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      <title>Sedimentary principles  by Lizbeth Ortiz</title>
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      <description>Made with serendipity</description>
      <language>en-us</language>
      <pubDate>2018-01-23 16:31:25 UTC</pubDate>
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         <title>uniformitarianism</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223864710</link>
         <description><![CDATA[<div>the theory that changes in the earth's crust during geological history have resulted from the action of continuous and uniform processes.</div>]]></description>
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         <pubDate>2018-01-23 16:32:27 UTC</pubDate>
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         <title>superposition</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223865903</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 16:34:09 UTC</pubDate>
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         <title>original horizontality</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223866912</link>
         <description><![CDATA[<div>The Principle of Original Horizontality states that layers of sediment are originally deposited horizontally under the action of gravity .</div>]]></description>
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         <pubDate>2018-01-23 16:35:37 UTC</pubDate>
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         <title>original lateral continuity</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223868353</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</div>]]></description>
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         <pubDate>2018-01-23 16:37:38 UTC</pubDate>
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         <title>cross-cutting relationships</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223869264</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 16:38:58 UTC</pubDate>
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         <title>inclusions</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223870260</link>
         <description><![CDATA[<div>inclusions of foreign rocks that are found in igneous rocks are named xenoliths. </div>]]></description>
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         <pubDate>2018-01-23 16:40:27 UTC</pubDate>
         <guid>https://padlet.com/3049101/hmt7b0ljihld/wish/223870260</guid>
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         <title>Mold and Cast fossils </title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223871631</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 cast can be made.Molds and casts are three dimensional and preserve the surface contours of the organism.</div>]]></description>
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         <pubDate>2018-01-23 16:42:21 UTC</pubDate>
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         <title>Petrification Fossils</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223872562</link>
         <description><![CDATA[<div>Petrified wood is the name given to a special type of fossilized remains of terrestrial vegetation. It is the result of a tree or tree-like plants having completely transitioned to stone by the process of permineralization.</div>]]></description>
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         <pubDate>2018-01-23 16:43:54 UTC</pubDate>
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         <title>Footprints and Trackways Fossils</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223873668</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 16:45:45 UTC</pubDate>
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         <title>Coprolites Fossils</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223874422</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 16:47:03 UTC</pubDate>
         <guid>https://padlet.com/3049101/hmt7b0ljihld/wish/223874422</guid>
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         <title>Whole Body or True Form Fossils</title>
         <author>3049101</author>
         <link>https://padlet.com/3049101/hmt7b0ljihld/wish/223875540</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><div><br></div>]]></description>
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         <pubDate>2018-01-23 16:48:49 UTC</pubDate>
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