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      <title>PADLET 4 PLATE TECTONICS by Karen Cruz</title>
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      <description>period 1    
3-29-18</description>
      <language>en-us</language>
      <pubDate>2018-03-29 15:19:52 UTC</pubDate>
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      <webMaster>hello@padlet.com</webMaster>
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         <title>ASTHENOSPHERE</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247291473</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 15:22:17 UTC</pubDate>
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         <title>FAULT</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247292045</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 15:23:32 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247292045</guid>
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         <title>TRANSFORM BOUNDARY</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247292563</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 15:24:40 UTC</pubDate>
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         <title>DIVERGENT BOUNDARY </title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247293637</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 15:26:27 UTC</pubDate>
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         <title>CONVERGENT BOUNDARY</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247294242</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><div><br></div>]]></description>
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         <pubDate>2018-03-29 15:27:55 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247294242</guid>
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      <item>
         <title>.RING OF FIRE</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247295464</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 15:30:38 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247295464</guid>
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         <title>MID ATLANTIC RIDGE</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247295940</link>
         <description><![CDATA[<div><br></div><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>]]></description>
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         <pubDate>2018-03-29 15:31:52 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247295940</guid>
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         <title>SUBDUCTION</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247296481</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 15:33:20 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247296481</guid>
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         <title>CONTINENTAL DRIFT</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247297316</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 15:34:38 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247297316</guid>
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         <title>PLATE TECTONICS</title>
         <author>304503</author>
         <link>https://padlet.com/304503/2kwlmhf4x7tq/wish/247297719</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 15:35:41 UTC</pubDate>
         <guid>https://padlet.com/304503/2kwlmhf4x7tq/wish/247297719</guid>
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