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	<id>https://energyeducation.ca/wiki/index.php?action=history&amp;feed=atom&amp;title=Sediment</id>
	<title>Sediment - Revision history</title>
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	<updated>2026-07-03T05:31:58Z</updated>
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		<title>Jmdonev: 1 revision imported</title>
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		<updated>2021-10-15T19:13:31Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
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				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 19:13, 15 October 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
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		<author><name>Jmdonev</name></author>
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		<id>https://energyeducation.ca/wiki/index.php?title=Sediment&amp;diff=10321&amp;oldid=prev</id>
		<title>energy&gt;Jmdonev at 23:08, 13 May 2021</title>
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		<updated>2021-05-13T23:08:06Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 23:08, 13 May 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Line 1:&lt;/td&gt;
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&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Category:Done &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2015&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;10&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;15&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Category:Done &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2021&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;01&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;31&lt;/ins&gt;]]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:Sediment_in_the_Gulf_of_Mexico_(2).jpg|360px|thumb|right|Figure 1. Sediment in the Gulf of Mexico.&amp;lt;ref&amp;gt;Wikimedia Commons. (September 16, 2015). &amp;#039;&amp;#039;Sediment in the Gulf of Mexico&amp;#039;&amp;#039; [Online]. Available: https://upload.wikimedia.org/wikipedia/commons/d/d3/Sediment_in_the_Gulf_of_Mexico_(2).jpg&amp;lt;/ref&amp;gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:Sediment_in_the_Gulf_of_Mexico_(2).jpg|360px|thumb|right|Figure 1. Sediment in the Gulf of Mexico.&amp;lt;ref&amp;gt;Wikimedia Commons. (September 16, 2015). &amp;#039;&amp;#039;Sediment in the Gulf of Mexico&amp;#039;&amp;#039; [Online]. Available: https://upload.wikimedia.org/wikipedia/commons/d/d3/Sediment_in_the_Gulf_of_Mexico_(2).jpg&amp;lt;/ref&amp;gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;onlyinclude&amp;gt;&#039;&#039;&#039;Sediment&#039;&#039;&#039; is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;some &lt;/del&gt;[[solid]] material &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;- whether heavy or light - &lt;/del&gt;that is moved by &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;some &lt;/del&gt;[[&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force&lt;/del&gt;]] &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and &lt;/del&gt;deposited in a new location. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The general term used to refer to the force that moves &lt;/del&gt;sediment is [[erosion]].&amp;lt;/onlyinclude&amp;gt; &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This erosion &lt;/del&gt;is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;described &lt;/del&gt;as the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;removal and transportation &lt;/del&gt;of sediment. Sediment varies &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;drastically &lt;/del&gt;in size&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/del&gt;and can be as small as a grain of sand or as large as a boulder. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Generally, sediment &lt;/del&gt;is composed of rocks, minerals, and the remains of plants and animals.&amp;lt;ref name=&quot;RE1&quot;&amp;gt;National Geographic Education. (September 12, 2015). &#039;&#039;Sediment&#039;&#039; [Online]. Available: http://education.nationalgeographic.com/encyclopedia/sediment/&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;onlyinclude&amp;gt;&#039;&#039;&#039;Sediment&#039;&#039;&#039; is [[solid]] material that is moved &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;around &lt;/ins&gt;by &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;natural processes, like [[wind]], &lt;/ins&gt;[[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;water&lt;/ins&gt;]]&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, [[ice]], or [[gravity]]. This solid material is then &lt;/ins&gt;deposited in a new location. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This transport-and-deposition process of &lt;/ins&gt;sediment is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;known as &lt;/ins&gt;[[erosion]].&amp;lt;/onlyinclude&amp;gt; &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The act of breaking down monolithic material into smaller pieces &lt;/ins&gt;is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;known &lt;/ins&gt;as &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[weathering]]. Weathering and erosion together are &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;two processes responsible for the movement &lt;/ins&gt;of sediment &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;across the globe&lt;/ins&gt;. Sediment varies in size and can be as small as a grain of sand or as large as a boulder. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sediment &lt;/ins&gt;is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;traditionally &lt;/ins&gt;composed of rocks, minerals, and the remains of plants and animals.