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      <title>BIOLOGY AND GEOLOGY by ISABEA</title>
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      <description>UNIT 4 AND 5 (REVIEW)</description>
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      <pubDate>2016-12-16 18:29:52 UTC</pubDate>
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         <title>MINERALS AND ROCKS</title>
         <author>guillen134</author>
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         <pubDate>2016-12-16 18:32:41 UTC</pubDate>
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         <title>MINERALS</title>
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         <pubDate>2016-12-16 18:33:55 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
         <link>https://padlet.com/guillen134/_alvinmesisabeapadlet/wish/144117392</link>
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         <pubDate>2016-12-16 18:39:55 UTC</pubDate>
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         <title>MOST MINERALS AND ROCKS ARE FOUND IN THE  GEOSPHERE.</title>
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         <pubDate>2016-12-16 18:41:33 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <pubDate>2016-12-17 09:36:40 UTC</pubDate>
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         <title>THE GEOSPHERE HAS GOT FOUR CHARACTERISTICS:</title>
         <author>guillen134</author>
         <link>https://padlet.com/guillen134/_alvinmesisabeapadlet/wish/144158372</link>
         <description><![CDATA[<div>-IT'S HOT:IF YOU GO DEPPER THE TEMPERATURES INCREASES.VOCANIC ERUPTIONS ARE AN EXAMPLE THEY SHOW THAT THE EARTH INTERIOR IS VERY HOT.<br>-IT'S MAGNETIG:THE COMPASS POINTS TO THE NORTH BECAUSE THE EARTH HAS GOT A MAGNETIC FIELD.THE SOURCE OF THIS MAGNETIC FIELD IS THE IRON CORE AT THE CENTRE OF THE EARTH.<br>-IT'S DENSE:THE MEAN DENSITY OF THE GEOSPHERE IS APPROXIMATELY DOUBLE THE DENSITY OF SURFACE ROCKS.<br>-IT HAS A LAYERED STRUCTURE:BY ANALYSING HOW SEISMIC WAVES  <br>FROM EARTHQUAKES SPREAD OUT AND TRAVEL THROUGHT DIFFERENT SOLID AND LIQUID MATERIALS.SCIENTISTS HAS BEEN ABLE TO IDENTIFY THE DIFFERENT LAYERS INSIDE THE EARTH.</div>]]></description>
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         <pubDate>2016-12-17 09:38:01 UTC</pubDate>
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         <title>A mineral is a solid,natural,inorganic(not made by humans) material that has a specific &quot;chemical formula&quot;.</title>
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         <pubDate>2016-12-17 09:48:59 UTC</pubDate>
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         <title>CLASIFICATION</title>
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         <pubDate>2016-12-17 09:51:29 UTC</pubDate>
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         <title>SILICATES</title>
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         <description><![CDATA[<div>Silicates are minerals that contain silicon and oxygen. Over 90% of the Earth's crust is made up of silicates.<br><br><br></div>]]></description>
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         <pubDate>2016-12-17 09:52:30 UTC</pubDate>
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         <title>NON-SILICATES</title>
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         <description><![CDATA[<div>The rest of the minerals are lumped into a group called non-silicates. Some important non-silicate minerals include: --Carbonates<br>-Halides . <br>-Oxides <br>-Sulfides.<br><br></div>]]></description>
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         <pubDate>2016-12-17 09:55:37 UTC</pubDate>
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         <title>PROPERTIES</title>
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         <description><![CDATA[]]></description>
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         <pubDate>2016-12-17 09:58:59 UTC</pubDate>
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         <title>HARDNESS</title>
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         <description><![CDATA[<div>The hardness describes how easy it is to scratch the surface of a mineral. Scientists often use the Moh's scale to describe hardness. Using the Moh's scale, a "1" is the softest mineral and a "10" is the hardest. One example of hardness is diamond. Diamond has a hardness of 10 because it is the hardest of all the minerals.<br>MOH'S SCALE<br><br><br><br><br></div>]]></description>
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         <pubDate>2016-12-17 10:05:06 UTC</pubDate>
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         <title>COLOUR</title>
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         <description><![CDATA[<div>Although color is often used to describe a mineral, it sometimes isn't the best way to tell one mineral from another as one type of mineral can come in several different colors.<br><br></div>]]></description>
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         <pubDate>2016-12-17 10:06:49 UTC</pubDate>
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         <title>LUSTRE</title>
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         <description><![CDATA[<div>Lutre describes how well a mineral reflects light. Examples of luster include glassy, metallic, brilliant, and dull.<br><br><br></div>]]></description>
