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      <title>Padlet 4- Plate tectonics  by Noel Jimenez</title>
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      <description></description>
      <language>en-us</language>
      <pubDate>2018-03-29 18:13:01 UTC</pubDate>
      <lastBuildDate>2018-03-29 18:34:01 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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      <item>
         <title>ASTHENOSPERE</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362118</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 18:21:50 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362118</guid>
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         <title>FAULT</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362162</link>
         <description><![CDATA[<div>an unattractive or unsatisfactory feature, especially in a piece of work or in a person's character.</div>]]></description>
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         <pubDate>2018-03-29 18:21:59 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362162</guid>
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         <title>TRANSFORM BOUNDARY</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362275</link>
         <description><![CDATA[<div><strong>Transform boundaries</strong> are places where plates slide sideways past each other. At <strong>transform boundaries</strong>lithosphere is neither created nor destroyed.&nbsp;</div>]]></description>
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         <pubDate>2018-03-29 18:22:19 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362275</guid>
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         <title>DIVERGENT BOUNDARY </title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362338</link>
         <description><![CDATA[<div>In plate tectonics, a <strong>divergent boundary</strong> or <strong>divergent</strong>plate <strong>boundary</strong></div>]]></description>
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         <pubDate>2018-03-29 18:22:32 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362338</guid>
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         <title>CONVERGENT BOUNDARY</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362406</link>
         <description><![CDATA[<div>In plate tectonics, a <strong>convergent boundary</strong>, also known as a destructive plate <strong>boundary</strong>, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle.</div>]]></description>
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         <pubDate>2018-03-29 18:22:44 UTC</pubDate>
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         <title>RING OF FIRE</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362487</link>
         <description><![CDATA[<div>The <strong>Ring of Fire</strong> 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 18:22:55 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362487</guid>
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         <title>MID ATLANTIC RIDGE</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362596</link>
         <description><![CDATA[<div>The Mid-Atlantic Ridge is a mid-ocean ridge, a divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world.</div>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-29 18:23:12 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362596</guid>
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         <title>SUBDUCTION</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362651</link>
         <description><![CDATA[<div>the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.</div>]]></description>
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         <pubDate>2018-03-29 18:23:21 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362651</guid>
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         <title>CONTINENTAL DRIFT</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362714</link>
         <description><![CDATA[<div>the gradual movement of the continents across the earth's surface through geological time.</div>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-29 18:23:31 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362714</guid>
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         <title> PLATE TECTONICS</title>
         <author>303995</author>
         <link>https://padlet.com/303995/w4mopr6wjd78/wish/247362766</link>
         <description><![CDATA[<div>a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates that move slowly over the underlying mantle.</div>]]></description>
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         <pubDate>2018-03-29 18:23:41 UTC</pubDate>
         <guid>https://padlet.com/303995/w4mopr6wjd78/wish/247362766</guid>
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