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      <title>Plate boundaries  by Jude Alphy Castillo</title>
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      <language>en-us</language>
      <pubDate>2022-09-14 06:03:15 UTC</pubDate>
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         <title>Plate boundaries</title>
         <author>jude98790</author>
         <link>https://padlet.com/jude98790/rj0anrtxs36zhphd/wish/2296014415</link>
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         <pubDate>2022-09-14 09:19:24 UTC</pubDate>
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         <title>Convergent plate boundaries</title>
         <author>jude98790</author>
         <link>https://padlet.com/jude98790/rj0anrtxs36zhphd/wish/2296055303</link>
         <description><![CDATA[<div>What is convergent plate boundaries base on searching on Google/books<br><br>A convergent boundary is an area on Earth where two or more lithospheric plates collide.<br><br>One plate eventually slide beneath the other, a process known as subduction.<br><br>The subduction zone can be defined by plane where many earthquake occur, called Wadati-Benioff zone.<br><br>These collision happen on scales of millions to tens of millions of year and can lead to volcanism, earthquakes, orogenesis, destruction of lithosphere, and deformation.&nbsp;<br><br>Convergent boundaries occur between oceanic-oceanic lithosphere , oceanic-continental lithosphere, and continental-continental lithosphere. The geologic features related to convergent boundaries vary depending on crust types.</div>]]></description>
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         <pubDate>2022-09-14 09:53:08 UTC</pubDate>
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         <title>Divergent plate boundaries</title>
         <author>jude98790</author>
         <link>https://padlet.com/jude98790/rj0anrtxs36zhphd/wish/2296057104</link>
         <description><![CDATA[<div>What is divergent plate boundaries base on searching on Google/books<br><br>In plate tectonic, a divergent boundary or divergent plate boundary(also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates&nbsp; that are moving away from each other.&nbsp;<br><br>Divergent boundaries within continents initially produce rifts, which eventually become rift Valleys.&nbsp;<br><br>Most active divergent plate boundaries occur between oceanic plates and exist</div>]]></description>
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         <pubDate>2022-09-14 09:54:22 UTC</pubDate>
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         <title>Transform plate boundaries </title>
         <author>jude98790</author>
         <link>https://padlet.com/jude98790/rj0anrtxs36zhphd/wish/2296061502</link>
         <description><![CDATA[<div>What is Transform plate boundaries base on searching on Google/books<br><br>A transform fault or transform boundary, sometimes called a strike-slip boundary, is a fault along a plate boundary where the motion is predominantly horizontal.<br><br>It ends abruptly where it connects to another plate boundary, either another transform, a spreading ridge, or a subduction zone.<br><br>A transform fault is a special case of a strike-slip fault that also forms a plate boundary</div>]]></description>
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         <pubDate>2022-09-14 09:57:56 UTC</pubDate>
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         <title>Conclusion </title>
         <author>jude98790</author>
         <link>https://padlet.com/jude98790/rj0anrtxs36zhphd/wish/2297745151</link>
         <description><![CDATA[<div>In Conclusion</div><div>Divergent, Convergent, and Transform plate boundaries are the three types of plate</div><div>movement theories that explain natural disasters like earthquakes, tsunamis, and volcanic</div><div>eruptions. The movements of each plate boundary can be away from each other causing a</div><div>separation, or continental drift; the plates can move parallel to each other and also move across</div><div>the plates. The theories involving plate tectonics and continental drift include a magnetic like</div><div>structure along the Earth’s crust or each continent has an anchor like structure that slowly pulls</div><div>the continents away from each other</div>]]></description>
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         <pubDate>2022-09-15 06:54:29 UTC</pubDate>
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