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	<title>File:5316 pia17062 Hottah WB-full2conglomerate.jpg - Revision history</title>
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	<updated>2026-07-06T12:34:12Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>http://marspedia.org/index.php?title=File:5316_pia17062_Hottah_WB-full2conglomerate.jpg&amp;diff=127542&amp;oldid=prev</id>
		<title>Suitupandshowup: NASA&#039;s Curiosity rover found evidence for an ancient, flowing stream on Mars at a few sites, including the rock outcrop pictured here, which the science team has named &quot;Hottah&quot; after Hottah Lake in Canada&#039;s Northwest Territories. It may look like a bro...</title>
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		<updated>2018-12-28T23:24:33Z</updated>

		<summary type="html">&lt;p&gt;NASA&amp;#039;s Curiosity rover found evidence for an ancient, flowing stream on Mars at a few sites, including the rock outcrop pictured here, which the science team has named &amp;quot;Hottah&amp;quot; after Hottah Lake in Canada&amp;#039;s Northwest Territories. It may look like a bro...&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;== Summary ==&lt;br /&gt;
NASA&amp;#039;s Curiosity rover found evidence for an ancient, flowing stream on Mars at a few sites, including the rock outcrop pictured here, which the science team has named &amp;quot;Hottah&amp;quot; after Hottah Lake in Canada&amp;#039;s Northwest Territories. It may look like a broken sidewalk, but this geological feature on Mars is actually exposed bedrock made up of smaller fragments cemented together, or what geologists call a sedimentary conglomerate. Scientists theorize that the bedrock was disrupted in the past, giving it the tilted angle, most likely via impacts from meteorites.&lt;br /&gt;
&lt;br /&gt;
Image credit:  NASA/JPL-Caltech/MSSS&lt;br /&gt;
&lt;br /&gt;
Source:  https://mars.nasa.gov/resources/5316/remnants-of-ancient-streambed-on-mars-white-balanced-view/&lt;br /&gt;
== Licensing ==&lt;br /&gt;
{{PD}}&lt;/div&gt;</summary>
		<author><name>Suitupandshowup</name></author>
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