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      <title>Earth Science Padlet by Isabella Pearson</title>
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      <description>Boundaries, boundaries, and more boundaries!</description>
      <language>en-us</language>
      <pubDate>2016-11-21 05:48:50 UTC</pubDate>
      <lastBuildDate>2017-05-17 04:24:09 UTC</lastBuildDate>
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         <title>Visual of Pangea</title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/139000018</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://vimeo.com/14258924" />
         <pubDate>2016-11-21 05:54:54 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/139000018</guid>
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         <title>Tectonic Map of the World </title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140106448</link>
         <description><![CDATA[]]></description>
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         <pubDate>2016-11-28 08:55:57 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140106448</guid>
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         <title>Divergent Boundary Animation </title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140106820</link>
         <description><![CDATA[<div><strong>Examples of divergent boundaries</strong> are the Mid-Atlantic Ridge and the Great Rift Valley. Iceland is an <strong>example</strong> of a country undergoing a continental <strong>divergent boundary</strong>. The Mid-Atlantic Ridge divides Iceland and is the <strong>boundary</strong> between the North American and Eurasian tectonic plates.</div>]]></description>
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         <pubDate>2016-11-28 08:58:52 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140106820</guid>
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         <title>Transform Boundary Animation </title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140107160</link>
         <description><![CDATA[<div>Examples of transform boundaries include the Alpine Fault of New Zealand, the San Andreas Fault and the Alpine Fault<strong>Transform</strong> faults are locations of recurring earthquake activity and faulting.</div>]]></description>
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         <pubDate>2016-11-28 09:01:19 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140107160</guid>
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         <title>Convergent Boundary Visual</title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140108013</link>
         <description><![CDATA[<div>A <strong>convergent boundary </strong>is an actively deforming region where two or more tectonic plates or fragments of the lithosphere move toward one another and collide. The Washington-Oregon coastline of the United States is an <strong>example</strong> of this type of <strong>convergent</strong> plate <strong>boundary</strong>. Here the Juan de Fuca oceanic plate is subducting beneath the westward moving North American continental plate.</div>]]></description>
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         <pubDate>2016-11-28 09:06:59 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140108013</guid>
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         <title>Oceanic-Oceanic Convergent Boundary </title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140222328</link>
         <description><![CDATA[<div>The features of a subduction zone where an oceanic plate subducts beneath another oceanic plate are the same as a continent-ocean subduction zone. </div>]]></description>
         <enclosure url="https://m.youtube.com/watch?v=SOmZODVotKk" />
         <pubDate>2016-11-28 15:58:10 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140222328</guid>
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         <title>Oceanic-Continental Convergent Boundary</title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140223401</link>
         <description><![CDATA[<div>When oceanic crust converges with continental crust, the denser oceanic plate plunges beneath the continental plate. This process, called <strong>subduction</strong>, occurs at the oceanic trenches.</div>]]></description>
         <enclosure url="https://m.youtube.com/watch?v=yirGrr_m49w" />
         <pubDate>2016-11-28 16:00:41 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140223401</guid>
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         <title>Continental-Continental Convergent Boundary</title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140224305</link>
         <description><![CDATA[<div>Continent-continent convergence creates some of the world’s largest mountains ranges. Magma cannot penetrate this thick crust, so there are no volcanoes, although the magma stays in the crust. </div>]]></description>
         <enclosure url="https://m.youtube.com/watch?v=mOPWXcKDOsQ" />
         <pubDate>2016-11-28 16:03:03 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140224305</guid>
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         <title>Evidence Supporting Plate Tectonics </title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140226210</link>
         <description><![CDATA[<div>- Sea Floor Magnetism: Stripes of magnetic material in the seafloor provide strong evidence for tectonic theory.<br><br>-Fossil Evidence: The continents have moved a great deal in the history of the planet, but they carry records of where they’ve been. Some of this evidence is the fossils of animals and plants. Tropical species found in the Antarctic and similar fossils found in western Africa and eastern South America tell a story of where those land masses used to be. <br><br>- Direct Measurement: Modern technology gives us a range of ways to directly measure the movement of tectonic plates. These methods are based around the idea of measuring distance between two points on Earth by using some intermediary transmitter in space.</div>]]></description>
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         <pubDate>2016-11-28 16:07:37 UTC</pubDate>
         <guid>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140226210</guid>
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         <title>How do the plates move?</title>
         <author>ipearson5119</author>
         <link>https://padlet.com/ipearson5119/earthsciencepadletvibes/wish/140228650</link>
         <description><![CDATA[]]></description>
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         <pubDate>2016-11-28 16:13:23 UTC</pubDate>
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