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      <title>Padlet 4-Plate Tectonics by Samantha Zamora</title>
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      <description>Made with a little mischief</description>
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      <pubDate>2018-03-29 16:22:36 UTC</pubDate>
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         <title>Plate tectonics</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247317354</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 16:23:50 UTC</pubDate>
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         <title>Continental Drift</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247317525</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 16:24:14 UTC</pubDate>
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         <title>Subduction</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247317766</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 16:24:45 UTC</pubDate>
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         <title>Mid-Atlantic Ridge</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247317963</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>
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         <pubDate>2018-03-29 16:25:11 UTC</pubDate>
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         <title>Ring Of Fire</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247318197</link>
         <description><![CDATA[<div>The Ring of Fire 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 16:25:46 UTC</pubDate>
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         <title>Convergent boundary</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247318410</link>
         <description><![CDATA[<div> 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 16:26:16 UTC</pubDate>
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         <title>Divergent boundary </title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247318636</link>
         <description><![CDATA[<div>s a linear feature that exists between two tectonic plates that are moving away from each other.</div>]]></description>
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         <pubDate>2018-03-29 16:26:54 UTC</pubDate>
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         <title>Transform boundary</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247318800</link>
         <description><![CDATA[<div><strong>Transform boundaries</strong> are places where plates slide sideways past each other.</div>]]></description>
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         <pubDate>2018-03-29 16:27:26 UTC</pubDate>
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         <title>Fault</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247319046</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 16:28:12 UTC</pubDate>
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         <title>Asthenosphere</title>
         <author>3033672</author>
         <link>https://padlet.com/3033672/4enqbee2esrv/wish/247319323</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 16:29:02 UTC</pubDate>
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