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	<id>https://www.conservapedia.com/index.php?action=history&amp;feed=atom&amp;title=Lava_fountain</id>
	<title>Lava fountain - Revision history</title>
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	<updated>2026-10-08T02:42:17Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.35.14</generator>
	<entry>
		<id>https://www.conservapedia.com/index.php?title=Lava_fountain&amp;diff=232518&amp;oldid=prev</id>
		<title>BrianCo: formatting, links &amp; cat</title>
		<link rel="alternate" type="text/html" href="https://www.conservapedia.com/index.php?title=Lava_fountain&amp;diff=232518&amp;oldid=prev"/>
		<updated>2007-07-14T22:25:09Z</updated>

		<summary type="html">&lt;p&gt;formatting, links &amp;amp; cat&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 22:25, July 14, 2007&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Image:Lava_fountain.jpg|300px|thumb|Lava fountain of the Pu`u `O`o cinder and spatter cone on Kilauea Volcano, Hawai`i.]]A jet of [[lava]] sprayed into the air by the rapid formation and expansion of gas bubbles in the molten rock is called a '''lava fountain'''. Lava fountains typically range from about 10 to 100 m in height, but occasionally reach more than 500 m. Lava fountains erupt from isolated &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;vents&lt;/del&gt;, along fissures, within active [[lava lake]]s, and from a [[lava tube]] when water gains access to the tube in a confined space.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Image:Lava_fountain.jpg|300px|thumb|Lava fountain of the Pu`u `O`o cinder and spatter cone on Kilauea Volcano, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Hawaii|&lt;/ins&gt;Hawai`i&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;]]&lt;/ins&gt;.]]A jet of [[lava]] sprayed into the air by the rapid formation and expansion of gas bubbles in the molten rock is called a '''lava fountain'''. Lava fountains typically range from about 10 to 100 m in height, but occasionally reach more than 500 m. Lava fountains erupt from isolated &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[vent]]s&lt;/ins&gt;, along &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[&lt;/ins&gt;fissures&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;]]&lt;/ins&gt;, within active [[lava lake]]s, and from a [[lava tube]] when water gains access to the tube in a confined space.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Category:&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Geology&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Category:&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Volcanology&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>BrianCo</name></author>
	</entry>
	<entry>
		<id>https://www.conservapedia.com/index.php?title=Lava_fountain&amp;diff=205337&amp;oldid=prev</id>
		<title>SharonS: New page: Lava fountain of the Pu`u `O`o cinder and spatter cone on Kilauea Volcano, Hawai`i.A jet of lava sprayed into the air by the rapid formation and...</title>
		<link rel="alternate" type="text/html" href="https://www.conservapedia.com/index.php?title=Lava_fountain&amp;diff=205337&amp;oldid=prev"/>
		<updated>2007-06-22T18:47:32Z</updated>

		<summary type="html">&lt;p&gt;New page: &lt;a href=&quot;/File:Lava_fountain.jpg&quot; title=&quot;File:Lava fountain.jpg&quot;&gt;300px|thumb|Lava fountain of the Pu`u `O`o cinder and spatter cone on Kilauea Volcano, Hawai`i.&lt;/a&gt;A jet of &lt;a href=&quot;/Lava&quot; title=&quot;Lava&quot;&gt;lava&lt;/a&gt; sprayed into the air by the rapid formation and...&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[Image:Lava_fountain.jpg|300px|thumb|Lava fountain of the Pu`u `O`o cinder and spatter cone on Kilauea Volcano, Hawai`i.]]A jet of [[lava]] sprayed into the air by the rapid formation and expansion of gas bubbles in the molten rock is called a '''lava fountain'''. Lava fountains typically range from about 10 to 100 m in height, but occasionally reach more than 500 m. Lava fountains erupt from isolated vents, along fissures, within active [[lava lake]]s, and from a [[lava tube]] when water gains access to the tube in a confined space.&lt;br /&gt;
&lt;br /&gt;
[[Category:Geology]]&lt;/div&gt;</summary>
		<author><name>SharonS</name></author>
	</entry>
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