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      <title>PADLET 4 PLATE TECTONICS by Andrea Lucio</title>
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      <description>Andrea Lucio P.4 3/28/18</description>
      <language>en-us</language>
      <pubDate>2018-03-29 15:24:06 UTC</pubDate>
      <lastBuildDate>2018-03-29 15:47:48 UTC</lastBuildDate>
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         <title>PLATE TECTONICS</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247297035</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 15:33:52 UTC</pubDate>
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         <title>CONTINENTAL DRIFT</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247297869</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 15:36:01 UTC</pubDate>
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         <title>SUBDUCTION</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247298113</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 15:36:37 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247298113</guid>
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         <title>MID ATLANTIC RIDGE</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247298683</link>
         <description><![CDATA[<div>a north-south suboceanic ridge in the Atlantic Ocean from Iceland to Antarctica on whose crest are several groups of islands; shown by plate tectonics to be the axis along which North America has split away from Eurasia, and along which South America has split away from Africa.</div>]]></description>
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         <pubDate>2018-03-29 15:38:03 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247298683</guid>
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         <title>RING OF FIRE</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247300483</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. In a 40,000 km (25,000 mi) horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and plate movements.</div>]]></description>
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         <pubDate>2018-03-29 15:42:34 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247300483</guid>
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         <title>CONVERGENT BOUNDARY</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247301105</link>
         <description><![CDATA[<div><strong>convergent</strong> plate <strong>boundary</strong>. (kən-vûr'jənt) 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 15:44:07 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247301105</guid>
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         <title>DIVERGENT BOUNDARY </title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247301390</link>
         <description><![CDATA[<div><strong>divergent</strong> plate <strong>boundary</strong> in Science. <strong>divergent</strong> plate <strong>boundary</strong>. (dĭ-vûr'jənt) 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 15:44:45 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247301390</guid>
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         <title>TRANSFORM BOUNDARY</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247301639</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 15:45:27 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247301639</guid>
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         <title>FAULT</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247301936</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 15:46:18 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247301936</guid>
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         <title>ASTHENOSPHERE</title>
         <author>303395</author>
         <link>https://padlet.com/303395/dqtfw0rnmey8/wish/247302310</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 15:47:18 UTC</pubDate>
         <guid>https://padlet.com/303395/dqtfw0rnmey8/wish/247302310</guid>
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