<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>Minerals and Rocks by Marilyn Larsen</title>
      <link>https://padlet.com/mlarsen8245/p31gu39y3asb</link>
      <description>Minerals are the building blocks of rocks</description>
      <language>en-us</language>
      <pubDate>2017-11-15 19:21:38 UTC</pubDate>
      <lastBuildDate>2024-05-31 21:41:38 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>Mineral Criteria</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207401649</link>
         <description><![CDATA[<div><em><mark>Naturally occurring</mark></em><em><br></em><em><mark>Inorganic</mark></em><em><br></em><em><mark>Solid<br>Definite chemical composition<br>Crystalline structure </mark></em></div>]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/0c430ed8a875c06d6b80bbbc3b4bc9fa/mineral_criteria.png" />
         <pubDate>2017-11-15 19:28:36 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207401649</guid>
      </item>
      <item>
         <title> Mineral Criteria</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207406007</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/30ae1998373665b1e2c989840c43d559/mineral.jpg" />
         <pubDate>2017-11-15 19:36:35 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207406007</guid>
      </item>
      <item>
         <title></title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207409280</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/95ac40aa46575d37d7dc1dcd6680db0d/mineral_properties.png" />
         <pubDate>2017-11-15 19:42:17 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207409280</guid>
      </item>
      <item>
         <title>Igneous, Metamorphic and Sedimentary</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207409921</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/9097076b576066b46f9bbae196ddfdcc/rock_types.png" />
         <pubDate>2017-11-15 19:43:33 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207409921</guid>
      </item>
      <item>
         <title>Observe the rock cycle</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207411110</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/523f5e49c3c21328937effd4bc265e21/rock_cycle.png" />
         <pubDate>2017-11-15 19:45:34 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207411110</guid>
      </item>
      <item>
         <title></title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207413494</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/49ec6613622ef4f834379660a78aff9c/rocks.png" />
         <pubDate>2017-11-15 19:50:03 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207413494</guid>
      </item>
      <item>
         <title>Minerals that only contain one element or type of atom.</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207417201</link>
         <description><![CDATA[]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/b0056f5bf83fa5209a77ecb78cc0c1f8/mineral_native.jpg" />
         <pubDate>2017-11-15 19:57:30 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207417201</guid>
      </item>
      <item>
         <title>How to make a crystal</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207421744</link>
         <description><![CDATA[<div><a href="https://www.wikihow.com/Make-Salt-Crystals">https://www.wikihow.com/Make-Salt-Crystals</a><br><br></div>]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/22914907/717e208beb6a6b464f9b4fa7aa2914f7/crystal.jpg" />
         <pubDate>2017-11-15 20:08:00 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207421744</guid>
      </item>
      <item>
         <title>Minerals that have two or more elements.</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207490286</link>
         <description><![CDATA[]]></description>
         <enclosure url="" />
         <pubDate>2017-11-16 01:08:53 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207490286</guid>
      </item>
      <item>
         <title>Igneous rocks are formed from the solidification of molten rock material. There are two basic types.</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207491552</link>
         <description><![CDATA[<div><a href="http://geology.com/rocks/igneous-rocks.shtml">http://geology.com/rocks/igneous-rocks.shtml</a></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-16 01:17:32 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207491552</guid>
      </item>
      <item>
         <title>Sedimentary rocks are formed by the accumulation of sediments. There are three basic types of sedimentary rocks.</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207492136</link>
         <description><![CDATA[<div><a href="http://geology.com/rocks/sedimentary-rocks.shtml">http://geology.com/rocks/sedimentary-rocks.shtml</a></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-16 01:20:52 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207492136</guid>
      </item>
      <item>
         <title>Metamorphic rocks have been modified by heat, pressure, and chemical processes, usually while buried deep below Earth&#39;s surface. </title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207492479</link>
         <description><![CDATA[<div><a href="http://geology.com/rocks/metamorphic-rocks.shtml">http://geology.com/rocks/metamorphic-rocks.shtml</a></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-16 01:22:53 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/207492479</guid>
      </item>
      <item>
         <title>Rocks definition</title>
         <author></author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208131647</link>
