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	<id>http://marspedia.org/index.php?action=history&amp;feed=atom&amp;title=Sapping</id>
	<title>Sapping - Revision history</title>
	<link rel="self" type="application/atom+xml" href="http://marspedia.org/index.php?action=history&amp;feed=atom&amp;title=Sapping"/>
	<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;action=history"/>
	<updated>2026-05-06T01:12:06Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.34.2</generator>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138171&amp;oldid=prev</id>
		<title>Suitupandshowup: tried to add picture</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138171&amp;oldid=prev"/>
		<updated>2021-08-16T17:44:55Z</updated>

		<summary type="html">&lt;p&gt;tried to add picture&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 17:44, 16 August 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-l4&quot; &gt;Line 4:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 4:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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:Nirgal Vallis Close-up.JPG|thumb|left|300px|Probable valleys made by sapping  Close-up of Nirgal Vallis, as seen by themis. Location is 27.6 S and 315.2 E. Image is 18.3 km wide.]]&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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.&amp;lt;ref&amp;gt;Gulick, V.  2001.  Origin of the Valley Networks on Mars: a Hydrological Perspective.   Geomorphology.  volume = 37.  issue = 3–4.  41–268&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Sharp, R. P., &amp;amp; Malin, M. C. 1975.  Channels on Mars. Geological Society of America Bulletin.  86(5).  593–609.&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.&amp;lt;ref&amp;gt;Gulick, V.  2001.  Origin of the Valley Networks on Mars: a Hydrological Perspective.   Geomorphology.  volume = 37.  issue = 3–4.  41–268&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Sharp, R. P., &amp;amp; Malin, M. C. 1975.  Channels on Mars. Geological Society of America Bulletin.  86(5).  593–609.&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138170:rev-138171 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138170&amp;oldid=prev</id>
		<title>Suitupandshowup: /* External links */ added to list</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138170&amp;oldid=prev"/>
		<updated>2021-08-16T17:41:22Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;External links: &lt;/span&gt; added to list&lt;/span&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 17:41, 16 August 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-l20&quot; &gt;Line 20:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;* [https://www.youtube.com/watch?v=cVuXQTnEd3Y Ground water erosion]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;* [https://www.youtube.com/watch?v=cVuXQTnEd3Y Ground water erosion]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;* [https://www.youtube.com/watch?v=sVM2w6jeI-g  Groundwater seepage landscapes from local or distal sources in experiments and on Mars]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138164:rev-138170 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138164&amp;oldid=prev</id>
		<title>Suitupandshowup: added ref</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138164&amp;oldid=prev"/>
		<updated>2021-08-14T19:00:40Z</updated>

		<summary type="html">&lt;p&gt;added ref&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 19:00, 14 August 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-l5&quot; &gt;Line 5:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 5:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.&amp;lt;ref&amp;gt;Gulick, V.  2001.  Origin of the Valley Networks on Mars: a Hydrological Perspective.   Geomorphology.  volume = 37.  issue = 3–4.  41–268&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.&amp;lt;ref&amp;gt;Gulick, V.  2001.  Origin of the Valley Networks on Mars: a Hydrological Perspective.   Geomorphology.  volume = 37.  issue = 3–4.  41–268&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Sharp, R. P., &amp;amp; Malin, M. C. 1975.  Channels on Mars. Geological Society of America Bulletin.  86(5).  593–609.&lt;/ins&gt;&amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;==See also==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;==See also==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138141:rev-138164 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138141&amp;oldid=prev</id>
		<title>Suitupandshowup: /* External links */ added to list</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138141&amp;oldid=prev"/>
