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	<id>https://future.figucarolina.org//w/index.php?action=history&amp;feed=atom&amp;title=Ozone_Hole</id>
	<title>Ozone Hole - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://future.figucarolina.org//w/index.php?action=history&amp;feed=atom&amp;title=Ozone_Hole"/>
	<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;action=history"/>
	<updated>2026-06-05T12:17:13Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=93100&amp;oldid=prev</id>
		<title>Earth Human Being: Text replacement - &quot;life form&quot; to &quot;life-form&quot;</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=93100&amp;oldid=prev"/>
		<updated>2023-08-30T09:50:26Z</updated>

		<summary type="html">&lt;p&gt;Text replacement - &amp;quot;life form&amp;quot; to &amp;quot;life-form&amp;quot;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&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 09:50, 30 August 2023&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-l11&quot;&gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&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;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;According to information from [[Ptaah]], nothing yet has changed regarding the increasing expansion of the opening in the ozone layer. One must assume, therefore, that the opening is enlarging and that the danger has not diminished in any way. The damage to the ozone layer poses equally as big a threat on the climate as do high ozone concentrations in the air, which also affect the weather and all life form organisms.&amp;lt;ref&amp;gt;[[FIGU Bulletin 008]]&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;According to information from [[Ptaah]], nothing yet has changed regarding the increasing expansion of the opening in the ozone layer. One must assume, therefore, that the opening is enlarging and that the danger has not diminished in any way. The damage to the ozone layer poses equally as big a threat on the climate as do high ozone concentrations in the air, which also affect the weather and all life&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;-&lt;/ins&gt;form organisms.&amp;lt;ref&amp;gt;[[FIGU Bulletin 008]]&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;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;/table&gt;</summary>
		<author><name>Earth Human Being</name></author>
	</entry>
	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=90270&amp;oldid=prev</id>
		<title>Earth Human Being: Text replacement - &quot;percent &quot; to &quot;per cent &quot;</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=90270&amp;oldid=prev"/>
		<updated>2023-07-19T11:03:15Z</updated>

		<summary type="html">&lt;p&gt;Text replacement - &amp;quot;percent &amp;quot; to &amp;quot;per cent &amp;quot;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 11:03, 19 July 2023&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;&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;[[Category:Meier Encyclopedia]]&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;[[Category:Meier Encyclopedia]]&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;&#039;&#039;&#039;The Ozone Hole&#039;&#039;&#039;: This term is applied to the destroyed [[Ozone Layer]] in the [[Earth]]&#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;percent &lt;/del&gt;but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;&#039;&#039;&#039;The Ozone Hole&#039;&#039;&#039;: This term is applied to the destroyed [[Ozone Layer]] in the [[Earth]]&#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;per cent &lt;/ins&gt;but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;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;/table&gt;</summary>
		<author><name>Earth Human Being</name></author>
	</entry>
	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=23054&amp;oldid=prev</id>
		<title>Daniel Leech at 11:46, 14 November 2016</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=23054&amp;oldid=prev"/>
		<updated>2016-11-14T11:46:00Z</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 11:46, 14 November 2016&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 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:Meier Encyclopedia]]&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;&amp;#039;&amp;#039;&amp;#039;The Ozone Hole&amp;#039;&amp;#039;&amp;#039;: This term is applied to the destroyed [[Ozone Layer]] in the [[Earth]]&amp;#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&amp;#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&amp;#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&amp;#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;#039;&amp;#039;&amp;#039;The Ozone Hole&amp;#039;&amp;#039;&amp;#039;: This term is applied to the destroyed [[Ozone Layer]] in the [[Earth]]&amp;#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&amp;#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&amp;#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&amp;#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;/table&gt;</summary>
		<author><name>Daniel Leech</name></author>
	</entry>
	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=22562&amp;oldid=prev</id>
		<title>Daniel Leech at 12:28, 31 August 2016</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=22562&amp;oldid=prev"/>
		<updated>2016-08-31T12:28:04Z</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 12:28, 31 August 2016&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-l21&quot;&gt;Line 21:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 21:&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;*[[Climate Change]]&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;*[[Climate Change]]&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;*[[Climate_change_-_The_facts_and_an_important_Plea|Climate change – The facts and an important Plea]]&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;*[[Climate_change_-_The_facts_and_an_important_Plea|Climate change – The facts and an important Plea]]&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;*[[Lifestyles and Health]]&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;&amp;lt;references/&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;references/&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Daniel Leech</name></author>
	</entry>
	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=21467&amp;oldid=prev</id>
		<title>Daniel Leech at 20:25, 20 May 2014</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=21467&amp;oldid=prev"/>
