<?xml version="1.0" encoding="UTF-8"?><rss version="2.0"
	xmlns:content="http://purl.org/rss/1.0/modules/content/"
	xmlns:wfw="http://wellformedweb.org/CommentAPI/"
	xmlns:dc="http://purl.org/dc/elements/1.1/"
	xmlns:atom="http://www.w3.org/2005/Atom"
	xmlns:sy="http://purl.org/rss/1.0/modules/syndication/"
	xmlns:slash="http://purl.org/rss/1.0/modules/slash/"
	>

<channel>
	<title>xenolith Archives - Geology North</title>
	<atom:link href="https://www.geologynorth.uk/tag/xenolith/feed/" rel="self" type="application/rss+xml" />
	<link>https://www.geologynorth.uk/tag/xenolith/</link>
	<description>No vestige of a beginning, - no prospect of an end</description>
	<lastBuildDate>Sat, 27 Jun 2020 14:50:06 +0000</lastBuildDate>
	<language>en-GB</language>
	<sy:updatePeriod>
	hourly	</sy:updatePeriod>
	<sy:updateFrequency>
	1	</sy:updateFrequency>
	<generator>https://wordpress.org/?v=6.1.1</generator>

<image>
	<url>https://www.geologynorth.uk/wp-content/uploads/2022/03/Icon-53x53.jpeg</url>
	<title>xenolith Archives - Geology North</title>
	<link>https://www.geologynorth.uk/tag/xenolith/</link>
	<width>32</width>
	<height>32</height>
</image> 
	<item>
		<title>Rigg Cairn, High Cantle to High Bleakhope</title>
		<link>https://www.geologynorth.uk/rigg-cairn-high-cantle-to-high-bleakhope/</link>
		
		<dc:creator><![CDATA[Stephen]]></dc:creator>
		<pubDate>Mon, 03 Nov 2014 16:26:03 +0000</pubDate>
				<category><![CDATA[Uncategorised]]></category>
		<category><![CDATA[course-grained porphyritic]]></category>
		<category><![CDATA[Dunmoor Hill]]></category>
		<category><![CDATA[Great Standrop]]></category>
		<category><![CDATA[High Bleakhope]]></category>
		<category><![CDATA[hornfels]]></category>
		<category><![CDATA[Linhope Spout]]></category>
		<category><![CDATA[Little Standrop]]></category>
		<category><![CDATA[medium-grained porphyritic]]></category>
		<category><![CDATA[quartz monzo-diorite]]></category>
		<category><![CDATA[Rig Cairn]]></category>
		<category><![CDATA[xenolith]]></category>
		<guid isPermaLink="false">http://www.geologynorth.uk/?p=16884</guid>

					<description><![CDATA[<p>We find a coarse-grained granitic rock at NT 94016 16737. This is pinker with fewer large white plagioclase phenocrysts than the rocks of Hedgehope Hill and Great Standrop but it has a similar grain size. Most of the terrain is trackless peat bog lacking any exposure of bedrock.Descending towards High Bleakhope, the pink medium-grained rock &#8230; <a href="https://www.geologynorth.uk/rigg-cairn-high-cantle-to-high-bleakhope/" class="more-link">Continue reading <span class="screen-reader-text">Rigg Cairn, High Cantle to High Bleakhope</span> <span class="meta-nav">&#8594;</span></a></p>
<p>The post <a rel="nofollow" href="https://www.geologynorth.uk/rigg-cairn-high-cantle-to-high-bleakhope/">Rigg Cairn, High Cantle to High Bleakhope</a> appeared first on <a rel="nofollow" href="https://www.geologynorth.uk">Geology North</a>.</p>
]]></description>
										<content:encoded><![CDATA[
<p>We find a coarse-grained granitic rock at NT 94016 16737. This is pinker with fewer large white plagioclase phenocrysts than the rocks of Hedgehope Hill and Great Standrop but it has a similar grain size. Most of the terrain is trackless peat bog lacking any exposure of bedrock.<br>Descending towards High Bleakhope, the pink medium-grained rock outcrops at NT 92469 16365. The outcrops around NT 92643 16262 are all of high colour index and correspond with the dioritic ‘marginal’ variety found on Dunmoor Hill and at Linhope Spout.<br>In places there are xenoliths of what appear to be hornfelsed andesite.</p>
<p>The post <a rel="nofollow" href="https://www.geologynorth.uk/rigg-cairn-high-cantle-to-high-bleakhope/">Rigg Cairn, High Cantle to High Bleakhope</a> appeared first on <a rel="nofollow" href="https://www.geologynorth.uk">Geology North</a>.</p>
]]></content:encoded>
					
		
		
			</item>
	</channel>
</rss>
