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	<title>rangitoto &#8211; Irreverent Outcrop</title>
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		<title>Volcano (part 1): shield volcanoes</title>
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		<pubDate>Sun, 04 Aug 2024 04:05:06 +0000</pubDate>
				<category><![CDATA[Travel blog]]></category>
		<category><![CDATA[basalt]]></category>
		<category><![CDATA[hawaii]]></category>
		<category><![CDATA[lord howe island]]></category>
		<category><![CDATA[rangitoto]]></category>
		<category><![CDATA[shield volcano]]></category>
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					<description><![CDATA[Shield volcanoes and stratovolcanoes are two major types of volcanoes. Other smaller-scale volcanic features also include cinder cones, volcanic domes, calderas etc. To put it simply, low-viscosity magma flows gently outward instead of erupts violently, resulting in shield volcanoes with gentle slopes. In contrast, stratovolcanoes form from viscous magma that often erupts violently and couldn&#8217;t ... <a title="Volcano (part 1): shield volcanoes" class="read-more" href="https://irreverentoutcrop.com/volcano-part-1-shield-volcanoes/" aria-label="Read more about Volcano (part 1): shield volcanoes">Read more</a>]]></description>
										<content:encoded><![CDATA[<p>Shield volcanoes and stratovolcanoes are two major types of volcanoes. Other smaller&#x2d;scale volcanic features also include cinder cones, volcanic domes, calderas etc. To put it simply, low&#x2d;viscosity magma flows gently outward instead of erupts violently, resulting in shield volcanoes with gentle slopes. In contrast, stratovolcanoes form from viscous magma that often erupts violently and couldn&rsquo;t&#8230;</p>
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