&amp;lt;ref name=&quot;RE1&quot;&amp;gt;National Geographic Education. (September 12, 2015). &#039;&#039;Sediment&#039;&#039; [Online]. Available: http://education.nationalgeographic.com/encyclopedia/sediment/&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sediment in [[water]] is generally small, and is present in nearly every body of water. When sediment in water is floating it is known as &#039;&#039;&#039;suspended sediment&#039;&#039;&#039;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Conversely, sediment &lt;/del&gt;that settles on the bottom of a waterway is known as &#039;&#039;&#039;bedded sediment&#039;&#039;&#039;.&amp;lt;ref name=&quot;RE3&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sediment in [[water]] is generally small, and is present in nearly every body of water. When sediment in water is floating it is known as &#039;&#039;&#039;suspended sediment&#039;&#039;&#039;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sediment &lt;/ins&gt;that settles on the bottom of a waterway is known as &#039;&#039;&#039;bedded sediment&#039;&#039;&#039;.&amp;lt;ref name=&quot;RE3&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;For a more in-depth exploration of sediment and its importance, click [http://www.fondriest.com/environmental-measurements/parameters/hydrology/sediment-transport-deposition/#std1a here].&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;For a more in-depth exploration of sediment and its importance, click [http://www.fondriest.com/environmental-measurements/parameters/hydrology/sediment-transport-deposition/#std1a here].&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Movement==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Movement==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The process of moving sediment from one place to another through a variety of different mechanisms is known as sediment transport. Transport of sediment in moderate amounts is important for diverse [[ecosystem]]s to exist. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Generally speaking, the greater &lt;/del&gt;the [[flow rate&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|flow&lt;/del&gt;]] the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;more &lt;/del&gt;sediment &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;that is moved&lt;/del&gt;.&amp;lt;ref name=&quot;RE3&quot;&amp;gt;Fundamentals of Environmental Measures. (September 16, 2016). &#039;&#039;Sediment Transport and Deposition&#039;&#039; [Online]. Available:  http://www.fondriest.com/environmental-measurements/parameters/hydrology/sediment-transport-deposition/&amp;lt;/ref&amp;gt; Another name for sediment transport is sediment load.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The process of moving sediment from one place to another through a variety of different mechanisms is known as sediment transport. Transport of sediment in moderate amounts is important for diverse [[ecosystem]]s to exist. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The amount of sediment that can be transported is dependent upon &lt;/ins&gt;the [[flow rate]] &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;of &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fluid, with greater amounts of &lt;/ins&gt;sediment &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;able to be transported at higher flow rates&lt;/ins&gt;. &amp;lt;ref name=&quot;RE3&quot;&amp;gt;Fundamentals of Environmental Measures. (September 16, 2016). &#039;&#039;Sediment Transport and Deposition&#039;&#039; [Online]. Available:  http://www.fondriest.com/environmental-measurements/parameters/hydrology/sediment-transport-deposition/&amp;lt;/ref&amp;gt; Another name for sediment transport is sediment load.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:DesertDunes01.jpg|thumb|right|Figure 2. Sand Dunes in an arid climate.&amp;lt;ref&amp;gt;Wikimedia Commons. (May 27 2020). &quot;Rub&#039; al Khali&quot; [Online]. Available: https://commons.wikimedia.org/wiki/File:Rub_al_Khali_002.JPG&amp;lt;/ref&amp;gt;]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Air===&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Air===&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Wind]] is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;one mechanism by which sediment can be moved&lt;/del&gt;. During a dust or sandstorm, wind can move dirt across a plane. Sand dunes are created when rocky sediment is worn down by wind and the sediment is deposited in one place.&amp;lt;ref name=&quot;RE1&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Wind]] &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;can move large volumes of sediment, and this &lt;/ins&gt;is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the main erosive force in arid environments.&amp;lt;ref name=&quot;des&quot;&amp;gt;&quot;Weathering and Erosional Processes in Deserts&quot;. (May 27, 2020) [Online]. Available:http://geologylearn.blogspot.com/2016/01/weathering-and-erosional-processes-in&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;html&amp;lt;/ref&amp;gt; &lt;/ins&gt;During a dust or sandstorm, wind can move dirt across a plane. Sand dunes are created when rocky sediment is worn down by wind and the sediment is deposited in one place.&amp;lt;ref name=&quot;RE1&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:AletschgletcherGlacier.jpg|thumb|right|Figure 3. The long tracts of sediment following the flowlines of the glacier are moraines.