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      <title>Padlet #4- Plate Tectonics by Lisbeth Cruz Rivera</title>
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      <language>en-us</language>
      <pubDate>2018-03-29 17:15:34 UTC</pubDate>
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         <title>Plate Tectonics</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247336972</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 17:17:04 UTC</pubDate>
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         <title>Continental Drift</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247337975</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 17:19:41 UTC</pubDate>
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         <title>Subduction</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247338526</link>
         <description><![CDATA[<div>he 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 17:21:13 UTC</pubDate>
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         <title>Mid-Atlantic Ridge</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247339201</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 17:22:47 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247339201</guid>
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         <title>Ring of fire</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247339891</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 17:24:37 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247339891</guid>
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         <title>Convergent boundary</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247340622</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 17:26:07 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247340622</guid>
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         <title>Divergent boundary</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247341271</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 17:27:42 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247341271</guid>
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         <title>Transform boundary</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247341850</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 17:29:08 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247341850</guid>
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         <title>Fault</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247342339</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 17:30:26 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247342339</guid>
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         <title>Asthenosphere</title>
         <author>304803</author>
         <link>https://padlet.com/304803/yswi19fsa500/wish/247342776</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 17:31:30 UTC</pubDate>
         <guid>https://padlet.com/304803/yswi19fsa500/wish/247342776</guid>
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