<?xml version="1.0"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="hr">
	<id>https://enciklopedija.cc/index.php?action=history&amp;feed=atom&amp;title=Ledenjak_Furtw%C3%A4ngler</id>
	<title>Ledenjak Furtwängler - Povijest promjena</title>
	<link rel="self" type="application/atom+xml" href="https://enciklopedija.cc/index.php?action=history&amp;feed=atom&amp;title=Ledenjak_Furtw%C3%A4ngler"/>
	<link rel="alternate" type="text/html" href="https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;action=history"/>
	<updated>2026-08-31T08:54:51Z</updated>
	<subtitle>Povijest promjena ove stranice na wikiju</subtitle>
	<generator>MediaWiki 1.42.3</generator>
	<entry>
		<id>https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;diff=607374&amp;oldid=prev</id>
		<title>WikiSysop: Zamjena teksta - &#039;&lt;!--&#039;&#039;&#039;Le(.*)&#039;&#039;&#039;--&gt;&#039; u &#039;&#039;</title>
		<link rel="alternate" type="text/html" href="https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;diff=607374&amp;oldid=prev"/>
		<updated>2025-06-22T08:12:45Z</updated>

		<summary type="html">&lt;p&gt;Zamjena teksta - &amp;#039;&amp;lt;!--&amp;#039;&amp;#039;&amp;#039;Le(.*)&amp;#039;&amp;#039;&amp;#039;--&amp;gt;&amp;#039; u &amp;#039;&amp;#039;&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;hr&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;←Starija inačica&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Inačica od 22. lipanj 2025. u 08:12&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;Redak 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Redak 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;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;lt;!--&#039;&#039;&#039;Ledenjak Furtwängler&#039;&#039;&#039;--&amp;gt;&lt;/del&gt;[[Datoteka:Glacier at summit of Mt Kilimanjaro 001.JPG|mini|desno|300px|Ledenjak Furtwängler (u prednjem dijelu)]]&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;[[Datoteka:Glacier at summit of Mt Kilimanjaro 001.JPG|mini|desno|300px|Ledenjak Furtwängler (u prednjem dijelu)]]&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;[[Datoteka:Kilimanjaro_Glaciers.jpg|mini|desno|300px|NASA-ina slika iz 2004. s lokacijama glavnih ledenjaka na planini Kilimanjaro. Područja koja nisu identificirana uglavnom su mali zaostali ledenjaci ili sniježišta.]]&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;[[Datoteka:Kilimanjaro_Glaciers.jpg|mini|desno|300px|NASA-ina slika iz 2004. s lokacijama glavnih ledenjaka na planini Kilimanjaro. Područja koja nisu identificirana uglavnom su mali zaostali ledenjaci ili sniježišta.]]&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>WikiSysop</name></author>
	</entry>
	<entry>
		<id>https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;diff=341148&amp;oldid=prev</id>
		<title>WikiSysop: Bot: Automatska zamjena teksta  (-{{cite web +{{Citiranje weba)</title>
		<link rel="alternate" type="text/html" href="https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;diff=341148&amp;oldid=prev"/>
		<updated>2021-11-20T06:49:13Z</updated>

