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	<title>Comments on: Geopuzzle: What are these things? (UPDATED)</title>
	<atom:link href="http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/feed/" rel="self" type="application/rss+xml" />
	<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/</link>
	<description>A blog about sedimentary geology.</description>
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		<title>By: Kyle House</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6146</link>
		<dc:creator><![CDATA[Kyle House]]></dc:creator>
		<pubDate>Tue, 08 Dec 2009 01:39:50 +0000</pubDate>
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		<description><![CDATA[Obviously clay pigeons. Imagine an aghast Kennewick-ish man at shooting practice when a giant flood from Montana rolls in. (?)

Symmetry is troubling for a primary feature. In any case, I want one.]]></description>
		<content:encoded><![CDATA[<p>Obviously clay pigeons. Imagine an aghast Kennewick-ish man at shooting practice when a giant flood from Montana rolls in. (?)</p>
<p>Symmetry is troubling for a primary feature. In any case, I want one.</p>
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		<title>By: lockwooddewitt</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6145</link>
		<dc:creator><![CDATA[lockwooddewitt]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 23:30:16 +0000</pubDate>
		<guid isPermaLink="false">http://clasticdetritus.com/?p=2832#comment-6145</guid>
		<description><![CDATA[Not too far from Howard&#039;s Okanagan Valley, and a similar looking environment.]]></description>
		<content:encoded><![CDATA[<p>Not too far from Howard&#8217;s Okanagan Valley, and a similar looking environment.</p>
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		<title>By: BrianR</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6144</link>
		<dc:creator><![CDATA[BrianR]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 23:24:15 +0000</pubDate>
		<guid isPermaLink="false">http://clasticdetritus.com/?p=2832#comment-6144</guid>
		<description><![CDATA[This site is along the Pend Oreille River near the town of Ione, Washington. Again, sorry about the confusion ... but those of you who felt confused can feel good about your geo-instincts!]]></description>
		<content:encoded><![CDATA[<p>This site is along the Pend Oreille River near the town of Ione, Washington. Again, sorry about the confusion &#8230; but those of you who felt confused can feel good about your geo-instincts!</p>
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		<title>By: Brian</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6143</link>
		<dc:creator><![CDATA[Brian]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 23:05:24 +0000</pubDate>
		<guid isPermaLink="false">http://clasticdetritus.com/?p=2832#comment-6143</guid>
		<description><![CDATA[Hey everybody ... my bad, the site is in NE Washington. Sorry about that.]]></description>
		<content:encoded><![CDATA[<p>Hey everybody &#8230; my bad, the site is in NE Washington. Sorry about that.</p>
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		<title>By: lockwooddewitt</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6142</link>
		<dc:creator><![CDATA[lockwooddewitt]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 21:53:43 +0000</pubDate>
		<guid isPermaLink="false">http://clasticdetritus.com/?p=2832#comment-6142</guid>
		<description><![CDATA[Following up on Andrew&#039;s comment, Missoula Flood beds were what came to my mind as well, but I was and am uncertain that 10 Ka would be enough time to get concretions of that size.  Anne, you&#039;ve spent some time looking at this stuff, haven&#039;t you?  Have you ever seen concretions in Missoula sediments?]]></description>
		<content:encoded><![CDATA[<p>Following up on Andrew&#8217;s comment, Missoula Flood beds were what came to my mind as well, but I was and am uncertain that 10 Ka would be enough time to get concretions of that size.  Anne, you&#8217;ve spent some time looking at this stuff, haven&#8217;t you?  Have you ever seen concretions in Missoula sediments?</p>
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		<title>By: Andrew</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6141</link>
		<dc:creator><![CDATA[Andrew]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 21:29:57 +0000</pubDate>
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		<description><![CDATA[I think you&#039;re misleading us by calling this exposure an outcrop of rocks. It looks like floppy sloppy lake beds, or Missoula Flood beds, east of the Wallula Gap. These would be clean silts with a component of fresh basalt particles, which would release calcium and iron promoting cementation. It&#039;s hard to tell, but it looks like the concretions are restricted to a few horizons. I&#039;ll bet these hockey pucks have very little strength. There would be no diagenesis. I also note that there are several dogbone concretions, where two grew together.

