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	<id>https://energyeducation.ca/wiki/index.php?action=history&amp;feed=atom&amp;title=Glacial_lake_outburst_flood</id>
	<title>Glacial lake outburst flood - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://energyeducation.ca/wiki/index.php?action=history&amp;feed=atom&amp;title=Glacial_lake_outburst_flood"/>
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	<updated>2026-04-26T22:54:49Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=9456&amp;oldid=prev</id>
		<title>Jmdonev: 1 revision imported</title>
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		<updated>2020-04-28T15:32:26Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
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				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 15:32, 28 April 2020&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>Jmdonev</name></author>
	</entry>
	<entry>
		<id>https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=9455&amp;oldid=prev</id>
		<title>energy&gt;Jmdonev at 22:57, 18 February 2020</title>
		<link rel="alternate" type="text/html" href="https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=9455&amp;oldid=prev"/>
		<updated>2020-02-18T22:57:10Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 22:57, 18 February 2020&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Category:Done &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2016&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;04&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;30&lt;/del&gt;]]  &lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[Category:Done &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2020&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;02&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;29&lt;/ins&gt;]]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;onlyinclude&amp;gt;&#039;&#039;&#039;Glacial lake outburst floods (GLOFs)&#039;&#039;&#039; are [[flood]]s that occur from an unstable natural dam formed from a [[glacier | glacial]] retreat.&amp;lt;ref name=RE4&amp;gt;”Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation&quot;, Intergovernmental Panel on Climate Change, New York, 2012.&amp;lt;/ref&amp;gt; &amp;lt;/onlyinclude&amp;gt; Glaciers are dynamic bodies of ice that change frequently.&amp;lt;ref name=RE3&amp;gt;&quot;Hazards - Glaciers, Climate, and Society&quot;, Glaciers.uoregon.edu, 2016. [Online]. Available: http://glaciers.uoregon.edu/hazards.html. [Accessed: 20- May- 2016].&amp;lt;/ref&amp;gt; When a glacier retreats, it can leave behind a large impression in the ground that fills with [[water]], turning it into a lake. This is typically known as a moraine.&amp;lt;ref name=RE4/&amp;gt; These lakes can be impounded by an unstable pile of debris and buried ice.&amp;lt;ref name=&quot;RE2”&amp;gt;”Glacial lake outburst flood (GLOF)&quot;, Swisseduc.ch, 2016. [Online]. Available: http://www.swisseduc.ch/glaciers/glossary/glof-2-en.html. [Accessed: 23- May- 2016].&amp;lt;/ref&amp;gt; As the [[climate]] warms, glaciers generally shrink. In many mountains such as the Andes, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Himalaya&lt;/del&gt;, Alps, Rockies, and elsewhere, the retreat of glacier tongues sometimes allows unstable moraine dammed lakes to form.&amp;lt;ref name=RE3/&amp;gt; Terminal moraines act as &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;dams &lt;/del&gt;for these lakes, but as the lakes swell from rising water levels and the retreating glacial ice tongue, the moraine dam can weaken. Moraine dams that become too weak may crumble under too much pressure from the swelling lake, creating a GLOF. If the moraine dams of a glacial lake fail, the water can burst out, leading to massive floods and debris flows with potentially extensive damage downstream, including loss of life and infrastructure.&amp;lt;ref name=&quot;RE1&quot;&amp;gt;&quot;Glacial Lakes and Glacial Lake Outburst Floods in Nepal&quot;, The International Centre for Integrated Mountain Development, 2011. [Online]. Available: http://www.icimod.org/dvds/201104_GLOF/reports/final_report.pdf. [Accessed: 24- May- 2016].&amp;lt;/ref&amp;gt; Alternatively, and more commonly, glacial ice from the retreating glacier can crash into lakes, generating giant waves that erode weak moraine dams in a matter of minutes, thereby also triggering GLOFs.&amp;lt;ref name=RE3/&amp;gt;  &lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;onlyinclude&amp;gt;&#039;&#039;&#039;Glacial lake outburst floods (GLOFs)&#039;&#039;&#039; are [[flood]]s that occur from an unstable natural &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/ins&gt;dam&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;formed from a [[glacier | glacial]] retreat.