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      <title>Geosphere/Lithosphere by jacarra hamm</title>
      <link>https://padlet.com/carrahamm1998/ja16uhyijdjs</link>
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      <language>en-us</language>
      <pubDate>2016-10-24 19:49:55 UTC</pubDate>
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         <title>soil composition</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132887196</link>
         <description><![CDATA[<div>Soil composition is an important aspect of nutrient management. While soil minerals and organic matter hold and store nutrients, soil water is what readily provides nutrients for plant uptake. Soil air, too, plays an integral role since many of the microorganisms that live in the soil need air to undergo the biological processes that release additional nutrients into the soil.</div>]]></description>
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         <pubDate>2016-10-25 01:50:05 UTC</pubDate>
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         <title>mountains</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132887386</link>
         <description><![CDATA[<div>A <strong>mountain range</strong> is a series or chain of <strong>mountains</strong> that are close together. The world's tallest <strong>mountain ranges form</strong> when pieces of Earth's crust—called plates—smash against each other, in a process called plate tectonics, and buckle up like the hood of a car in a head-on collision.</div>]]></description>
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         <pubDate>2016-10-25 01:51:48 UTC</pubDate>
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         <title>earthquakes</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132887922</link>
         <description><![CDATA[<div>Earthquakes are usually caused when rock underground suddenly breaks along a fault. This sudden release of energy causes the seismic waves that make the ground shake. When two blocks of rock or two plates are rubbing against each other, they stick a little. They don't just slide smoothly; the rocks catch on each other. The rocks are still pushing against each other, but not moving. After a while, the rocks break because of all the pressure that's built up. When the rocks break, the earthquake occurs. During the earthquake and afterward, the plates or blocks of rock start moving, and they continue to move until they get stuck again. The spot underground where the rock breaks is called the <strong>focus</strong> of the earthquake. </div>]]></description>
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         <pubDate>2016-10-25 01:57:49 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132887922</guid>
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         <title>volcano</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132888679</link>
         <description><![CDATA[<div>A volcanic eruption is one of the most dangerous and magnificent natural disasters.  When a volcano erupts, the volcano sends out ash clouds, lava and even volcanic bombs.  There is a high risk of danger from slow moving lava; though, the lava might move slowly, it is very dangerous and can cause a lot of damage to property and human life.</div>]]></description>
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         <pubDate>2016-10-25 02:05:33 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132888679</guid>
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      <item>
         <title>geyser</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132888801</link>
         <description><![CDATA[<div>A <strong><em>geyser</em></strong> is a vent in Earth's surface that periodically ejects a column of hot water and steam. Even a small <strong><em>geyser</em></strong> is an amazing phenomenon; however some <strong><em>geysers</em></strong> have eruptions that blast thousands of gallons of boiling hot water up to a few hundred feet in the air. Old Faithful is the world's best known <strong><em>geyser</em></strong>.</div>]]></description>
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         <pubDate>2016-10-25 02:06:53 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132888801</guid>
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         <title>landslide</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132888947</link>
         <description><![CDATA[<div><br>Landslides are a serious geologic hazard common to almost every State in the United States. It is estimated that in the United States they cause in excess of $1 billion in damages and from about 25 to 50 deaths each year. Globally, landslides cause billions of dollars in damages and thousands of deaths and injuries each year (Schuster, 1996; Kirshbaum and others, 2009).</div>]]></description>
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         <pubDate>2016-10-25 02:08:37 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132888947</guid>
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         <title>rock cycle</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132889208</link>
         <description><![CDATA[<div>The <strong>rock cycle</strong> is a basic concept in geology that describes the time-consuming transitions through geologic time among the three main <strong>rock</strong> types: sedimentary, metamorphic, and igneous.</div>]]></description>
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         <pubDate>2016-10-25 02:11:35 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132889208</guid>
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         <title>types of rock</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132889466</link>
         <description><![CDATA[<div>The three main types, or classes, of rock are <strong>sedimentary</strong>, <strong>metamorphic</strong>, and <strong>igneous</strong> and the differences among them have to do with how they are formed. <strong>Sedimentary</strong> rocks are formed from particles of sand, shells, pebbles, and other fragments of material. Together, all these particles are called sediment.</div>]]></description>
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         <pubDate>2016-10-25 02:14:32 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132889466</guid>
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         <title>landfills</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132976022</link>
         <description><![CDATA[<div> <strong><em>landfill</em></strong> site (also known as a tip, dump, rubbish dump, garbage dump or dumping ground and historically as a midden) is a site for the disposal of waste materials by burial and is the oldest form of waste treatment (although the burial part is modern; historically, refuse was just left in piles or thrown into pits).</div>]]></description>
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         <pubDate>2016-10-25 12:51:02 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132976022</guid>
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         <title>water and minerals of the lithosphere</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132978890</link>
         <description><![CDATA[<div>Water is considered to have a significant effect on mantle rheology, either by weakening of crystal structure by dilute solid solution in olivine and pyroxenes or by causing low temperature partial melting. The role of water in the uppermost mantle has been explored to 6 GPa (~190 km) by a novel experimental approach in which the silicate melting solidus, the stability of hydrous phases and the water contents in nominally hydrous minerals (NAMs) were determined in each experiment. By varying water contents, including ‘dry’ and from ~500 ppm to 14.5 wt % H2O, i.e. from water in nominally anhydrous minerals (NAMs) to vapour-leaching conditions, we were able to clarify melting and vapour-leaching regimes. We determined the solidus and melting behaviour, and pargasite stability in model fertile lherzolite (MORB source) between 1.5 and 6 GPa. </div>]]></description>
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         <pubDate>2016-10-25 12:58:38 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132978890</guid>
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      <item>
         <title>abiotic and biotic</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132982061</link>
         <description><![CDATA[]]></description>
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         <pubDate>2016-10-25 13:06:51 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132982061</guid>
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      <item>
         <title>abiotic and biotic</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132982219</link>
         <description><![CDATA[<div>The living things in an ecosystem are called <strong>biotic</strong> factors. Living things include plants, animals, bacteria, fungi and more. The non living parts of an ecosystem are called <strong>abiotic</strong> factors. In an ecosystem some <strong>abiotic</strong> factors are sunlight, temperature atmospheric gases water and soil.</div>]]></description>
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         <pubDate>2016-10-25 13:07:18 UTC</pubDate>
         <guid>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132982219</guid>
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      <item>
         <title>nonrenewable and renewable resources</title>
         <author>carrahamm1998</author>
         <link>https://padlet.com/carrahamm1998/ja16uhyijdjs/wish/132982855</link>
         <description><![CDATA[<div>Nonrenewable resources are those found inside the earth, and they took millions of years to form. These include the fossil fuels, <strong><em>oil</em></strong>, natural gas, and <strong><em>coal</em></strong> and <strong><em>nuclear</em></strong> energy. Today, close to 84% of the total amount of energy used globally comes from fossil fuels.are those which can be replenished over time by some natural process, including farming. These resources have the ability to be renewed over a short period of time.<br>R</div>]]></description>
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         <pubDate>2016-10-25 13:08:55 UTC</pubDate>
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