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	<updated>2026-09-30T16:14:08Z</updated>
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	<entry>
		<id>https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52454</id>
		<title>Some information on geology</title>
		<link rel="alternate" type="text/html" href="https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52454"/>
		<updated>2004-10-06T20:56:14Z</updated>

		<summary type="html">&lt;p&gt;216.146.97.241: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;/div&gt;</summary>
		<author><name>216.146.97.241</name></author>
	</entry>
	<entry>
		<id>https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52453</id>
		<title>Some information on geology</title>
		<link rel="alternate" type="text/html" href="https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52453"/>
		<updated>2004-10-06T20:52:33Z</updated>

		<summary type="html">&lt;p&gt;216.146.97.241: Physical Geology&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&amp;lt;h1&amp;gt;Volcanism&amp;lt;/h1&amp;gt;&lt;br /&gt;
There are three(3) types of lavas formed by volcanoes.  Mafic, Intermediate, and Felsic.&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;B&amp;gt;&amp;lt;U&amp;gt;Mafic&amp;lt;/B&amp;gt;&amp;lt;U&amp;gt;(Basaltic)&amp;lt;/U&amp;gt;&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%SiO2: &amp;lt; 50%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%FeMg: 4%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Temp: up to 1500C&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Viscosity: Low&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Eruptive Behavior: gentle&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Distribution: divergent plate boundries, hot spots, convergent plate boundries&amp;lt;/li&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&amp;lt;B&amp;gt;&amp;lt;U&amp;gt;Intermediate&amp;lt;/B&amp;gt;&amp;lt;U&amp;gt;(Andesitic)&amp;lt;/U&amp;gt;&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%SiO2: ~60%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%FeMg: ~3%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Temp: ~1000C&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Viscosity: Intermediate&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Eruptive Behavior: explosive&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Distribution: convergent plate boundries&amp;lt;/li&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&amp;lt;B&amp;gt;&amp;lt;U&amp;gt;Felsic&amp;lt;/B&amp;gt;&amp;lt;U&amp;gt;(Rhyolitic)&amp;lt;/U&amp;gt;&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%SiO2: &amp;gt;70%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%FeMg: 2%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Temp: 700C&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Viscosity: High&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Eruptive Behavior: explosive&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Distribution: hot spots in continental crusts (Yellowstone National Park)&amp;lt;/li&amp;gt;&lt;/div&gt;</summary>
		<author><name>216.146.97.241</name></author>
	</entry>
	<entry>
		<id>https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52452</id>
		<title>Some information on geology</title>
		<link rel="alternate" type="text/html" href="https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52452"/>
		<updated>2004-10-06T20:49:45Z</updated>

		<summary type="html">&lt;p&gt;216.146.97.241: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;There are three(3) types of lavas formed by volcanoes.  Mafic, Intermediate, and Felsic.&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;B&amp;gt;&amp;lt;U&amp;gt;Mafic&amp;lt;/B&amp;gt;&amp;lt;U&amp;gt;(Basaltic)&amp;lt;/U&amp;gt;&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%SiO2: &amp;lt; 50%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%FeMg: 4%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Temp: up to 1500C&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Viscosity: Low&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Eruptive Behavior: gentle&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Distribution: divergent plate boundries, hot spots, convergent plate boundries&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;B&amp;gt;&amp;lt;U&amp;gt;Intermediate&amp;lt;/B&amp;gt;&amp;lt;U&amp;gt;(Andesitic)&amp;lt;/U&amp;gt;&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%SiO2: ~60%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%FeMg: ~3%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Temp: ~1000C&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Viscosity: Intermediate&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Eruptive Behavior: explosive&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Distribution: convergent plate boundries&amp;lt;/li&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&amp;lt;B&amp;gt;&amp;lt;U&amp;gt;Felsic&amp;lt;/B&amp;gt;(Rhyolitic)&amp;lt;U&amp;gt;&amp;lt;/U&amp;gt;&amp;lt;br&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%SiO2: &amp;gt;70%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;%FeMg: 2%&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Temp: 700C&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Viscosity: High&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Eruptive Behavior: explosive&amp;lt;/li&amp;gt;&lt;br /&gt;
&amp;lt;li&amp;gt;Distribution: hot spots in continental crusts (Yellowstone National Park)&amp;lt;/li&amp;gt;&lt;/div&gt;</summary>
		<author><name>216.146.97.241</name></author>
	</entry>
	<entry>
		<id>https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52451</id>
		<title>Some information on geology</title>
		<link rel="alternate" type="text/html" href="https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52451"/>
		<updated>2004-10-05T17:23:49Z</updated>