		<updated>2021-08-13T22:03:37Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;External links: &lt;/span&gt; added to list&lt;/span&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 22:03, 13 August 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-l18&quot; &gt;Line 18:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 18:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;* [https://www.youtube.com/watch?v=zHMhX1u-_Dk) – What is GROUNDWATER SAPPING? What does GROUNDWATER SAPPING mean? GROUNDWATER SAPPING meaning]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;* [https://www.youtube.com/watch?v=zHMhX1u-_Dk) – What is GROUNDWATER SAPPING? What does GROUNDWATER SAPPING mean? GROUNDWATER SAPPING meaning]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;* [https://www.youtube.com/watch?v=cVuXQTnEd3Y Ground water erosion]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138140:rev-138141 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138140&amp;oldid=prev</id>
		<title>Suitupandshowup: /* External links */ added to list</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138140&amp;oldid=prev"/>
		<updated>2021-08-13T22:01:40Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;External links: &lt;/span&gt; added to list&lt;/span&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
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				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 22:01, 13 August 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-l17&quot; &gt;Line 17:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 17:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;== External links ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;== External links ==&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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;* [https://www.youtube.com/watch?v=&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Jr1Xu2i&lt;/del&gt;-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Uc0 Video (04:32&lt;/del&gt;) – &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Evidence: Water &amp;quot;Vigorously&amp;quot; Flowed On Mars – September, 2012&lt;/del&gt;]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;* [https://www.youtube.com/watch?v=&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;zHMhX1u&lt;/ins&gt;-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;_Dk&lt;/ins&gt;) – &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;What is GROUNDWATER SAPPING? What does GROUNDWATER SAPPING mean? GROUNDWATER SAPPING meaning&lt;/ins&gt;]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138139:rev-138140 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138139&amp;oldid=prev</id>
		<title>Suitupandshowup at 21:58, 13 August 2021</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138139&amp;oldid=prev"/>
		<updated>2021-08-13T21:58:51Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 21:58, 13 August 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;
&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: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Rosenberry &lt;/del&gt;, D. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;  Ground-water Sapping &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the Generation of Natural Ampitheaters&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; University of Colorado websit &lt;/del&gt;&amp;lt;/ref&amp;gt; &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;. &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places&lt;/ins&gt;. &amp;lt;ref&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;gt;Nash&lt;/ins&gt;, D. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; 1996.  GROUNDWATER SAPPING AND VALLEY DEVELOPMENT IN THE HACKNESS HILLS, NORTH YORKSHIRE, ENGLAND.  Earth Surface Processes &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;LandformsVolume 21, Issue 9 p&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;781-795&lt;/ins&gt;&amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places. &lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138138&amp;oldid=prev</id>
		<title>Suitupandshowup at 21:58, 13 August 2021</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138138&amp;oldid=prev"/>
		<updated>2021-08-13T21:58:09Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 21:58, 13 August 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;
&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;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;gt;   &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;ref&amp;gt;Nash, D.  1996.  GROUNDWATER SAPPING AND VALLEY DEVELOPMENT IN THE HACKNESS HILLS, NORTH YORKSHIRE, ENGLAND.  Earth Surface Processes and LandformsVolume 21, Issue 9 p. 781-795&amp;lt;/ref&amp;gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places.  &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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138137&amp;oldid=prev</id>
		<title>Suitupandshowup at 21:57, 13 August 2021</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138137&amp;oldid=prev"/>
		<updated>2021-08-13T21:57:23Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 21:57, 13 August 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;
