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	<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?action=history&amp;feed=atom&amp;title=Caryn_Peak</id>
	<title>Caryn Peak - Revision history</title>
	<link rel="self" type="application/atom+xml" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?action=history&amp;feed=atom&amp;title=Caryn_Peak"/>
	<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;action=history"/>
	<updated>2026-07-04T21:57:00Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.35.1</generator>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1906&amp;oldid=prev</id>
		<title>EWImportBoss: 10 revisions imported</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1906&amp;oldid=prev"/>
		<updated>2021-01-30T09:44:41Z</updated>

		<summary type="html">&lt;p&gt;10 revisions imported&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 09:44, 30 January 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>EWImportBoss</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=193&amp;oldid=prev</id>
		<title>EWImportBoss: 1 revision imported</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=193&amp;oldid=prev"/>
		<updated>2021-01-30T09:21:13Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 09:21, 30 January 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>EWImportBoss</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1905&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 11:02, 19 May 2006</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1905&amp;oldid=prev"/>
		<updated>2006-05-19T11:02:18Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 11:02, 19 May 2006&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=192&amp;oldid=prev</id>
		<title>Import&gt;DianeDuane at 11:02, 19 May 2006</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=192&amp;oldid=prev"/>
		<updated>2006-05-19T11:02:18Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 11:02, 19 May 2006&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea [[Sohm Abyssal Plain]] at the very end of [[Hudson Canyon]], and is the place where the [[Twelve, Song of the | Song of the Twelve]] is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea [[Sohm Abyssal Plain]] at the very end of [[Hudson Canyon]], and is the place where the [[Twelve, Song of the | Song of the Twelve]] is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the [[Kelvin Seamounts]] (or more recently, the [[New England Seamounts]]), which rise from the ocean floor off the east coast of North America.  The [[Cetacean | cetacean]] name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Image:Caryn_Peak.jpg|left|thumb|200px|Caryn Peak]]&lt;/ins&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the [[Kelvin Seamounts]] (or more recently, the [[New England Seamounts]]), which rise from the ocean floor off the east coast of North America.  The [[Cetacean | cetacean]] name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Image:Houghton_600.jpg|right|thumb|200px|Caryn Peak, [[Sohm Abyssal Plain]], and [[Kelvin Seamounts]]]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Image:Houghton_600.jpg|right|thumb|200px|Caryn Peak, [[Sohm Abyssal Plain]], and [[Kelvin Seamounts]]]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Import&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1904&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 10:53, 19 May 2006</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1904&amp;oldid=prev"/>
		<updated>2006-05-19T10:53:09Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 10:53, 19 May 2006&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l6&quot; &gt;Line 6:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 6:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;See also: [[Celebratory interventions (&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cetactean&lt;/del&gt;)]]: [[Lone Power]]: [[Matters of place]]:  [[Topography and wizardry]].  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;See also: [[Celebratory interventions (&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cetacean&lt;/ins&gt;)]]: [[Lone Power]]: [[Matters of place]]:  [[Topography and wizardry]].  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;(Note:  It's interesting to discover that as early as 1986, scientists investigating underwater topography had noted in the journals that [http://ams.allenpress.com/amsonline/?request=get-toc&amp;amp;issn=1520-0485&amp;amp;volume=16&amp;amp;issue=1 something a little unusual] was going on with the movement of deep currents in the area.  Other studies have mentioned peculiarities having to do with the area's magnetic field, possibly connected to the detection of [http://www.gsajournals.org/gsaonline/?request=get-abstract&amp;amp;doi=10.1130%2F0016-7606(1978)89%3C1656:STATRI%3E2.0.CO%3B2 indicators in the Kelvin Seamounts] suggesting a large crustal movement along this fault area during the Mesozoic period. Something to do with a much earlier enactment of the ''Song''?...)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;(Note:  It's interesting to discover that as early as 1986, scientists investigating underwater topography had noted in the journals that [http://ams.allenpress.com/amsonline/?request=get-toc&amp;amp;issn=1520-0485&amp;amp;volume=16&amp;amp;issue=1 something a little unusual] was going on with the movement of deep currents in the area.  Other studies have mentioned peculiarities having to do with the area's magnetic field, possibly connected to the detection of [http://www.gsajournals.org/gsaonline/?request=get-abstract&amp;amp;doi=10.1130%2F0016-7606(1978)89%3C1656:STATRI%3E2.0.CO%3B2 indicators in the Kelvin Seamounts] suggesting a large crustal movement along this fault area during the Mesozoic period. Something to do with a much earlier enactment of the ''Song''?...)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1903&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 10:48, 19 May 2006</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1903&amp;oldid=prev"/>