         <description><![CDATA[<div>the solid mineral material forming part of the surface of the earth and other similar planets, exposed on the surface or underlying the soil or oceans.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-17 14:55:46 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208131647</guid>
      </item>
      <item>
         <title>Petrology from Nathan</title>
         <author></author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208134091</link>
         <description><![CDATA[<div>The study of rocks</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-17 14:59:53 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208134091</guid>
      </item>
      <item>
         <title></title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208531661</link>
         <description><![CDATA[<div>Click on the plus sign and add something about the Flame Test or Acid Test or Specific Gravity Test</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:30:37 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208531661</guid>
      </item>
      <item>
         <title></title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208531885</link>
         <description><![CDATA[<div>Click on the + sign and add some types of Compound Materials.  Add a picture and label it.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:32:07 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208531885</guid>
      </item>
      <item>
         <title>Two types of Igneous Rocks</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532115</link>
         <description><![CDATA[<div><strong>Intrusive igneous rocks</strong> crystallize below Earth's surface, and the slow cooling that occurs there allows large crystals to form. Examples of intrusive igneous rocks are <a href="http://geology.com/rocks/diorite.shtml"><strong>diorite</strong></a>, <a href="http://geology.com/rocks/gabbro.shtml"><strong>gabbro</strong></a>, <a href="http://geology.com/rocks/granite.shtml"><strong>granite</strong></a>, <a href="http://geology.com/rocks/pegmatite.shtml"><strong>pegmatite</strong></a>, and <a href="http://geology.com/rocks/peridotite.shtml"><strong>peridotite</strong></a>.</div><div><strong>Extrusive igneous rocks</strong> erupt onto the surface, where they cool quickly to form small crystals. Some cool so quickly that they form an amorphous glass. These rocks include <a href="http://geology.com/rocks/andesite.shtml"><strong>andesite</strong></a>, <a href="http://geology.com/rocks/basalt.shtml"><strong>basalt</strong></a>, <a href="http://geology.com/rocks/obsidian.shtml"><strong>obsidian</strong></a>, <a href="http://geology.com/rocks/pumice.shtml"><strong>pumice</strong></a>, <a href="http://geology.com/rocks/rhyolite.shtml"><strong>rhyolite</strong></a>, <a href="http://geology.com/rocks/scoria.shtml"><strong>scoria</strong></a>, and <a href="http://geology.com/rocks/tuff.shtml"><strong>tuff</strong></a>.</div><div>Pictures and brief descriptions of some common igneous rock types are shown on this page.</div><div><a href="http://geology.com/rocks/diorite.shtml"><strong><figure class="attachment attachment--preview" data-trix-attachment="{&quot;contentType&quot;:&quot;image&quot;,&quot;height&quot;:285,&quot;url&quot;:&quot;http://geology.com/rocks/pictures/quartz-diorite.jpg&quot;,&quot;width&quot;:380}" data-trix-content-type="image"><img src="http://geology.com/rocks/pictures/quartz-diorite.jpg" width="380" height="285"><figcaption class="attachment__caption"></figcaption></figure></strong><strong>Diorite</strong></a><strong> </strong>is a coarse-grained, intrusive igneous rock that contains a mixture of <a href="http://geology.com/minerals/feldspar.shtml"><strong>feldspar</strong></a>, pyroxene, <a href="http://geology.com/minerals/hornblende.shtml"><strong>hornblende</strong></a>, and sometimes <a href="http://geology.com/minerals/quartz.shtml"><strong>quartz</strong></a>. The specimen shown above is about two inches (five centimeters) across.</div><div><a href="http://geology.com/rocks/basalt.shtml"><strong><figure class="attachment attachment--preview" data-trix-attachment="{&quot;contentType&quot;:&quot;image&quot;,&quot;height&quot;:285,&quot;url&quot;:&quot;http://geology.com/rocks/pictures/basalt.jpg&quot;,&quot;width&quot;:380}" data-trix-content-type="image"><img src="http://geology.com/rocks/pictures/basalt.jpg" width="380" height="285"><figcaption class="attachment__caption"></figcaption></figure></strong><strong>Basalt</strong></a> is a fine-grained, dark-colored extrusive igneous rock composed mainly of <a href="http://geology.com/minerals/plagioclase.shtml"><strong>plagioclase</strong></a> and pyroxene. The specimen shown is about two inches (five centimeters) across.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:33:03 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532115</guid>
      </item>
      <item>
         <title></title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532194</link>
         <description><![CDATA[<div>Click on the + sign and add some important vocabulary words or I will have to choose them.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:33:37 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532194</guid>
      </item>
      <item>
         <title>Three types of Sedimentary Rocks</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532632</link>
