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<channel>
	<title>State of the Planet &#187; Andes</title>
	<atom:link href="http://blogs.ei.columbia.edu/tag/andes/feed/" rel="self" type="application/rss+xml" />
	<link>http://blogs.ei.columbia.edu</link>
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		<title>Managing Water in a Dry Land</title>
		<link>http://blogs.ei.columbia.edu/2013/06/17/managing-water-in-a-dry-land/</link>
		<comments>http://blogs.ei.columbia.edu/2013/06/17/managing-water-in-a-dry-land/#comments</comments>
		<pubDate>Mon, 17 Jun 2013 20:55:16 +0000</pubDate>
		<dc:creator>Francesco Fiondella</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[chile]]></category>
		<category><![CDATA[climate matters]]></category>
		<category><![CDATA[Dam]]></category>
		<category><![CDATA[drought]]></category>
		<category><![CDATA[puclaro]]></category>
		<category><![CDATA[rain]]></category>
		<category><![CDATA[snow]]></category>
		<category><![CDATA[Water]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=37398</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2013/06/8696938783_d5cba10549_h-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="The Puclaro Reservoir is at around 10% of it&#039;s peak in 2009, indicated by lines on the mountain in the background. The dam is in the distance. Without the reservoir, farmers, mines and other water users have lost one of their key buffers against drought. Francesco Fiondella" />Since 2010, the Earth Institute’s International Research Institute for Climate and Society along with UNESCO and their colleagues in Chile have been working with Elqui’s water authority to help them use seasonal forecasts as way to better allocate water and prepare for droughts.]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2013/06/17/managing-water-in-a-dry-land/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>End of the Line &#8211; Good Byes to a Great Field Season in Peru</title>
		<link>http://blogs.ei.columbia.edu/2011/08/07/end-of-the-line-good-byes-to-a-great-field-season-in-peru/</link>
		<comments>http://blogs.ei.columbia.edu/2011/08/07/end-of-the-line-good-byes-to-a-great-field-season-in-peru/#comments</comments>
		<pubDate>Sun, 07 Aug 2011 13:00:29 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=16738</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/08/Evening-storm-approaching-Olleros-north-of-Coropuna1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Evening storm approaching Olleros, north of Coropuna" />After more than six weeks trawling the Peruvian Andes in search of palaeoclimate clues, our field team is visiting the last site, a potential calibration sites near Coropuna. The objective of that ongoing work is to refine the cosmogenic surface-exposure method for the tropics, thereby improving the precision of new and existing datasets. ]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/08/07/end-of-the-line-good-byes-to-a-great-field-season-in-peru/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>On the Subject of Dust</title>
		<link>http://blogs.ei.columbia.edu/2011/07/25/on-the-subject-of-dust/</link>
		<comments>http://blogs.ei.columbia.edu/2011/07/25/on-the-subject-of-dust/#comments</comments>
		<pubDate>Mon, 25 Jul 2011 07:29:05 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=16307</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/07/Kurt-high-on-the-slopes-of-Ampato2-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Kurt high on the slopes of Ampato" />Our field team has set camp at 5045 m on the dusty slopes of Ampato, an extinct, ice-clad volcano in the Western Cordillera. This is the very mountain from which Juanita, the famous Incan ‘ice maiden’, was plucked back in 1995. The tents are clustered in the lee of a large glacial erratic and, now the clouds have cleared, the view is second to none, taking in the dry plains far below and myriad volcanic peaks in every direction.]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/07/25/on-the-subject-of-dust/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Going West</title>
		<link>http://blogs.ei.columbia.edu/2011/07/17/going-west/</link>
		<comments>http://blogs.ei.columbia.edu/2011/07/17/going-west/#comments</comments>
		<pubDate>Sun, 17 Jul 2011 19:21:40 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=16300</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/07/Heading-west-to-Arequipa1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Heading west to Arequipa" />After a busy few weeks in the Cordillera Carabaya, our field team has said goodbye to the snowy, tempestuous climate of the eastern Andes and is moving west to the desert of Arequipa. Here the mountains are massive, isolated volcanoes, many of which exceed 6000 m in elevation. In fact, Coropuna is the third highest mountain in Peru and certainly the most sprawling.]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/07/17/going-west/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Mad Dogs and Englishmen</title>
		<link>http://blogs.ei.columbia.edu/2011/07/11/mad-dogs-and-englishmen/</link>
		<comments>http://blogs.ei.columbia.edu/2011/07/11/mad-dogs-and-englishmen/#comments</comments>
		<pubDate>Tue, 12 Jul 2011 03:32:50 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=16177</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/07/Mooch-arrives-in-our-camp-Cordillera-Carabaya2-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Mooch arrives in our camp, Cordillera Carabaya" />Our field team has acquired a dog, ¨”Mooch”. Walking back to camp yesterday, amid driving snow and fully laden with rock samples, there he was exploring what passes for our kitchen. Unlike most Andean dogs -  ferocious beasts trained to keep geologists from harassing the livestock – this one is a cheerful soul, happy to hang around and be fed whatever is going, and always up for affection. ]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/07/11/mad-dogs-and-englishmen/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Ancient mud from the high Andes</title>