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         <pubDate>2016-12-17 10:08:34 UTC</pubDate>
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         <title>STREAK</title>
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         <description><![CDATA[<div>Streak is the color of the mineral in powdered form. One way to determine the streak is to rub the mineral across a rough hard surface like a tile.<br><br><br></div>]]></description>
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         <pubDate>2016-12-17 10:09:51 UTC</pubDate>
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         <title>CLEAVAGE</title>
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         <description><![CDATA[<div>Cleavage describes how a mineral breaks up into pieces. Some minerals break up into small cubes while others may break up into thin sheets.<br><br><br></div>]]></description>
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         <pubDate>2016-12-17 10:10:54 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <pubDate>2016-12-17 10:17:23 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <pubDate>2016-12-17 10:17:56 UTC</pubDate>
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         <title></title>
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         <pubDate>2016-12-17 10:19:06 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <description><![CDATA[]]></description>
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         <pubDate>2016-12-17 10:21:14 UTC</pubDate>
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         <title>ROCKS</title>
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         <pubDate>2016-12-17 10:23:30 UTC</pubDate>
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         <title>A rock is a solid made up of a bunch of different minerals. Rocks are generally not uniform or made up of exact structures that can be described by scientific formulas.</title>
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         <pubDate>2016-12-17 10:25:54 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <description><![CDATA[]]></description>
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         <pubDate>2016-12-17 16:44:56 UTC</pubDate>
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         <title>TYPES</title>
         <author>guillen134</author>
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         <pubDate>2016-12-17 16:47:05 UTC</pubDate>
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         <title>SEDIMENTARY</title>
         <author>guillen134</author>
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         <description><![CDATA[]]></description>
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         <pubDate>2016-12-17 17:03:26 UTC</pubDate>
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         <title>THEY ARE FORM OF SEDIMENTS OR FRAGMENTS OF OTHER ROCKS.</title>
         <author>guillen134</author>
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         <pubDate>2016-12-17 17:07:49 UTC</pubDate>
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         <title>USES</title>
         <author>guillen134</author>
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         <description><![CDATA[]]></description>
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         <pubDate>2016-12-21 12:24:09 UTC</pubDate>
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         <title>MAGMATIC</title>
         <author>guillen134</author>
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         <pubDate>2016-12-21 12:26:41 UTC</pubDate>
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         <title>METAMORPHIC</title>
         <author>guillen134</author>
         <link>https://padlet.com/guillen134/_alvinmesisabeapadlet/wish/144572769</link>
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         <pubDate>2016-12-21 12:27:31 UTC</pubDate>
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         <title>ROCKSTHAT ARE TRANSFORMED DEEP UNDERGROUND WITH EXTREME HEAT AND PRESSURE.</title>
         <author>guillen134</author>
         <link>https://padlet.com/guillen134/_alvinmesisabeapadlet/wish/144572862</link>
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         <pubDate>2016-12-21 12:28:52 UTC</pubDate>
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         <title>THEY ARE FOUND IN DEEP ZONES,WHERE THE TEMPERATURE IS EXTREMELY HIGH.IN THIS ZONES WE FOUND MAGMA.WHEN THIS MAGMA,COOLS DOWN ,SOLIDIFIES AND FORMS MAGMATIC ROCKS.</title>
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         <pubDate>2016-12-21 12:33:20 UTC</pubDate>
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         <title>AGGREGATES,ORNAMENTAL ROCKS,QUARRIED ROCKS AND OTHER CONSTRUCTION MATERIALS,AS WELL AS FOSSIL FUELS</title>
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         <pubDate>2016-12-21 12:36:40 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <pubDate>2016-12-21 12:46:29 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <pubDate>2016-12-21 12:47:38 UTC</pubDate>
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         <title></title>
         <author>guillen134</author>
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         <pubDate>2016-12-21 12:48:22 UTC</pubDate>
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         <pubDate>2016-12-21 12:49:48 UTC</pubDate>
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