         <description><![CDATA[<div><strong>Clastic sedimentary rocks</strong> such as <a href="http://geology.com/rocks/breccia.shtml"><strong>breccia</strong></a>, <a href="http://geology.com/rocks/conglomerate.shtml"><strong>conglomerate</strong></a>, <a href="http://geology.com/rocks/sandstone.shtml"><strong>sandstone</strong></a>, <a href="http://geology.com/rocks/siltstone.shtml"><strong>siltstone</strong></a>, and <a href="http://geology.com/rocks/shale.shtml"><strong>shale</strong></a> are formed from mechanical weathering debris.</div><div><strong>Chemical sedimentary rocks</strong>, such as <a href="http://geology.com/rocks/rock-salt.shtml"><strong>rock salt</strong></a>, <a href="http://geology.com/rocks/iron-ore.shtml"><strong>iron ore</strong></a>, <a href="http://geology.com/rocks/chert.shtml"><strong>chert</strong></a>, <a href="http://geology.com/rocks/flint.shtml"><strong>flint</strong></a>, some <a href="http://geology.com/rocks/dolomite.shtml"><strong>dolomites</strong></a>, and some <a href="http://geology.com/rocks/limestone.shtml"><strong>limestones</strong></a>, form when dissolved materials precipitate from solution.</div><div><strong>Organic sedimentary rocks</strong> such as <a href="http://geology.com/rocks/coal.shtml"><strong>coal</strong></a>, some <a href="http://geology.com/rocks/dolomite.shtml"><strong>dolomites</strong></a>, and some <a href="http://geology.com/rocks/limestone.shtml"><strong>limestones</strong></a>, form from the accumulation of plant or animal debris.</div><div>Photos and brief descriptions of some common sedimentary rock types are shown on this page.</div><div><a href="http://geology.com/rocks/coal.shtml"><strong><figure class="attachment attachment--preview" data-trix-attachment="{&quot;contentType&quot;:&quot;image&quot;,&quot;height&quot;:285,&quot;url&quot;:&quot;http://geology.com/rocks/pictures/coal-anthracite.jpg&quot;,&quot;width&quot;:380}" data-trix-content-type="image"><img src="http://geology.com/rocks/pictures/coal-anthracite.jpg" width="380" height="285"><figcaption class="attachment__caption"></figcaption></figure></strong><strong>Coal</strong></a> is an organic sedimentary rock that forms mainly from plant debris. The plant debris usually accumulates in a swamp environment. Coal is combustible and is often mined for use as a fuel. The specimen shown above is about two inches (five centimeters) across.</div><div><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:37:10 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532632</guid>
      </item>
      <item>
         <title>Two types of Metamorphic Rocks</title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532758</link>
         <description><![CDATA[<div>There are two basic types of metamorphic rocks.<strong>Foliated metamorphic rocks</strong> such as <a href="http://geology.com/rocks/gneiss.shtml"><strong>gneiss</strong></a>, <a href="http://geology.com/rocks/phyllite.shtml"><strong>phyllite</strong></a>, <a href="http://geology.com/rocks/schist.shtml"><strong>schist</strong></a>, and <a href="http://geology.com/rocks/slate.shtml"><strong>slate</strong></a> have a layered or banded appearance that is produced by exposure to heat and directed pressure.</div><div><strong>Non-foliated metamorphic rocks</strong> such as <a href="http://geology.com/rocks/hornfels.shtml"><strong>hornfels</strong></a>, <a href="http://geology.com/rocks/marble.shtml"><strong>marble</strong></a>, <a href="http://geology.com/rocks/quartzite.shtml"><strong>quartzite</strong></a>, and <a href="http://geology.com/rocks/novaculite.shtml"><strong>novaculite</strong></a> do not have a layered or banded appearance. Pictures and brief descriptions of some common types of metamorphic rocks are shown on this page.<br><a href="http://geology.com/rocks/gneiss.shtml"><strong><figure class="attachment attachment--preview" data-trix-attachment="{&quot;contentType&quot;:&quot;image&quot;,&quot;height&quot;:285,&quot;url&quot;:&quot;http://geology.com/rocks/pictures/gneiss.jpg&quot;,&quot;width&quot;:380}" data-trix-content-type="image"><img src="http://geology.com/rocks/pictures/gneiss.jpg" width="380" height="285"><figcaption class="attachment__caption"></figcaption></figure></strong></a></div><div><a href="http://geology.com/rocks/gneiss.shtml"><strong>Gneiss</strong></a> is a foliated metamorphic rock that has a banded appearance and is made up of granular mineral grains. It typically contains abundant <a href="http://geology.com/minerals/quartz.shtml"><strong>quartz</strong></a> or <a href="http://geology.com/minerals/feldspar.shtml"><strong>feldspar</strong></a> minerals. The specimen shown above is about two inches (five centimeters) across.<br><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:38:35 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208532758</guid>
      </item>
      <item>
         <title></title>
         <author>mlarsen8245</author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208533667</link>
         <description><![CDATA[<div>Click on the + sign and add something about the rock cycle.</div>]]></description>
         <enclosure url="" />
         <pubDate>2017-11-19 21:47:07 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208533667</guid>
      </item>
      <item>
         <title>Calcite By: Jace G.</title>
         <author></author>
         <link>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208922282</link>
         <description><![CDATA[<div>Calcite is a carbonate mineral and the most stable poly-morph of calcium carbonate.</div>]]></description>
         <enclosure url="https://padletuploads.blob.core.windows.net/prod/237898953/5ed00c3f6791d147147519a81d8e330d/calcite_marble_85.jpg" />
         <pubDate>2017-11-20 23:39:54 UTC</pubDate>
         <guid>https://padlet.com/mlarsen8245/p31gu39y3asb/wish/208922282</guid>
      </item>
   </channel>
</rss>
