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	<title>Glacial and interglacial periods - Revision history</title>
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	<updated>2026-04-28T20:51:56Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>https://energyeducation.ca/wiki/index.php?title=Glacial_and_interglacial_periods&amp;diff=6897&amp;oldid=prev</id>
		<title>Jmdonev: 1 revision imported: Doing upload, largely of old redirects.</title>
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		<updated>2018-06-04T16:52:29Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported: Doing upload, largely of old redirects.&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 16:52, 4 June 2018&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>
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		<title>Jmdonev at 21:04, 1 June 2018</title>
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		<updated>2018-06-01T21:04:08Z</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 21:04, 1 June 2018&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 2018-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;05&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;18&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 2018-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;06&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;01&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;div&gt;An [[ice age]] is a period of time where [[Global surface temperature|global temperatures]] drop so significantly that [[glacier]]s advance and encompass over one third of [[Earth]]’s surface both [[Latitude|laterally]] and [[Longitude|longitudinally]].&amp;lt;onlyinclude&amp;gt; During an ice age, a &amp;#039;&amp;#039;&amp;#039;glacial&amp;#039;&amp;#039;&amp;#039; is the period of time where glacial advancement occurs.&amp;lt;ref&amp;gt;S. Marshak, Earth: Portrait of a Planet, 3rd ed. New York: W.W. Norton, 2008. Part VI, pp. 791 &amp;amp; 797. [Accessed: 02-Mar-2018].&amp;lt;/ref&amp;gt; Similarly, an &amp;#039;&amp;#039;&amp;#039;interglacial&amp;#039;&amp;#039;&amp;#039; or interglacial period is the warmer period of time between ice ages where glaciers retreat and [[Rising sea level|sea levels rise]].&amp;lt;/onlyinclude&amp;gt;&amp;lt;ref name=&amp;quot;ref1&amp;quot;/&amp;gt; Over the last 450,000 years, glacials have lasted anywhere from 70,000 to 90,000 years whereas interglacials last approximately 10,000 years.&amp;lt;ref&amp;gt;S. G. Philander, Ed., Encyclopedia of global warming and climate change, vol. 2, 3 vols. Los Angeles: SAGE, 2008. pp. 519-522.&amp;lt;/ref&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;An [[ice age]] is a period of time where [[Global surface temperature|global temperatures]] drop so significantly that [[glacier]]s advance and encompass over one third of [[Earth]]’s surface both [[Latitude|laterally]] and [[Longitude|longitudinally]].&amp;lt;onlyinclude&amp;gt; During an ice age, a &amp;#039;&amp;#039;&amp;#039;glacial&amp;#039;&amp;#039;&amp;#039; is the period of time where glacial advancement occurs.&amp;lt;ref&amp;gt;S. Marshak, Earth: Portrait of a Planet, 3rd ed. New York: W.W. Norton, 2008. Part VI, pp. 791 &amp;amp; 797. [Accessed: 02-Mar-2018].&amp;lt;/ref&amp;gt; Similarly, an &amp;#039;&amp;#039;&amp;#039;interglacial&amp;#039;&amp;#039;&amp;#039; or interglacial period is the warmer period of time between ice ages where glaciers retreat and [[Rising sea level|sea levels rise]].&amp;lt;/onlyinclude&amp;gt;&amp;lt;ref name=&amp;quot;ref1&amp;quot;/&amp;gt; Over the last 450,000 years, glacials have lasted anywhere from 70,000 to 90,000 years whereas interglacials last approximately 10,000 years.&amp;lt;ref&amp;gt;S. G. Philander, Ed., Encyclopedia of global warming and climate change, vol. 2, 3 vols. Los Angeles: SAGE, 2008. pp. 519-522.&amp;lt;/ref&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;[[File:mxti9nqwax9allwndsil.png|thumb|800px|Figure 1: The globe on the left displays 18,000 years before present during the most recent glacial with ice coverage. The globe on the right displays the present day Holocene interglacial with significantly less glacial coverage. &amp;lt;ref name=ref1&amp;gt;“Glacial-Interglacial Cycles | National Centers for Environmental Information (NCEI) formerly known as National Climatic Data Center (NCDC).” [Online]. Available: https://www.ncdc.noaa.gov/abrupt-climate-change/Glacial-Interglacial%20Cycles. [Accessed: 02-Mar-2018].&amp;lt;/ref&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:mxti9nqwax9allwndsil.png|thumb|800px|Figure 1: The globe on the left displays 18,000 years before present during the most recent glacial with ice coverage. The globe on the right displays the present day Holocene interglacial with significantly less glacial coverage. &amp;lt;ref name=ref1&amp;gt;“Glacial-Interglacial Cycles | National Centers for Environmental Information (NCEI) formerly known as National Climatic Data Center (NCDC).” [Online]. Available: https://www.ncdc.noaa.gov/abrupt-climate-change/Glacial-Interglacial%20Cycles. [Accessed: 02-Mar-2018].