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      <title>Padlet #6 Rocks and Minerals by Lorelie Garcia Gonzalez</title>
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      <description>Made with a stroke of good luck</description>
      <language>en-us</language>
      <pubDate>2018-04-26 15:46:54 UTC</pubDate>
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         <title>Igneous Rock</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255709739</link>
         <description><![CDATA[<div>Igneous rock, or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava.</div>]]></description>
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         <pubDate>2018-04-26 15:52:27 UTC</pubDate>
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         <title>Sedimentary Rock</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255710121</link>
         <description><![CDATA[<div>Rock that has formed through the deposition and solidification of sediment, especially sediment transported by water (rivers, lakes, and oceans), ice ( glaciers ), and wind. Sedimentary rocks are often deposited in layers, and frequently contain fossils. Note : Limestone and shale are common sedimentary rocks</div>]]></description>
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         <pubDate>2018-04-26 15:53:20 UTC</pubDate>
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         <title>Metamorphic Rock</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255711185</link>
         <description><![CDATA[<div>Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form". The original rock is subjected to heat and pressure, causing profound physical or chemical change.</div>]]></description>
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         <pubDate>2018-04-26 15:55:26 UTC</pubDate>
         <guid>https://padlet.com/3049561/l78zffqsvnbr/wish/255711185</guid>
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         <title>Rock Cycle</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255713824</link>
         <description><![CDATA[<div>The Rock Cycle is a group of changes. Igneous rock can change into sedimentary rock or into metamorphic rock. Sedimentary rock can change into metamorphic rock or into igneous rock. Metamorphic rock can change into igneous or sedimentary rock. Igneous rock forms when magma cools and makes crystals.</div>]]></description>
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         <pubDate>2018-04-26 16:00:08 UTC</pubDate>
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         <title> Weathering</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255716822</link>
         <description><![CDATA[<div>Weathering is the breaking down of rocks, soil, and minerals as well as wood and artificial materials through contact with the Earth's atmosphere, water, and biological organisms.</div>]]></description>
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         <pubDate>2018-04-26 16:06:13 UTC</pubDate>
         <guid>https://padlet.com/3049561/l78zffqsvnbr/wish/255716822</guid>
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         <title> Erosion</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255717392</link>
         <description><![CDATA[<div>In earth science, erosion is the action of surface processes that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transport it away to another location.</div>]]></description>
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         <pubDate>2018-04-26 16:07:11 UTC</pubDate>
         <guid>https://padlet.com/3049561/l78zffqsvnbr/wish/255717392</guid>
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         <title>Rock Strata</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255717889</link>
         <description><![CDATA[<div>in geology and related fields, a stratum is a layer of sedimentary rock or soil, or igneous rock that were formed at the Earth's surface, with internally consistent characteristics that distinguish it from other layers.</div>]]></description>
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         <pubDate>2018-04-26 16:08:12 UTC</pubDate>
         <guid>https://padlet.com/3049561/l78zffqsvnbr/wish/255717889</guid>
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         <title>Cementation</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255718344</link>
         <description><![CDATA[<div>the binding together of particles or other things by cement.</div>]]></description>
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         <pubDate>2018-04-26 16:09:12 UTC</pubDate>
         <guid>https://padlet.com/3049561/l78zffqsvnbr/wish/255718344</guid>
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         <title>Compaction</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255718823</link>
         <description><![CDATA[<div><strong>compaction</strong>. (kəm-pāk'shən) The process by which the porosity of a given form of sediment is decreased as a result of its mineral grains being squeezed together by the weight of overlying sediment or by mechanical means. The American Heritage® Science Dictionary.</div>]]></description>
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         <pubDate>2018-04-26 16:10:16 UTC</pubDate>
         <guid>https://padlet.com/3049561/l78zffqsvnbr/wish/255718823</guid>
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         <title>Fossils</title>
         <author>3049561</author>
         <link>https://padlet.com/3049561/l78zffqsvnbr/wish/255719512</link>
         <description><![CDATA[<div>A fossil is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, hair, petrified wood, oil, coal, and DNA remnants</div>]]></description>
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         <pubDate>2018-04-26 16:11:42 UTC</pubDate>
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