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      <title>Padlet 4-plate techonics by </title>
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      <pubDate>2018-03-29 16:23:26 UTC</pubDate>
      <lastBuildDate>2018-03-29 16:34:37 UTC</lastBuildDate>
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         <title>Plate techonics</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247317800</link>
         <description><![CDATA[<div>a theory explaining the structure of the earth's crust</div>]]></description>
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         <pubDate>2018-03-29 16:24:50 UTC</pubDate>
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         <title>Continental drift</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247318162</link>
         <description><![CDATA[<div>the gradual movement of the continents across the earth's surface through geological time.</div>]]></description>
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         <pubDate>2018-03-29 16:25:43 UTC</pubDate>
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         <title>Subduction</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247318548</link>
         <description><![CDATA[<div>the sideways and downward movement of the edge of a plate</div>]]></description>
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         <pubDate>2018-03-29 16:26:38 UTC</pubDate>
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         <title>Mid-Atlantic Ridge</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247318728</link>
         <description><![CDATA[<div>&nbsp;a divergent tectonic plate or constructive plate boundary</div>]]></description>
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         <pubDate>2018-03-29 16:27:15 UTC</pubDate>
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         <title>Ring of fire</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247319200</link>
         <description><![CDATA[<div> is a major area in the basin of the Pacific Ocean where a large number of earthquakes and volcanic eruptions occur</div>]]></description>
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         <pubDate>2018-03-29 16:28:40 UTC</pubDate>
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         <title>Convergent Boundary</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247319471</link>
         <description><![CDATA[<div>&nbsp;is a region of active deformation where two or more tectonic plates</div>]]></description>
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         <pubDate>2018-03-29 16:29:30 UTC</pubDate>
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         <title>Divergent Boundary</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247319769</link>
         <description><![CDATA[<div> A tectonic boundary where two plates are moving away</div>]]></description>
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         <pubDate>2018-03-29 16:30:21 UTC</pubDate>
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         <title>Transform Boundary Fault</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247320017</link>
         <description><![CDATA[<div>Are places where plates slide sideways past each other</div>]]></description>
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         <pubDate>2018-03-29 16:31:04 UTC</pubDate>
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         <title>Fault</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247320668</link>
         <description><![CDATA[<div>It is a planar fracture or discontinuity in a volume of rock</div>]]></description>
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         <pubDate>2018-03-29 16:32:59 UTC</pubDate>
         <guid>https://padlet.com/3062231/3smt3o4uncxs/wish/247320668</guid>
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         <title>Asthenosphere</title>
         <author>3062231</author>
         <link>https://padlet.com/3062231/3smt3o4uncxs/wish/247320989</link>
         <description><![CDATA[<div>the upper layer of the earth's mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur.</div>]]></description>
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         <pubDate>2018-03-29 16:34:04 UTC</pubDate>
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