<?xml version="1.0"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="en">
		<id>https://www.explainxkcd.com/wiki/index.php?action=history&amp;feed=atom&amp;title=3141%3A_Mantle_Model</id>
		<title>3141: Mantle Model - Revision history</title>
		<link rel="self" type="application/atom+xml" href="https://www.explainxkcd.com/wiki/index.php?action=history&amp;feed=atom&amp;title=3141%3A_Mantle_Model"/>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;action=history"/>
		<updated>2026-04-14T08:01:46Z</updated>
		<subtitle>Revision history for this page on the wiki</subtitle>
		<generator>MediaWiki 1.30.0</generator>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=407171&amp;oldid=prev</id>
		<title>82.132.238.95: /* Explanation */ Added in the volcanic 'bookends' that (some suggest!) ushered in the start and end of the Roman Empire. Though take it with a pinch of salt, if not actual stratospheric volcanic gas... ;)</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=407171&amp;oldid=prev"/>
				<updated>2026-02-25T17:07:31Z</updated>
		
		<summary type="html">&lt;p&gt;‎&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Explanation: &lt;/span&gt; Added in the volcanic &amp;#039;bookends&amp;#039; that (some suggest!) ushered in the start and end of the Roman Empire. Though take it with a pinch of salt, if not actual stratospheric volcanic gas... ;)&lt;/span&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 17:07, 25 February 2026&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-l20&quot; &gt;Line 20:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years. This orogeny is not related to the original {{w|Appalachian orogeny}}, which began much earlier, 325-260 million years ago. A leading theory about the Adirondack uplift is that it's driven by a hotspot atop a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years. This orogeny is not related to the original {{w|Appalachian orogeny}}, which began much earlier, 325-260 million years ago. A leading theory about the Adirondack uplift is that it's driven by a hotspot atop a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, the foremost one of which, {{w|Siberian Traps}} volcanism, is thought to have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, the foremost one of which, {{w|Siberian Traps}} volcanism, is thought to have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, of the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, of the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, although there are claims that {{w|Volcanic winter of 536|vulcanism elsewhere in the world}} contributed to the fall of Rome and/or its other more direct causes, just as there are that {{w|Mount Okmok#43 BCE: Okmok II eruption|a prior event}} helped it to rise in the first place&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved. Dan Cooper is an alias of the hijacker, whose real name is unknown. This is one of several xkcd cartoons referring to [[D.B. Cooper]], including [[1400: D.B. Cooper]], in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; The hijacking itself had nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved. Dan Cooper is an alias of the hijacker, whose real name is unknown. This is one of several xkcd cartoons referring to [[D.B. Cooper]], including [[1400: D.B. Cooper]], in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; The hijacking itself had nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>82.132.238.95</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=403219&amp;oldid=prev</id>
		<title>BunsenH: Undo revision 403216 by 112.206.102.74 (talk) spam</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=403219&amp;oldid=prev"/>
				<updated>2026-01-09T14:53:50Z</updated>
		
		<summary type="html">&lt;p&gt;Undo revision 403216 by &lt;a href=&quot;/wiki/index.php/Special:Contributions/112.206.102.74&quot; title=&quot;Special:Contributions/112.206.102.74&quot;&gt;112.206.102.74&lt;/a&gt; (&lt;a href=&quot;/wiki/index.php?title=User_talk:112.206.102.74&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;User talk:112.206.102.74 (page does not exist)&quot;&gt;talk&lt;/a&gt;) spam&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 14:53, 9 January 2026&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-l24&quot; &gt;Line 24:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 24:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Antle plumes (in the title text) are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These little sand hills are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Antle plumes (in the title text) are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These little sand hills are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&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;color:black; 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;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; 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;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;https://www.abcya.com/games/keyboard_challenge&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Transcript==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Transcript==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>BunsenH</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=403216&amp;oldid=prev</id>
		<title>112.206.102.74 at 11:37, 9 January 2026</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=403216&amp;oldid=prev"/>
				<updated>2026-01-09T11:37:42Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 11:37, 9 January 2026&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-l24&quot; &gt;Line 24:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 24:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Antle plumes (in the title text) are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These little sand hills are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Antle plumes (in the title text) are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These little sand hills are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;https://www.abcya.com/games/keyboard_challenge&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Transcript==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Transcript==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>112.206.102.74</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=387131&amp;oldid=prev</id>
		<title>Underdevelopedprefrontalcortex: Earth surface -&gt; Earth's surface in transcript, fixes error</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=387131&amp;oldid=prev"/>
				<updated>2025-09-19T07:03:27Z</updated>
		
