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      <title>Remake of Convection Currents Takeaways  by Joseph Ilk</title>
      <link>https://padlet.com/joseph_ilk/n0grrawccgqq</link>
      <description>After watching the video about convection currents in the mantle, record 3 takeaways that you have about the role the mantle plays in the structure of the Earth. </description>
      <language>en-us</language>
      <pubDate>2017-03-02 14:18:52 UTC</pubDate>
      <lastBuildDate>2017-03-02 16:50:01 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>Daksh Jain</title>
         <author>daksh_jain</author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157385552</link>
         <description><![CDATA[<div>The mantle has convection , and the mantle can get hotter than others. The mantle is kind of like rock which is not solid and not quite liquad. It can heat up some sorts of things which can make convection which gose into a cycle.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:25:49 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157385552</guid>
      </item>
      <item>
         <title>Claire Vargas </title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157385561</link>
         <description><![CDATA[<div>When the substance that the mantle is made out of is colder it is more dense.  The mantle has the power to pull the crust. The mantle is made out of a substance that is not quite a solid and not a total liquid because there are parts in the mantle that are hotter than the other.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:25:50 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157385561</guid>
      </item>
      <item>
         <title>Shayleigh MacDonald</title>
         <author>shayleigh_macdonald</author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157385637</link>
         <description><![CDATA[<div>The mantel has some  convection that turns in a cycle. It isn't a solid but it isn't a liquid. Certain areas of the mantel are hotter than other areas. It is able to move the crust when parts of the mantel heat up and spread throughout the mantel.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:26:02 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157385637</guid>
      </item>
      <item>
         <title>Alex Peretz</title>
         <author>alexander_peretz</author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386188</link>
         <description><![CDATA[<div>The mantel has convection.  The warm water is less dense so it rises when the cold water sinks because it is more dense.  The liquid heats up and moves around more in the mantle.  The water enters a cycle and will eventually all turn one color.<br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:27:22 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386188</guid>
      </item>
      <item>
         <title>Julianna Ratkowski</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386284</link>
         <description><![CDATA[<div>The mantle has convection when it starts off hot in an area then rises and goes around like a cycle. It then gets cool again but once it reaches the hot spot once again it goes back to being warm. This cycle happens just like it does in the real world and the real mantle and layers of the earth. When there is more heat under the mantle it will start to rise and touch the crust. But if it is cold it will stay down because of the heat taking over.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:27:37 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386284</guid>
      </item>
      <item>
         <title>Zack Bugajski</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386309</link>
         <description><![CDATA[<div>the stuff in the mantle has convection when the liquid stuff gets hotter it starts to rise and then it rises up and drags some crust up with it. Then it starts to cools down. Then it sinks and this process repeats over, and over in a circle pattern.. </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:27:40 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386309</guid>
      </item>
      <item>
         <title>Nate Brown</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386761</link>
         <description><![CDATA[<div>The mantle is just like convection as it goes in a cycle. When the liquid gets heated it goes towards the surface and becomes more solid and some goes off to the side and brings some of the crust along with it. Then it will go down and get more liquid and colder and then go back to the heat source to repeat the process just like a cycle.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:28:44 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386761</guid>
      </item>
      <item>
         <title>Evan Berger- The Mantle </title>
         <author>evan_berger</author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386902</link>
         <description><![CDATA[<div>-In the mantle people think that the mantle is like the water demonstration-( how the water is hot and then cold)<br>-When rock in the mantle moves it may move the crust and then causing the plates to move<br>-The more cooling material the area has the less dense the area will be<br><br>In real life the minerals are the things that are moving and not the water</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:29:03 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386902</guid>
      </item>
      <item>
         <title>Ben mertes</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386944</link>
         <description><![CDATA[<div>the mantle has something called convection <br><br>some spots on the mantle is hotter then the other spots.<br><br>when the crust heats up it is able to potential spread around the mantle. And the heats up the mantle some what. <br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:29:10 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157386944</guid>
      </item>
      <item>
         <title>Lauryn Klinger</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387051</link>
         <description><![CDATA[<div>The mantle has convection. The mantle is made up of a substance that is not quite liquid, but not quite solid, so it can move around. When the substance gets warmer, it rises up to the top. Then it cools off, and circles back down to the bottom. It can pull the crust and mantle down with it, which moves the plate. Its like when you heat up the water, and it circles back down, and then heats up again. That is what is happening in the mantle, but it can cause drastic changes in the earths crust.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:29:23 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387051</guid>
      </item>
      <item>
         <title>Alqussam Kayed- The Mantle</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387314</link>
         <description><![CDATA[<div>When the warm water goes into the cold waters direction then it becomes less dense. This is called convection. Also the mantle clearly has convection. When heat spread into something it becomes less dense.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:30:03 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387314</guid>
      </item>
      <item>
         <title>Sophia Kuspa</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387337</link>
         <description><![CDATA[<div>Some spots of the mantel are hotter than other parts. The mantel has something called convection which goes in a cycle . The mantel is able to pull a part he crust if it gets to a very hot temperature.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:30:07 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387337</guid>
