<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>padlet 4 plate techtonics by Hector Aranda</title>
      <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l</link>
      <description></description>
      <language>en-us</language>
      <pubDate>2018-03-29 17:45:06 UTC</pubDate>
      <lastBuildDate>2025-04-29 19:13:15 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>plate techtonics</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247349505</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><div><br></div><div><br></div><div><br></div>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/217613188/eaa6cf1a84cabb3e9b0becb1d376da3d/download__4_.jpeg" />
         <pubDate>2018-03-29 17:48:00 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247349505</guid>
      </item>
      <item>
         <title>continental drift</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247351714</link>
         <description><![CDATA[<ol><li>the gradual movement of the continents across the earth's surface through geological time.</li></ol><div><br></div><div><br></div><div><br></div>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/217613188/db8b6db5da181d27b690f7c00c36915d/download__5_.jpeg" />
         <pubDate>2018-03-29 17:53:55 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247351714</guid>
      </item>
      <item>
         <title>subduction</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247351833</link>
         <description><![CDATA[<ol><li>the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.</li></ol><div><br></div><div><br></div>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/217613188/298462d576a9f6f26e546adbcf93e54d/download__2_.png" />
         <pubDate>2018-03-29 17:54:16 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247351833</guid>
      </item>
      <item>
         <title>mid atlantic ridge</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247352150</link>
         <description><![CDATA[<div>The Mid-Atlantic Ridge 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>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/217613188/010277200a6b4cbbc4521bfebf4f8a10/download__3_.jpeg" />
         <pubDate>2018-03-29 17:55:06 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247352150</guid>
      </item>
      <item>
         <title>ring of fire</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247352407</link>
         <description><![CDATA[<div>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://padlet-uploads.storage.googleapis.com/217613188/445064605319ac88e2c641c9af4c9482/download__1_.png" />
         <pubDate>2018-03-29 17:55:47 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247352407</guid>
      </item>
      <item>
         <title>convergent boundary</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247352906</link>
         <description><![CDATA[<div>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="https://padlet-uploads.storage.googleapis.com/217613188/1ab1bd81a378db79a12fd84f484b6892/download__2_.jpeg" />
         <pubDate>2018-03-29 17:57:12 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247352906</guid>
      </item>
      <item>
         <title>divergent boundary</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247353254</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="https://padlet-uploads.storage.googleapis.com/217613188/3fde85306d50c47a3372da2756d26927/download__1_.jpeg" />
         <pubDate>2018-03-29 17:58:07 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/247353254</guid>
      </item>
      <item>
         <title>transform boundary</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/248436590</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="https://padlet-uploads.storage.googleapis.com/217613188/0b1ca1f507ad17845409eedf3c755844/download.jpeg" />
         <pubDate>2018-04-04 11:03:18 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/248436590</guid>
      </item>
      <item>
         <title>fault</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/248436716</link>
         <description><![CDATA[<div> In geology, a place where sections of the crust of the Earth move relative to each other. (See earthquake and San Andreas <strong>fault</strong>.) Note: <strong>Faults</strong> tend to occur near the edges of tectonic plates.</div>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/217613188/ac6f465be8cbf9da864b90d8058221a7/download.png" />
         <pubDate>2018-04-04 11:04:02 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/248436716</guid>
      </item>
      <item>
         <title>asthenosphere</title>
         <author>HECTORTHEKIDJR</author>
         <link>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/248436880</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://padlet-uploads.storage.googleapis.com/217613188/e70eebb00915a4b9349336f194c7dfdb/Earthlayers.png" />
         <pubDate>2018-04-04 11:05:01 UTC</pubDate>
         <guid>https://padlet.com/HECTORTHEKIDJR/1e8vert5948l/wish/248436880</guid>
      </item>
   </channel>
</rss>
