<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>Plate tectonics by Ma&#39;Kel Anderson</title>
      <link>https://padlet.com/3100241/ir6o88c6f1co</link>
      <description>Made with a dash of wit AND MY HANDS!!!!!!!!!!!!!</description>
      <language>en-us</language>
      <pubDate>2018-03-29 17:23:12 UTC</pubDate>
      <lastBuildDate>2025-10-01 03:54:15 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>plate tectonics</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247340799</link>
         <description><![CDATA[<div>a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates that move slowly over the underlying mantle.</div>]]></description>
         <enclosure url="http://3.bp.blogspot.com/-VNAC-cPFOTE/Ud0IIp3btmI/AAAAAAAAFtk/SO5trSqjUzY/s1600/subduction+1.jpg" />
         <pubDate>2018-03-29 17:26:36 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247340799</guid>
      </item>
      <item>
         <title>continental drift </title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247341079</link>
         <description><![CDATA[<div>the gradual movement of the continents across the earth's surface through geological time.</div>]]></description>
         <enclosure url="http://2.bp.blogspot.com/-FiMj-MKvT1Y/Ty1PbBEHE9I/AAAAAAAAAE4/SzCFLGpw3ao/s1600/continental-drift.jpg" />
         <pubDate>2018-03-29 17:27:16 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247341079</guid>
      </item>
      <item>
         <title>subduction</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247341741</link>
         <description><![CDATA[<div>the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.</div>]]></description>
         <enclosure url="https://lh3.googleusercontent.com/-WqKtGNo8bko/TXpHtofuooI/AAAAAAAAAmk/6Ajl9MOzHS0/s1600/Earthquake_subduction+zone.gif" />
         <pubDate>2018-03-29 17:28:52 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247341741</guid>
      </item>
      <item>
         <title>Mid-atlantic ridge</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247341926</link>
         <description><![CDATA[<div>a north-south suboceanic ridge in the Atlantic Ocean from Iceland to Antarctica on whose crest are several groups of islands; shown by plate tectonics to be the axis along which North America has split away from Eurasia, and along which South America has split away from Africa. </div>]]></description>
         <enclosure url="http://www.crystalinks.com/midatlanticridgenoaa.jpg" />
         <pubDate>2018-03-29 17:29:19 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247341926</guid>
      </item>
      <item>
         <title>ring of fire</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247342613</link>
         <description><![CDATA[<div>The <strong>Ring of Fire</strong> is a major area in the basin of the Pacific Ocean where a large number of earthquakes and volcanic eruptions occur. In a 40,000 km (25,000 mi) horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and plate movements.</div><div><br></div>]]></description>
         <enclosure url="https://upload.wikimedia.org/wikipedia/commons/thumb/5/52/Pacific_Ring_of_Fire.svg/1280px-Pacific_Ring_of_Fire.svg.png" />
         <pubDate>2018-03-29 17:31:05 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247342613</guid>
      </item>
      <item>
         <title>convergent boundary</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247343056</link>
         <description><![CDATA[<div><strong>convergent</strong> plate <strong>boundary</strong>. (kən-vûr'jənt) A tectonic<strong>boundary</strong> where two plates are moving toward each other. If the two plates are of equal density, they usually push up against each other, forming a mountain chain. If they are of unequal density, one plate usually sinks beneath the other in a subduction zone.</div>]]></description>
         <enclosure url="http://www.tasaclips.com/illustrations/Convergent_Boundary.jpg" />
         <pubDate>2018-03-29 17:32:09 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247343056</guid>
      </item>
      <item>
         <title>divergent boundary </title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247343353</link>
         <description><![CDATA[<div><strong>divergent</strong> plate <strong>boundary</strong> in Science. <strong>divergent</strong> plate<strong>boundary</strong>. (dĭ-vûr'jənt) A tectonic <strong>boundary</strong> where two plates are moving away from each other and new crust is forming from magma that rises to the Earth's surface between the two plates.</div>]]></description>
         <enclosure url="http://study.com/cimages/videopreview/study-divergent_115709.jpg" />
         <pubDate>2018-03-29 17:33:01 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247343353</guid>
      </item>
      <item>
         <title>transform boundary </title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247344109</link>
         <description><![CDATA[<div><strong>Transform boundaries</strong> are places where plates slide sideways past each other. At <strong>transform boundaries </strong>lithosphere is neither created nor destroyed. Many <strong>transform boundaries</strong> are found on the sea floor, where they connect segments of diverging mid-ocean ridges. California's San Andreas fault is a <strong>transform boundary</strong>.</div>]]></description>
         <enclosure url="http://academic.brooklyn.cuny.edu/geology/grocha/plates/images/transform1.jpg" />
         <pubDate>2018-03-29 17:34:48 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247344109</guid>
      </item>
      <item>
         <title>fault</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247344456</link>
         <description><![CDATA[<div><br>(of a rock formation) be broken by a fault or faults</div>]]></description>
         <enclosure url="http://geotripperimages.com/images/DSC01776%20Normal%20fault%20in%20Mosaic%20Canyon.jpg" />
         <pubDate>2018-03-29 17:35:32 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247344456</guid>
      </item>
      <item>
         <title>asthenosphere</title>
         <author>3100241</author>
         <link>https://padlet.com/3100241/ir6o88c6f1co/wish/247344754</link>
         <description><![CDATA[<div>the upper layer of the earth's mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur.</div>]]></description>
         <enclosure url="https://upload.wikimedia.org/wikipedia/commons/thumb/8/8a/Earth-cutaway-schematic-english.svg/1200px-Earth-cutaway-schematic-english.svg.png" />
         <pubDate>2018-03-29 17:36:17 UTC</pubDate>
         <guid>https://padlet.com/3100241/ir6o88c6f1co/wish/247344754</guid>
      </item>
   </channel>
</rss>
