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		<id>http://wiki.geodynamics.umaine.edu/index.php?action=history&amp;feed=atom&amp;title=Topographic_Anisotropy_Figure_7</id>
		<title>Topographic Anisotropy Figure 7 - Revision history</title>
		<link rel="self" type="application/atom+xml" href="http://wiki.geodynamics.umaine.edu/index.php?action=history&amp;feed=atom&amp;title=Topographic_Anisotropy_Figure_7"/>
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		<updated>2026-10-29T14:40:15Z</updated>
		<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=298&amp;oldid=prev</id>
		<title>Nick at 19:14, 13 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=298&amp;oldid=prev"/>
				<updated>2015-03-13T19:14:12Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 19:14, 13 March 2015&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;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png|center|&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;350px&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png|center|&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;330px&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Nick</name></author>	</entry>

	<entry>
		<id>http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=212&amp;oldid=prev</id>
		<title>Nick at 17:44, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=212&amp;oldid=prev"/>
				<updated>2015-03-10T17:44:00Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 17:44, 10 March 2015&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;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png|center|&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;300px&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png|center|&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;350px&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Nick</name></author>	</entry>

	<entry>
		<id>http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=211&amp;oldid=prev</id>
		<title>Nick at 17:43, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=211&amp;oldid=prev"/>
				<updated>2015-03-10T17:43:53Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 17:43, 10 March 2015&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;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png|center|&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;400px&lt;/del&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png|center|&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;300px&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Nick</name></author>	</entry>

	<entry>
		<id>http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=210&amp;oldid=prev</id>
		<title>Nick at 17:43, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=210&amp;oldid=prev"/>
				<updated>2015-03-10T17:43:48Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 17:43, 10 March 2015&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;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;[[File:Vario figures copy Page 07.png&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;|center|400px&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Nick</name></author>	</entry>

	<entry>
		<id>http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=209&amp;oldid=prev</id>
		<title>Nick at 17:43, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=209&amp;oldid=prev"/>
				<updated>2015-03-10T17:43:36Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 17:43, 10 March 2015&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;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 class=&quot;diffchange diffchange-inline&quot;&gt;[[File:Vario figures copy Page 07.png]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;#160;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude&amp;#160; and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Nick</name></author>	</entry>

	<entry>
		<id>http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=189&amp;oldid=prev</id>
		<title>Nick: Created page with &quot;  '''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single poin...&quot;</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_7&amp;diff=189&amp;oldid=prev"/>
				<updated>2015-03-10T17:29:20Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;  &amp;#039;&amp;#039;&amp;#039;Figure 7&amp;#039;&amp;#039;&amp;#039;: A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single poin...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&lt;br /&gt;
&lt;br /&gt;
'''Figure 7''': A) Plane gently dipping southeast; a simplified replication of low relief planar topography found in Canterbury Plains. B) Anisotropy measured at single point in center of Canterbury Plains delta. Anisotropy measured up to maximum wavelength of 25 km. C) Anisotropy magnitude  and D) orientation map at 1 km, E) F) 5 km, and G) H) 10 km wavelength.&lt;/div&gt;</summary>
		<author><name>Nick</name></author>	</entry>

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