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	<title>State of the Planet &#187; Earth&#8217;s Plates</title>
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		<title>Probing an Oceanic Plate</title>
		<link>http://blogs.ei.columbia.edu/2011/11/30/probing-an-oceanic-plate/</link>
		<comments>http://blogs.ei.columbia.edu/2011/11/30/probing-an-oceanic-plate/#comments</comments>
		<pubDate>Wed, 30 Nov 2011 12:36:49 +0000</pubDate>
		<dc:creator>Jim Gaherty</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Earth's Plates]]></category>
		<category><![CDATA[Earth's Tectonic Plates]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Langseth]]></category>
		<category><![CDATA[marine geophysics]]></category>
		<category><![CDATA[plate tectonics]]></category>
		<category><![CDATA[seismology]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=20289</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/11/pacbasin_intro_sml-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Google Earth map of the experiment (dubbed NoMelt) in the central Pacific Ocean basin." />Everything that we understand about the rhythms of the Earth’s surface – the slow growth of mountain chains, the creeping expansion of the ocean basins, the abrupt upheaval of a major earthquake, the explosive eruption of a volcano – is viewed through the context of plate tectonics.  This simple yet highly successful model for describing [<a href="http://blogs.ei.columbia.edu/2011/11/30/probing-an-oceanic-plate/">...</a>]]]></description>
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