		<summary type="html">&lt;p&gt;Earth surface -&amp;gt; Earth&amp;#039;s surface in transcript, fixes error&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 07:03, 19 September 2025&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-l36&quot; &gt;Line 36:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 36:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;:[On the Earth’s surface are various rock formations that align with the locations of plumes just below.] &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;:[On the Earth’s surface are various rock formations that align with the locations of plumes just below.] &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;:[The formations are labeled:]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;:[The formations are labeled:]&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;color:black; 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;:Every feature of the Earth surface that we have a hard time explaining&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;:Every feature of the Earth&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/ins&gt;surface that we have a hard time explaining&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;:[Caption below the panel:]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;:[Caption below the panel:]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Underdevelopedprefrontalcortex</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386872&amp;oldid=prev</id>
		<title>DKMell: clarification</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386872&amp;oldid=prev"/>
				<updated>2025-09-17T00:45:28Z</updated>
		
		<summary type="html">&lt;p&gt;clarification&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 00:45, 17 September 2025&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-l16&quot; &gt;Line 16:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 16:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* {{w|Hawaii}}. A {{w|Hotspot (geology)|hotspot}}, hypothesized to sit atop a mantle plume, did indeed create the Hawaiian Islands.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* {{w|Hawaii}}. A {{w|Hotspot (geology)|hotspot}}, hypothesized to sit atop a mantle plume, did indeed create the Hawaiian Islands.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* {{w|Yellowstone}}. This area of hot springs, geysers, and other geothermal phenomena is in the {{w|Yellowstone Caldera}}, which some geologists believe sits atop a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* {{w|Yellowstone}}. This area of hot springs, geysers, and other geothermal phenomena is in the {{w|Yellowstone Caldera}}, which some geologists believe sits atop a mantle plume.&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;color:black; 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;* {{w|Iceland}}. Essentially the same as Hawaii, except for being at the edge of two plates instead of in the middle of one.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;* {{w|Iceland}}. Essentially the same as Hawaii, except for being at the edge of two &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{w|tectonic &lt;/ins&gt;plates&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;}} &lt;/ins&gt;instead of in the middle of one.&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;color:black; 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 {{w|East African Rift}}. This area in East Africa is a developing divergent &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;{{w|&lt;/del&gt;tectonic plate&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;}} &lt;/del&gt;boundary where the African plate is in the process of splitting into two tectonic plates. Mantle plumes and hotspots have been theorized to have initiated and continued this divergence.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|East African Rift}}. This area in East Africa is a developing divergent tectonic plate boundary where the African plate is in the process of splitting into two tectonic plates. Mantle plumes and hotspots have been theorized to have initiated and continued this divergence.&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;color:black; 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 {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years. This orogeny is not related to the original {{w|Appalachian orogeny}}, which began much earlier, 325-260 million years ago. A leading theory about the Adirondack uplift is that it's driven by a hotspot &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;(&lt;/del&gt;mantle plume&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;)&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years. This orogeny is not related to the original {{w|Appalachian orogeny}}, which began much earlier, 325-260 million years ago. A leading theory about the Adirondack uplift is that it's driven by a hotspot &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;atop a &lt;/ins&gt;mantle plume.&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;color:black; 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 {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;could &lt;/del&gt;have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the foremost &lt;/ins&gt;one of which, {{w|Siberian Traps}} volcanism, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is thought to &lt;/ins&gt;have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, of the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic winter of 536|Volcanic winter of AD 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, of the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}.&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;color:black; 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 {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved. Dan &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;B. &lt;/del&gt;Cooper is an alias of the hijacker, whose real name is unknown. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mount St. Helens Erupted.{{Actual citation needed}} &lt;/del&gt;This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;However, the &lt;/del&gt;hijacking itself &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;probably has &lt;/del&gt;nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved. Dan Cooper is an alias of the hijacker, whose real name is unknown. This is one of several xkcd cartoons referring to [[D.B. Cooper]], including [[1400: D.B. Cooper]]&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, &lt;/ins&gt;in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;The &lt;/ins&gt;hijacking itself &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;had &lt;/ins&gt;nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.{{cn}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Antle plumes (in the title text) are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These little sand hills are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Antle plumes (in the title text) are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These little sand hills are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>DKMell</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386831&amp;oldid=prev</id>
		<title>DKMell: minor fixes</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386831&amp;oldid=prev"/>
				<updated>2025-09-16T17:59:02Z</updated>
		
