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      <title>Ch. 4.5 Plate Tectonics by </title>
      <link>https://padlet.com/yvonne_su/platetectonics</link>
      <description>What are three types of plate boundaries? What happens in each?</description>
      <language>en-us</language>
      <pubDate>2016-10-16 21:11:07 UTC</pubDate>
      <lastBuildDate>2026-02-09 03:27:51 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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      <item>
         <title>Plate Tectonics</title>
         <author>yvonne_su</author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/130999556</link>
         <description><![CDATA[<div>What happens when two oceanic or continental plates meet?</div>]]></description>
         <enclosure url="http://www.pmfias.com/wp-content/uploads/2015/12/Plate-Tectonics-Interaction-of-Plates.jpg" />
         <pubDate>2016-10-16 21:14:56 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/130999556</guid>
      </item>
      <item>
         <title>Sirtiney C.</title>
         <author>1367470183</author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131193878</link>
         <description><![CDATA[<div>At some convergent boundaries, an <strong>oceanic plate</strong> collides with a <strong>continental plate</strong>.<strong>Oceanic crust</strong> tends to be denser and thinner than <strong>continental crust</strong>, so the denser <strong>oceanic crust</strong> gets bent and pulled under, or subducted, beneath the lighter and thicker <strong>continental crust</strong>. This forms what is called a subduction zone.<br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:49:38 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131193878</guid>
      </item>
      <item>
         <title>Warnest</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131194942</link>
         <description><![CDATA[<div>oceanic crust tends to be denser and thinner than contintal  crust so the denser oceanic crust gets bent and pulled under.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:51:42 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131194942</guid>
      </item>
      <item>
         <title>Sirtiney</title>
         <author>1367470183</author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131195148</link>
         <description><![CDATA[<div>when two oceanic or contineal plates meet it </div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:52:02 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131195148</guid>
      </item>
      <item>
         <title>Daniel</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131195548</link>
         <description><![CDATA[<div>One type of plate boundaries is faults and faults breaks in Earth's crust where rocks have slipped past each other. Another type of plate boundary is spreading boundary and spreading boundary is the place where two plates move apart or diverge. The last type of plate boundary is colliding boundary and colliding boundary is the place where two plates come together or converge.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:52:52 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131195548</guid>
      </item>
      <item>
         <title>Samuel</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131195726</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:53:14 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131195726</guid>
      </item>
      <item>
         <title>Eric&amp;nbsp;</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131195856</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:53:30 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131195856</guid>
      </item>
      <item>
         <title>Abel</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131196015</link>
         <description><![CDATA[<div>Three types of plate boundaries are     the  spreading,  the plate, and crust.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:53:50 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131196015</guid>
      </item>
      <item>
         <title>Valeria Vilches</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131196317</link>
         <description><![CDATA[<div><em><br></em>There are three types of plate boundaries. One of those types of plate boundaries are spreading boundaries. The spreading boundary is the place where two plates move apart, or diverge. Another type of plate boundaries is colliding boundaries. Colliding boundaries is the place where two plates come together or converge. The last one is the sliding boundaries. Sliding boundaries is a place where two plates slide past each other, moving in opposite directions.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:54:34 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131196317</guid>
      </item>
      <item>
         <title>Brianna </title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131197202</link>
         <description><![CDATA[<div>divergent, convergent, and transform <strong>plate boundaries</strong>. This image shows the <strong>three</strong> main <strong>types of plate boundaries</strong>: divergent, convergent, and transform</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 15:56:21 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131197202</guid>
      </item>
      <item>
         <title>Samantha Alfaro</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131199569</link>
         <description><![CDATA[<div>The three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries.In the spreading boundary two plates move apart, or diverge.During the colliding boundary two plates come together, or converge.As you can see the colliding and spreading bounderies are simalar, the only difference is that one of them pulls apart and the other comes together. More over, during a sliding boundary two plates slip past each other and move in the opposite direction. In conclusion, earthquakes usually happen around these three bounderies.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:02:35 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131199569</guid>
      </item>
      <item>
         <title>Marianne</title>
         <author>1367469872</author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131199798</link>
