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      <title>plate tectonics by Roberto Jara</title>
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      <description>Made with big dreams</description>
      <language>en-us</language>
      <pubDate>2018-03-29 16:05:31 UTC</pubDate>
      <lastBuildDate>2018-03-29 16:12:23 UTC</lastBuildDate>
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         <title>plate tectonics</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247310154</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 16:06:39 UTC</pubDate>
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         <title>continental drift</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247310500</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 16:07:33 UTC</pubDate>
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         <title>subduction</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247310740</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 16:08:06 UTC</pubDate>
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         <title>Mid-Atlantic Ridge</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247310949</link>
         <description><![CDATA[<div>he 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.he 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 16:08:42 UTC</pubDate>
         <guid>https://padlet.com/303968/8jeai2rc8mhj/wish/247310949</guid>
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         <title>Ring of fire</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247311192</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 16:09:19 UTC</pubDate>
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         <title>convergent boundary</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247311451</link>
         <description><![CDATA[<div>The Cascade Mountain Range is a line of volcanoes above the melting oceanic plate. The Andes Mountain Range of western South America is another example of a convergent boundary between an oceanic and continental plate. Here the Nazca Plate is subducting beneath the South American plate</div>]]></description>
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         <pubDate>2018-03-29 16:09:56 UTC</pubDate>
         <guid>https://padlet.com/303968/8jeai2rc8mhj/wish/247311451</guid>
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         <title>divergent boundary</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247311625</link>
         <description><![CDATA[<div>In plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) 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 16:10:27 UTC</pubDate>
         <guid>https://padlet.com/303968/8jeai2rc8mhj/wish/247311625</guid>
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         <title>Transform boundary</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247311809</link>
         <description><![CDATA[<div>Transform boundaries are places where plates slide sideways past each other. At transform boundaries lithosphere is neither created nor destroyed. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. California's San Andreas fault is a transform boundary</div>]]></description>
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         <pubDate>2018-03-29 16:10:57 UTC</pubDate>
         <guid>https://padlet.com/303968/8jeai2rc8mhj/wish/247311809</guid>
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      <item>
         <title>Fault</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247312100</link>
         <description><![CDATA[<div>A fault is a fracture along which the blocks of crust on either side have moved relative to one another parallel to the fracture. Strike-slip, normal, and reverse faults. A reverse fault with a small dip angle is called a thrust fault.</div>]]></description>
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         <pubDate>2018-03-29 16:11:44 UTC</pubDate>
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         <title>asthenosphere</title>
         <author>303968</author>
         <link>https://padlet.com/303968/8jeai2rc8mhj/wish/247312268</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 16:12:12 UTC</pubDate>
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