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      <title>PADLET 4 PLATE TECTONICS by Alexander Gonzalez</title>
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      <description></description>
      <language>en-us</language>
      <pubDate>2018-03-29 15:19:58 UTC</pubDate>
      <lastBuildDate>2025-11-22 18:44:32 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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         <title>ASTHENOSPERE</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247290802</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>
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         <pubDate>2018-03-29 15:21:04 UTC</pubDate>
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         <title>FAULT</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247290956</link>
         <description><![CDATA[<div>In geology, a <strong>fault</strong> is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock-mass movement. ... Energy release associated with rapid movement on active <strong>faults</strong> is the cause of most earthquakes.</div>]]></description>
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         <pubDate>2018-03-29 15:21:19 UTC</pubDate>
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         <title>TRANSFORM BOUNDARY</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291084</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>
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         <pubDate>2018-03-29 15:21:33 UTC</pubDate>
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         <title>DIVERGENT BOUNDARY</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291258</link>
         <description><![CDATA[<div>In plate tectonics, a <strong>divergent boundary</strong> or <strong>boundary</strong> (also known as a constructive <strong>boundary</strong> or an extensional <strong>boundary</strong>) is a linear feature that exists between two tectonic plates that are moving away from each other.</div>]]></description>
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         <pubDate>2018-03-29 15:21:53 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291258</guid>
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         <title>CONVERGENT BOUNDARY</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291356</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>
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         <pubDate>2018-03-29 15:22:05 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291356</guid>
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         <title>RING OF FIRE</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291476</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>]]></description>
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         <pubDate>2018-03-29 15:22:18 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291476</guid>
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         <title>MID ATLANTIC RIDGE</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291602</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>
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         <pubDate>2018-03-29 15:22:36 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291602</guid>
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         <title>SUBDUCTION</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291713</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>
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         <pubDate>2018-03-29 15:22:50 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291713</guid>
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         <title>CONTINENTAL DRIFT</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291811</link>
         <description><![CDATA[<div>the gradual movement of the continents across the earth's surface through geological time.</div>]]></description>
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         <pubDate>2018-03-29 15:23:02 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291811</guid>
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         <title>PLATE TECTONICS</title>
         <author>3097213</author>
         <link>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291936</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>
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         <pubDate>2018-03-29 15:23:16 UTC</pubDate>
         <guid>https://padlet.com/3097213/4h0wv1yal1wr/wish/247291936</guid>
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