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      <title>padlet 4 - plate tectonics by Jose Calderon</title>
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      <description>Made with a dash of wit</description>
      <language>en-us</language>
      <pubDate>2018-03-29 19:05:14 UTC</pubDate>
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         <title>plate tectonics </title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247375907</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 19:06:27 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247375907</guid>
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         <title>Continental Drift </title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247376351</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 19:08:05 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247376351</guid>
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         <title>subduction</title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247376903</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 19:09:53 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247376903</guid>
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         <title>mid-atlantic ridge</title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247377042</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 19:10:23 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247377042</guid>
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         <title>ring of five </title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247377393</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 19:11:48 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247377393</guid>
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         <title>convergent boundary </title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247377464</link>
         <description><![CDATA[<div>In plate tectonics, a <strong>convergent boundary</strong>, 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 19:12:06 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247377464</guid>
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         <title>divergent boundary</title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247377699</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 19:12:59 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247377699</guid>
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         <title>transform boundary </title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247378067</link>
         <description><![CDATA[<div><strong>Transform</strong> Plate <strong>Boundaries</strong> are locations where two plates slide past one another. The fracture zone that forms a <strong>transform</strong> plate <strong>boundary</strong> is known as a<strong>a transform fault</strong>. Most <strong>transform faults</strong> are found in the ocean basin and connect offsets in the mid-ocean ridges.</div>]]></description>
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         <pubDate>2018-03-29 19:14:30 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247378067</guid>
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         <title>asthenosphere</title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247378375</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 19:15:47 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247378375</guid>
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         <title>Fault</title>
         <author>304800</author>
         <link>https://padlet.com/304800/1zginjmu0rzn/wish/247384556</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 19:39:00 UTC</pubDate>
         <guid>https://padlet.com/304800/1zginjmu0rzn/wish/247384556</guid>
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