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	<title>tourmaline Archives - Geology North</title>
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	<title>tourmaline Archives - Geology North</title>
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		<title>Woolhope Crag and the Cheviot</title>
		<link>https://www.geologynorth.uk/woolhope-crag-and-the-cheviot/</link>
		
		<dc:creator><![CDATA[Stephen]]></dc:creator>
		<pubDate>Fri, 23 Aug 2013 21:04:55 +0000</pubDate>
				<category><![CDATA[Uncategorised]]></category>
		<category><![CDATA[boundaries]]></category>
		<category><![CDATA[evolved granite]]></category>
		<category><![CDATA[excursions]]></category>
		<category><![CDATA[fine-grained]]></category>
		<category><![CDATA[Harthope valley]]></category>
		<category><![CDATA[hydrothermal alteration]]></category>
		<category><![CDATA[hypotheses]]></category>
		<category><![CDATA[mafic content]]></category>
		<category><![CDATA[quartz]]></category>
		<category><![CDATA[quartz monzo-diorite]]></category>
		<category><![CDATA[The Cheviot]]></category>
		<category><![CDATA[tourmaline]]></category>
		<category><![CDATA[Wool hope crag]]></category>
		<guid isPermaLink="false">http://www.geologynorth.uk/?p=16867</guid>

					<description><![CDATA[<p>We go to see if the theory of the darker rocks making tougher landscape features, would hold at Woolhope Crag (NT 92264 22169). The answer was ambiguous. There is certainly plenty of dioritic rock there but there is also a pale fine-grained granophyric rock. We subsequently made our way up the north slopes of the &#8230; <a href="https://www.geologynorth.uk/woolhope-crag-and-the-cheviot/" class="more-link">Continue reading <span class="screen-reader-text">Woolhope Crag and the Cheviot</span> <span class="meta-nav">&#8594;</span></a></p>
<p>The post <a rel="nofollow" href="https://www.geologynorth.uk/woolhope-crag-and-the-cheviot/">Woolhope Crag and the Cheviot</a> appeared first on <a rel="nofollow" href="https://www.geologynorth.uk">Geology North</a>.</p>
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										<content:encoded><![CDATA[<p>We go to see if the theory of the darker rocks making tougher landscape features, would hold at Woolhope Crag (NT 92264 22169).<br />
The answer was ambiguous. There is certainly plenty of dioritic rock there but there is also a pale fine-grained granophyric rock. We subsequently made our way up the north slopes of the Cheviot, and found plenty of scattered exposures which revealed more of the granophyric rock. We have classified this type on the map as ‘Evolved’ granite.<br />
Descending from Cheviot summit on the main path for Langlee in the Harthope valley, we found distinct quartz veining with tourmaline content (approx. NT 918 209). There is the possibility that this quartz veining is the result of hydrothermal penetration on lines of weakness between different types of plutonic rock.<br />
We need to pay another visit to investigate this.</p>
<p>The post <a rel="nofollow" href="https://www.geologynorth.uk/woolhope-crag-and-the-cheviot/">Woolhope Crag and the Cheviot</a> appeared first on <a rel="nofollow" href="https://www.geologynorth.uk">Geology North</a>.</p>
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