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	<title>State of the Planet &#187; seafloor</title>
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		<title>Time and Technology and the Really Down Deep</title>
		<link>http://blogs.ei.columbia.edu/2011/06/08/time-and-technology-and-the-really-down-deep/</link>
		<comments>http://blogs.ei.columbia.edu/2011/06/08/time-and-technology-and-the-really-down-deep/#comments</comments>
		<pubDate>Wed, 08 Jun 2011 22:20:12 +0000</pubDate>
		<dc:creator>David Funkhouser</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Earthquakes]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[oceans]]></category>
		<category><![CDATA[seafloor]]></category>
		<category><![CDATA[sonar]]></category>
		<category><![CDATA[Volcanoes]]></category>

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		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/06/LamontSeamountsColumbia1-150x110.png" class="attachment-post-thumbnail wp-post-image" alt="The Lamont Seamounts are an example of the view from the seafloor synthesized by a team of oceanographers at Lamont-Doherty Earth Observatory. The seamounts are due west of El Salvador, at about 9.55 degrees N, 104 degrees W." />Two years before Google Earth was launched, Bill Ryan and Suzanne Carbotte, oceanographers at the Lamont-Doherty Earth Observatory, began a project to transform the way we look at the ocean. They started collecting reams of data that had been gathered by scientists sailing on research vessels all over the world since the 1980s, one ship [<a href="http://blogs.ei.columbia.edu/2011/06/08/time-and-technology-and-the-really-down-deep/">...</a>]]]></description>
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