&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;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;gt;   &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;ref&amp;gt;https://onlinelibrary.wiley.com/doi/abs/10.1002/%28SICI%291096-9837%28199609%2921%3A9%3C781%3A%3AAID-ESP616%3E3.0.CO%3B2-O&amp;lt;/ref&amp;gt;  &lt;/del&gt;&amp;lt;ref&amp;gt;Nash, D.  1996.  GROUNDWATER SAPPING AND VALLEY DEVELOPMENT IN THE HACKNESS HILLS, NORTH YORKSHIRE, ENGLAND.  Earth Surface Processes and LandformsVolume 21, Issue 9 p. 781-795&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places. &amp;lt;ref&amp;gt;Nash, D.  1996.  GROUNDWATER SAPPING AND VALLEY DEVELOPMENT IN THE HACKNESS HILLS, NORTH YORKSHIRE, ENGLAND.  Earth Surface Processes and LandformsVolume 21, Issue 9 p. 781-795&amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138136:rev-138137 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138136&amp;oldid=prev</id>
		<title>Suitupandshowup at 21:56, 13 August 2021</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138136&amp;oldid=prev"/>
		<updated>2021-08-13T21:56:46Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 21:56, 13 August 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;
&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;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;gt;   &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places.&amp;lt;ref&amp;gt;https://onlinelibrary.wiley.com/doi/abs/10.1002/%28SICI%291096-9837%28199609%2921%3A9%3C781%3A%3AAID-ESP616%3E3.0.CO%3B2-O&amp;lt;/ref &amp;lt;ref&amp;gt;Nash, D.  1996. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;  Groundwater Sapping and Valley Development in the Hackness Hills&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;North Yorkshire&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;England&lt;/del&gt;.  &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;volume  &lt;/del&gt;21&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;.  issue  &lt;/del&gt;9. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;781–795&lt;/del&gt;&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places.&amp;lt;ref&amp;gt;https://onlinelibrary.wiley.com/doi/abs/10.1002/%28SICI%291096-9837%28199609%2921%3A9%3C781%3A%3AAID-ESP616%3E3.0.CO%3B2-O&amp;lt;/ref&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;gt;  &lt;/ins&gt;&amp;lt;ref&amp;gt;Nash, D.  1996. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; GROUNDWATER SAPPING AND VALLEY DEVELOPMENT IN THE HACKNESS HILLS&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;NORTH YORKSHIRE&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;ENGLAND&lt;/ins&gt;.  &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Earth Surface Processes and LandformsVolume &lt;/ins&gt;21&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, Issue &lt;/ins&gt;9 &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;p&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;781-795&lt;/ins&gt;&amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138135:rev-138136 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>http://marspedia.org/index.php?title=Sapping&amp;diff=138135&amp;oldid=prev</id>
		<title>Suitupandshowup at 21:54, 13 August 2021</title>
		<link rel="alternate" type="text/html" href="http://marspedia.org/index.php?title=Sapping&amp;diff=138135&amp;oldid=prev"/>
		<updated>2021-08-13T21:54:40Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 21:54, 13 August 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;
&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;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;gt;   &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;Sapping is a type of erosion where the ground seems to have collapsed into wide valleys.  Steep-sided U-shaped valleys of fairly uniform width with box-like, &amp;quot;theater-shaped&amp;quot; headwalls are characteristic of sapping. &amp;lt;ref&amp;gt;Kocher, R. and J. Piper.  1986.   Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys.   Journal of Geophysical Research.  volume = 91.  Issue = B13|pages = 175–192.&amp;lt;/ref&amp;gt;  Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. &amp;lt;ref Rosenberry , D.   Ground-water Sapping and the Generation of Natural Ampitheaters.  University of Colorado websit &amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places.&amp;lt;ref&amp;gt;Nash, D.  1996.   Groundwater Sapping and Valley Development in the Hackness Hills, North Yorkshire, England.  volume  21.  issue  9. 781–795&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; 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;Valleys made by sapping occur throughout the world including in  England, Colorado, Hawai’i, New Zealand, and other places.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;ref&amp;gt;https://onlinelibrary.wiley.com/doi/abs/10.1002/%28SICI%291096-9837%28199609%2921%3A9%3C781%3A%3AAID-ESP616%3E3.0.CO%3B2-O&amp;lt;/ref &lt;/ins&gt;&amp;lt;ref&amp;gt;Nash, D.  1996.   Groundwater Sapping and Valley Development in the Hackness Hills, North Yorkshire, England.  volume  21.  issue  9. 781–795&amp;lt;/ref&amp;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;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; 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:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138134:rev-138135 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
</feed>