People in my forum bring me concretions all the time; I add them to &lt;a href=&quot;http://geology.about.com/od/more_sedrocks/ig/concretionpics/&quot; rel=&quot;nofollow&quot;&gt;my photo collection&lt;/a&gt;.]]></description>
		<content:encoded><![CDATA[<p>I think you&#8217;re misleading us by calling this exposure an outcrop of rocks. It looks like floppy sloppy lake beds, or Missoula Flood beds, east of the Wallula Gap. These would be clean silts with a component of fresh basalt particles, which would release calcium and iron promoting cementation. It&#8217;s hard to tell, but it looks like the concretions are restricted to a few horizons. I&#8217;ll bet these hockey pucks have very little strength. There would be no diagenesis. I also note that there are several dogbone concretions, where two grew together.</p>
<p>People in my forum bring me concretions all the time; I add them to <a href="http://geology.about.com/od/more_sedrocks/ig/concretionpics/" rel="nofollow">my photo collection</a>.</p>
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		<title>By: Anne Jefferson</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6140</link>
		<dc:creator><![CDATA[Anne Jefferson]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 21:00:28 +0000</pubDate>
		<guid isPermaLink="false">http://clasticdetritus.com/?p=2832#comment-6140</guid>
		<description><![CDATA[I&#039;m with Lockwood in wanting to know more specifically where these are located, because flat siltstones do not jibe with mental geologic map of Oregon Are we looking at another Anthropocene stratigraphic marker - the skeet-shooting clay pigeon layer?]]></description>
		<content:encoded><![CDATA[<p>I&#8217;m with Lockwood in wanting to know more specifically where these are located, because flat siltstones do not jibe with mental geologic map of Oregon Are we looking at another Anthropocene stratigraphic marker &#8211; the skeet-shooting clay pigeon layer?</p>
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		<title>By: Howard Allen</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6139</link>
		<dc:creator><![CDATA[Howard Allen]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 20:44:20 +0000</pubDate>
		<guid isPermaLink="false">http://clasticdetritus.com/?p=2832#comment-6139</guid>
		<description><![CDATA[Concretions, possibly calcareous, possibly nucleated by mollusc shells (that lowermost object in the third close-up photo looks suspiciously like a clam valve, but maybe just a superficial resemblance). The deposits could be lacustrine; very similar-looking beds with very similar-looking concretions occur in south-central British Columbia (Okanagan Valley); there they are Quaternary lake bed deposits.]]></description>
		<content:encoded><![CDATA[<p>Concretions, possibly calcareous, possibly nucleated by mollusc shells (that lowermost object in the third close-up photo looks suspiciously like a clam valve, but maybe just a superficial resemblance). The deposits could be lacustrine; very similar-looking beds with very similar-looking concretions occur in south-central British Columbia (Okanagan Valley); there they are Quaternary lake bed deposits.</p>
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		<title>By: lockwooddewitt</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6138</link>
		<dc:creator><![CDATA[lockwooddewitt]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 17:53:34 +0000</pubDate>
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		<description><![CDATA[I&#039;m going with concretions as well.  Odd shapes such as these ellipsoids are pretty common.  It also looks as if there are distinct horizons where the objects are forming, which is, again, typical for concretions.

My only puzzlement is that in the far NE portion of the state, I don&#039;t know of mudstones/siltstones like this... almost everything is igneous or metamorphic.  And almost everything older than the CRB is seriously deformed. Did your reader say more specifically what the location is?]]></description>
		<content:encoded><![CDATA[<p>I&#8217;m going with concretions as well.  Odd shapes such as these ellipsoids are pretty common.  It also looks as if there are distinct horizons where the objects are forming, which is, again, typical for concretions.</p>
<p>My only puzzlement is that in the far NE portion of the state, I don&#8217;t know of mudstones/siltstones like this&#8230; almost everything is igneous or metamorphic.  And almost everything older than the CRB is seriously deformed. Did your reader say more specifically what the location is?</p>
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		<title>By: quantum_flux</title>
		<link>http://clasticdetritus.com/2009/12/07/geopuzzle-what-are-these-things/#comment-6137</link>
		<dc:creator><![CDATA[quantum_flux]]></dc:creator>
		<pubDate>Mon, 07 Dec 2009 17:38:03 +0000</pubDate>
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		<description><![CDATA[....oh, the round ones look like river rocks of some sort, perhaps rounded out cement from abrasive silty erosion from upstream?]]></description>
		<content:encoded><![CDATA[<p>&#8230;.oh, the round ones look like river rocks of some sort, perhaps rounded out cement from abrasive silty erosion from upstream?</p>
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