<?xml version="1.0" encoding="UTF-8"?><!-- generator="wordpress/2.3.1" -->
<rss version="2.0"
	xmlns:content="http://purl.org/rss/1.0/modules/content/"
	xmlns:dc="http://purl.org/dc/elements/1.1/"
	>
<channel>
	<title>Comments on: Where on (Google) Earth? #82</title>
	<link>http://greengabbro.net/2007/12/25/where-on-google-earth-82/</link>
	<description>rock out to the apparatus</description>
	<pubDate>Tue, 30 Sep 2008 23:52:19 +0000</pubDate>
	<generator>http://wordpress.org/?v=2.3.1</generator>
		<item>
		<title>By: Ron Schott</title>
		<link>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-25087</link>
		<dc:creator>Ron Schott</dc:creator>
		<pubDate>Wed, 02 Jan 2008 02:26:28 +0000</pubDate>
		<guid>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-25087</guid>
		<description>&lt;a href="http://ron.outcrop.org/blog/?p=130" rel="nofollow"&gt;WoGE #83&lt;/a&gt; is up.</description>
		<content:encoded><![CDATA[<p><a href="http://ron.outcrop.org/blog/?p=130" rel="nofollow">WoGE #83</a> is up.</p>
]]></content:encoded>
	</item>
	<item>
		<title>By: Lab Lemming</title>
		<link>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-25049</link>
		<dc:creator>Lab Lemming</dc:creator>
		<pubDate>Tue, 01 Jan 2008 01:27:00 +0000</pubDate>
		<guid>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-25049</guid>
		<description>For some reason, all your posts list as having zero comments when viewing your blog.</description>
		<content:encoded><![CDATA[<p>For some reason, all your posts list as having zero comments when viewing your blog.</p>
]]></content:encoded>
	</item>
	<item>
		<title>By: Lab Lemming</title>
		<link>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-25046</link>
		<dc:creator>Lab Lemming</dc:creator>
		<pubDate>Tue, 01 Jan 2008 01:07:23 +0000</pubDate>
		<guid>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-25046</guid>
		<description>It looks to me like water is running downhill in that photo.  Possibly with a clastic sediment load.</description>
		<content:encoded><![CDATA[<p>It looks to me like water is running downhill in that photo.  Possibly with a clastic sediment load.</p>
]]></content:encoded>
	</item>
	<item>
		<title>By: Ron Schott</title>
		<link>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-24868</link>
		<dc:creator>Ron Schott</dc:creator>
		<pubDate>Thu, 27 Dec 2007 22:19:25 +0000</pubDate>
		<guid>http://greengabbro.net/2007/12/25/where-on-google-earth-82/#comment-24868</guid>
		<description>I'm no fluvial geomorphologist, so I can't tell you too much about why the rivers in this area are alternately braided and meandering, but as a hard rock geologist I can tell you that it has something to do with the 1991 eruption of Mount Pinatubo.  These valleys around the volcano, including &lt;a href="http://ron.outcrop.org/kml/WoGE82.kmz" rel="nofollow"&gt;these on the west side&lt;/a&gt;, were filled with an estimated 4-8 cubic kilometers of pyroclastic material during the cataclysmic eruption on June 15th.  My guess is that in those areas where the pyroclastic material is voluminous enough you tend to get a braided channel morphology; other areas - perhaps where the deposits were not so thick or have already been significantly eroded away - show a meandering character that probably was prevalent prior to the eruption.

It's scary how quick I found this one once I started looking.  The grey colors in the drainages screamed out "recent pyroclastic eruption" and The Philippines was the first place I went looking - probably because of the lushness of the vegetation outside of the floodplains.

Google Scholar offers these references in a search on "&lt;a href="http://scholar.google.com/scholar?hl=en&#38;num=10&#38;as_epq=&#38;as_oq=&#38;as_eq=&#38;lr=&#38;cr=&#38;as_ft=i&#38;as_filetype=&#38;as_qdr=all&#38;as_nlo=&#38;as_nhi=&#38;as_occt=any&#38;as_dt=i&#38;as_sitesearch=&#38;as_rights=&#38;safe=images&#38;q=pinatubo+fluvial+geomorphology&#38;um=1&#38;ie=UTF-8&#38;sa=N&#38;tab=ws" rel="nofollow"&gt;pinatubo fluvial geomorphology&lt;/a&gt;".</description>
		<content:encoded><![CDATA[<p>I&#8217;m no fluvial geomorphologist, so I can&#8217;t tell you too much about why the rivers in this area are alternately braided and meandering, but as a hard rock geologist I can tell you that it has something to do with the 1991 eruption of Mount Pinatubo.  These valleys around the volcano, including <a href="http://ron.outcrop.org/kml/WoGE82.kmz" rel="nofollow">these on the west side</a>, were filled with an estimated 4-8 cubic kilometers of pyroclastic material during the cataclysmic eruption on June 15th.  My guess is that in those areas where the pyroclastic material is voluminous enough you tend to get a braided channel morphology; other areas - perhaps where the deposits were not so thick or have already been significantly eroded away - show a meandering character that probably was prevalent prior to the eruption.</p>
<p>It&#8217;s scary how quick I found this one once I started looking.  The grey colors in the drainages screamed out &#8220;recent pyroclastic eruption&#8221; and The Philippines was the first place I went looking - probably because of the lushness of the vegetation outside of the floodplains.</p>
<p>Google Scholar offers these references in a search on &#8220;<a href="http://scholar.google.com/scholar?hl=en&amp;num=10&amp;as_epq=&amp;as_oq=&amp;as_eq=&amp;lr=&amp;cr=&amp;as_ft=i&amp;as_filetype=&amp;as_qdr=all&amp;as_nlo=&amp;as_nhi=&amp;as_occt=any&amp;as_dt=i&amp;as_sitesearch=&amp;as_rights=&amp;safe=images&amp;q=pinatubo+fluvial+geomorphology&amp;um=1&amp;ie=UTF-8&amp;sa=N&amp;tab=ws" rel="nofollow">pinatubo fluvial geomorphology</a>&#8220;.</p>
]]></content:encoded>
	</item>
</channel>
</rss>
