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	<title>State of the Planet &#187; glaciers</title>
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	<link>http://blogs.ei.columbia.edu</link>
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		<title>When the World Ended in Ice</title>
		<link>http://blogs.ei.columbia.edu/2012/06/29/when-the-world-ended-in-ice/</link>
		<comments>http://blogs.ei.columbia.edu/2012/06/29/when-the-world-ended-in-ice/#comments</comments>
		<pubDate>Fri, 29 Jun 2012 16:02:50 +0000</pubDate>
		<dc:creator>Kevin Krajick</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Climate]]></category>
		<category><![CDATA[Climate Science]]></category>
		<category><![CDATA[glaciation]]></category>
		<category><![CDATA[glaciers]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[New York City]]></category>
		<category><![CDATA[New York metro area]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=28413</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2012/06/glacier-front-ny-150x110.png" class="attachment-post-thumbnail wp-post-image" alt="A classic map of the ice lobe that covered the New York metro area until the end of the last ice age. (R.D. Salisbury, 1902)" />A mile or so of glacial ice covering much of North America and plowing down from the north once terminated in the New York metropolitan area, at a front stretching roughly from exit 13 on the New Jersey Turnpike (Rahway), on across southern Staten Island, the Bensonhurst neighborhood of Brooklyn, and northeastward through Long Island. But exactly when that ice started [<a href="http://blogs.ei.columbia.edu/2012/06/29/when-the-world-ended-in-ice/">...</a>]]]></description>
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		<slash:comments>2</slash:comments>
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		<item>
		<title>An Interactive Map of Scientific Fieldwork</title>
		<link>http://blogs.ei.columbia.edu/2012/05/07/an-interactive-map-of-scientific-fieldwork/</link>
		<comments>http://blogs.ei.columbia.edu/2012/05/07/an-interactive-map-of-scientific-fieldwork/#comments</comments>
		<pubDate>Mon, 07 May 2012 20:21:07 +0000</pubDate>
		<dc:creator>David Funkhouser</dc:creator>
				<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Africa]]></category>
		<category><![CDATA[Antarctica]]></category>
		<category><![CDATA[Asia]]></category>
		<category><![CDATA[Atlantic Ocean]]></category>
		<category><![CDATA[Caribbean]]></category>
		<category><![CDATA[Climate Science]]></category>
		<category><![CDATA[Earthquakes]]></category>
		<category><![CDATA[education]]></category>
		<category><![CDATA[Energy]]></category>
		<category><![CDATA[Environment]]></category>
		<category><![CDATA[glaciers]]></category>
		<category><![CDATA[Greenland]]></category>
		<category><![CDATA[India]]></category>
		<category><![CDATA[International Research Institute for Climate and Society]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[New York City]]></category>
		<category><![CDATA[North America]]></category>
		<category><![CDATA[Pacific Ocean]]></category>
		<category><![CDATA[South America]]></category>
		<category><![CDATA[volcanos]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=26205</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2012/05/Field-guide-map-Screen-shot-2012-05-07-at-3-26-28-PM-150x110.png" class="attachment-post-thumbnail wp-post-image" alt="Field work guide map, Earth Institute, Lamont-Doherrt Earth Observatory" />Earth Institute scientists explore how the physical world works on every continent -- over and under the arctic ice, in the grasslands of Mongolia, on volcanoes in Patagonia, over subduction zones in Papua New Guinea, and on the streets of New York City.]]></description>
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		<slash:comments>0</slash:comments>
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		<item>
		<title>At the Bottom of the Bottom of the World</title>
		<link>http://blogs.ei.columbia.edu/2012/03/12/at-the-bottom-of-the-bottom-of-the-world/</link>
		<comments>http://blogs.ei.columbia.edu/2012/03/12/at-the-bottom-of-the-bottom-of-the-world/#comments</comments>
		<pubDate>Mon, 12 Mar 2012 15:27:36 +0000</pubDate>
		<dc:creator>CERC Guest Blogger</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Ecosystems]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Water]]></category>
		<category><![CDATA[Ancient History]]></category>
		<category><![CDATA[Antarctica]]></category>
		<category><![CDATA[eco matters]]></category>
		<category><![CDATA[glaciers]]></category>
		<category><![CDATA[Lake Vostok]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=23778</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2012/03/Lake_Vostok_Sat_Photo-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="A satellite image of Vostok, a subglacial body of water larger than Lake Ontario. (Wikimedia Commons)" />As we in North America emerge from a remarkably mild winter, the brief and sunny summer in the world’s deep south is drawing to a rapid close. Antarctica’s days are becoming shorter, and come the vernal equinox the South Pole will enter into its yearly hibernation—six months of dusk and night. Researchers from Columbia University and elsewhere have spent these bright months bearing the chill in pursuit of access to a realm deep beneath the soaring, scathing surface of the glacier.]]></description>
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		<slash:comments>0</slash:comments>
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		<title>Rhone Glacier Finely Tuned to Climate Changes</title>
		<link>http://blogs.ei.columbia.edu/2011/06/03/rhone-glacier-finely-tuned-to-climate-changes/</link>
		<comments>http://blogs.ei.columbia.edu/2011/06/03/rhone-glacier-finely-tuned-to-climate-changes/#comments</comments>
		<pubDate>Fri, 03 Jun 2011 16:58:21 +0000</pubDate>
		<dc:creator>David Funkhouser</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Alps]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Climate Science]]></category>
		<category><![CDATA[glaciers]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Rhone River]]></category>
		<category><![CDATA[Switzerland]]></category>
		<category><![CDATA[Western Europe]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=15225</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/06/glacier-postcard-old-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="The Rhone Glacier c. 1900. Residents of the village of Gletsch, down the valley from the Rhone Glacier, have kept track of the ice since 1602. “Their water supply, the availability of farmland is controlled by where the glacier is,” said researcher Brent Goehring. For more glacier photos, go to: http://www.swisseduc.ch/glaciers/index-en.html" />By chiseling hunks of stone from recently exposed bedrock near the edge of the Rhone Glacier, scientists were able to decipher the comings and goings of the ice over the past 11,000 years. That should help predict what will happen to glaciers in the warming world to come. ]]></description>
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