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      <title>Padlet #3 Pangea by Gilbert Rivera</title>
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      <language>en-us</language>
      <pubDate>2018-03-23 16:32:50 UTC</pubDate>
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         <title>Pangea</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245556702</link>
         <description><![CDATA[<div>A former “supercontinent” on the Earth. In the distant past a large landmass, <strong>Pangaea</strong>, included all the present continents, which broke up and drifted apart.</div>]]></description>
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         <pubDate>2018-03-23 16:34:11 UTC</pubDate>
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         <title>Continental Drift</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245558417</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>2018-03-23 16:36:50 UTC</pubDate>
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         <title>Fossil</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245559476</link>
         <description><![CDATA[<div>The remains or impression of a prehistoric organism preserved in petrified form or as a mold or cast in rock.</div>]]></description>
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         <pubDate>2018-03-23 16:38:46 UTC</pubDate>
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         <title>Ice age</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245560260</link>
         <description><![CDATA[<div>An ice<strong><em> age</em></strong> is a period of long-term reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers.</div>]]></description>
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         <pubDate>2018-03-23 16:40:11 UTC</pubDate>
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         <title>Supercontinent</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245562262</link>
         <description><![CDATA[<div>The <strong><em>supercontinent</em></strong> Pangaea is believed to have formed when earlier continental landmasses came together sometime before the Permian Period, staying together until after the Triassic Period, when it broke into the smaller <strong><em>supercontinents</em></strong> Laurasia and Gondwanaland.</div>]]></description>
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         <pubDate>2018-03-23 16:43:24 UTC</pubDate>
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         <title>Alfred Wegener</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245563754</link>
         <description><![CDATA[<div> German geophysicist who proposed the <strong>theory</strong> of continental drift (1880-1930) Synonyms: <strong>Wegener</strong> Example of: geophysicist. a geologist who uses physical principles to study the properties of the earth.</div>]]></description>
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         <pubDate>2018-03-23 16:45:49 UTC</pubDate>
         <guid>https://padlet.com/305158/jln5f4utnzzo/wish/245563754</guid>
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         <title>Landmass</title>
         <author>305158</author>
         <link>https://padlet.com/305158/jln5f4utnzzo/wish/245565122</link>
         <description><![CDATA[<div>A large continuous area of <strong><em>land</em></strong>, as opposed to seas or islands. <strong><em>landmass</em></strong> in <strong><em>Science</em></strong>. <strong><em>landmass</em></strong>. (lānd'mās') A large, continuous area of <strong><em>land</em></strong>, such as a continent or a very large island.</div>]]></description>
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         <pubDate>2018-03-23 16:48:04 UTC</pubDate>
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