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      <title>South American Subduction Zones by Maria Leech</title>
      <link>https://padlet.com/myles1019/ux50okzcb1ma</link>
      <description></description>
      <language>en-us</language>
      <pubDate>2017-03-16 01:29:45 UTC</pubDate>
      <lastBuildDate>2023-05-09 03:39:42 UTC</lastBuildDate>
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         <title>Relation to surface features</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160409485</link>
         <description><![CDATA[<ul><li>Nazca Plate (oceanic lithosphere) + South American Plate (continental crust) = Andes Mountains&nbsp;</li><li>Atacama (a.k.a. Peru-Chile) Trench</li><li>Volcanism</li></ul>]]></description>
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         <pubDate>2017-03-16 01:42:25 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160409485</guid>
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      <item>
         <title>In 10 million years...</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160409552</link>
         <description><![CDATA[<ul><li>Height of the Andes could double in just 2 - 4 Ma (making the average mountain 11,886 meters tall!)<ul><li>Delamination process&nbsp;</li></ul></li></ul><div><a href="http://uk.reuters.com/article/science-mountains-andes-dc-idUKN0531341020080605?pageNumber=2&amp;virtualBrandChannel=0">http://uk.reuters.com/article/science-mountains-andes-dc-idUKN0531341020080605?pageNumber=2&amp;virtualBrandChannel=0</a>&nbsp;<br><br></div><ul><li>Megathrust quakes (+8.5) due to "locked" plates could be extremely disastrous to human infrastructure &nbsp;</li></ul><div><a href="http://www.livescience.com/13941-megathrust-earthquakes-chile-japan-subduction-zones.html">http://www.livescience.com/13941-megathrust-earthquakes-chile-japan-subduction-zones.html</a></div>]]></description>
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         <pubDate>2017-03-16 01:42:52 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160409552</guid>
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      <item>
         <title></title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160409863</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 01:45:42 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160409863</guid>
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      <item>
         <title>Surface Features</title>
         <author>joe_j_whitmore</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160410763</link>
         <description><![CDATA[<div>subduction zone is the cause for the mountainous topography on the western side of the continent . Lack of tectonic movement is represented by the plateau on the eastern side. The subducting slab has also caused volcanoes to be present on the western side of the continent, these are part of the Pacific Ring of Fire.</div>]]></description>
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         <pubDate>2017-03-16 01:53:17 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160410763</guid>
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      <item>
         <title></title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160411407</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:00:06 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160411407</guid>
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      <item>
         <title>Dip of Slab ~33 degrees</title>
         <author>jackstickings</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160411911</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:05:06 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160411911</guid>
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      <item>
         <title>Dip of slab</title>
         <author>maxjfromnz</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160412335</link>
         <description><![CDATA[<div>37 degrees at the Northern End<br>33 degrees in Southern End<br><br><br></div>]]></description>
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         <pubDate>2017-03-16 02:09:11 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160412335</guid>
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      <item>
         <title></title>
         <author>michaellees27</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160412575</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:12:13 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160412575</guid>
      </item>
      <item>
         <title>3.7cm movement east yearly on the nazca plate</title>
         <author>jackstickings</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414104</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2017-03-16 02:28:52 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414104</guid>
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         <title>Depth Data</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414742</link>
         <description><![CDATA[<ul><li>Shallow, less powerful quakes along the coast at the plate boundaries&nbsp;</li><li>Deeper, stronger quakes farther inland</li><li>Some very deep quakes (+600 km) are an effect of&nbsp; internal deformation of the subducting Nazca plate</li><li><a href="https://pubs.usgs.gov/of/2010/1083/e/">https://pubs.usgs.gov/of/2010/1083/e/</a></li></ul>]]></description>
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         <pubDate>2017-03-16 02:39:37 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414742</guid>
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      <item>
         <title>Fault characteristic </title>
         <author>joe_j_whitmore</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414900</link>
         <description><![CDATA[<div>Friction from the subducting oceanic plate creates fracture and deformation. This is the reason for the small frequent earthquakes that occur along the fault&nbsp;<br><br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-16 02:42:01 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414900</guid>
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      <item>
         <title>Volcanism in the Andes</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414973</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:43:08 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160414973</guid>
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      <item>
         <title></title>
         <author>joe_j_whitmore</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415092</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:44:23 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415092</guid>
      </item>
      <item>
         <title>Andes</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415522</link>
         <description><![CDATA[<div>"The convergence of the Nazca and South American Plates has deformed and pushed up limestone strata to form towering peaks of the Andes, as seen here in the Pachapaqui mining area in Peru"<br><br></div>]]></description>
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         <pubDate>2017-03-16 02:49:41 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415522</guid>
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      <item>
         <title>Topography Cross Section</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415805</link>
         <description><![CDATA[<div>Topography and depth down to the Moho over a North-Soutprofile . The vertical (E-W lines) define the highly seismically attenuated region.<br><br><a href="http://www.geo.arizona.edu/geo5xx/geo527/Andes/geology.html">http://www.geo.arizona.edu/geo5xx/geo527/Andes/geology.html</a></div>]]></description>
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         <pubDate>2017-03-16 02:53:28 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415805</guid>
      </item>
      <item>
         <title>Timeline</title>
         <author>myles1019</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415993</link>
         <description><![CDATA[<ul><li>Start: Paleozoic</li><li>"The present day mountain belt was developed mainly during the Mesozoic to Recent"<ul><li>Opening of the Atlantic MOR</li><li>Easterly direction of the slab's dip</li></ul></li></ul><div><a href="http://www.geo.arizona.edu/geo5xx/geo527/Andes/intro.html">http://www.geo.arizona.edu/geo5xx/geo527/Andes/intro.html</a></div>]]></description>
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         <pubDate>2017-03-16 02:55:49 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160415993</guid>
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         <title>Cross Section</title>
         <author>jackstickings</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160416207</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:58:32 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160416207</guid>
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      <item>
         <title></title>
         <author>joe_j_whitmore</author>
         <link>https://padlet.com/myles1019/ux50okzcb1ma/wish/160416429</link>
         <description><![CDATA[]]></description>
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         <pubDate>2017-03-16 02:59:57 UTC</pubDate>
         <guid>https://padlet.com/myles1019/ux50okzcb1ma/wish/160416429</guid>
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