         <description><![CDATA[<div>the two types of plate boundaries are continental plate, and oceanic plate. </div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:03:08 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131199798</guid>
      </item>
      <item>
         <title>Giselle Santiago</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131199823</link>
         <description><![CDATA[<div>There are three types of plate boundaries. One of those types of plate boundaries are spreading boundaries. The spreading boundary is the place where two plates move apart, or diverge. Another type of  plate boundaries is colliding boundaries. Colliding boundaries is the place where two plates come together or converge. The last one is the sliding boundaries. Sliding boundaries is a place where two plates slide past each other, moving in opposite directions.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:03:13 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131199823</guid>
      </item>
      <item>
         <title>Ryan</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131200437</link>
         <description><![CDATA[<div>At some convergent boundaries, an oceanic plate collides with a continental plate.oceanic crust tends to be denser and thinner than continental crust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thick continental crust. This forms what is called a subduction zone.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:04:28 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131200437</guid>
      </item>
      <item>
         <title>Rubi</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131201226</link>
         <description><![CDATA[<div>The three types of plate boundaries  are spreading boundary , colliding boundary , and sliding boundary.What happens in each of the boundaries is in spreading boundary is when two plates move apart , or diverge. Colliding boundary is where two plates come together , or converge. Lastly sliding boundary is where two plates slip past each other moving the opposite directions.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:06:18 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131201226</guid>
      </item>
      <item>
         <title>kasandra</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131201457</link>
         <description><![CDATA[<div>there are two types of boundaries&nbsp; they are&nbsp;Spreading </div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:06:54 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131201457</guid>
      </item>
      <item>
         <title>Jasmine</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131201467</link>
         <description><![CDATA[<div>There are three types of plate boundries are speading boundries ,cold boundries and sliding boundries.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:06:54 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131201467</guid>
      </item>
      <item>
         <title>Zaira</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131201510</link>
         <description><![CDATA[<div>three types of boudering are speading ,colliding and slidingbounderings</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:07:00 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131201510</guid>
      </item>
      <item>
         <title>Samantha Bello</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131201810</link>
         <description><![CDATA[<div>Three types of plate boundaries are<br>spreading boundaries, colliding boundaries, and sliding boundaries.       Spreading boundaries happen when the place where two plates move apart. Colliding boundaries happen when the place of two plates come together. Sliding boundaries happen when two plates slip past each other and they move in the opposite direction.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:07:39 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131201810</guid>
      </item>
      <item>
         <title>Thomas</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131201903</link>
         <description><![CDATA[<div>The three types of plate boundaries         are spreading boundary,colliding boundary, and sliding boundary.Spreading boundary occurs at the mid-west and if it develops on land, two slabs of Earth's crust slides apart.Colliding boundary is when the two plates determine which one comes out from the top.Sliding boundary is when two plates are carrying oceanic crust meets at the trench, the plate that is less dense divers under the other plate and returns to the mantel.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:07:51 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131201903</guid>
      </item>
      <item>
         <title>Zion Davis</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131202098</link>
         <description><![CDATA[<div>Three types of plate boundaries<br>&nbsp;are spreading, colliding,&nbsp; and sliding boundaries.&nbsp;</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:08:18 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131202098</guid>
      </item>
      <item>
         <title>hi rudi</title>
         <author>1367470183</author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131202135</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:08:22 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131202135</guid>
      </item>
      <item>
         <title>Damian A.</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131202233</link>
         <description><![CDATA[<div><br></div><div>There are <strong>three kinds of plate</strong> tectonic <strong>boundaries</strong> divergent, convergent, and transform <strong>plate boundaries</strong>. This image shows the <strong>three</strong> main <strong>types of plate boundaries</strong> divergent, convergent, and transform</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:08:35 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131202233</guid>
      </item>
      <item>
         <title>Steven </title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131202368</link>
         <description><![CDATA[<div>There a three types of plate boundaries one of them are spreading boundaries&nbsp;</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:08:50 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131202368</guid>