&amp;lt;ref&amp;gt;Wikimedia Commons. (May 27 2020). &quot;Frosser Aletschgletscher&quot; [Online]. Available: https://commons.wikimedia.org/wiki/File:Grosser_Aletschgletscher_3178.JPG&amp;lt;/ref&amp;gt;]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Ice===&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Ice===&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Glaciers can move &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely &lt;/del&gt;large &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;pieces of &lt;/del&gt;sediment by &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;freezing them into &lt;/del&gt;the glacier and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;depositing them &lt;/del&gt;elsewhere as the ice sheet moves across the landscape or melts. Sediment &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;from &lt;/del&gt;glaciers &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is &lt;/del&gt;called &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;moraine&lt;/del&gt;.&amp;lt;ref name=&quot;RE1&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Glaciers can move large sediment &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;blocks, as rocks or debris that fall onto a glacier will be incorporated &lt;/ins&gt;by the glacier and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;transported as the glacier flows under [[gravity]]. This sediment gets deposited &lt;/ins&gt;elsewhere as the ice sheet moves across the landscape or melts&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Glaciers also produce incredibly fine-grained sediment known as &#039;&#039;&#039;rock  flour&#039;&#039;&#039; at their base, as sediment that is stuck onto the bottom of the glacier gets ground against the bedrock below&lt;/ins&gt;. Sediment &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;piles deposited along the sides and at the toes of &lt;/ins&gt;glaciers &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;are &lt;/ins&gt;called &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;moraines&lt;/ins&gt;.&amp;lt;ref name=&quot;RE1&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Water===&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Water===&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Water can wash medium or small sediment &lt;/del&gt;from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a &lt;/del&gt;river &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;into a delta&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Generally, &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;stronger &lt;/del&gt;the flow of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the water the more &lt;/del&gt;sediment &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;it will be able to move&lt;/del&gt;. If flow is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;strong &lt;/del&gt;enough, the motion of the water can suspend particles &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;water &lt;/del&gt;as they move downstream or simply push them along the bottom of the waterway.&amp;lt;ref name=&quot;RE3&quot;/&amp;gt;  &lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As rain falls on land and makes its way to the nearest river, it picks up bits of dust and other fine particulate &lt;/ins&gt;from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the land surface and transports these particles into the &lt;/ins&gt;river. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Rivers then carry this sediment all &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;way to &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean where sediment is commonly deposited to form deltas. Rivers with higher &lt;/ins&gt;flow &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rates can transport larger amounts &lt;/ins&gt;of sediment. If flow is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fast &lt;/ins&gt;enough, the motion of the water can suspend particles &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;above &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;riverbed &lt;/ins&gt;as they move downstream or simply push them along the bottom of the waterway.&amp;lt;ref name=&quot;RE3&quot;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;gt; &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;==Ecological Importance==&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;A certain amount of sediment movement is necessary for a healthy, evolving ecosystem. The movement of sediment from one place to another enriches ecosystems with new nutrients and shapes the landscape. The supplementation of nutrients through sediment movement is important in maintaining a strong degree of biodiversity.&amp;lt;ref name=&quot;bio&quot;&amp;gt;Covich, Alan. (May 27, 2020). &quot;The importance of sediment for biodiversity&quot; [Online]. Accesible: https://sednet.org/download/SpecialSession4-Summary.pdf&amp;lt;/ref&lt;/ins&gt;&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;=&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;=Importance==&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Too much sediment in an environment can have detrimental effects&amp;lt;ref name&lt;/ins&gt;=&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&quot;sed&quot;&amp;gt;Government of Canada. (May 27 2020). &quot;Water Pollution: erosion and sedimentation&quot; [Online]. Accessible: https://www.canada.ca/en/environment-climate-change/services/water-overview/pollution-causes-effects/erosion-sedimentation.html&amp;lt;/ref&amp;gt;. The presence of too much sediment in a body &lt;/ins&gt;of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;water is known as sediment [[pollution]]. Although some &lt;/ins&gt;sediment is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;introduced into water through natural erosion processes, human activities such as building, bridge&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and roadway construction accelerate the transport &lt;/ins&gt;of sediment &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;into terrestrial waterways&amp;lt;ref name=&quot;sed&quot;/&amp;gt;. Sediment pollution degrades water quality and clarity. Decreased water clarity can make it difficult for animals &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;see food beneath the surface &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;inhibits vegetation growth. Too much sediment in stream beds disrupts the natural food chain by destroying the habitat &lt;/ins&gt;of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely small stream organisms, which in turn impacts fish populations&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Excess introduction &lt;/ins&gt;of nutrients &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;can result &lt;/ins&gt;in &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;harmful extreme algal blooms and [[eutrophication]]&lt;/ins&gt;.