&amp;lt;ref name=RE4&amp;gt;”Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation&quot;, Intergovernmental Panel on Climate Change, New York, 2012.&amp;lt;/ref&amp;gt; &amp;lt;/onlyinclude&amp;gt; Glaciers are dynamic bodies of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/ins&gt;ice&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;that change frequently.&amp;lt;ref name=RE3&amp;gt;&quot;Hazards - Glaciers, Climate, and Society&quot;, Glaciers.uoregon.edu, 2016. [Online]. Available: http://glaciers.uoregon.edu/hazards.html. [Accessed: 20- May- 2016].&amp;lt;/ref&amp;gt; When a glacier retreats, it can leave behind a large impression in the ground that fills with [[water]], turning it into a lake. This is typically known as a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/ins&gt;moraine&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]]&lt;/ins&gt;.&amp;lt;ref name=RE4/&amp;gt; These lakes can be impounded by an unstable pile of debris and buried ice.&amp;lt;ref name=&quot;RE2”&amp;gt;”Glacial lake outburst flood (GLOF)&quot;, Swisseduc.ch, 2016. [Online]. Available: http://www.swisseduc.ch/glaciers/glossary/glof-2-en.html. [Accessed: 23- May- 2016].&amp;lt;/ref&amp;gt; As the [[climate]] warms, glaciers generally shrink. In many mountains such as the Andes, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Himalayas&lt;/ins&gt;, Alps, Rockies, and elsewhere, the retreat of glacier tongues sometimes allows unstable moraine dammed lakes to form.&amp;lt;ref name=RE3/&amp;gt; Terminal moraines act as &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[dam]]s &lt;/ins&gt;for these lakes, but as the lakes swell from rising water levels and the retreating glacial ice tongue, the moraine dam can weaken. Moraine dams that become too weak may crumble under too much pressure from the swelling lake, creating a GLOF. If the moraine dams of a glacial lake fail, the water can burst out, leading to massive floods and debris flows with potentially extensive damage downstream, including loss of life and infrastructure.&amp;lt;ref name=&quot;RE1&quot;&amp;gt;&quot;Glacial Lakes and Glacial Lake Outburst Floods in Nepal&quot;, The International Centre for Integrated Mountain Development, 2011. [Online]. Available: http://www.icimod.org/dvds/201104_GLOF/reports/final_report.pdf. [Accessed: 24- May- 2016].&amp;lt;/ref&amp;gt; Alternatively, and more commonly, glacial ice from the retreating glacier can crash into lakes, generating giant waves that erode weak moraine dams in a matter of minutes, thereby also triggering GLOFs.&amp;lt;ref name=RE3/&amp;gt;  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;gallery caption=&amp;quot;Glacial lake outburst flood in Alaska&amp;quot; mode=packed heights=280px&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;gallery caption=&amp;quot;Glacial lake outburst flood in Alaska&amp;quot; mode=packed heights=280px&amp;gt;&lt;/div&gt;&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-l8&quot;&gt;Line 8:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 8:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;File:Hubbard_Glacier_August_14.2002.jpg|&amp;lt;ref name =USGS/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;File:Hubbard_Glacier_August_14.2002.jpg|&amp;lt;ref name =USGS/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;/gallery&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;/gallery&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;In the summer of 2002 Alaska&#039;s Hubbard glacier pinched off the connection between Russel Fjord and Disenchantment bay. This made the Russel Fjord into a glacial lake, for a short period of time. The lake rose 15 m above sea level. When the lake burst, it sent almost 2 million cubic feet of water per second back into the bay.&amp;lt;ref name =USGS/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;In the summer of 2002 Alaska&#039;s Hubbard glacier pinched off the connection between Russel Fjord and Disenchantment bay. This made the Russel Fjord into a glacial lake, for a short period of time. The lake rose 15 &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[meter|&lt;/ins&gt;m&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;above sea level. When the lake burst, it sent almost 2 million &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/ins&gt;cubic feet&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;of water per &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/ins&gt;second&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;back into the bay.&amp;lt;ref name =USGS/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;In the past century, GLOFs have caused disasters in high mountain regions of the world which include the Andes, areas in Caucasus and Central Asia, the Himalayas, North America and the European Alps.