		<link>http://blogs.ei.columbia.edu/2011/07/08/ancient-mud-from-the-high-andes/</link>
		<comments>http://blogs.ei.columbia.edu/2011/07/08/ancient-mud-from-the-high-andes/#comments</comments>
		<pubDate>Fri, 08 Jul 2011 16:22:05 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=16110</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/07/Sampling-a-sediment-core-for-radiocarbon-samples1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Sampling a sediment core for radiocarbon samples" />Thanks in large part to Matt, an undergraduate from Pacific Lutheran University in Washington, our field team now has more than sixty samples for surface-exposure dating. This is no easy feat, for collecting these samples requires a great deal of hammering on granite boulders with nothing more than a hammer and chisel. There are other ways of doing it, such as using small explosive charges, rock saws, or splitting wedges, but we find that good old-fashioned hammering is by far the safest way. ]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/07/08/ancient-mud-from-the-high-andes/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>A typical day in the high Andes</title>
		<link>http://blogs.ei.columbia.edu/2011/07/02/a-typical-day-in-the-high-andes/</link>
		<comments>http://blogs.ei.columbia.edu/2011/07/02/a-typical-day-in-the-high-andes/#comments</comments>
		<pubDate>Sat, 02 Jul 2011 20:32:09 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=15967</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/07/Gordon-and-Matt-mapping-Holocene-moraines-above-Veluyoccocha1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="Gordon and Matt mapping Holocene moraines above Veluyoccocha" />Each morning starts the same in the Andes: the frost is heavy on the insides of our tents and falls with the slightest movement, while the realization that it´s going to be a freezing exit from the  sleeping bag is tempered by gratitude that the thirteen hour night is over. Yes, sunrise in the Andes is a momentous occasion each day, one that feels a million miles away from home.]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/07/02/a-typical-day-in-the-high-andes/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Foreigners in a Strange Land</title>
		<link>http://blogs.ei.columbia.edu/2011/06/26/foreigners-in-a-strange-land-crucero/</link>
		<comments>http://blogs.ei.columbia.edu/2011/06/26/foreigners-in-a-strange-land-crucero/#comments</comments>
		<pubDate>Mon, 27 Jun 2011 03:40:08 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=15855</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/06/stars-over-Laguna-Aricoma1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="stars over Laguna Aricoma" />After a very cold morning in Crucero, the sun burned off the clouds to reveal the black peaks of the Cordillera Carabaya to the east. There´s not so much snow left on the hills these days, just a few glacier patches clinging to the south faces of the highest summits. ]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/06/26/foreigners-in-a-strange-land-crucero/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Into Thin(ner) Air &#8211; On Route to the Cordillera Carabaya</title>
		<link>http://blogs.ei.columbia.edu/2011/06/23/into-thinner-air-en-route-to-the-cordillera-carabaya/</link>
		<comments>http://blogs.ei.columbia.edu/2011/06/23/into-thinner-air-en-route-to-the-cordillera-carabaya/#comments</comments>
		<pubDate>Fri, 24 Jun 2011 02:37:09 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[General Earth Institute]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=15809</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/06/El-Misti-rising-above-the-puna-en-route-to-Aricoma1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="El Misti rising above the puna, en route to Aricoma" />This morning we left Arequipa and the comforts of the tourist trail, driving east across the puna towards the Andes proper. Our route took us along the newly constructed Caraterra Interoceanica - a highway linking the Pacific coast of Peru to ports in Brazil - and up to elevations of 4700 m. Along the way we passed the smoking Volcan Ubinas, Peru's most active volcano, and the enormous inland sea of Lake Titicaca.]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/06/23/into-thinner-air-en-route-to-the-cordillera-carabaya/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>At the Feet of El Misti</title>
		<link>http://blogs.ei.columbia.edu/2011/06/22/at-the-feet-of-el-misti/</link>
		<comments>http://blogs.ei.columbia.edu/2011/06/22/at-the-feet-of-el-misti/#comments</comments>
		<pubDate>Wed, 22 Jun 2011 19:23:37 +0000</pubDate>
		<dc:creator>Gisela Winckler</dc:creator>
				<category><![CDATA[Climate]]></category>
		<category><![CDATA[Earth Sciences]]></category>
		<category><![CDATA[Andes]]></category>
		<category><![CDATA[climate change]]></category>
		<category><![CDATA[Glacial Melting]]></category>
		<category><![CDATA[Global Warming]]></category>
		<category><![CDATA[Lamont-Doherty Earth Observatory]]></category>
		<category><![CDATA[Peru Glaciers]]></category>
		<category><![CDATA[South America]]></category>

		<guid isPermaLink="false">http://blogs.ei.columbia.edu/?p=15751</guid>
		<description><![CDATA[<img width="150" height="110" src="http://blogs.ei.columbia.edu/wp-content/uploads/2011/06/ISS021-E-8370-71_lrg1-150x110.jpg" class="attachment-post-thumbnail wp-post-image" alt="ISS021-E-8370-71_lrg" />What a difference a day makes! We've said goodbye to the sprawling metropolis of Lima and now are happily settled in Arequipa - the White City. This name refers to the white sillar rock used in the construction of the old colonial city and which is in fact a pyroclastic deposit from the volcanoes towering above us. From our hotel room I can see the massive bell-shaped peak of El Misti (5800 m), the only active volcano of the group, and it's looking particularly snowy this year. ]]></description>
		<wfw:commentRss>http://blogs.ei.columbia.edu/2011/06/22/at-the-feet-of-el-misti/feed/</wfw:commentRss>
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