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      <title>Types of folded Rocks by Yousef Fituri</title>
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      <language>en-us</language>
      <pubDate>2024-02-12 08:35:27 UTC</pubDate>
      <lastBuildDate>2024-02-12 08:53:10 UTC</lastBuildDate>
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         <title>Syncline Folds</title>
         <author>fituriyousef</author>
         <link>https://padlet.com/fituriyousef/g0uh206u4sclywen/wish/2880696795</link>
         <description><![CDATA[<p>Synclines have a concave-upward shape, resembling a trough or basin, with the youngest rock layers usually found in the center and progressively older layers towards the edges.</p>]]></description>
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         <pubDate>2024-02-12 08:46:49 UTC</pubDate>
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         <title>Anticline Folds</title>
         <author>fituriyousef</author>
         <link>https://padlet.com/fituriyousef/g0uh206u4sclywen/wish/2880698855</link>
         <description><![CDATA[<p>Anticlines have a convex-upward shape, resembling an arch or a crest, with the oldest rock layers typically found in the center and progressively younger layers towards the edges.</p>]]></description>
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         <pubDate>2024-02-12 08:49:20 UTC</pubDate>
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         <title>Monocline Folds</title>
         <author>fituriyousef</author>
         <link>https://padlet.com/fituriyousef/g0uh206u4sclywen/wish/2880701963</link>
         <description><![CDATA[<p>Monoclines typically have a simple geometry, consisting of a single steeply inclined limb or flexure, with the opposite limb being relatively flat or gently dipping. Monoclines can appear as linear or curvilinear features in the landscape, depending on the orientation and shape of the underlying rock layers. They may be several kilometers in length and can be observed in various geological settings, including mountainous regions, plateaus, and basins.</p>]]></description>
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