		<summary type="html">&lt;p&gt;minor fixes&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 17:59, 16 September 2025&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-l14&quot; &gt;Line 14:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 14:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The title text extends this further, suggesting with increasing absurdity that mantle plumes account for other things that don't have a direct explanation:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The title text extends this further, suggesting with increasing absurdity that mantle plumes account for other things that don't have a direct explanation:&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;color:black; 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;* {{w|Hawaii}}. A hotspot, hypothesized to sit atop a mantle plume, did indeed create the Hawaiian Islands&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;* {{w|Hawaii}}. A &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{w|Hotspot (geology)|&lt;/ins&gt;hotspot&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;}}&lt;/ins&gt;, hypothesized to sit atop a mantle plume, did indeed create the Hawaiian Islands.&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;color:black; 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;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;* {{w|Iceland}}. The same as Hawaii, essentially. Except for being at the edge of two plates instead of in the middle of one&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* {{w|Yellowstone}}. This area of hot springs, geysers, and other geothermal phenomena is in the {{w|Yellowstone Caldera}}, which some geologists believe sits atop a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* {{w|Yellowstone}}. This area of hot springs, geysers, and other geothermal phenomena is in the {{w|Yellowstone Caldera}}, which some geologists believe sits atop a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;* {{w|Iceland}}. Essentially the same as Hawaii, except for being at the edge of two plates instead of in the middle of one.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|East African Rift}}. This area in East Africa is a developing divergent {{w|tectonic plate}} boundary where the African plate is in the process of splitting into two tectonic plates. Mantle plumes and hotspots have been theorized to have initiated and continued this divergence.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|East African Rift}}. This area in East Africa is a developing divergent {{w|tectonic plate}} boundary where the African plate is in the process of splitting into two tectonic plates. Mantle plumes and hotspots have been theorized to have initiated and continued this divergence.&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;color:black; 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 {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;, and this &lt;/del&gt;orogeny is not related to the original Appalachian orogeny. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;One &lt;/del&gt;theory is that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;their uplift is &lt;/del&gt;driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;. This &lt;/ins&gt;orogeny is not related to the original &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{w|&lt;/ins&gt;Appalachian orogeny&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;}}, which began much earlier, 325-260 million years ago&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;A leading &lt;/ins&gt;theory &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;about the Adirondack uplift &lt;/ins&gt;is that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;it's &lt;/ins&gt;driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;of &lt;/ins&gt;the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic winter of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;536|Volcanic winter of AD &lt;/ins&gt;536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&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;color:black; 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 {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;, so Randall says it was caused by mantle plumes&lt;/del&gt;. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Mt. &lt;/del&gt;St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Mount &lt;/ins&gt;St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&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;color:black; 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 {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{cn}}&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;color:black; 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;* Antle plumes are a pun on &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the word &lt;/del&gt;&amp;quot;ant&amp;quot; and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the phrase &lt;/del&gt;&amp;quot;mantle plumes&amp;quot;. These &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;things &lt;/del&gt;are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;, &lt;/del&gt;from the material excavated from their tunnels&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;. Randall apparently finds these sand or soil hills weird and inexplicable enough that they require an obscure cause&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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;* Antle plumes &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;(in the title text) &lt;/ins&gt;are a pun on &amp;quot;ant&amp;quot; and &amp;quot;mantle plumes&amp;quot;. These &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;little sand hills &lt;/ins&gt;are probably actually {{w|anthills}} (&amp;quot;ant-hill plumes&amp;quot;) and are created by ants at the entrances to their underground nests from the material excavated from their tunnels.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Transcript==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Transcript==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>DKMell</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386798&amp;oldid=prev</id>
		<title>216.221.83.168: Fixed wiki link to Volcanic winter of 536 (lowercase winter)</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386798&amp;oldid=prev"/>
				<updated>2025-09-16T15:05:51Z</updated>
		
