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      <title>Faults and Folds by Evie McCleery</title>
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      <description>By Evie and Hailey</description>
      <language>en-us</language>
      <pubDate>2018-10-05 17:15:53 UTC</pubDate>
      <lastBuildDate>2026-03-02 13:38:07 UTC</lastBuildDate>
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         <title>Anticline</title>
         <author>evelyn_mccleery_2023</author>
         <link>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/289742752</link>
         <description><![CDATA[<div>An upward fold ; a fold of rock layers with a convex shape pointing upwards (ARCH)<br><br>This fault is caused by comperssional stress and usually occurs along with syncline. <br><a href="https://www.radford.edu/jtso/GeologyofVirginia/Structures/GeologyOfVAStructures4-2e.html">https://www.radford.edu/jtso/GeologyofVirginia/Structures/GeologyOfVAStructures4-2e.html</a>&nbsp;</div>]]></description>
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         <pubDate>2018-10-05 17:24:14 UTC</pubDate>
         <guid>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/289742752</guid>
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         <title>Monocline </title>
         <author>hailey_bonne_2023</author>
         <link>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/289744727</link>
         <description><![CDATA[<div>A bend in the rock strata that are otherwise uniformly dipping or horizontal.<figure class="attachment attachment--preview" data-trix-attachment="{&quot;contentType&quot;:&quot;image&quot;,&quot;height&quot;:208,&quot;url&quot;:&quot;http://ok-t.ru/studopediaru/baza13/488108693897.files/image008.jpg&quot;,&quot;width&quot;:329}" data-trix-content-type="image"><img src="http://ok-t.ru/studopediaru/baza13/488108693897.files/image008.jpg" width="329" height="208"><figcaption class="attachment__caption"></figcaption></figure></div>]]></description>
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         <pubDate>2018-10-05 17:28:06 UTC</pubDate>
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         <title>Syncline</title>
         <author>evelyn_mccleery_2023</author>
         <link>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/289744759</link>
         <description><![CDATA[<div>A downward fold; a fold of rock layers with a convex side towards the Earth (SINK) <br><br>This fault is caused by comperssional stress and usually occurs with a anticline<br><a href="https://www.radford.edu/jtso/GeologyofVirginia/Structures/GeologyOfVAStructures4-2e.html">https://www.radford.edu/jtso/GeologyofVirginia/Structures/GeologyOfVAStructures4-2e.html</a> <figure class="attachment attachment--preview"><img src="http://pirate.shu.edu/~schoenma/images/15_fold-syncline..1gif.gif" width="300" height="224"><figcaption class="attachment__caption"></figcaption></figure></div>]]></description>
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         <pubDate>2018-10-05 17:28:08 UTC</pubDate>
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         <title>Normal</title>
         <author>evelyn_mccleery_2023</author>
         <link>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/290395158</link>
         <description><![CDATA[<div>This fault is caused when tensional stress is when rock slabs are pulled apart from each other. </div>]]></description>
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         <pubDate>2018-10-08 16:57:10 UTC</pubDate>
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         <title>Strike- slip</title>
         <author>evelyn_mccleery_2023</author>
         <link>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/290395276</link>
         <description><![CDATA[<div>"This fault is caused by horizontal compression but they release their energy by rock displacement in a horizontal direction almost parallel to the compression force". (<a href="https://www.britannica.com/science/strike-slip-fault">https://www.britannica.com/science/strike-slip-fault</a>)</div>]]></description>
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         <pubDate>2018-10-08 16:57:25 UTC</pubDate>
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         <title>Reverse</title>
         <author>hailey_bonne_2023</author>
         <link>https://padlet.com/evelyn_mccleery_2023/91tiz0khltzy/wish/290400924</link>
         <description><![CDATA[<div><strong>Reverse faults</strong> occur where two blocks of rock are forced together by compression. </div>]]></description>
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         <pubDate>2018-10-08 17:08:19 UTC</pubDate>
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