<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>Padlet 4- Plate tectonics  by </title>
      <link>https://padlet.com/304971/gytzm3kif53b</link>
      <description>Made with a wink and a smile</description>
      <language>en-us</language>
      <pubDate>2018-03-29 16:21:33 UTC</pubDate>
      <lastBuildDate>2025-12-31 16:51:10 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>Plate tectonics</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247316323</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://earthguide.ucsd.edu/eoc/teachers/t_tectonics/images/tectonic_plates/tectonic_plates_lg.png" />
         <pubDate>2018-03-29 16:22:27 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247316323</guid>
      </item>
      <item>
         <title>Continental Drift</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247316458</link>
         <description><![CDATA[<div>the gradual movement of the continents across the earth's surface through geological time.</div>]]></description>
         <enclosure url="https://62e528761d0685343e1c-f3d1b99a743ffa4142d9d7f1978d9686.ssl.cf2.rackcdn.com/files/62631/area14mp/cysfbpyv-1414063343.jpg" />
         <pubDate>2018-03-29 16:22:46 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247316458</guid>
      </item>
      <item>
         <title>Subduction</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247316679</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 16:22:57 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247316679</guid>
      </item>
      <item>
         <title>Mid-Atlantic Ridge </title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317023</link>
         <description><![CDATA[<div>The Mid-Atlantic<strong> </strong>Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world.</div><div><br></div>]]></description>
         <enclosure url="http://media.web.britannica.com/eb-media/25/129925-004-3C24B9B2.gif" />
         <pubDate>2018-03-29 16:23:04 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317023</guid>
      </item>
      <item>
         <title>Ring of fire</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317148</link>
         <description><![CDATA[<div>The Ring<strong> </strong>of<strong> </strong>Fire 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>]]></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 16:23:22 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317148</guid>
      </item>
      <item>
         <title>Convergent boundary</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317235</link>
         <description><![CDATA[<div>A tectonic boundary 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 16:23:34 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317235</guid>
      </item>
      <item>
         <title>Divergent boundary</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317384</link>
         <description><![CDATA[<div>divergent plate boundary in Science. divergent plate boundary.  A tectonic boundary 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 16:23:53 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317384</guid>
      </item>
      <item>
         <title>Transform boundary</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317478</link>
         <description><![CDATA[<div>The final type of boundary is one where the two plates slide against each other in a sideways motion. These boundaries between plates is referred to as transform<strong> </strong>boundaries. As two plates slide past one another, in a transform<strong> </strong>boundary, neither plate is added to at the boundary, nor destroyed.</div>]]></description>
         <enclosure url="http://academic.brooklyn.cuny.edu/geology/grocha/plates/images/transform1.jpg" />
         <pubDate>2018-03-29 16:24:07 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317478</guid>
      </item>
      <item>
         <title>Fault</title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317515</link>
         <description><![CDATA[<div>a crack in the Earth's crust. Typically, faults<strong> </strong>are associated with, or form, the boundaries between Earth's tectonic plates. In an active fault, the pieces of the Earth's crust along a fault move over time.</div>]]></description>
         <enclosure url="http://www.sanandreasfault.org/4020_A.jpg" />
         <pubDate>2018-03-29 16:24:12 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317515</guid>
      </item>
      <item>
         <title>Asthenosphere </title>
         <author>304971</author>
         <link>https://padlet.com/304971/gytzm3kif53b/wish/247317554</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 16:24:16 UTC</pubDate>
         <guid>https://padlet.com/304971/gytzm3kif53b/wish/247317554</guid>
      </item>
   </channel>
</rss>