		<summary type="html">&lt;p&gt;Fixed wiki link to Volcanic winter of 536 (lowercase winter)&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:05, 16 September 2025&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-l20&quot; &gt;Line 20:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Winter &lt;/del&gt;of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or, more specifically, the original and western capital city of {{w|Rome}}. The decline was a complex issue caused by many non-mantle-plume-related factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to the newer, eastern capital city of {{w|Constantinople}}. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;winter &lt;/ins&gt;of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>216.221.83.168</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386797&amp;oldid=prev</id>
		<title>216.221.83.168: Some edits for clarity and formality of tone, and some wiki links for the city of Rome and especially Constantinople (as it does not exist under that name today)</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386797&amp;oldid=prev"/>
				<updated>2025-09-16T15:04:39Z</updated>
		
		<summary type="html">&lt;p&gt;Some edits for clarity and formality of tone, and some wiki links for the city of Rome and especially Constantinople (as it does not exist under that name today)&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:04, 16 September 2025&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-l20&quot; &gt;Line 20:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or more specifically, the original and western capital city of Rome. The decline was caused by &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a lot of &lt;/del&gt;factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Constantinople&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;all &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which had nothing to do with mantle plumes, but doesn't have a single very clear explanation&lt;/del&gt;. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic Winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}, or&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, &lt;/ins&gt;more specifically, the original and western capital city of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{w|&lt;/ins&gt;Rome&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;}}&lt;/ins&gt;. The decline was &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a complex issue &lt;/ins&gt;caused by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;many non-mantle-plume-related &lt;/ins&gt;factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the newer&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;eastern capital city &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{w|Constantinople}}&lt;/ins&gt;. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic Winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>216.221.83.168</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386793&amp;oldid=prev</id>
		<title>216.221.83.168: Clarification that 'decline of Rome' could refer to the empire or the city specifically. The next sentence comments on some factors that are city-specific, not empire-wide.</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386793&amp;oldid=prev"/>
				<updated>2025-09-16T14:58:17Z</updated>
		
		<summary type="html">&lt;p&gt;Clarification that &amp;#039;decline of Rome&amp;#039; could refer to the empire or the city specifically. The next sentence comments on some factors that are city-specific, not empire-wide.&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 14:58, 16 September 2025&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-l20&quot; &gt;Line 20:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}. The decline was caused by a lot of factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to Constantinople, all of which had nothing to do with mantle plumes, but doesn't have a single very clear explanation. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic Winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, or more specifically, the original and western capital city of Rome&lt;/ins&gt;. The decline was caused by a lot of factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to Constantinople, all of which had nothing to do with mantle plumes, but doesn't have a single very clear explanation. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes. This could instead allude to the {{w|Volcanic Winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>216.221.83.168</name></author>	</entry>