		<updated>2014-05-20T20:25:19Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 20:25, 20 May 2014&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;&#039;&#039;&#039;The Ozone Hole&#039;&#039;&#039;: This term is applied to the destroyed [[Ozone &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;layer&lt;/del&gt;]] in the [[Earth]]&#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;&#039;&#039;&#039;The Ozone Hole&#039;&#039;&#039;: This term is applied to the destroyed [[Ozone &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Layer&lt;/ins&gt;]] in the [[Earth]]&#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;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 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=&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;==Further Reading==&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;==Further Reading==&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;*[[Prior Knowledge Of Ozone Depletion]]&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;*[[Ozone]]&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;*[[Ozone]]&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;*[[Ozone Layer]]&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;*[[Ozone Layer]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Daniel Leech</name></author>
	</entry>
	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=21450&amp;oldid=prev</id>
		<title>Daniel Leech at 14:17, 15 May 2014</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=21450&amp;oldid=prev"/>
		<updated>2014-05-15T14:17:58Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 14:17, 15 May 2014&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;&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;#039;&amp;#039;&amp;#039;The Ozone Hole&amp;#039;&amp;#039;&amp;#039;: This term is applied to the destroyed [[Ozone layer]] in the [[Earth]]&amp;#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&amp;#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&amp;#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&amp;#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;#039;&amp;#039;&amp;#039;The Ozone Hole&amp;#039;&amp;#039;&amp;#039;: This term is applied to the destroyed [[Ozone layer]] in the [[Earth]]&amp;#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&amp;#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&amp;#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&amp;#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&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;&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;&amp;lt;div class=&quot;illustration&quot;&amp;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;[[File:World_UV_Mean.png]]&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;&amp;lt;/div&amp;gt;&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;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;/table&gt;</summary>
		<author><name>Daniel Leech</name></author>
	</entry>
	<entry>
		<id>https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=21441&amp;oldid=prev</id>
		<title>Daniel Leech: Created page with &quot;&#039;&#039;&#039;The Ozone Hole&#039;&#039;&#039;: This term is applied to the destroyed Ozone layer in the Earth&#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the...&quot;</title>
		<link rel="alternate" type="text/html" href="https://future.figucarolina.org//w/index.php?title=Ozone_Hole&amp;diff=21441&amp;oldid=prev"/>
		<updated>2014-05-15T13:35:25Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;&amp;#039;&amp;#039;&amp;#039;The Ozone Hole&amp;#039;&amp;#039;&amp;#039;: This term is applied to the destroyed &lt;a href=&quot;/w/index.php?title=Ozone_layer&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;Ozone layer (page does not exist)&quot;&gt;Ozone layer&lt;/a&gt; in the &lt;a href=&quot;/Billy_Meier/Earth&quot; title=&quot;Earth&quot;&gt;Earth&lt;/a&gt;&amp;#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;The Ozone Hole&amp;#039;&amp;#039;&amp;#039;: This term is applied to the destroyed [[Ozone layer]] in the [[Earth]]&amp;#039;s atmosphere above Antarctica. The destruction of the ozone layer is primarily the result of the terrestrial population&amp;#039;s utilization of materials which wreak negative chemical and physical effects. The leading cause for the ozone layer&amp;#039;s destruction is the use of chlorofluorocarbons (CFCs). Once released, they slowly rise into the atmosphere and reach the stratosphere over a ten to fifteen year period. There they break down, releasing highly reactive chlorine atoms and chlorine oxides which, in turn, react with the ozone and split it into oxygen. The ozone hole above the Antarctic was discovered in 1985 -- approximately ten years, therefore, after I notified terrestrial scientists of the ozone layer&amp;#039;s destruction on behalf of the Pleiadians/Plejarans (see Semjase Contact Notes Block #1, page 64a). By the end of 1992 further evaluations revealed that the hole was even larger than before. Over an expanse of nearly 23 million square kilometers [approximately 9 million square miles] above the South Pole, the ozone layer in the atmosphere by this time had already decreased by more than 50 percent. In comparison to 1991 figures, the ozone hole not only had expanded by 15 percent but the ozone had become thinner. These facts were the result of the interaction of the CFCs with halogens and sulfuric acid aerosols, which reached the atmosphere through the volcanic outbreaks of Pinatubo (June 1991) and Mount Hudson (August 1991). The aerosols seize nitrogen compounds and release reactive chlorine compounds that lead to the breakdown of the ozone. Strong evidence exists which reveals that the ozone layer in the northern hemisphere is greatly damaged and is also thinning.&lt;br /&gt;
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Damage to the ozone layer, among other things, produces severe biological consequences such as the increased mutation rates and a rapid escalation of cancerous skin diseases&amp;lt;ref&amp;gt;http://en.wikipedia.org/wiki/Skin_neoplasms&amp;lt;/ref&amp;gt;. Now it is mandatory that we also take into account the negative and harmful effects of ozone depletion on our climate.&amp;lt;ref&amp;gt;[[FIGU Bulletin 008]]&amp;lt;/ref&amp;gt;&lt;br /&gt;
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According to information from [[Ptaah]], nothing yet has changed regarding the increasing expansion of the opening in the ozone layer. One must assume, therefore, that the opening is enlarging and that the danger has not diminished in any way. The damage to the ozone layer poses equally as big a threat on the climate as do high ozone concentrations in the air, which also affect the weather and all life form organisms.&amp;lt;ref&amp;gt;[[FIGU Bulletin 008]]&amp;lt;/ref&amp;gt;&lt;br /&gt;
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==Further Reading==&lt;br /&gt;
*[[Ozone]]&lt;br /&gt;
*[[Ozone Layer]]&lt;br /&gt;
*[[Ozone Hole]]&lt;br /&gt;
*[[HAARP]]&lt;br /&gt;
*[[Climate Change]]&lt;br /&gt;
*[[Climate_change_-_The_facts_and_an_important_Plea|Climate change – The facts and an important Plea]]&lt;br /&gt;
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==References==&lt;br /&gt;
&amp;lt;references/&amp;gt;&lt;/div&gt;</summary>
		<author><name>Daniel Leech</name></author>
	</entry>
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