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      <title>Plate Boundaries  by Molly Marshall</title>
      <link>https://padlet.com/molly_marshall/7lh1n0fgukpb</link>
      <description>Made with eyes on the prize</description>
      <language>en-us</language>
      <pubDate>2018-03-09 14:45:09 UTC</pubDate>
      <lastBuildDate>2025-10-24 12:56:53 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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      <item>
         <title>Continental-Continental</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241873182</link>
         <description><![CDATA[<div>Convection Currents pull two continental plates apart. Then magma rises in the middle, cools, hardens, and sinks forming a valley. Eventually being filled with ocean water, which then makes it turn into seafloor spreading. </div>]]></description>
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         <pubDate>2018-03-14 13:47:40 UTC</pubDate>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241895048</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 14:21:28 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241895048</guid>
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      <item>
         <title>Ocean-Ocean</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241896730</link>
         <description><![CDATA[<div>Convection Currents pull two oceanic plates apart. Hot less dense magma rises in the middle, cools, and hardens, pushing the old seafloor out.<br><br></div>]]></description>
         <enclosure url="https://youtu.be/_RZpb85nChw" />
         <pubDate>2018-03-14 14:23:37 UTC</pubDate>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241924897</link>
         <description><![CDATA[￼]]></description>
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         <pubDate>2018-03-14 15:05:03 UTC</pubDate>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241925888</link>
         <description><![CDATA[￼]]></description>
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         <pubDate>2018-03-14 15:06:22 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241925888</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241928631</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://geology8b-9.wikispaces.com/file/view/d.jpg/88987877/d.jpg" />
         <pubDate>2018-03-14 15:10:17 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241928631</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241931379</link>
         <description><![CDATA[<div>Convection Currents move two plates (ocean or continental) in opposite directions or in the same direction at different speeds.</div>]]></description>
         <enclosure url="https://youtu.be/KGbUfMJkt6c" />
         <pubDate>2018-03-14 15:14:21 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241931379</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241936453</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 15:22:23 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241936453</guid>
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      <item>
         <title>Ocean-Continental </title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241937703</link>
         <description><![CDATA[<div>Convection Currents cause denser ocean plates to dive under continental plate. Ocean plate melts, forms magma and magma rises forming volcanoes.</div>]]></description>
         <enclosure url="https://youtu.be/nMODToEYsaM" />
         <pubDate>2018-03-14 15:24:21 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241937703</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241940847</link>
         <description><![CDATA[]]></description>
         <enclosure url="http://www.passmyexams.co.uk/GCSE/physics/images/oceanic_continental.gif" />
         <pubDate>2018-03-14 15:29:19 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241940847</guid>
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      <item>
         <title>Ocean-Ocean</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241943213</link>
         <description><![CDATA[<div>Convection Currents cause two ocean plates to move toward each other. One plate is always older, cooler and denser , so the one that is denser will dive under the less dense ocean plate</div>]]></description>
         <enclosure url="https://youtu.be/BgeYflWTSXo" />
         <pubDate>2018-03-14 15:33:10 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241943213</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241946087</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 15:36:51 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/241946087</guid>
      </item>
      <item>
         <title>Continental-Continental</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242104188</link>
         <description><![CDATA[<div>Convection Currents cause two continental plates to move towards each other. Both plates are the same density, therefore causing no subduction to occur. As the two plates collide, then they start to crumble up and create mountains.</div>]]></description>
         <enclosure url="https://youtu.be/_fGz0eWp59Y" />
         <pubDate>2018-03-14 20:35:41 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242104188</guid>
      </item>
      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242108352</link>
         <description><![CDATA[<div>Divergent Boundaries are two plates that move away from each other.</div>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-14 20:49:47 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242108352</guid>
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      <item>
         <title>Fun Facts About some Divergent Boundaries</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242109161</link>
         <description><![CDATA[<ul><li>Iceland has a divergent plate boundary running through it.</li><li>The Mid-Atlantic Ridge is one example of a divergent ocean-ocean plate boundary.</li><li>The Great Rift Valley is an example of a divergent continental-continental plate boundary</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-14 20:52:48 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242109161</guid>
      </item>
      <item>
         <title>Fun Facts About some Transform Boundaries.</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242111537</link>
         <description><![CDATA[<div>The San Andreas Fault is one example of a transform boundary.</div>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-14 21:01:34 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242111537</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242113231</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:08:38 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242113231</guid>
      </item>
      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242113470</link>
         <description><![CDATA[<div>Convergent Boundaries are two plates that move towards each other</div>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-14 21:09:43 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242113470</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242113882</link>
         <description><![CDATA[<div>Transform Boundaries are when two plates slide past each other.</div>]]></description>
         <enclosure url="" />
         <pubDate>2018-03-14 21:11:31 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242113882</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242114774</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:15:20 UTC</pubDate>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115066</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:16:24 UTC</pubDate>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115246</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:17:15 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115246</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115502</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:18:14 UTC</pubDate>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115724</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:19:09 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115724</guid>
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      <item>
         <title></title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115984</link>
         <description><![CDATA[]]></description>
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         <pubDate>2018-03-14 21:20:07 UTC</pubDate>
         <guid>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242115984</guid>
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      <item>
         <title>Fun Facts About some Convergent Boundaries</title>
         <author>molly_marshall</author>
         <link>https://padlet.com/molly_marshall/7lh1n0fgukpb/wish/242116128</link>
         <description><![CDATA[<ul><li>The Andes Mountains are an example of a ocean-continental convergent boundary.</li><li>The Aleutain Islands are an example of a ocean-ocean convergent boundary</li><li>The Himalayan Mountains are an example of a continental-continental convergent boundary</li></ul>]]></description>
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         <pubDate>2018-03-14 21:20:38 UTC</pubDate>
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