		<updated>2006-05-19T10:48:30Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 10:48, 19 May 2006&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;SOHM ABYSSAL PLAIN &lt;/del&gt;at the very end of [[Hudson Canyon]], and is the place where the [[Twelve, Song of the | Song of the Twelve]] is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Sohm Abyssal Plain]] &lt;/ins&gt;at the very end of [[Hudson Canyon]], and is the place where the [[Twelve, Song of the | Song of the Twelve]] is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;KELVIN SEAMOUNTS &lt;/del&gt;(or more recently, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;NEW ENGLAND SEAMOUNTS&lt;/del&gt;), which rise from the ocean floor off the east coast of North America.  The [[Cetacean | cetacean]] name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Kelvin Seamounts]] &lt;/ins&gt;(or more recently, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[New England Seamounts]]&lt;/ins&gt;), which rise from the ocean floor off the east coast of North America.  The [[Cetacean | cetacean]] name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[Image:Houghton_600.jpg|right|thumb|200px|Caryn Peak, [[Sohm Abyssal Plain]], and [[Kelvin Seamounts]]]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;See also: &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;CELEBRATORY INTERVENTIONS &lt;/del&gt;(&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;CETACEAN&lt;/del&gt;)&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;: KELVIN SEAMOUNTS&lt;/del&gt;: [[Lone Power]]: &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;MATTERS OF PLACE&lt;/del&gt;:  &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;TOPOGRAPHY AND WIZARDRY&lt;/del&gt;.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;See also: &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Celebratory interventions &lt;/ins&gt;(&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cetactean&lt;/ins&gt;)&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;]]&lt;/ins&gt;: [[Lone Power]]: &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Matters of place]]&lt;/ins&gt;:  &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Topography and wizardry]]&lt;/ins&gt;.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;(Note:  It's interesting to discover that as early as 1986, scientists investigating underwater topography had noted in the journals that [http://ams.allenpress.com/amsonline/?request=get-toc&amp;amp;issn=1520-0485&amp;amp;volume=16&amp;amp;issue=1 something a little unusual] was going on with the movement of deep currents in the area.  Other studies have mentioned peculiarities having to do with the area's magnetic field, possibly connected to the detection of [http://www.gsajournals.org/gsaonline/?request=get-abstract&amp;amp;doi=10.1130%2F0016-7606(1978)89%3C1656:STATRI%3E2.0.CO%3B2 indicators in the Kelvin Seamounts] suggesting a large crustal movement along this fault area during the Mesozoic period. Something to do with a much earlier enactment of the ''Song''?...)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;(Note:  It's interesting to discover that as early as 1986, scientists investigating underwater topography had noted in the journals that [http://ams.allenpress.com/amsonline/?request=get-toc&amp;amp;issn=1520-0485&amp;amp;volume=16&amp;amp;issue=1 something a little unusual] was going on with the movement of deep currents in the area.  Other studies have mentioned peculiarities having to do with the area's magnetic field, possibly connected to the detection of [http://www.gsajournals.org/gsaonline/?request=get-abstract&amp;amp;doi=10.1130%2F0016-7606(1978)89%3C1656:STATRI%3E2.0.CO%3B2 indicators in the Kelvin Seamounts] suggesting a large crustal movement along this fault area during the Mesozoic period. Something to do with a much earlier enactment of the ''Song''?...)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1902&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 13:35, 12 June 2005</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1902&amp;oldid=prev"/>
		<updated>2005-06-12T13:35:25Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 13:35, 12 June 2005&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea SOHM ABYSSAL PLAIN at the very end of [[Hudson Canyon]], and is the place where the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;SONG OF THE TWELVE &lt;/del&gt;is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea SOHM ABYSSAL PLAIN at the very end of [[Hudson Canyon]], and is the place where the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Twelve, Song of the | Song of the Twelve]] &lt;/ins&gt;is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the KELVIN SEAMOUNTS (or more recently, the NEW ENGLAND SEAMOUNTS), which rise from the ocean floor off the east coast of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;NORTH AMERICA&lt;/del&gt;.  The [[Cetacean | cetacean]] name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the KELVIN SEAMOUNTS (or more recently, the NEW ENGLAND SEAMOUNTS), which rise from the ocean floor off the east coast of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;North America&lt;/ins&gt;.  The [[Cetacean | cetacean]] name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1901&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 11:55, 21 March 2005</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1901&amp;oldid=prev"/>
