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	<id>https://marspedia.org/index.php?action=history&amp;feed=atom&amp;title=Zhurong</id>
	<title>Zhurong - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://marspedia.org/index.php?action=history&amp;feed=atom&amp;title=Zhurong"/>
	<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;action=history"/>
	<updated>2026-06-09T00:44:43Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=142526&amp;oldid=prev</id>
		<title>Suitupshowup: /* Summary */ added more info</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=142526&amp;oldid=prev"/>
		<updated>2025-02-25T19:46:11Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Summary: &lt;/span&gt; added more info&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;
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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 19:46, 25 February 2025&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;div&gt;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&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;Examination of the fine layers of rocks by Zhurong rover, led researchers to interpret them as sedimentary structures typical of formation in a marine environment.  This is evidence for the hypothesis for an ocean in the   Hesperian period.&amp;lt;ref&amp;gt;https://academic.oup.com/nsr/article/10/9/nwad137/7160482&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt; Xiano, L., et al.  2023.    https://academic.oup.com/nsr/article/10/9/nwad137/7160482.  National Science Review, Volume 10, Issue 9, September 2023, nwad137, https://doi.org/10.1093/nsr/nwad137&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;Examination of the fine layers of rocks by Zhurong rover, led researchers to interpret them as sedimentary structures typical of formation in a marine environment.  This is evidence for the hypothesis for an ocean in the   Hesperian period&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;.  The rocks were from the Vastitas Borealis Formation (VBF)&lt;/ins&gt;.&amp;lt;ref&amp;gt;https://academic.oup.com/nsr/article/10/9/nwad137/7160482&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt; Xiano, L., et al.  2023.    https://academic.oup.com/nsr/article/10/9/nwad137/7160482.  National Science Review, Volume 10, Issue 9, September 2023, nwad137, https://doi.org/10.1093/nsr/nwad137&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Suitupshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=142525&amp;oldid=prev</id>
		<title>Suitupshowup: /* Summary */</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=142525&amp;oldid=prev"/>
		<updated>2025-02-25T19:44:21Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Summary&lt;/span&gt;&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 19:44, 25 February 2025&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;div&gt;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&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;Examination of the fine layers of rocks by Zhurong rover, led researchers to interpret &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;these to represent &lt;/del&gt;sedimentary structures typical of formation in a marine environment.  This is evidence for the hypothesis for an ocean in the   Hesperian period.&amp;lt;ref&amp;gt;https://academic.oup.com/nsr/article/10/9/nwad137/7160482&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt; Xiano, L., et al.  2023.    https://academic.oup.com/nsr/article/10/9/nwad137/7160482.  National Science Review, Volume 10, Issue 9, September 2023, nwad137, https://doi.org/10.1093/nsr/nwad137&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;Examination of the fine layers of rocks by Zhurong rover, led researchers to interpret &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;them as &lt;/ins&gt;sedimentary structures typical of formation in a marine environment.  This is evidence for the hypothesis for an ocean in the   Hesperian period.&amp;lt;ref&amp;gt;https://academic.oup.com/nsr/article/10/9/nwad137/7160482&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt; Xiano, L., et al.  2023.    https://academic.oup.com/nsr/article/10/9/nwad137/7160482.  National Science Review, Volume 10, Issue 9, September 2023, nwad137, https://doi.org/10.1093/nsr/nwad137&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Suitupshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=142524&amp;oldid=prev</id>
		<title>Suitupshowup: added new info and ref</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=142524&amp;oldid=prev"/>
		<updated>2025-02-25T19:43:20Z</updated>

		<summary type="html">&lt;p&gt;added new info and 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;
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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 19:43, 25 February 2025&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;/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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&amp;lt;/ref&amp;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;&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;Examination of the fine layers of rocks by Zhurong rover, led researchers to interpret these to represent sedimentary structures typical of formation in a marine environment.  This is evidence for the hypothesis for an ocean in the   Hesperian period.&amp;lt;ref&amp;gt;https://academic.oup.com/nsr/article/10/9/nwad137/7160482&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt; Xiano, L., et al.  2023.    https://academic.oup.com/nsr/article/10/9/nwad137/7160482.  National Science Review, Volume 10, Issue 9, September 2023, nwad137, https://doi.org/10.1093/nsr/nwad137&amp;lt;/ref&amp;gt;&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&amp;lt;/ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Suitupshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=142521&amp;oldid=prev</id>
		<title>Suitupshowup: /* Summary */ added ref and new info supporting an ocean</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=142521&amp;oldid=prev"/>
		<updated>2025-02-25T13:57:47Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Summary: &lt;/span&gt; added ref and new info supporting an ocean&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 13:57, 25 February 2025&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;/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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&amp;lt;/ref&amp;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;&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;A large team of researchers announced the discovery of beaches near Zhurong.  Radar on the rover found beds that slope the same amount as beds on the Earth.  These beaches support the idea of a large ocean on the north end of the planet.&amp;lt;ref&amp;gt;Penn State. &amp;quot;Gulf of Mars: Rover finds evidence of 'vacation-style' beaches on Mars.&amp;quot; ScienceDaily. ScienceDaily, 24 February 2025. &amp;lt;www.sciencedaily.com/releases/2025/02/250224155110.htm&amp;gt;.&amp;lt;/ref&amp;gt;  &amp;lt;ref&amp;gt;Jianhui Li, Hai Liu, Xu Meng, Diwen Duan, Haijing Lu, Jinhai Zhang, Fengshou Zhang, Derek Elsworth, Benjamin T. Cardenas, Michael Manga, Bin Zhou, Guangyou Fang. Ancient ocean coastal deposits imaged on Mars. Proceedings of the National Academy of Sciences, 2025; 122 (9) DOI: 10.1073/pnas.2422213122&amp;lt;/ref&amp;gt;&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;==Technical Innovations==&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;==Technical Innovations==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Suitupshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=140176&amp;oldid=prev</id>