&amp;lt;ref name=RE4/&amp;gt; There are many examples in Nepal in which loss of lives and property have occurred as a result of glacial lake outburst floods.&amp;lt;ref name=RE1/&amp;gt; Glaciers, being ice sheets, can indicate increased [[air]] [[temperature]] due to being sensitive to [[climate change]].&amp;lt;ref name=RE1/&amp;gt; Glacial lakes are not only a risk of potential danger, but they are also an important natural resource, providing a [[fresh water]] source for people.&amp;lt;ref name=RE1/&amp;gt; Over the past 20-30 years, human measures to mitigate unstable glacier lakes in the Himalaya and European Alps may have prevented some potential GLOF disasters.&amp;lt;ref name=RE4/&amp;gt; Research has shown that due to global climate change and retreating glaciers, there is an escalated risk in GLOFs worldwide.&amp;lt;ref name=RE3/&amp;gt; This is leading glacial lakes to swell and increase the risk of flooding. For example, in Bhutan, a region with 677 glaciers and 2,794 glacial lakes has &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;experience &lt;/del&gt;more than 21 glacial lake outburst floods in the last two centuries.&amp;lt;ref name=RE1/&amp;gt;  From the 21 mentioned, 4 of the outbursts have occurred in the last 40 years.&amp;lt;ref name=RE1/&amp;gt; &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;However, because &lt;/del&gt;GLOFs are quite rare, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;it &lt;/del&gt;is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;uncertain whether their frequency of occurrence is changing at either the regional or global scale. Researchers argue that outburst floods from moraine dammed lakes in North America for example may have increased due &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a reduction in &lt;/del&gt;the number of the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lakes since &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;end &lt;/del&gt;of the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Little Ice Age&lt;/del&gt;.&amp;lt;ref &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;name=RE4/&lt;/del&gt;&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;In the past century, GLOFs have caused disasters in high mountain regions of the world which include the Andes, areas in Caucasus and Central Asia, the Himalayas, North America and the European Alps.&amp;lt;ref name=RE4/&amp;gt; There are many examples in Nepal in which loss of lives and property have occurred as a result of glacial lake outburst floods.&amp;lt;ref name=RE1/&amp;gt; Glaciers, being ice sheets, can indicate increased [[air]] [[temperature]] due to being sensitive to [[climate change]].&amp;lt;ref name=RE1/&amp;gt; Glacial lakes are not only a risk of potential danger, but they are also an important natural resource, providing a [[fresh water]] source for people.&amp;lt;ref name=RE1/&amp;gt; Over the past 20-30 years, human measures to mitigate unstable glacier lakes in the Himalaya and European Alps may have prevented some potential GLOF disasters.&amp;lt;ref name=RE4/&amp;gt; Research has shown that due to global climate change and retreating glaciers, there is an escalated risk in GLOFs worldwide.&amp;lt;ref name=RE3/&amp;gt; This is leading glacial lakes to swell and increase the risk of flooding. For example, in Bhutan, a region with 677 glaciers and 2,794 glacial lakes&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/ins&gt;has &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;experienced &lt;/ins&gt;more than 21 glacial lake outburst floods in the last two centuries.&amp;lt;ref name=RE1/&amp;gt;  From the 21 mentioned, 4 of the outbursts have occurred in the last 40 years.&amp;lt;ref name=RE1/&amp;gt; GLOFs are quite rare, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;which makes exact statistics about them difficult. Climate change &lt;/ins&gt;is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;expected &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significantly increase &lt;/ins&gt;the number of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;GLOFs in &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;coming decades, although &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;number hasn&#039;t increased yet.&amp;lt;ref&amp;gt;&quot;Climate change and the global pattern &lt;/ins&gt;of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;moraine-dammed glacial lake outburst floods&quot; by Harrison et al, available here: https://www.&lt;/ins&gt;the&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;-cryosphere.net/12/1195/2018/ Accessed February 18th, 2020&lt;/ins&gt;.