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	<title>Geology Archives - The Burgess Shale Geoscience Foundation</title>
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	<description>One Of The World&#039;s Most Important Fossil Sites</description>
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		<title>The Geology of the Burgess Shale (Part 3): The Cathedral Escarpment</title>
		<link>https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-the-cathedral-escarpment-part-3/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 09 May 2019 21:28:03 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Geology]]></category>
		<category><![CDATA[Mount Stephen]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
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					<description><![CDATA[<p>A spectacular submarine cliff over 100 metres high &#8211; the Cathedral Escarpment- marked the front of the algal limestones of the Cathedral Formation. The Cathedral Escarpment was initially thought to be a product of prolific algal growth and sediment accumulation during a period of sea level rise. A re-interpretation suggested that the escarpment is the [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-the-cathedral-escarpment-part-3/">The Geology of the Burgess Shale (Part 3): The Cathedral Escarpment</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
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		<title>The Geology of the Burgess Shale (Part 2): What Rocks Tell Us About Life</title>
		<link>https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-what-rocks-tell-us-about-life-part-2/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 18 Apr 2019 22:42:08 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Geology]]></category>
		<category><![CDATA[Mount Stephen]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
		<category><![CDATA[Walcott Quarry]]></category>
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					<description><![CDATA[<p>The picture above features fossil ridge, situated behind and to the right of the hikers; as well as, Mt Wapta, situated behind and slightly to the left of the hikers. The former is where the Walcott Quarry is located.&#160;&#160;Below we describe why fossil ridge and Mount Wapta have mudstone (shale) rocks lower down on the [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-what-rocks-tell-us-about-life-part-2/">The Geology of the Burgess Shale (Part 2): What Rocks Tell Us About Life</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
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		<title>The Geology of the Burgess Shale (Part 1): The Gog Group</title>
		<link>https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-what-lies-beneath-part-1/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Fri, 22 Mar 2019 01:59:21 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Cambrian]]></category>
		<category><![CDATA[Geology]]></category>
		<category><![CDATA[Gog]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=2266</guid>

					<description><![CDATA[<p>The Gog Group underlies the Cambrian rocks where the Burgess Shale fossils are found.  Those of you not wearing a bathing suit and a life preserver would be ill prepared if you somehow found yourself in Yoho National Park in the Cambrian. Beginning in the Early Cambrian (~541 million years ago), sea levels rose and [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-what-lies-beneath-part-1/">The Geology of the Burgess Shale (Part 1): The Gog Group</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
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