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		<id>http://wiki.geodynamics.umaine.edu/index.php?action=history&amp;feed=atom&amp;title=Topographic_Anisotropy_Figure_6</id>
		<title>Topographic Anisotropy Figure 6 - Revision history</title>
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		<updated>2026-10-29T19:01:13Z</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_6&amp;diff=297&amp;oldid=prev</id>
		<title>Nick at 19:13, 13 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_6&amp;diff=297&amp;oldid=prev"/>
				<updated>2015-03-13T19:13:50Z</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 19:13, 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 06.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 06.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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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_6&amp;diff=207&amp;oldid=prev</id>
		<title>Nick at 17:42, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_6&amp;diff=207&amp;oldid=prev"/>
				<updated>2015-03-10T17:42:55Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&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 17:42, 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 06.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 06.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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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_6&amp;diff=206&amp;oldid=prev</id>
		<title>Nick at 17:42, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_6&amp;diff=206&amp;oldid=prev"/>
				<updated>2015-03-10T17:42:44Z</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 17:42, 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 06.png|center|&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;500px&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 06.png|center|&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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_6&amp;diff=205&amp;oldid=prev</id>
		<title>Nick at 17:42, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_6&amp;diff=205&amp;oldid=prev"/>
				<updated>2015-03-10T17:42:36Z</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 17:42, 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 06.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 06.png&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;|center|500px&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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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_6&amp;diff=204&amp;oldid=prev</id>
		<title>Nick at 17:42, 10 March 2015</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_6&amp;diff=204&amp;oldid=prev"/>
				<updated>2015-03-10T17:42:21Z</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 17:42, 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 06.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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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_6&amp;diff=188&amp;oldid=prev</id>
		<title>Nick: Created page with &quot;  '''Figure 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in...&quot;</title>
		<link rel="alternate" type="text/html" href="http://wiki.geodynamics.umaine.edu/index.php?title=Topographic_Anisotropy_Figure_6&amp;diff=188&amp;oldid=prev"/>
				<updated>2015-03-10T17:28:39Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;  &amp;#039;&amp;#039;&amp;#039;Figure 6&amp;#039;&amp;#039;&amp;#039;: A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in...&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 6''': A) Low relief trough bisecting high relief plateau; a simplified replication of fault damage influenced topography. B) Anisotropy measured at single point in Marlborough. Anisotropy measured up to maximum wavelength of 37.5 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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