&amp;lt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;/&lt;/ins&gt;ref&amp;gt; &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Climate change is causing significant [[glacial retreat]], which is expected to continue in coming decades. &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Below is a video explaining climate change impacts and the risks associated with glacial lake outburst floods in regions of the Himalayas. [http://karakoram.co/portfolio/science/ For more information:]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Below is a video explaining climate change impacts and the risks associated with glacial lake outburst floods in regions of the Himalayas. [http://karakoram.co/portfolio/science/ For more information:]&lt;/div&gt;&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-l17&quot;&gt;Line 17:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 17:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;iframe width=&amp;quot;760&amp;quot; height=&amp;quot;455&amp;quot; src=&amp;quot;https://www.youtube.com/embed/T-AAm0w-KjA&amp;quot; frameborder=&amp;quot;0&amp;quot; allowfullscreen&amp;gt;&amp;lt;/iframe&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;iframe width=&amp;quot;760&amp;quot; height=&amp;quot;455&amp;quot; src=&amp;quot;https://www.youtube.com/embed/T-AAm0w-KjA&amp;quot; frameborder=&amp;quot;0&amp;quot; allowfullscreen&amp;gt;&amp;lt;/iframe&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;/html&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;/html&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;== For Further Reading ==&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;For further information please see the related pages below:&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[[Glacier]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[[Glacial and interglacial periods]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[[Climate change]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*[[Ice age]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;*Or explore a [[Special:Random| random page]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==References==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==References==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{reflist}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{reflist}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[Category: Uploaded]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>energy&gt;Jmdonev</name></author>
	</entry>
	<entry>
		<id>https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=4628&amp;oldid=prev</id>
		<title>Jmdonev: 1 revision imported: From the summer</title>
		<link rel="alternate" type="text/html" href="https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=4628&amp;oldid=prev"/>
		<updated>2016-09-17T22:29:48Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported: From the summer&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 22:29, 17 September 2016&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>Jmdonev</name></author>
	</entry>
	<entry>
		<id>https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=4627&amp;oldid=prev</id>
		<title>Jmdonev at 03:13, 4 September 2016</title>
		<link rel="alternate" type="text/html" href="https://energyeducation.ca/wiki/index.php?title=Glacial_lake_outburst_flood&amp;diff=4627&amp;oldid=prev"/>
		<updated>2016-09-04T03:13:38Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[Category:Done 2016-04-30]] &lt;br /&gt;
&amp;lt;onlyinclude&amp;gt;&amp;#039;&amp;#039;&amp;#039;Glacial lake outburst floods (GLOFs)&amp;#039;&amp;#039;&amp;#039; are [[flood]]s that occur from an unstable natural dam formed from a [[glacier | glacial]] retreat.&amp;lt;ref name=RE4&amp;gt;”Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation&amp;quot;, Intergovernmental Panel on Climate Change, New York, 2012.&amp;lt;/ref&amp;gt; &amp;lt;/onlyinclude&amp;gt; Glaciers are dynamic bodies of ice that change frequently.&amp;lt;ref name=RE3&amp;gt;&amp;quot;Hazards - Glaciers, Climate, and Society&amp;quot;, Glaciers.uoregon.edu, 2016. [Online]. Available: http://glaciers.uoregon.edu/hazards.html. [Accessed: 20- May- 2016].&amp;lt;/ref&amp;gt; When a glacier retreats, it can leave behind a large impression in the ground that fills with [[water]], turning it into a lake. This is typically known as a moraine.&amp;lt;ref name=RE4/&amp;gt; These lakes can be impounded by an unstable pile of debris and buried ice.&amp;lt;ref name=&amp;quot;RE2”&amp;gt;”Glacial lake outburst flood (GLOF)&amp;quot;, Swisseduc.ch, 2016. [Online]. Available: http://www.swisseduc.ch/glaciers/glossary/glof-2-en.html. [Accessed: 23- May- 2016].