      </item>
      <item>
         <title>Ethan Moncada</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387344</link>
         <description><![CDATA[<div>The mantle has convection. The convection helps the plates move. The mantle also has enough power to pull the crust. The mantle is made up of a substance that is like a solid but not really. It is definitely not a liquid.  So there are parts that are in the mantle that are/can be hotter than some of the other parts in the mantle</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:30:08 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387344</guid>
      </item>
      <item>
         <title>Isabelle Liermann</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387502</link>
         <description><![CDATA[<div>The mantle is not quite solid, not quite liquid rock that is often moving because of convection. Some spots in the mantle are hotter than others due to the core, which heats up this semi-melted rock. Because things get hotter when they are less dense, the hot rock which is now liquid floats up to the top which cools the rock down. Cooler, solid rock then moves into that warm spot, gets heated up and melted, and the whole convection process happens again. Because of the force of the rock moving up in some parts and moving down in others, this makes the tectonic plates move.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:30:32 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387502</guid>
      </item>
      <item>
         <title>luke henn</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387687</link>
         <description><![CDATA[<div>The matte has a convection that helps all of the plats move. When the warm water hit with the cold water it becomes more dense. Some spots in the mantal  are hotter then others so it heats up the liquid rock</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:31:03 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387687</guid>
      </item>
      <item>
         <title>Angie Wolke</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387898</link>
         <description><![CDATA[<div>The mantle is not a liquid nor a solid,&nbsp; and it has convection. The convection helps to move the plates. The rocks and minerals are liquids because the heat from the core melted them, then they rise, and then convection takes place, the rocks become solids, and dense, and go down. Then the cycle starts over. And the warm water is less dense than cold water.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:31:30 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157387898</guid>
      </item>
      <item>
         <title>Emma Ulch</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157388133</link>
         <description><![CDATA[<div>The mantle has convection,&nbsp; which helps the plates move. The mantle is not quite liquid, but not solid. &nbsp; Some parts of the mantle are warmer, than other areas.&nbsp; The mantle has enough power to pull the force. </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:32:05 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157388133</guid>
      </item>
      <item>
         <title>Molly Soczka</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157388157</link>
         <description><![CDATA[<div>The mantle heats up the asthenoshpere, but also making hot spots to heat up the liquidy minerals for them to rise then turn more solid and dense.<br><br>The mantle has convection that can make the plates move from the hot spots which starts a cycle between how dense or hot things are.<br><br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:32:09 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157388157</guid>
      </item>
      <item>
         <title>Juan Vazquez</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157388380</link>
         <description><![CDATA[<div>The mantle has convection. It moves in a circle like a cycle. When the mantle heats up it moves upward and then it cools down and it can takes down the crust with it causing many disasters.  </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:32:43 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157388380</guid>
      </item>
      <item>
         <title>Emilio De La Cruz </title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389098</link>
         <description><![CDATA[<div>The mantle&nbsp;is not a liquid but it isn't a solid either. What they call the mantle is a convection. It helps the plates move so it can get the heat around the mantle. When there is only one part that is heat up it will be less dense and </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:34:22 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389098</guid>
      </item>
      <item>
         <title>Devon</title>
         <author>devon_pena</author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389321</link>
         <description><![CDATA[<div>The mantle has convection   <br>it has a cycle where it keeps repeating itself  and it drags the crust </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:34:50 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389321</guid>
      </item>
      <item>
         <title>Bella</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389386</link>
         <description><![CDATA[<div>The mantle has convection in it so, the substance, can not be a solid nor a liquid because of it. The heated part makes the molecules move faster so then they move up and they start to loose its heat-and it comes back down, then the cycle starts again. An it takes the crust with it to creating earthquakes and sink holes</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:35:02 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389386</guid>
      </item>
      <item>
         <title>Manmeet Dhillon</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389787</link>
         <description><![CDATA[<div>The mantle has convection because there is a cycle happening. The mantle is not a solid, though it is not a liquid also. The minerals in the mantle that are by the heated areas are </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:35:59 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389787</guid>
      </item>
      <item>
         <title>Jordan S.</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389818</link>
         <description><![CDATA[<div>The mantle has convection, which can cause it to form new land. The mantle is half and half both a liquid and solid. It also seems to go in a circle as the liquid side of it inside heats cools then heats up once more.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:36:06 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157389818</guid>
      </item>
      <item>
         <title>Aprya Outlaw</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157394715</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:48:16 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157394715</guid>
      </item>
      <item>
         <title>Kendall Kahl</title>
         <author></author>
         <link>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157394722</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2017-03-02 16:48:17 UTC</pubDate>
         <guid>https://padlet.com/joseph_ilk/n0grrawccgqq/wish/157394722</guid>
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