		<updated>2005-03-21T11:55:02Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 11:55, 21 March 2005&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea SOHM ABYSSAL PLAIN at the very end of [[Hudson Canyon]], and is the place where the SONG OF THE TWELVE is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea SOHM ABYSSAL PLAIN at the very end of [[Hudson Canyon]], and is the place where the SONG OF THE TWELVE is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the KELVIN SEAMOUNTS (or more recently, the NEW ENGLAND SEAMOUNTS), which rise from the ocean floor off the east coast of NORTH AMERICA.  The &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;CETACEAN &lt;/del&gt;name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the KELVIN SEAMOUNTS (or more recently, the NEW ENGLAND SEAMOUNTS), which rise from the ocean floor off the east coast of NORTH AMERICA.  The &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Cetacean | cetacean]] &lt;/ins&gt;name for Caryn Peak is &amp;quot;the [[Sea's Tooth]]&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1900&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 11:54, 21 March 2005</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1900&amp;oldid=prev"/>
		<updated>2005-03-21T11:54:19Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 11:54, 21 March 2005&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea SOHM ABYSSAL PLAIN at the very end of [[Hudson Canyon]], and is the place where the SONG OF THE TWELVE is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Also known as &amp;quot;Caryn Seamount&amp;quot;. (Latitude 36&amp;amp;deg; 40'N, longitude 67&amp;amp;deg; 56'W) The Peak is a volcanic formation which stands some six thousand feet high, taller than five Empire State Buildings stacked on top of one another. It rises out of the undersea SOHM ABYSSAL PLAIN at the very end of [[Hudson Canyon]], and is the place where the SONG OF THE TWELVE is traditionally enacted.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the KELVIN SEAMOUNTS (or more recently, the NEW ENGLAND SEAMOUNTS), which rise from the ocean floor off the east coast of NORTH AMERICA.  The CETACEAN name for Caryn Peak is &amp;quot;the Sea's Tooth&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Peak is nearly the southernmost and probably the farthest-flung of a chain of undersea mountains, called by humans the KELVIN SEAMOUNTS (or more recently, the NEW ENGLAND SEAMOUNTS), which rise from the ocean floor off the east coast of NORTH AMERICA.  The CETACEAN name for Caryn Peak is &amp;quot;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[&lt;/ins&gt;Sea's Tooth&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;]]&lt;/ins&gt;&amp;quot;. ([[DW]])&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
	<entry>
		<id>http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1899&amp;oldid=prev</id>
		<title>newimport&gt;DianeDuane at 13:26, 14 March 2005</title>
		<link rel="alternate" type="text/html" href="http://errantryconcordance.com/mediawiki-1.35.1/index.php?title=Caryn_Peak&amp;diff=1899&amp;oldid=prev"/>
		<updated>2005-03-14T13:26:46Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left diff-editfont-monospace&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 13:26, 14 March 2005&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l4&quot; &gt;Line 4:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 4:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;See also: CELEBRATORY INTERVENTIONS (CETACEAN): KELVIN SEAMOUNTS: &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;LONE POWER&lt;/del&gt;: MATTERS OF PLACE:  TOPOGRAPHY AND WIZARDRY.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;See also: CELEBRATORY INTERVENTIONS (CETACEAN): KELVIN SEAMOUNTS: &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[Lone Power]]&lt;/ins&gt;: MATTERS OF PLACE:  TOPOGRAPHY AND WIZARDRY.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;(Note:  It's interesting to discover that as early as 1986, scientists investigating underwater topography had noted in the journals that [http://ams.allenpress.com/amsonline/?request=get-toc&amp;amp;issn=1520-0485&amp;amp;volume=16&amp;amp;issue=1 something a little unusual] was going on with the movement of deep currents in the area.  Other studies have mentioned peculiarities having to do with the area's magnetic field, possibly connected to the detection of [http://www.gsajournals.org/gsaonline/?request=get-abstract&amp;amp;doi=10.1130%2F0016-7606(1978)89%3C1656:STATRI%3E2.0.CO%3B2 indicators in the Kelvin Seamounts] suggesting a large crustal movement along this fault area during the Mesozoic period. Something to do with a much earlier enactment of the ''Song''?...)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;(Note:  It's interesting to discover that as early as 1986, scientists investigating underwater topography had noted in the journals that [http://ams.allenpress.com/amsonline/?request=get-toc&amp;amp;issn=1520-0485&amp;amp;volume=16&amp;amp;issue=1 something a little unusual] was going on with the movement of deep currents in the area.  Other studies have mentioned peculiarities having to do with the area's magnetic field, possibly connected to the detection of [http://www.gsajournals.org/gsaonline/?request=get-abstract&amp;amp;doi=10.1130%2F0016-7606(1978)89%3C1656:STATRI%3E2.0.CO%3B2 indicators in the Kelvin Seamounts] suggesting a large crustal movement along this fault area during the Mesozoic period. Something to do with a much earlier enactment of the ''Song''?...)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>newimport&gt;DianeDuane</name></author>
	</entry>
</feed>