		<summary type="html">&lt;p&gt;216.146.97.241: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;There are three types of lavas formed by volcanoes.  Mafic, Intermediate, and Felsic.&amp;lt;br&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Mafic&#039;&#039;&#039;(Basaltic)&amp;lt;br&amp;gt;&lt;br /&gt;
%SiO2: &amp;lt; 50%&amp;lt;br&amp;gt;&lt;br /&gt;
%FeMg: 4%&amp;lt;br&amp;gt;&lt;br /&gt;
Temp: up to 1500C&amp;lt;br&amp;gt;&lt;br /&gt;
Viscosity: Low&amp;lt;br&amp;gt;&lt;br /&gt;
Eruptive Behavior: gentle&amp;lt;br&amp;gt;&lt;br /&gt;
Distribution: divergent plate boundries, hot spots, convergent plate boundries&amp;lt;br&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Intermediate&#039;&#039;&#039;(Andesitic)&amp;lt;br&amp;gt;&lt;br /&gt;
%SiO2: ~60%&amp;lt;br&amp;gt;&lt;br /&gt;
%FeMg: ~3%&amp;lt;br&amp;gt;&lt;br /&gt;
Temp: ~1000C&amp;lt;br&amp;gt;&lt;br /&gt;
Viscosity: Intermediate&amp;lt;br&amp;gt;&lt;br /&gt;
Eruptive Behavior: explosive&amp;lt;br&amp;gt;&lt;br /&gt;
Distribution: convergent plate boundries&amp;lt;br&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Felsic&#039;&#039;&#039;(Rhyolitic)&amp;lt;br&amp;gt;&lt;br /&gt;
%SiO2: &amp;gt;70%&amp;lt;br&amp;gt;&lt;br /&gt;
%FeMg: 2%&amp;lt;br&amp;gt;&lt;br /&gt;
Temp: 700C&amp;lt;br&amp;gt;&lt;br /&gt;
Viscosity: High&amp;lt;br&amp;gt;&lt;br /&gt;
Eruptive Behavior: explosive&amp;lt;br&amp;gt;&lt;br /&gt;
Distribution: hot spots in continental crusts (Yellowstone National Park)&lt;/div&gt;</summary>
		<author><name>216.146.97.241</name></author>
	</entry>
	<entry>
		<id>https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52450</id>
		<title>Some information on geology</title>
		<link rel="alternate" type="text/html" href="https://ideawaza.com/index.php?title=Some_information_on_geology&amp;diff=52450"/>
		<updated>2004-10-05T17:19:32Z</updated>

		<summary type="html">&lt;p&gt;216.146.97.241: Types Of Lava&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;There are three types of lavas formed by volcanoes.  Mafic, Intermediate, and Felsic.&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Mafic&#039;&#039;&#039;(Basaltic)&lt;br /&gt;
%SiO2: &amp;lt; 50%&lt;br /&gt;
%FeMg: 4%&lt;br /&gt;
Temp: up to 1500C&lt;br /&gt;
Viscosity: Low&lt;br /&gt;
Eruptive Behavior: gentle&lt;br /&gt;
Distribution: divergent plate boundries, hot spots, convergent plate boundries&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Intermediate&#039;&#039;&#039;(Andesitic)&lt;br /&gt;
%SiO2: ~60%&lt;br /&gt;
%FeMg: ~3%&lt;br /&gt;
Temp: ~1000C&lt;br /&gt;
Viscosity: Intermediate&lt;br /&gt;
Eruptive Behavior: explosive&lt;br /&gt;
Distribution: convergent plate boundries&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Felsic&#039;&#039;&#039;(Rhyolitic)&lt;br /&gt;
%SiO2: &amp;gt;70%&lt;br /&gt;
%FeMg: 2%&lt;br /&gt;
Temp: 700C&lt;br /&gt;
Viscosity: High&lt;br /&gt;
Eruptive Behavior: explosive&lt;br /&gt;
Distribution: hot spots in continental crusts (Yellowstone National Park)&lt;/div&gt;</summary>
		<author><name>216.146.97.241</name></author>
	</entry>
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