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	<title>State of the Planet &#187; continental plates</title>
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		<title>Where Continents Divide, and Rocks Rise from the Deep</title>
		<link>http://blogs.ei.columbia.edu/2011/12/06/where-continents-divide-and-rocks-rise-from-the-deep/</link>
		<comments>http://blogs.ei.columbia.edu/2011/12/06/where-continents-divide-and-rocks-rise-from-the-deep/#comments</comments>
		<pubDate>Wed, 07 Dec 2011 02:04:55 +0000</pubDate>
		<dc:creator>David Funkhouser</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[AGU 2011]]></category>
		<category><![CDATA[American Geophysical Union]]></category>
		<category><![CDATA[continental plates]]></category>
		<category><![CDATA[Earthquakes]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Papua New Guinea]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=20708</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/12/cdpapua-bbmapfinal-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Map shows locations of seismometers deployed to study movements of the earth around eastern Papua New Guinea." />Along the Woodlark Rift in eastern Papua New Guinea, continents are breaking apart, “like a snake opening its mouth.” Geologic processes that are still a mystery are actively stretching the crust and pushing huge masses of rock, formed under immense pressures as deep as 100 kilometers below, to the surface.]]></description>
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