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      <title>Sedimentary Principals and Fossils by Anthony Cortez</title>
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      <description>Sedimentary Principals and Fossils</description>
      <language>en-us</language>
      <pubDate>2018-01-23 17:35:46 UTC</pubDate>
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         <title>Principle of uniformitarianism</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223904414</link>
         <description><![CDATA[<div>Uniformitarianism is a geological doctrine. It states that current geologic processes, occurring at the same rates observed today, in the same manner, account for all of Earth's geological features</div>]]></description>
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         <pubDate>2018-01-23 17:38:01 UTC</pubDate>
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         <title>Principle of superposition</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223905019</link>
         <description><![CDATA[<div>In physics and systems theory, the superposition principle, also known as superposition property, states that, for all linear systems, the net response caused by two or more stimuli is the sum of the responses that would have been caused by each stimulus individually.</div>]]></description>
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         <pubDate>2018-01-23 17:39:00 UTC</pubDate>
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         <title>Principle of original horizontality</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223905309</link>
         <description><![CDATA[<div>The Principle of Original Horizontality states that layers of sediment are originally deposited horizontally under the action of gravity . It is a relative dating technique. The principle is important to the analysis of folded and tilted strata.</div>]]></description>
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         <pubDate>2018-01-23 17:39:33 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223905309</guid>
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         <title>Principle of original lateral continuity</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223905610</link>
         <description><![CDATA[<div>The principle of lateral continuity states that layers of sediment initially extend laterally in all directions; in other words, they are laterally continuous. As a result, rocks that are otherwise similar, but are now separated by a valley or other erosional feature, can be assumed to be originally continuous.</div>]]></description>
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         <pubDate>2018-01-23 17:40:05 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223905610</guid>
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         <title>principle of cross-cutting relationships</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223905921</link>
         <description><![CDATA[<div>Cross-cutting relationships is a principle of geology that states that the geologic feature which cutsanother is the younger of the two features. It is a relative dating technique in geology.</div>]]></description>
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         <pubDate>2018-01-23 17:40:34 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223905921</guid>
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         <title>Principle of inclusions</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223906080</link>
         <description><![CDATA[<div>This is a restatement of Charles Lyell's original principle of inclusions and components from his 1830 to 1833 multi-volume Principles of Geology, which states that, with sedimentary rocks, if inclusions (or clasts) are found in a formation, then the inclusions must be older than the formation that contains them.</div><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:40:49 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223906080</guid>
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         <title>Mold and Cast fossils </title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223906775</link>
         <description><![CDATA[<div>Shells, bone, and wood often form as molds or casts. Some trace fossils (ichnofossils), such as tracks and burrows can form as casts or molds. Tracks andburrows can provide clues to the behavior and biomechanics of an organism while it was alive. Concretions often encapsulate a fossil mold and cast.</div>]]></description>
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         <pubDate>2018-01-23 17:41:54 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223906775</guid>
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         <title>Petrification Fossils</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223907281</link>
         <description><![CDATA[<div>A <strong><em>petrified fossil</em></strong> is different from other <strong><em>fossils</em></strong> such as resin <strong><em>fossils</em></strong> or permineralized <strong><em>fossils</em></strong> because the original material of the organism is still intact in resin <strong><em>fossils</em></strong> or permineralized <strong><em>fossils</em></strong>. </div>]]></description>
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         <pubDate>2018-01-23 17:42:47 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223907281</guid>
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         <title>Footprints and Trackways Fossils</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223907717</link>
         <description><![CDATA[<div>A fossil trackway is a type of trace fossil, a trackway made by an organism. Many fossil trackways were made by dinosaurs, early tetrapods, and other quadrupeds and bipeds on land. Marine organisms also made many ancient trackways (such as the trails of trilobites and eurypterids like Hibbertopterus).</div>]]></description>
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         <pubDate>2018-01-23 17:43:36 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223907717</guid>
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         <title>Coprolites Fossils</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223908254</link>
         <description><![CDATA[<div>A <strong><em>coprolite</em></strong> is <strong><em>fossilized</em></strong> feces. <strong><em>Coprolites</em></strong> are classified as trace <strong><em>fossils</em></strong> as opposed to body <strong><em>fossils</em></strong>, as they give evidence for the animal's behaviour (in this case, diet) rather than morphology.</div>]]></description>
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         <pubDate>2018-01-23 17:44:32 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223908254</guid>
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      <item>
         <title>Whole Body or True Form Fossils</title>
         <author>304892</author>
         <link>https://padlet.com/304892/avf8plh9amzi/wish/223908635</link>
         <description><![CDATA[<div>A true form fossil is a fossil of the whole/entire body of the organism, like an actual animal or animal part. True form fossilsare formed when the animals soft tissues or hard parts did not decay over the years.</div>]]></description>
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         <pubDate>2018-01-23 17:45:10 UTC</pubDate>
         <guid>https://padlet.com/304892/avf8plh9amzi/wish/223908635</guid>
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