      </item>
      <item>
         <title>Michael.R</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131202977</link>
         <description><![CDATA[<div>The three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. The place where two plates move apart, or diverge, is called a spreading boundary. The place where two plates come together, or converge, is a colliding boundary. A sliding boundary is a place where two plates slip past each other, moving in opposite directions. </div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:10:11 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131202977</guid>
      </item>
      <item>
         <title>Natalie Janean Contreras          The three types of plate boundaries are colliding. Anther one is sliding. The last one is spreading.</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131203178</link>
         <description><![CDATA[<div><br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:10:42 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131203178</guid>
      </item>
      <item>
         <title>Sergio Hermosillo</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131204597</link>
         <description><![CDATA[<div>There are three types of plate boundaries. One of those types of plate boundaries are spreading boundaries.oceanic crust tends to be denser and thinner than continental crust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thick continental crust.. Another type of plate boundary is spreading boundary and spreading boundary is the place where two plates move apart or diverge.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:13:51 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131204597</guid>
      </item>
      <item>
         <title>Isabella Gutierrez</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131204851</link>
         <description><![CDATA[<div>There are three types of plate boundaries. The first type is the spreading boundary. The spreading boundary is the place where two plates move apart, or diverge. The second type of plate boundary is colliding boundary. The colliding boundary is when two plates come together, or converge. The last type is sliding boundary. The sliding boundary is a place where two plates slip past each other, moving in opposite directions. Earthquakes  occur frequently along these boundaries.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:14:30 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131204851</guid>
      </item>
      <item>
         <title>Carlos R.</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131205224</link>
         <description><![CDATA[<div>There are three types of plate boundaries. One of those types of plate boundaries are spreading boundaries.oceanic crust tends to be denser and thinner than continental crust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thick continental crust.. Another type of plate boundary is spreading boundary and spreading boundary is the place where two plates move apart or diverge.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:15:20 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131205224</guid>
      </item>
      <item>
         <title>Ramon Arguelles</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131205485</link>
         <description><![CDATA[<div>there are at least three tectonic bounderis.A Tectonic plates is the geological theory that states convection currents in the mantle.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:15:56 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131205485</guid>
      </item>
      <item>
         <title>Eric</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131205774</link>
         <description><![CDATA[<div>There are three types of plate boundaries. One of those types of plate boundaries are spreading boundaries. The spreading boundary is the place where two plates move apart, or diverge. Another type of plate boundaries is colliding boundaries. Colliding boundaries is the place where two plates come together or converge. The last one is the sliding boundaries. Sliding boundaries is a place where two plates slide past each other, moving in opposite directions.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:16:29 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131205774</guid>
      </item>
      <item>
         <title>Samuel</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131207036</link>
         <description><![CDATA[<div>There are three types of plate boundaries. One of those types of plate boundaries are spreading boundaries.oceanic crust tends to be denser and thinner than continental crust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thick continental crust.. Another type of plate boundary is spreading boundary and spreading boundary is the place where two plates move apart or diverge.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:19:00 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131207036</guid>
      </item>
      <item>
         <title>Luis Garcia</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131210600</link>
         <description><![CDATA[<div>The three plates of boundaries.The first one is spreading boundaries.the other one is&nbsp; colliding boundary and the sliding boundary it is a place where two plates slip past each other moving in opposite directions.<br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:24:31 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131210600</guid>
      </item>
      <item>
         <title>monse</title>
         <author></author>
         <link>https://padlet.com/yvonne_su/platetectonics/wish/131213478</link>
         <description><![CDATA[<div><br></div><div>There are <strong>three kinds of plate</strong> tectonic <strong>boundaries</strong>: divergent, convergent, and transform <strong>plate boundaries</strong>. This image shows the <strong>three</strong> main <strong>types of plate boundaries</strong>: divergent, convergent, and transform.</div>]]></description>
         <enclosure url="" />
         <pubDate>2016-10-17 16:30:35 UTC</pubDate>
         <guid>https://padlet.com/yvonne_su/platetectonics/wish/131213478</guid>
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