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      <title>Sedimentary Principals and Fossils  by Mark Daniel Vanta</title>
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      <description></description>
      <language>en-us</language>
      <pubDate>2018-01-23 17:34:04 UTC</pubDate>
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         <title>Principle of uniformitarianism</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223903105</link>
         <description><![CDATA[<div>a geological doctrine that processes acting in the same manner as at present and over long spans of time are sufficient to account for all current geological features and all past geological changes — compare catastrophism.</div><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:36:03 UTC</pubDate>
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         <title>Principle of superposition</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223903951</link>
         <description><![CDATA[<div>Geology. a basic law of geochronology, stating that in any undisturbed sequence of rocks deposited in layers, the youngest layer is on top and the oldest on bottom, each layer being younger than the one beneath it and older than the one above it.</div>]]></description>
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         <pubDate>2018-01-23 17:37:27 UTC</pubDate>
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         <title>Principle of original horizontality</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223904412</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 17:38:01 UTC</pubDate>
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         <title>Principle of original lateral continuity</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223904699</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><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:38:28 UTC</pubDate>
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         <title>principle of cross-cutting relationships</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223905277</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><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:39:29 UTC</pubDate>
         <guid>https://padlet.com/3044111/lfws7lvsjyz2/wish/223905277</guid>
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         <title>Principle of inclusions</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223905663</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 17:40:10 UTC</pubDate>
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         <title>Mold and Cast fossils </title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223906227</link>
         <description><![CDATA[<div>Organisms buried in sediment may decay or dissolve away leaving a cavity or mold. If the space is subsequently filled with sediment, an external castcan be made. Molds and casts are three dimensional and preserve the surface contours of the organism.</div><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:41:02 UTC</pubDate>
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         <title>Petrification Fossils</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223907152</link>
         <description><![CDATA[<div>In geology, petrifaction or petrification is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals.</div><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:42:33 UTC</pubDate>
         <guid>https://padlet.com/3044111/lfws7lvsjyz2/wish/223907152</guid>
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         <title>Footprints and Trackways Fossils</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223907666</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, earlytetrapods, 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><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:43:30 UTC</pubDate>
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         <title>Coprolites Fossils</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223907807</link>
         <description><![CDATA[<div>A coprolite is fossilized feces. Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour (in this case, diet) rather than morphology. The name is derived from the Greek words κόπρος (kopros, meaning "dung") and λίθος (lithos, meaning "stone").</div>]]></description>
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         <pubDate>2018-01-23 17:43:44 UTC</pubDate>
         <guid>https://padlet.com/3044111/lfws7lvsjyz2/wish/223907807</guid>
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         <title>Whole Body or True Form Fossils</title>
         <author>3044111</author>
         <link>https://padlet.com/3044111/lfws7lvsjyz2/wish/223908262</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. How Are TheyFormed ? True form fossils are formed when the animals soft tissues or hard parts did not decay over the years. Comments.</div><div><br></div>]]></description>
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         <pubDate>2018-01-23 17:44:32 UTC</pubDate>
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