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	<title>State of the Planet &#187; plate tectonics</title>
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		<title>A Talk with Sean Solomon, Lamont-Doherty&#8217;s New Director</title>
		<link>http://blogs.ei.columbia.edu/2012/09/21/a-talk-with-sean-solomon-lamont-dohertys-new-director/</link>
		<comments>http://blogs.ei.columbia.edu/2012/09/21/a-talk-with-sean-solomon-lamont-dohertys-new-director/#comments</comments>
		<pubDate>Fri, 21 Sep 2012 15:30:56 +0000</pubDate>
		<dc:creator>Kim Martineau</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Climate Science]]></category>
		<category><![CDATA[Geochemistry]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[marine geology]]></category>
		<category><![CDATA[Oceanography]]></category>
		<category><![CDATA[plate tectonics]]></category>
		<category><![CDATA[Solar System]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=29893</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2012/08/Sean-Solomon-2-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Sean Solomon" />"The Observatory has remained a powerhouse in Earth science research and a very special place. The scientists here are true explorers—creative and fiercely independent."]]></description>
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		<title>Rolling into Open Water in the Central Pacific</title>
		<link>http://blogs.ei.columbia.edu/2011/12/05/rolling-into-open-water-in-the-central-pacific/</link>
		<comments>http://blogs.ei.columbia.edu/2011/12/05/rolling-into-open-water-in-the-central-pacific/#comments</comments>
		<pubDate>Tue, 06 Dec 2011 00:48:22 +0000</pubDate>
		<dc:creator>Jim Gaherty</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Earth's Tectonic Plates]]></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=20601</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/12/langseth_broadside_dock-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="The Langseth at dock in Honolulu.  Bridge cabins/labs are to the right; waist-deck where OBS operations occur is in the center; and the large aft streamer platform is on the left.  Top center is the PSO observation tower, over 85 ft above the waterline." />We nicknamed our project NoMelt because we seek to characterize a mature, pristine oceanic plate far from its volcanic origin at a Mid-Ocean Ridge, and away from areas of pronounced volcanism and melting that subsequently alter the structure of the plate.  Our site in the central Pacific fits these scientific needs. However, one downside is [<a href="http://blogs.ei.columbia.edu/2011/12/05/rolling-into-open-water-in-the-central-pacific/">...</a>]]]></description>
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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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