&amp;lt;/ref&amp;gt; As the [[climate]] warms, glaciers generally shrink. In many mountains such as the Andes, Himalaya, Alps, Rockies, and elsewhere, the retreat of glacier tongues sometimes allows unstable moraine dammed lakes to form.&amp;lt;ref name=RE3/&amp;gt; Terminal moraines act as dams for these lakes, but as the lakes swell from rising water levels and the retreating glacial ice tongue, the moraine dam can weaken. Moraine dams that become too weak may crumble under too much pressure from the swelling lake, creating a GLOF. If the moraine dams of a glacial lake fail, the water can burst out, leading to massive floods and debris flows with potentially extensive damage downstream, including loss of life and infrastructure.&amp;lt;ref name=&amp;quot;RE1&amp;quot;&amp;gt;&amp;quot;Glacial Lakes and Glacial Lake Outburst Floods in Nepal&amp;quot;, The International Centre for Integrated Mountain Development, 2011. [Online]. Available: http://www.icimod.org/dvds/201104_GLOF/reports/final_report.pdf. [Accessed: 24- May- 2016].&amp;lt;/ref&amp;gt; Alternatively, and more commonly, glacial ice from the retreating glacier can crash into lakes, generating giant waves that erode weak moraine dams in a matter of minutes, thereby also triggering GLOFs.&amp;lt;ref name=RE3/&amp;gt; &lt;br /&gt;
&lt;br /&gt;
&amp;lt;gallery caption=&amp;quot;Glacial lake outburst flood in Alaska&amp;quot; mode=packed heights=280px&amp;gt;&lt;br /&gt;
File:Russel_Lake_GLOF.PNG|&amp;lt;ref name =USGS/&amp;gt;&lt;br /&gt;
File:Hubbard_Glacier_May_20.2000.jpg|&amp;lt;ref name =USGS&amp;gt;USGS (Accessed September 3rd, 2016) [Online], Available: http://pubs.usgs.gov/fs/fs-001-03/&amp;lt;/ref&amp;gt;&lt;br /&gt;
File:Hubbard_Glacier_July_16.2002.jpg|&amp;lt;ref name =USGS/&amp;gt;&lt;br /&gt;
File:Hubbard_Glacier_August_14.2002.jpg|&amp;lt;ref name =USGS/&amp;gt;&lt;br /&gt;
&amp;lt;/gallery&amp;gt;&lt;br /&gt;
In the summer of 2002 Alaska&amp;#039;s Hubbard glacier pinched off the connection between Russel Fjord and Disenchantment bay. This made the Russel Fjord into a glacial lake, for a short period of time. The lake rose 15 m above sea level. When the lake burst, it sent almost 2 million cubic feet of water per second back into the bay.&amp;lt;ref name =USGS/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
In the past century, GLOFs have caused disasters in high mountain regions of the world which include the Andes, areas in Caucasus and Central Asia, the Himalayas, North America and the European Alps.&amp;lt;ref name=RE4/&amp;gt; There are many examples in Nepal in which loss of lives and property have occurred as a result of glacial lake outburst floods.&amp;lt;ref name=RE1/&amp;gt; Glaciers, being ice sheets, can indicate increased [[air]] [[temperature]] due to being sensitive to [[climate change]].&amp;lt;ref name=RE1/&amp;gt; Glacial lakes are not only a risk of potential danger, but they are also an important natural resource, providing a [[fresh water]] source for people.&amp;lt;ref name=RE1/&amp;gt; Over the past 20-30 years, human measures to mitigate unstable glacier lakes in the Himalaya and European Alps may have prevented some potential GLOF disasters.&amp;lt;ref name=RE4/&amp;gt; Research has shown that due to global climate change and retreating glaciers, there is an escalated risk in GLOFs worldwide.&amp;lt;ref name=RE3/&amp;gt; This is leading glacial lakes to swell and increase the risk of flooding. For example, in Bhutan, a region with 677 glaciers and 2,794 glacial lakes has experience more than 21 glacial lake outburst floods in the last two centuries.&amp;lt;ref name=RE1/&amp;gt;  From the 21 mentioned, 4 of the outbursts have occurred in the last 40 years.&amp;lt;ref name=RE1/&amp;gt; However, because GLOFs are quite rare, it is uncertain whether their frequency of occurrence is changing at either the regional or global scale. Researchers argue that outburst floods from moraine dammed lakes in North America for example may have increased due to a reduction in the number of the lakes since the end of the Little Ice Age.&amp;lt;ref name=RE4/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Below is a video explaining climate change impacts and the risks associated with glacial lake outburst floods in regions of the Himalayas. [http://karakoram.co/portfolio/science/ For more information:]&lt;br /&gt;
&lt;br /&gt;
&amp;lt;html&amp;gt;&lt;br /&gt;
&amp;lt;iframe width=&amp;quot;760&amp;quot; height=&amp;quot;455&amp;quot; src=&amp;quot;https://www.youtube.com/embed/T-AAm0w-KjA&amp;quot; frameborder=&amp;quot;0&amp;quot; allowfullscreen&amp;gt;&amp;lt;/iframe&amp;gt;&lt;br /&gt;
&amp;lt;/html&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;/div&gt;</summary>
		<author><name>Jmdonev</name></author>
	</entry>
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