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      <title>Lecture blog by Zev Jagalur</title>
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      <description>PLEASE TELL ME THIS IS SATISFACTORY!( GRIN)</description>
      <language>en-us</language>
      <pubDate>2017-04-26 20:12:00 UTC</pubDate>
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         <title>Blog on lecture</title>
         <author>zev_jagalur</author>
         <link>https://padlet.com/zev_jagalur/hl2jjoyk5zcr/wish/168494230</link>
         <description><![CDATA[<div><br>Today, in the lecture we learned that :&nbsp; &nbsp;<br>continental drift&nbsp; is a theory that the continents slowly move over time<br>At one time, long ago,&nbsp; the continents were together in one giant landmass. The supercontinent is a large landmass made up of all or most of the continental blocks. The name of the supercontinent was Pangea. It was the supercontinent that existed during the late Paleozoic, early Mesozoic period.&nbsp; It assembled about 335 million years ago. It began to&nbsp; break&nbsp; apart about 175 million years ago.<br>Alfred Wegener - cartographer who first proposed Continental drift- but he was dismissed and ridiculed for being a crackpot. He got lost and (we think) died trying to prove his theories in the Arctic.<br>Pangaea slowly&nbsp; broke apart into the world we know today.<br>EVIDENCE OF CONTINENTAL DRIFT:<br>1.Puzzle fit of Continents(ex. South America&nbsp; fits nicely into&nbsp; Africa)<br>2. Fossil Correlation- land based fossils&nbsp; found on widely separate continents<br>3.Glacial Evidence found in Currently WARM climate areas<br>4. MOUNTAIN RANGES across OCEANS OCEANS OCEANS<br>5.Direct Measurement from Space</div>]]></description>
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         <pubDate>2017-04-26 20:13:55 UTC</pubDate>
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