https://marspedia.org/index.php?action=history&feed=atom&title=File%3AB17_016128_1596glaciersmarssocietywithglaciersjpg.jpg 2026-04-19T11:56:19Z Revision history for this page on the wiki MediaWiki 1.34.2 https://marspedia.org/index.php?title=File:B17_016128_1596glaciersmarssocietywithglaciersjpg.jpg&diff=138534&oldid=prev 2021-09-07T22:04:29Z

<p><span dir="auto"><span class="autocomment">Summary</span></span></p> <table class="diff diff-contentalign-left" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #222; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 22:04, 7 September 2021</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1" >Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</td></tr> <tr><td class='diff-marker'> </td><td style="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;"><div>== Summary ==</div></td><td class='diff-marker'> </td><td style="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;"><div>== Summary ==</div></td></tr> <tr><td class='diff-marker'>−</td><td style="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;"><div><del class="diffchange diffchange-inline">Channels from </del>past glaciers in <del class="diffchange diffchange-inline">a </del>crater<del class="diffchange diffchange-inline">, called crater B</del>.  <del class="diffchange diffchange-inline">It is believed that past glaciers that were on </del>the <del class="diffchange diffchange-inline">crater wall made </del>channels <del class="diffchange diffchange-inline">and a lake</del>.  This crater represents another way that lakes can be created in craters.   </div></td><td class='diff-marker'>+</td><td style="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;"><div> </div></td></tr> <tr><td colspan="2"> </td><td class='diff-marker'>+</td><td style="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;"><div><ins class="diffchange diffchange-inline">White parts are where </ins>past glaciers <ins class="diffchange diffchange-inline">were located.  They eventually made channels that formed a lake </ins>in <ins class="diffchange diffchange-inline">the center of the </ins>crater.  <ins class="diffchange diffchange-inline">Now </ins>the channels <ins class="diffchange diffchange-inline">have become inverted</ins>.  This crater represents another way that lakes can be created in craters.   </div></td></tr> <tr><td class='diff-marker'> </td><td style="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;"></td><td class='diff-marker'> </td><td style="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;"></td></tr> <tr><td class='diff-marker'> </td><td style="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;"><div>Source:  http://viewer.mars.asu.edu/planetview/inst/ctx/B17_016128_1596_XI_20S317W#P=B17_016128_1596_XI_20S317W&amp;T=2</div></td><td class='diff-marker'> </td><td style="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;"><div>Source:  http://viewer.mars.asu.edu/planetview/inst/ctx/B17_016128_1596_XI_20S317W#P=B17_016128_1596_XI_20S317W&amp;T=2</div></td></tr> <!-- diff cache key marspediaorg_www-mwmars_:diff::1.12:old-138533:rev-138534 --> </table>

Suitupandshowup https://marspedia.org/index.php?title=File:B17_016128_1596glaciersmarssocietywithglaciersjpg.jpg&diff=138533&oldid=prev 2021-09-07T22:02:22Z

<p>Channels from past glaciers in a crater, called crater B. It is believed that past glaciers that were on the crater wall made channels and a lake. This crater represents another way that lakes can be created in craters. Source: http://viewer.mars.asu.edu/planetview/inst/ctx/B17_016128_1596_XI_20S317W#P=B17_016128_1596_XI_20S317W&amp;T=2 Credit: NASA/MSSS</p> <p><b>New page</b></p><div>== Summary ==<br /> Channels from past glaciers in a crater, called crater B. It is believed that past glaciers that were on the crater wall made channels and a lake. This crater represents another way that lakes can be created in craters. <br /> <br /> Source: http://viewer.mars.asu.edu/planetview/inst/ctx/B17_016128_1596_XI_20S317W#P=B17_016128_1596_XI_20S317W&amp;T=2<br /> <br /> Credit: NASA/MSSS<br /> <br /> == Licensing ==<br /> {{PD}}</div>

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