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      <title>PADLET 4 PLATE TECTONICS by Damaris Torres</title>
      <link>https://padlet.com/3033861/ijqid290skns</link>
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      <language>en-us</language>
      <pubDate>2018-03-29 16:24:06 UTC</pubDate>
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         <title> PLATE TECTONICS</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247317965</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 16:25:12 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247317965</guid>
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         <title>CONTINENTAL DRIFT</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247318653</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 16:26:59 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247318653</guid>
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         <title>SUBDUCTION</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247319141</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 16:28:30 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247319141</guid>
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         <title>MID ATLANTIC RIDGE</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247319570</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 16:29:48 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247319570</guid>
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         <title>RING OF FIRE</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247320194</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 16:31:31 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247320194</guid>
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         <title>CONVERGENT BOUNDARY</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247320656</link>
         <description><![CDATA[<div>A tectonic <strong>boundary</strong> where two plates are moving toward each other. If the two plates are of equal density, they usually push up against each other, forming a mountain chain. If they are of unequal density, one plate usually sinks beneath the other in a subduction zone.</div>]]></description>
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         <pubDate>2018-03-29 16:32:57 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247320656</guid>
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         <title>DIVERGENT BOUNDARY </title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247321184</link>
         <description><![CDATA[<div>A tectonic <strong>boundary</strong> where two plates are moving away from each other and new crust is forming from magma that rises to the Earth's surface between the two plates.</div>]]></description>
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         <pubDate>2018-03-29 16:34:38 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247321184</guid>
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      <item>
         <title>TRANSFORM BOUNDARY</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247321636</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 16:36:05 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247321636</guid>
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         <title>FAULT</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247322571</link>
         <description><![CDATA[<div>A <strong>fault</strong> is a crack in the Earth's crust. Typically, <strong>faults </strong>are associated with, or form, the boundaries between Earth's tectonic plates. In an active <strong>fault</strong>, the pieces of the Earth's crust along a <strong>fault</strong> move over time. The moving rocks can cause earthquakes.</div>]]></description>
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         <pubDate>2018-03-29 16:38:36 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247322571</guid>
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      <item>
         <title>ASTHENOSPERE</title>
         <author>3033861</author>
         <link>https://padlet.com/3033861/ijqid290skns/wish/247323255</link>
         <description><![CDATA[<div>he 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 16:40:34 UTC</pubDate>
         <guid>https://padlet.com/3033861/ijqid290skns/wish/247323255</guid>
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