		<title>Suitupshowup: /* Summary */ added new info and ref</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=140176&amp;oldid=prev"/>
		<updated>2023-08-12T22:43:18Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Summary: &lt;/span&gt; added new info and ref&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 22:43, 12 August 2023&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-l15&quot; &gt;Line 15:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 15:&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;Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it, and then the water could carry dissolved minerals around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it, and then the water could carry dissolved minerals around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&amp;lt;/ref&amp;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;&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;China's Zhurong rover that has studied the Utopia Planitia region of Mars has found dunes that lie in different directions. That different set of directions means that the wind direction made about a 70 degree change in direction.  The researchers found that the dunes were formed when the tilt changed and caused a shift in the winds.  At about the same time, layers in the Martian northern ice caps show a change.&amp;lt;ref&amp;gt;Liu, J., et al.  2023. Martian dunes indicative of wind regime shift in line with end of ice age.  Nature&amp;lt;/ref&amp;gt;&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;==Technical Innovations==&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;==Technical Innovations==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Suitupshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=139956&amp;oldid=prev</id>
		<title>RichardWSmith: /* Technical Innovations */ grammar</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=139956&amp;oldid=prev"/>
		<updated>2023-02-28T00:21:50Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Technical Innovations: &lt;/span&gt; grammar&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 00:21, 28 February 2023&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;/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;==Technical Innovations==&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;==Technical Innovations==&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: #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;Under two circular windows are ten containers which hold N-undecane (a chemical used as sex pheromone by cockroaches and moths), which will melt in the Martian day time, and freeze at night.  This chemical has a high heat of fusion, so it will release a fair amount of heat just when the Martian night is getting coldest.  It was hoped that this would prolong the life of the Rover by keeping batteries and key electronics warmer at night.&amp;lt;ref&amp;gt;https://twitter.com/CNDeepSpace/status/1478755108074627074&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;Under two circular windows are ten containers which hold N-undecane (a chemical used as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a &lt;/ins&gt;sex pheromone by cockroaches and moths), which will melt in the Martian day time, and freeze at night.  This chemical has a high heat of fusion, so it will release a fair amount of heat just when the Martian night is getting coldest.  It was hoped that this would prolong the life of the Rover by keeping batteries and key electronics warmer at night.&amp;lt;ref&amp;gt;https://twitter.com/CNDeepSpace/status/1478755108074627074&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;==End of Mission==&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;==End of Mission==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-139955:rev-139956 --&gt;
&lt;/table&gt;</summary>
		<author><name>RichardWSmith</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=139955&amp;oldid=prev</id>
		<title>RichardWSmith: Is Zhurong dead?  Added section on technical innovations.</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=139955&amp;oldid=prev"/>
		<updated>2023-02-28T00:20:28Z</updated>

		<summary type="html">&lt;p&gt;Is Zhurong dead?  Added section on technical innovations.&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 00:20, 28 February 2023&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;Zhurong is a six-wheeled rover built by China.  It landed on Mars in the area called Utopia Planitia on May 14, 2021.   Zhurong is about the size of NASA's twin Mars rovers Spirit and Opportunity.  It has six scientific instruments, including two panoramic cameras, a ground-penetrating radar and a magnetic field detector. Like America's Curiosity and Perseverance Martian rovers, Zhurong  has a laser to zap rocks and thereby study their compositions.&amp;lt;ref&amp;gt;https://www.space.com/china-mars-rover-landing-success-tianwen-1-zhurong&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;Zhurong is a six-wheeled rover built by China.  It landed on Mars in the area called Utopia Planitia on May 14, 2021.   Zhurong is about the size of NASA's twin Mars rovers Spirit and Opportunity.  It has six scientific instruments, including two panoramic cameras, a ground-penetrating radar and a magnetic field detector. Like America's Curiosity and Perseverance Martian rovers, Zhurong  has a laser to zap rocks and thereby study their compositions.&amp;lt;ref&amp;gt;https://www.space.com/china-mars-rover-landing-success-tianwen-1-zhurong&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 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;==Summary==&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;div&gt;&amp;lt;gallery class=&amp;quot;center&amp;quot;  widths=&amp;quot;380px&amp;quot; heights=&amp;quot;360px&amp;quot;&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;&amp;lt;gallery class=&amp;quot;center&amp;quot;  widths=&amp;quot;380px&amp;quot; heights=&amp;quot;360px&amp;quot;&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 colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 12:&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;&amp;lt;/gallery&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;&amp;lt;/gallery&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.  &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it, and then the water could carry dissolved minerals around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.   &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 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;Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it, and then the water could carry dissolved minerals around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&amp;lt;/ref&amp;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;&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;==Technical Innovations==&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;Under two circular windows are ten containers which hold N-undecane (a chemical used as sex pheromone by cockroaches and moths), which will melt in the Martian day time, and freeze at night.  This chemical has a high heat of fusion, so it will release a fair amount of heat just when the Martian night is getting coldest.  It was hoped that this would prolong the life of the Rover by keeping batteries and key electronics warmer at night.&amp;lt;ref&amp;gt;https://twitter.com/CNDeepSpace/status/1478755108074627074&amp;lt;/ref&amp;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;&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;==End of Mission==&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;Solar cells have a short life on Mars (due to dust build up), and as of late February, 2023, the Zhurong rover has been immobile for months.  It should have woken up last month.  Zhurong had anti dust coatings on its solar cells, but moving dust on Mars builds up static charges which cause them to stick to surfaces strongly.  China has not announced the end of the mission, so perhaps the engineers hope that the rover may still recover.&amp;lt;ref&amp;gt;https://www.nature.com/articles/d41586-023-00111-3&amp;lt;/ref&amp;gt;&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;div&gt;== References ==&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;== References ==&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;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138962:rev-139955 --&gt;
&lt;/table&gt;</summary>
		<author><name>RichardWSmith</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=138962&amp;oldid=prev</id>
		<title>Suitupandshowup at 16:00, 13 May 2022</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=138962&amp;oldid=prev"/>
		<updated>2022-05-13T16:00:13Z</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 16:00, 13 May 2022&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-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&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;&amp;lt;/gallery&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;&amp;lt;/gallery&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.  Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it and then the water could carry dissolved minerals around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.  Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, &lt;/ins&gt;and then the water could carry dissolved minerals around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;== References ==&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;== References ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138961:rev-138962 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=138961&amp;oldid=prev</id>
		<title>Suitupandshowup at 15:59, 13 May 2022</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=138961&amp;oldid=prev"/>
		<updated>2022-05-13T15:59:34Z</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 15:59, 13 May 2022&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-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&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;&amp;lt;/gallery&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;&amp;lt;/gallery&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.  Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it and then the water could carry dissolved &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;mineral &lt;/del&gt;around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.  Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it and then the water could carry dissolved &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;minerals &lt;/ins&gt;around.  The minerals could then be deposited when water evaporated.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;== References ==&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;== References ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138960:rev-138961 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
	<entry>
		<id>https://marspedia.org/index.php?title=Zhurong&amp;diff=138960&amp;oldid=prev</id>
		<title>Suitupandshowup at 15:58, 13 May 2022</title>
		<link rel="alternate" type="text/html" href="https://marspedia.org/index.php?title=Zhurong&amp;diff=138960&amp;oldid=prev"/>
		<updated>2022-05-13T15:58:47Z</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 15:58, 13 May 2022&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-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&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;&amp;lt;/gallery&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;&amp;lt;/gallery&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;Research published in May, 2022 described chemical evidence for water discovered by the Zhurong Rover.   Hydrated sulfate/silica materials were identified on the Amazonian-age terrain at the landing site. These hydrated minerals were found in bright-toned rocks.  Authors of the research interpreted these minerals to be from a &amp;quot;duricrust.&amp;quot;  The duricrust was formed either by groundwater rising or subsurface ice melting. This duricrust was created just under the surface,and then was uncovered by erosion&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;.  Finding these minerals here suggests that water may have been present at later times then thought.  Perhaps liquid water appeared after impacts or from hot magma under the surface.  We know there is much ice under the surface and any heat might melt it and then the water could carry dissolved mineral around.  The minerals could then be deposited when water evaporated&lt;/ins&gt;.&amp;lt;ref&amp;gt;https://www.science.org/doi/10.1126/sciadv.abn8555&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt;Liu, Y., et al.  2022.  Zhurong reveals recent aqueous activities in Utopia Planitia, Mars.  Science Advances.  VOL. 8, NO. 19&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;== References ==&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;== References ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

&lt;!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138959:rev-138960 --&gt;
&lt;/table&gt;</summary>
		<author><name>Suitupandshowup</name></author>
		
	</entry>
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