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      <pubDate>2018-03-29 18:09:54 UTC</pubDate>
      <lastBuildDate>2018-03-29 18:21:36 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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         <title>Plate Tectonics</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247358254</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 18:10:39 UTC</pubDate>
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         <title>Continental Drift</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247358324</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 18:10:52 UTC</pubDate>
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         <title>Subduction</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247358392</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 18:11:04 UTC</pubDate>
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         <title>Mid-Atlantic Ridge</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247358451</link>
         <description><![CDATA[<div>The <strong>Mid</strong>-<strong>Atlantic Ridge</strong> (MAR) is a <strong>mid</strong>-ocean <strong>ridge</strong>, a divergent tectonic plate or constructive plate boundary located along the floor of the<strong>Atlantic</strong> Ocean, and part of the longest mountain range in the world.</div><div><br></div>]]></description>
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         <pubDate>2018-03-29 18:11:14 UTC</pubDate>
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         <title>Ring of fire</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247358623</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 18:11:51 UTC</pubDate>
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         <title>Convergent Boundary</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247358967</link>
         <description><![CDATA[<div>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 18:12:42 UTC</pubDate>
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         <title>Divergent Boundary</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247359272</link>
         <description><![CDATA[<div>In plate tectonics, a <strong>divergent boundary</strong> or <strong>divergent</strong>plate <strong>boundary</strong> (also known as a constructive <strong>boundary</strong> or an extensional <strong>boundary</strong>) is 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 18:13:31 UTC</pubDate>
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         <title>Transform Boundary</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247359312</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. Many<strong>transform boundaries</strong> are found on the sea floor, where they connect segments of diverging mid-ocean ridges. California's San Andreas fault is a <strong>transform boundary</strong>.</div>]]></description>
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         <pubDate>2018-03-29 18:13:36 UTC</pubDate>
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         <title>Fault</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247359406</link>
         <description><![CDATA[<div>In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock-mass movement. </div>]]></description>
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         <pubDate>2018-03-29 18:13:50 UTC</pubDate>
         <guid>https://padlet.com/3049361/rt25jlnxw40e/wish/247359406</guid>
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         <title>Asthenosphere</title>
         <author>3049361</author>
         <link>https://padlet.com/3049361/rt25jlnxw40e/wish/247359493</link>
         <description><![CDATA[<div>The asthenosphere is the highly viscous, mechanically weak and ductilely deforming region of the upper mantle of the Earth. It lies below the lithosphere, at depths between approximately 80 and 200 km below the surface. </div>]]></description>
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         <pubDate>2018-03-29 18:14:05 UTC</pubDate>
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