&amp;lt;ref name=&quot;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;RE2&lt;/ins&gt;&quot;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;gt;US EPA. (September 16, 2016). &#039;&#039;What is Sediment Pollution?&#039;&#039; [Online]. Available: http://cfpub.epa.gov/npstbx/files/ksmo_sediment.pdf&amp;lt;&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ref&lt;/ins&gt;&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;A certain amount &lt;/del&gt;of sediment &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement &lt;/del&gt;is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;necessary for a healthy&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;evolving ecosystem. The movement &lt;/del&gt;of sediment &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;from one place &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;another enriches ecosystems with new nutrients &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;shapes landscapes &lt;/del&gt;of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;other areas&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The supplementation &lt;/del&gt;of nutrients &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;through sediment movement results &lt;/del&gt;in &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;areas that are very diverse - such as river deltas&lt;/del&gt;.&amp;lt;ref name=&quot;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;RE1&lt;/del&gt;&quot;/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Although important, too much sediment in a body of water can be harmful. The presence of too much sediment in a body of water is known as sediment &lt;/del&gt;[[&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;pollution&lt;/del&gt;]]&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Although some sediment is introduced into water by a process of natural erosion, the majority of sediment enters through accelerated erosion as a result of human activities, particularly construction activities. Sediment pollution degrades water quality and clarity. Decreased water clarity can make it difficult for animals to see their food in the water an prevents vegetation from growing in water. Too much sediment in stream beds disrupts the natural food chain by destroying the habitat of extremely small stream organisms - this in turn decreases fish populations. As well, although some introduction of nutrients through sediment is important, too many nutrients can result in harmful extreme algal blooms and &lt;/del&gt;[[&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;eutrophication&lt;/del&gt;]]&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;.&amp;lt;ref name=&quot;RE2&quot;&amp;gt;US EPA. (September 16, 2016). &#039;&#039;What is Sediment Pollution?&#039;&#039; &lt;/del&gt;[&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Online&lt;/del&gt;]&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Available&lt;/del&gt;: &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cfpub.epa.gov/npstbx/files/ksmo_sediment.pdf&amp;lt;/ref&amp;gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;==For Further Reading== &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[[Gas]] &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[[Hydrocarbon combustion]] &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*&lt;/ins&gt;[[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Greenhouse gas&lt;/ins&gt;]]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*&lt;/ins&gt;[[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Greenhouse effect&lt;/ins&gt;]]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[&lt;/ins&gt;[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Carbon capture and storage]&lt;/ins&gt;]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*Or explore a [[Special&lt;/ins&gt;:&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Random|random page]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==References==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==References==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{reflist}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{reflist}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;category&lt;/del&gt;: &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Ed edit&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Category&lt;/ins&gt;:&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Uploaded&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>energy&gt;Jmdonev</name></author>
	</entry>
	<entry>
		<id>https://energyeducation.ca/wiki/index.php?title=Sediment&amp;diff=3808&amp;oldid=prev</id>
		<title>J.williams: 1 revision imported</title>
		<link rel="alternate" type="text/html" href="https://energyeducation.ca/wiki/index.php?title=Sediment&amp;diff=3808&amp;oldid=prev"/>
		<updated>2015-11-13T01:47:18Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
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				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 01:47, 13 November 2015&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>J.williams</name></author>
	</entry>
	<entry>
