<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>Weathering by Malgosia P.</title>
      <link>https://padlet.com/m_plociennik/weathering</link>
      <description>notes</description>
      <language>en-us</language>
      <pubDate>2017-11-12 10:16:48 UTC</pubDate>
      <lastBuildDate>2025-05-12 11:45:18 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url>https://padlet-assets.s3.amazonaws.com/icons/Brightnessdown.png</url>
      </image>
      <item>
         <title></title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205959849</link>
         <description><![CDATA[<div>&nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp;<strong>WEATHERING <br></strong>&nbsp;<strong>Weathering is the breakdown of rocks at the Earth’s surface, by the action of rainwater, extremes of temperature, and biological activity. It does not involve the removal of rock material.&nbsp;<br></strong>&nbsp;             There are three types of weathering, <a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3561.html">physical</a>, <a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3564.html">chemical</a> and <a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3568.html">biological</a></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 10:19:23 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205959849</guid>
      </item>
      <item>
         <title>                      physical weathering</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205960734</link>
         <description><![CDATA[<div> Physical weathering is caused by the effects of changing temperature on rocks, causing the rock to break apart. The process is sometimes assisted by water. <br>            </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 10:28:45 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205960734</guid>
      </item>
      <item>
         <title>                       chemical weathering</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205963776</link>
         <description><![CDATA[<div> Chemical weathering is caused by rain water reacting with the mineral grains in rocks to form new minerals (clays) and soluble salts. These reactions occur particularly when the water is slightly acidic. <br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 10:58:39 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205963776</guid>
      </item>
      <item>
         <title>   biological weathering</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205963812</link>
         <description><![CDATA[<div> Living organisms contribute to the weathering process in many ways: <br> Many animals, such as these Piddock shells, bore into rocks for protection either by scraping away the grains or secreting acid to dissolve the rock. <a href="https://www.geolsoc.org.uk/ks3/webdav/site/GSL/shared/images/education_and_careers/RockCycle/Processes/Weathering/bio3.jpg"> photo</a><br> Trees put down roots through joints or cracks in the rock in order to find moisture.<a href="https://www.geolsoc.org.uk/ks3/webdav/site/GSL/shared/images/education_and_careers/RockCycle/Processes/Weathering/bio2.jpg"> photo</a></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 10:58:51 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205963812</guid>
      </item>
      <item>
         <title>Where does it occur?</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205964146</link>
         <description><![CDATA[<div> Physical weathering happens especially in places places where there is little soil and few plants grow, such as in mountain regions and hot deserts. </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 11:02:12 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205964146</guid>
      </item>
      <item>
         <title>How does it occur?</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205964438</link>
         <description><![CDATA[<div>Either through repeated melting and freezing of water <strong>(mountains and tundra)</strong> or through expansion and contraction of the surface layer of rocks that are baked by the sun <strong>(hot deserts</strong>).</div><div> There are two types of physical weathering :<br><a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3562.html">freeze - thaw</a>        <a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page4268.html">movie </a><br> <br>     </div>]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/84395320/53f1afdac73acfe86b27ec6645a01553/2442248_orig.png" />
         <pubDate>2017-11-12 11:05:03 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205964438</guid>
      </item>
      <item>
         <title>Where does it occur?</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205965445</link>
         <description><![CDATA[<div> These chemical processes need water, and occur more rapidly at higher temperature, so warm, damp climates are best. </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 11:15:38 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205965445</guid>
      </item>
      <item>
         <title>How does it occur?</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205965706</link>
         <description><![CDATA[<div><strong> Solution</strong> - removal of rock in solution by acidic rainwater. In particular, limestone is weathered by rainwater containing dissolved CO2, (this process is sometimes called carbonation) <a href="https://www.geolsoc.org.uk/ks3/webdav/site/GSL/shared/images/education_and_careers/RockCycle/Processes/Weathering/solution1.jpg">photo</a>   <a href="https://www.geolsoc.org.uk/ks3/webdav/site/GSL/shared/images/education_and_careers/RockCycle/Processes/Weathering/hydrolysis2.jpg"> </a><br> <strong>Hydrolysis</strong> - the breakdown of rock by acidic water to produce clay and soluble salts <a href="https://www.geolsoc.org.uk/ks3/webdav/site/GSL/shared/images/education_and_careers/RockCycle/Processes/Weathering/hydrolysis2.jpg">photo</a><br><strong> Oxidation </strong>- the breakdown of rock by oxygen and water, often giving iron-rich rocks a rusty-coloured weathered surface </div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 11:18:32 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205965706</guid>
      </item>
      <item>
         <title>Quiz</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205966721</link>
         <description><![CDATA[<div><a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3639.html">quiz about weathering</a></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-12 11:28:39 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205966721</guid>
      </item>
      <item>
         <title>Another type of physical weathering:   </title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205970384</link>
         <description><![CDATA[<div><a href="https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3563.html">exfoliation </a> </div>]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/84395320/42943cd31a686a9171444aa84e31e28e/9975670_orig.jpg" />
         <pubDate>2017-11-12 12:19:30 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205970384</guid>
      </item>
      <item>
         <title>MASS  WASTING MOVEMENTS</title>
         <author>m_plociennik</author>
         <link>https://padlet.com/m_plociennik/weathering/wish/205970804</link>
         <description><![CDATA[<ul><li><strong>Landslides/ landslip</strong>, is a rapid movement of a large mass of earth and rocks down a hill&nbsp;</li><li>&nbsp;falls - slow movement of rocks down a hill .A fall or topple happens when <a href="http://www.onegeology.org/extra/kids/rocks_and_minerals.html">rocks</a>&nbsp; and other <a href="http://www.onegeology.org/extra/kids/sedimentary.html">sediments</a>&nbsp; fall through the air and land at the bottom of a slope.&nbsp; The pile of rubble at the base of the slope is called a talus cone.&nbsp;</li></ul><div><br></div><div><br><br></div>]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/84395320/4087bbe51e4c983f6be5bb4d28bc39f1/1024px_TalusConesIsfjorden.jpg" />
         <pubDate>2017-11-12 12:26:10 UTC</pubDate>
         <guid>https://padlet.com/m_plociennik/weathering/wish/205970804</guid>
      </item>
   </channel>
</rss>