&amp;lt;/ref&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;Another major difference between glacials and interglacials are the changes in sea level. During a glacial, sea levels drop an average of 100m as water is evaporated and stored in the growing glaciers and ice sheets. During an interglacial, sea levels rise as ice sheets and glaciers melt with the increase in temperature, thus resulting in an increase in volume of the ocean as water is heated.&amp;lt;ref&amp;gt; Poore, R.Z., Williams, R.S., Jr., and Tracey, Christopher, 2000, &quot;Sea level and climate&quot;, U.S. Geological Survey Fact Sheet 002–00, 2 p., [Online]. Available: https://pubs.usgs.gov/fs/fs2-00/. [Accessed: 12-Mar-2018].&amp;lt;/ref&amp;gt; However, due to the combustion of [[&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Fossil fuels| &lt;/del&gt;fossil &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fuels&lt;/del&gt;]] resulting in an increase in [[Global warming|global warming]], the icecaps are melting at a more rapid pace annually—raising the sea level by an average of 3.2 mm/yr and over 70 mm since 1995.&amp;lt;ref&amp;gt;NASA, &quot;Climate Change: Vital Signs of the Planet: Sea Level&quot;, [Online]. Available: https://climate.nasa.gov/vital-signs/sea-level/. [Accessed: 12-Mar-2018].&amp;lt;/ref&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;Another major difference between glacials and interglacials are the changes in sea level. During a glacial, sea levels drop an average of 100m as water is evaporated and stored in the growing glaciers and ice sheets. During an interglacial, sea levels rise as ice sheets and glaciers melt with the increase in temperature, thus resulting in an increase in volume of the ocean as water is heated.&amp;lt;ref&amp;gt; Poore, R.Z., Williams, R.S., Jr., and Tracey, Christopher, 2000, &quot;Sea level and climate&quot;, U.S. Geological Survey Fact Sheet 002–00, 2 p., [Online]. Available: https://pubs.usgs.gov/fs/fs2-00/. [Accessed: 12-Mar-2018].&amp;lt;/ref&amp;gt; However, due to the combustion of [[fossil &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fuel&lt;/ins&gt;]]&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;s &lt;/ins&gt;resulting in an increase in [[Global warming|global warming]], the icecaps are melting at a more rapid pace annually—raising the sea level by an average of 3.2 mm/yr and over 70 mm since 1995.&amp;lt;ref&amp;gt;NASA, &quot;Climate Change: Vital Signs of the Planet: Sea Level&quot;, [Online]. Available: https://climate.nasa.gov/vital-signs/sea-level/. [Accessed: 12-Mar-2018].&amp;lt;/ref&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;Presently, we are experiencing an abnormally long interglacial called the [[Holocene]] that has lasted nearly 11,000 years. A new glaciation has been expected to begin; however, due to human induced [[Climate change|climate change]] or [[Natural vs anthropogenic climate change| anthropogenic climate change]], the next glaciation is being delayed anywhere from a few thousand to hundreds of thousands of years. Therefore, it is expected that the Holocene interglacial may last at least another 150,000 years.&amp;lt;ref&amp;gt;Ganopolski, A., Winkelmann, R., Schellnuber, H. J., “Cristical insolation – CO2 relation for diagnosing past and future glacial inception”, Nature, vol. 529, p. 200, Jan 2016.&amp;lt;/ref&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;Presently, we are experiencing an abnormally long interglacial called the [[Holocene]] that has lasted nearly 11,000 years. A new glaciation has been expected to begin; however, due to human induced [[Climate change|climate change]] or [[Natural vs anthropogenic climate change| anthropogenic climate change]], the next glaciation is being delayed anywhere from a few thousand to hundreds of thousands of years. Therefore, it is expected that the Holocene interglacial may last at least another 150,000 years.&amp;lt;ref&amp;gt;Ganopolski, A., Winkelmann, R., Schellnuber, H. J., “Cristical insolation – CO2 relation for diagnosing past and future glacial inception”, Nature, vol. 529, p. 200, Jan 2016.&amp;lt;/ref&amp;gt;  &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_and_interglacial_periods&amp;diff=6347&amp;oldid=prev</id>
		<title>Jmdonev: 1 revision imported</title>
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		<updated>2018-05-18T22:53:15Z</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 22:53, 18 May 2018&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_and_interglacial_periods&amp;diff=6346&amp;oldid=prev</id>
		<title>Jmdonev at 21:26, 18 May 2018</title>
		<link rel="alternate" type="text/html" href="https://energyeducation.ca/wiki/index.php?title=Glacial_and_interglacial_periods&amp;diff=6346&amp;oldid=prev"/>