		<id>https://energyeducation.ca/wiki/index.php?title=Sediment&amp;diff=3807&amp;oldid=prev</id>
		<title>Jmdonev at 02:41, 22 September 2015</title>
		<link rel="alternate" type="text/html" href="https://energyeducation.ca/wiki/index.php?title=Sediment&amp;diff=3807&amp;oldid=prev"/>
		<updated>2015-09-22T02:41:00Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[Category:Done 2015-10-15]]&lt;br /&gt;
[[File:Sediment_in_the_Gulf_of_Mexico_(2).jpg|360px|thumb|right|Figure 1. Sediment in the Gulf of Mexico.&amp;lt;ref&amp;gt;Wikimedia Commons. (September 16, 2015). &amp;#039;&amp;#039;Sediment in the Gulf of Mexico&amp;#039;&amp;#039; [Online]. Available: https://upload.wikimedia.org/wikipedia/commons/d/d3/Sediment_in_the_Gulf_of_Mexico_(2).jpg&amp;lt;/ref&amp;gt;]]&lt;br /&gt;
&lt;br /&gt;
&amp;lt;onlyinclude&amp;gt;&amp;#039;&amp;#039;&amp;#039;Sediment&amp;#039;&amp;#039;&amp;#039; is some [[solid]] material - whether heavy or light - that is moved by some [[force]] and deposited in a new location. The general term used to refer to the force that moves sediment is [[erosion]].&amp;lt;/onlyinclude&amp;gt; This erosion is described as the removal and transportation of sediment. Sediment varies drastically in size, and can be as small as a grain of sand or as large as a boulder. Generally, sediment is composed of rocks, minerals, and the remains of plants and animals.&amp;lt;ref name=&amp;quot;RE1&amp;quot;&amp;gt;National Geographic Education. (September 12, 2015). &amp;#039;&amp;#039;Sediment&amp;#039;&amp;#039; [Online]. Available: http://education.nationalgeographic.com/encyclopedia/sediment/&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Sediment in [[water]] is generally small, and is present in nearly every body of water. When sediment in water is floating it is known as &amp;#039;&amp;#039;&amp;#039;suspended sediment&amp;#039;&amp;#039;&amp;#039;. Conversely, sediment that settles on the bottom of a waterway is known as &amp;#039;&amp;#039;&amp;#039;bedded sediment&amp;#039;&amp;#039;&amp;#039;.&amp;lt;ref name=&amp;quot;RE3&amp;quot;/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
For a more in-depth exploration of sediment and its importance, click [http://www.fondriest.com/environmental-measurements/parameters/hydrology/sediment-transport-deposition/#std1a here].&lt;br /&gt;
&lt;br /&gt;
==Movement==&lt;br /&gt;
The process of moving sediment from one place to another through a variety of different mechanisms is known as sediment transport. Transport of sediment in moderate amounts is important for diverse [[ecosystem]]s to exist. Generally speaking, the greater the [[flow rate|flow]] the more sediment that is moved.&amp;lt;ref name=&amp;quot;RE3&amp;quot;&amp;gt;Fundamentals of Environmental Measures. (September 16, 2016). &amp;#039;&amp;#039;Sediment Transport and Deposition&amp;#039;&amp;#039; [Online]. Available:  http://www.fondriest.com/environmental-measurements/parameters/hydrology/sediment-transport-deposition/&amp;lt;/ref&amp;gt; Another name for sediment transport is sediment load.&lt;br /&gt;
&lt;br /&gt;
===Air===&lt;br /&gt;
[[Wind]] is one mechanism by which sediment can be moved. During a dust or sandstorm, wind can move dirt across a plane. Sand dunes are created when rocky sediment is worn down by wind and the sediment is deposited in one place.&amp;lt;ref name=&amp;quot;RE1&amp;quot;/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
===Ice===&lt;br /&gt;
Glaciers can move extremely large pieces of sediment by freezing them into the glacier and depositing them elsewhere as the ice sheet moves across the landscape or melts. Sediment from glaciers is called moraine.&amp;lt;ref name=&amp;quot;RE1&amp;quot;/&amp;gt;&lt;br /&gt;
===Water===&lt;br /&gt;
Water can wash medium or small sediment from a river into a delta. Generally, the stronger the flow of the water the more sediment it will be able to move. If flow is strong enough, the motion of the water can suspend particles in the water as they move downstream or simply push them along the bottom of the waterway.&amp;lt;ref name=&amp;quot;RE3&amp;quot;/&amp;gt; &lt;br /&gt;
&lt;br /&gt;
==Importance==&lt;br /&gt;
A certain amount of sediment movement is necessary for a healthy, evolving ecosystem. The movement of sediment from one place to another enriches ecosystems with new nutrients and shapes landscapes of other areas. The supplementation of nutrients through sediment movement results in areas that are very diverse - such as river deltas.&amp;lt;ref name=&amp;quot;RE1&amp;quot;/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Although important, too much sediment in a body of water can be harmful. The presence of too much sediment in a body of water is known as sediment [[pollution]]. Although some sediment is introduced into water by a process of natural erosion, the majority of sediment enters through accelerated erosion as a result of human activities, particularly construction activities. Sediment pollution degrades water quality and clarity. Decreased water clarity can make it difficult for animals to see their food in the water an prevents vegetation from growing in water. Too much sediment in stream beds disrupts the natural food chain by destroying the habitat of extremely small stream organisms - this in turn decreases fish populations. As well, although some introduction of nutrients through sediment is important, too many nutrients can result in harmful extreme algal blooms and [[eutrophication]].&amp;lt;ref name=&amp;quot;RE2&amp;quot;&amp;gt;US EPA. (September 16, 2016). &amp;#039;&amp;#039;What is Sediment Pollution?&amp;#039;&amp;#039; [Online]. Available: http://cfpub.epa.gov/npstbx/files/ksmo_sediment.pdf&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
[[category: Ed edit]]&lt;/div&gt;</summary>
		<author><name>Jmdonev</name></author>
	</entry>
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