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      <title>ROCKS CYCLE by JHON NICOLE MONCADA DETABLAN</title>
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      <pubDate>2024-09-04 05:03:45 UTC</pubDate>
      <lastBuildDate>2024-09-10 12:48:13 UTC</lastBuildDate>
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         <title>IGNEOUS ROCK</title>
         <author>s2015045_11</author>
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         <description><![CDATA[<p>hardening of rock and magma results into this type of rock</p>]]></description>
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         <pubDate>2024-09-10 07:12:33 UTC</pubDate>
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         <title>SEDIMENTARY ROCK</title>
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         <description><![CDATA[<p>Formed from compaction and sediments from worn out rocks. First, it goes through deposition, then compaction, then last is cementation. </p>]]></description>
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         <pubDate>2024-09-10 07:14:31 UTC</pubDate>
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         <title>METAMORPHIC ROCK</title>
         <author>s2015045_11</author>
         <link>https://padlet.com/s2015045_11/x36y7jaun4wwfdyg/wish/3111520698</link>
         <description><![CDATA[<p>Rocks that have been changed from igneous, sedimentary, or any previous metamorphic rock. </p>]]></description>
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         <pubDate>2024-09-10 07:15:37 UTC</pubDate>
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         <title>SOLIDIFICATION </title>
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         <pubDate>2024-09-10 07:18:22 UTC</pubDate>
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         <title>MELTING</title>
         <author>s2015045_11</author>
         <link>https://padlet.com/s2015045_11/x36y7jaun4wwfdyg/wish/3111526309</link>
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         <pubDate>2024-09-10 07:18:46 UTC</pubDate>
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         <title>WEATHERING &amp; EROSION</title>
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         <pubDate>2024-09-10 07:50:25 UTC</pubDate>
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         <title>HEAT and/or CHEMICAL ACTION</title>
         <author>s2015045_11</author>
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         <pubDate>2024-09-10 07:57:13 UTC</pubDate>
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         <title>Rock Cycle</title>
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         <description><![CDATA[<p>The rock cycle is a web of processes that outlines how each of the three major rock types—igneous, metamorphic, and sedimentary—form and break down based on the different applications of heat and pressure over time. For example, sedimentary rock shale becomes slate when heat and pressure are added. The more heat and pressure you add, the further the rock metamorphoses until it becomes gneiss. If it is heated further, the rock will melt completely and reform as an igneous rock.</p>]]></description>
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         <pubDate>2024-09-10 07:58:02 UTC</pubDate>
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         <title>MELTING</title>
         <author>s2015045_11</author>
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         <pubDate>2024-09-10 08:00:23 UTC</pubDate>
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         <title>HEAT and/or CHEMICAL ACTION</title>
         <author>s2015045_11</author>
         <link>https://padlet.com/s2015045_11/x36y7jaun4wwfdyg/wish/3111603851</link>
         <description><![CDATA[]]></description>
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         <pubDate>2024-09-10 08:01:38 UTC</pubDate>
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         <title>MAGMA</title>
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         <pubDate>2024-09-10 08:02:29 UTC</pubDate>
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         <title>METAMORPHIC ROCKS</title>
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         <pubDate>2024-09-10 08:11:31 UTC</pubDate>
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         <title>SEDIMENTARY ROCKS</title>
         <author>s2402432_1</author>
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         <pubDate>2024-09-10 08:13:31 UTC</pubDate>
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         <title>SEDIMENTS</title>
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         <pubDate>2024-09-10 08:15:18 UTC</pubDate>
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         <title></title>
         <author>s2015045_11</author>
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         <pubDate>2024-09-10 11:55:18 UTC</pubDate>
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         <title></title>
         <author>s14110521</author>
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         <pubDate>2024-09-10 12:22:05 UTC</pubDate>
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