		<updated>2018-05-18T21:26:10Z</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 2018-05-18]] &lt;br /&gt;
An [[ice age]] is a period of time where [[Global surface temperature|global temperatures]] drop so significantly that [[glacier]]s advance and encompass over one third of [[Earth]]’s surface both [[Latitude|laterally]] and [[Longitude|longitudinally]].&amp;lt;onlyinclude&amp;gt; During an ice age, a &amp;#039;&amp;#039;&amp;#039;glacial&amp;#039;&amp;#039;&amp;#039; is the period of time where glacial advancement occurs.&amp;lt;ref&amp;gt;S. Marshak, Earth: Portrait of a Planet, 3rd ed. New York: W.W. Norton, 2008. Part VI, pp. 791 &amp;amp; 797. [Accessed: 02-Mar-2018].&amp;lt;/ref&amp;gt; Similarly, an &amp;#039;&amp;#039;&amp;#039;interglacial&amp;#039;&amp;#039;&amp;#039; or interglacial period is the warmer period of time between ice ages where glaciers retreat and [[Rising sea level|sea levels rise]].&amp;lt;/onlyinclude&amp;gt;&amp;lt;ref name=&amp;quot;ref1&amp;quot;/&amp;gt; Over the last 450,000 years, glacials have lasted anywhere from 70,000 to 90,000 years whereas interglacials last approximately 10,000 years.&amp;lt;ref&amp;gt;S. G. Philander, Ed., Encyclopedia of global warming and climate change, vol. 2, 3 vols. Los Angeles: SAGE, 2008. pp. 519-522.&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
[[File:mxti9nqwax9allwndsil.png|thumb|800px|Figure 1: The globe on the left displays 18,000 years before present during the most recent glacial with ice coverage. The globe on the right displays the present day Holocene interglacial with significantly less glacial coverage. &amp;lt;ref name=ref1&amp;gt;“Glacial-Interglacial Cycles | National Centers for Environmental Information (NCEI) formerly known as National Climatic Data Center (NCDC).” [Online]. Available: https://www.ncdc.noaa.gov/abrupt-climate-change/Glacial-Interglacial%20Cycles. [Accessed: 02-Mar-2018].&amp;lt;/ref&amp;gt;]]&lt;br /&gt;
&lt;br /&gt;
Another major difference between glacials and interglacials are the changes in sea level. During a glacial, sea levels drop an average of 100m as water is evaporated and stored in the growing glaciers and ice sheets. During an interglacial, sea levels rise as ice sheets and glaciers melt with the increase in temperature, thus resulting in an increase in volume of the ocean as water is heated.&amp;lt;ref&amp;gt; Poore, R.Z., Williams, R.S., Jr., and Tracey, Christopher, 2000, &amp;quot;Sea level and climate&amp;quot;, U.S. Geological Survey Fact Sheet 002–00, 2 p., [Online]. Available: https://pubs.usgs.gov/fs/fs2-00/. [Accessed: 12-Mar-2018].&amp;lt;/ref&amp;gt; However, due to the combustion of [[Fossil fuels| fossil fuels]] resulting in an increase in [[Global warming|global warming]], the icecaps are melting at a more rapid pace annually—raising the sea level by an average of 3.2 mm/yr and over 70 mm since 1995.&amp;lt;ref&amp;gt;NASA, &amp;quot;Climate Change: Vital Signs of the Planet: Sea Level&amp;quot;, [Online]. Available: https://climate.nasa.gov/vital-signs/sea-level/. [Accessed: 12-Mar-2018].&amp;lt;/ref&amp;gt;  &lt;br /&gt;
&lt;br /&gt;
Presently, we are experiencing an abnormally long interglacial called the [[Holocene]] that has lasted nearly 11,000 years. A new glaciation has been expected to begin; however, due to human induced [[Climate change|climate change]] or [[Natural vs anthropogenic climate change| anthropogenic climate change]], the next glaciation is being delayed anywhere from a few thousand to hundreds of thousands of years. Therefore, it is expected that the Holocene interglacial may last at least another 150,000 years.&amp;lt;ref&amp;gt;Ganopolski, A., Winkelmann, R., Schellnuber, H. J., “Cristical insolation – CO2 relation for diagnosing past and future glacial inception”, Nature, vol. 529, p. 200, Jan 2016.&amp;lt;/ref&amp;gt; &lt;br /&gt;
&lt;br /&gt;
[[File:ice_ages2.gif|center|800px|thumb|Figure 2: Glacial-interglacial cycles over the past 450,000 years to present. Glacials historically last anywhere from 7 to 9 times longer than interglacials.&amp;lt;ref&amp;gt;Utah Geological Survey. “Glad You Asked: Ice Ages – What are they and what causes them?&amp;quot;. [Online]. Available: https://geology.utah.gov/map-pub/survey-notes/glad-you-asked/ice-ages-what-are-they-and-what-causes-them/.[Accessed: 12-Mar-2018]&amp;lt;/ref&amp;gt;]]&lt;br /&gt;
&lt;br /&gt;
== For Further Reading ==&lt;br /&gt;
For further information please see the related pages below:&lt;br /&gt;
*[[Ice age]]&lt;br /&gt;
*[[Rising sea level]]&lt;br /&gt;
*[[Glacial lake outburst flood]] (also called [[GLOF]]s&lt;br /&gt;
*[[Glacier]]&lt;br /&gt;
*[[Climate change]]&lt;br /&gt;
*Or explore a [[Special:Random|random page]]&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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