	<entry>
		<id>https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386791&amp;oldid=prev</id>
		<title>216.221.83.168: Mount Vesuvius is not considered a hotspot volcano and is therefore considered not the direct result of mantle plumes</title>
		<link rel="alternate" type="text/html" href="https://www.explainxkcd.com/wiki/index.php?title=3141:_Mantle_Model&amp;diff=386791&amp;oldid=prev"/>
				<updated>2025-09-16T14:55:44Z</updated>
		
		<summary type="html">&lt;p&gt;Mount Vesuvius is not considered a hotspot volcano and is therefore considered not the direct result of mantle plumes&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&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 style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 14:55, 16 September 2025&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-l20&quot; &gt;Line 20:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Adirondack_Mountains#Geology|Adirondack uplift}}. The Adirondack Mountains began uplifting in the past 10 million years, and this orogeny is not related to the original Appalachian orogeny. One theory is that their uplift is driven by a hotspot (mantle plume).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|Permian extinction}}, also called the 'Great Dying' and more formally as the Permian-Triassic extinction event, is the largest of the {{w|List of extinction events|&amp;quot;big five&amp;quot; mass extinctions}} since vertebrate life appeared on Earth. There are several hypotheses as to why it happened, one of which, {{w|Siberian Traps}} volcanism, could have happened because of a mantle plume.&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;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}. The decline was caused by a lot of factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to Constantinople, all of which had nothing to do with mantle plumes, but doesn't have a single very clear explanation. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending. This could &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;also &lt;/del&gt;allude to the {{w|Volcanic Winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; 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 decline of Rome refers to the end of the {{w|Roman Empire}}. The decline was caused by a lot of factors, including changing social pressures, financial exhaustion after a series of wars, pressure from neighboring rivals, and siphoning of resources and attention to Constantinople, all of which had nothing to do with mantle plumes, but doesn't have a single very clear explanation. One contributing factor could relate to the eruption of {{w|Mount Vesuvius}}, which was a tragedy, but not empire-ending&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;. Mount Vesuvius is also generally considered to be the result of [https://www.researchgate.net/publication/227292973_Late-Quaternary_volcanism_and_transtensional_tectonics_in_the_Bay_of_Naples_Campanian_continental_margin_Italy tectonic-boundary volcanism], not directly related to mantle plumes&lt;/ins&gt;. This could &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instead &lt;/ins&gt;allude to the {{w|Volcanic Winter of 536}}, which was, in all likelihood, caused by a volcano, and which did hasten the decline of the Roman Empire in the age of Justinian.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|DB Cooper}} airplane hijacking occurred in 1971 and remains unsolved, so Randall says it was caused by mantle plumes. Dan B. Cooper is an alias of the hijacker, whose real name is unknown. Nine years later, a mantle plume covered what was left of the evidence, along with a large portion of the Pacific Northwest, in volcanic ash as Mt. St. Helens Erupted.{{Actual citation needed}} This is one of several xkcd cartoons referring to [[D. B. Cooper]], including [[1400: D.B. Cooper]] in which Cueball suggested that Cooper might have become filmmaker {{w|Tommy Wiseau}}, and [[2498: Forest Walk]], in which Cooper is seen stuck in a tree on [[Beret Guy]]'s property.&amp;#160; However, the hijacking itself probably has nothing to do with mantle plumes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* The {{w|balrog}} in {{w|Moria, Middle-earth|Moria}} is a fictional beast in {{w|J.R.R. Tolkien}}'s {{w|legendarium}} that first appeared in ''{{w|The Lord of the Rings}}''. It too has nothing to do with mantle plumes, but it was revealed by the dwarves, who &amp;quot;delved too greedily and too deep and awoke a terror of shadow and flame.&amp;quot;&amp;#160; If we were to delve sufficiently greedily and deep that we dug into a mantle plume, we would indeed be greeted by a terrible amount of flame, although the shadow aspect is unconfirmed.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>216.221.83.168</name></author>	</entry>

	</feed>