reflist}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Natural disasters in Indonesia]]&lt;br /&gt;
[[Category:2006 in Indonesia]]&lt;br /&gt;
[[Category:Geology of Indonesia]]&lt;br /&gt;
[[Category:Mud volcanoes]]&lt;br /&gt;
&lt;br /&gt;
{{Indonesia-geo-stub}}&lt;/div&gt;</summary>
		<author><name>Prab</name></author>
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