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	<title>Futurity.org &#187; magma</title>
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		<title>Deep-sea volcanoes air volatile side</title>
		<link>http://www.futurity.org/earth-environment/deep-sea-volcanoes-air-volatile-side/</link>
		<comments>http://www.futurity.org/earth-environment/deep-sea-volcanoes-air-volatile-side/#comments</comments>
		<pubDate>Tue, 29 Mar 2011 16:02:24 +0000</pubDate>
		<dc:creator>Katherine Gombay-McGill</dc:creator>
				<category><![CDATA[Earth & Environment]]></category>
		<category><![CDATA[carbon cycle]]></category>
		<category><![CDATA[earth sciences]]></category>
		<category><![CDATA[geology]]></category>
		<category><![CDATA[magma]]></category>
		<category><![CDATA[McGill University]]></category>
		<category><![CDATA[oceanography]]></category>
		<category><![CDATA[seafloor]]></category>
		<category><![CDATA[volcano]]></category>

		<guid isPermaLink="false">http://www.futurity.org/?p=31085</guid>
		<description><![CDATA[<p><img src="http://www.futurity.org/wp-content/uploads/2011/03/glowing_magma_1.jpg"></p><p class="first"><strong>MCGILL (CAN) —</strong> Deep-sea volcanoes do more than gush magma flow—in some cases high concentrations of CO2 cause massive underwater explosions.<span id="more-31085"></span></p><p>Between 75 and 80 percent of all volcanic activity on Earth takes place at deep-sea, mid-ocean ridges. Most produce effusive lava flows rather than explosive eruptions, both because the levels of magmatic gas tends to be low, and because the volcanoes are under a lot of pressure from the surrounding water.</p><p>]]></description>
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		<title>Seafloor dynamics at work splitting continent</title>
		<link>http://www.futurity.org/earth-environment/seafloor-dynamics-at-work-splitting-continent/</link>
		<comments>http://www.futurity.org/earth-environment/seafloor-dynamics-at-work-splitting-continent/#comments</comments>
		<pubDate>Tue, 03 Nov 2009 20:12:46 +0000</pubDate>
		<dc:creator>Jonathan Sherwood-Rochester</dc:creator>
				<category><![CDATA[Earth & Environment]]></category>
		<category><![CDATA[Africa]]></category>
		<category><![CDATA[Cindy Ebinger]]></category>
		<category><![CDATA[continents]]></category>
		<category><![CDATA[earth sciences]]></category>
		<category><![CDATA[earthquakes]]></category>
		<category><![CDATA[Ethiopia]]></category>
		<category><![CDATA[geophysics]]></category>
		<category><![CDATA[magma]]></category>
		<category><![CDATA[nature]]></category>
		<category><![CDATA[oceans]]></category>
		<category><![CDATA[seismology]]></category>
		<category><![CDATA[University of Leeds]]></category>
		<category><![CDATA[University of Rochester]]></category>
		<category><![CDATA[volcano]]></category>

		<guid isPermaLink="false">http://futurity.org/?p=5416</guid>
		<description><![CDATA[<p><img src="http://www.futurity.org/wp-content/uploads/"></p><div class="post_photo_350"><img class="alignright size-full wp-image-5417" title="africa_ocean2" src="http://futurity.org/wp-content/uploads/2009/11/africa_ocean2.jpg" alt="africa_ocean2" width="400" height="290" /></div>
<p class="wp-caption-text" style="width: 400px;">Reconstruction of events showed that the rift did not open in a series of small earthquakes over an extended period of time, but tore open along its entire 35-mile length in just days. A volcano called Dabbahu at the northern end of the rift erupted first, then magma pushed up through the middle of the rift area and began &#8220;unzipping&#8221; the rift in both directions, says Cindy Ebinger.</p>
<p class="first"><strong>U. ROCHESTER (US)—</strong>In 2005, a gigantic, 35-mile-long rift broke open the desert ground in Ethiopia. At the time, some geologists believed the rift was the beginning of a new ocean as two parts of the African continent pulled apart, but the claim was controversial.<span id="more-5416"></span></p><p>Now, scientists from several countries have confirmed that the volcanic processes at work beneath the Ethiopian rift are nearly identical to those at the bottom of the world&#8217;s oceans, and the rift is indeed likely the beginning of a new sea.</p><p>]]></description>
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