		<summary type="html">&lt;p&gt;Bot: Automatska zamjena teksta  (-{{cite web +{{Citiranje weba)&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;hr&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;←Starija inačica&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Inačica od 20. studeni 2021. u 06:49&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l16&quot;&gt;Redak 16:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Redak 16:&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;    | volume = 7 | pages = 419–31 | date = 2013 | accessdate = 2014-10-08 | doi=10.5194/tc-7-419-2013| doi-access = free }}&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;    | volume = 7 | pages = 419–31 | date = 2013 | accessdate = 2014-10-08 | doi=10.5194/tc-7-419-2013| doi-access = free }}&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;div&gt;&amp;lt;ref name=&amp;quot;Stedman&amp;quot;&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;ref name=&amp;quot;Stedman&amp;quot;&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;   {{&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cite web &lt;/del&gt;| url = http://www.climbmountkilimanjaro.com/the-history-of-kilimanjaro/history-of-kilimanjaro-after-meyer/index.html&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;   {{&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Citiranje weba &lt;/ins&gt;| url = http://www.climbmountkilimanjaro.com/the-history-of-kilimanjaro/history-of-kilimanjaro-after-meyer/index.html&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;    | title = History of Kilimanjaro: After Meyer | work = Excerpt from &amp;quot;Kilimanjaro&amp;quot; | author = Stedman, Henry&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;    | title = History of Kilimanjaro: After Meyer | work = Excerpt from &amp;quot;Kilimanjaro&amp;quot; | author = Stedman, Henry&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;    | publisher = Climb Mount Kilimanjaro | accessdate = 2007-05-03&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;    | publisher = Climb Mount Kilimanjaro | accessdate = 2007-05-03&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-l22&quot;&gt;Redak 22:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Redak 22:&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;    | archivedate= 2008-09-08}}&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;    | archivedate= 2008-09-08}}&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;div&gt;&amp;lt;ref name=&amp;quot;T&amp;amp;D&amp;quot;&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;ref name=&amp;quot;T&amp;amp;D&amp;quot;&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;   {{&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cite web &lt;/del&gt;| url = http://research.bpcrc.osu.edu/Icecore/publications/Thompson_and_Davis_Ice_Cores_Africa_2013.pdf  &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;   {{&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Citiranje weba &lt;/ins&gt;| url = http://research.bpcrc.osu.edu/Icecore/publications/Thompson_and_Davis_Ice_Cores_Africa_2013.pdf  &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;    | title = Ice Core Records | author1 = Thompson, L. G. | author2 = Davis, M. E. | publisher = The Ohio State University&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;    | title = Ice Core Records | author1 = Thompson, L. G. | author2 = Davis, M. E. | publisher = The Ohio State University&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;    | date = 2013 | accessdate = 2016-03-07}}&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;    | date = 2013 | accessdate = 2016-03-07}}&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;div&gt;&amp;lt;ref name=&amp;quot;Thompson2002&amp;quot;&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;ref name=&amp;quot;Thompson2002&amp;quot;&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;   {{&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cite web &lt;/del&gt;| last = Thompson | first = Lonnie G. | authorlink =&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;   {{&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Citiranje weba &lt;/ins&gt;| last = Thompson | first = Lonnie G. | authorlink =&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;    | url = http://www.geo.umass.edu/climate/doug/pubs/thompson_etal_sci02.pdf&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;    | url = http://www.geo.umass.edu/climate/doug/pubs/thompson_etal_sci02.pdf&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;    | title = Kilimanjaro Ice Core Records: Evidence of Holocene Climate Change in Tropical Africa | format = pdf | work =&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;    | title = Kilimanjaro Ice Core Records: Evidence of Holocene Climate Change in Tropical Africa | format = pdf | work =&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>WikiSysop</name></author>
	</entry>
	<entry>
		<id>https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;diff=165277&amp;oldid=prev</id>
		<title>WikiSysop: Bot: Automatski unos stranica</title>
		<link rel="alternate" type="text/html" href="https://enciklopedija.cc/index.php?title=Ledenjak_Furtw%C3%A4ngler&amp;diff=165277&amp;oldid=prev"/>
		<updated>2021-09-27T02:56:10Z</updated>

		<summary type="html">&lt;p&gt;Bot: Automatski unos stranica&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Nova stranica&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;lt;!--&amp;#039;&amp;#039;&amp;#039;Ledenjak Furtwängler&amp;#039;&amp;#039;&amp;#039;--&amp;gt;[[Datoteka:Glacier at summit of Mt Kilimanjaro 001.JPG|mini|desno|300px|Ledenjak Furtwängler (u prednjem dijelu)]]&lt;br /&gt;
[[Datoteka:Kilimanjaro_Glaciers.jpg|mini|desno|300px|NASA-ina slika iz 2004. s lokacijama glavnih ledenjaka na planini Kilimanjaro. Područja koja nisu identificirana uglavnom su mali zaostali ledenjaci ili sniježišta.]]&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;[[Ledenjak]] Furtwangler&amp;#039;&amp;#039;&amp;#039; nalazi se u blizini [[vrh|vrha]] [[Kilimandžaro|planine Kilimanjaro]] u [[Tanzanija|Tanzaniji]]. Ledenjak je dobio ime po [[Walter Furtwängler|Walteru Furtwängleru]] koji je, zajedno sa [[Siegfried König|Siegfriedom Königom]], bio u četvrtoj grupa planinara koja se popela na vrh Kilimandžara 1912. godine.&amp;lt;ref name=&amp;quot;Stedman&amp;quot;/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Ledenik je mali ostatak [[Kilimandžaro|ledene kape]] koja je nekad bila na vrhu Kilimandžara. Gotovo 85% ledenog pokrivača nestalo je između listopada 1912. i lipnja 2011.&amp;lt;ref name=&amp;quot;Retreat&amp;quot;/&amp;gt; Prema trenutnoj brzini otapanja, procjenjuje se da će većina leda nestati do 2040. godine i &amp;quot;vrlo je malo vjerojatno da će ijedno ledeno tijelo ostati nakon 2060. godine&amp;quot;,&amp;lt;ref name=&amp;quot;Retreat&amp;quot;/&amp;gt; iako sezonski [[snijeg]] i dalje pada nekoliko mjeseci godišnje. &amp;lt;ref&amp;gt; [http://www.geology.ohio-state.edu/news_detail.php?newsId=1] &amp;quot;Snows of Kilimanjaro Disappearing, Glacial Ice Loss Increasing&amp;quot; Ohio State University, 2006.&amp;lt;/ref&amp;gt; &amp;lt;ref&amp;gt; Tyson Peter: [http://www.pbs.org/wgbh/nova/kilimanjaro/vanishing.html] &amp;quot;Vanishing into Thin Air&amp;quot; 2006.&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Ledenjak Furtwängler kontinuirano postoji tek otprilike od 1650. godine, što odgovara vrlo visokim razinama u kenijskom jezeru [[Naivasha]] i početku [[Maunderov minimum|Maunderovog minimuma]].&amp;lt;ref name=&amp;quot;T&amp;amp;D&amp;quot;/&amp;gt; Između mjerenja 1976. i 2000. godine, površina ovog ledenjaka prepolovljena je sa 113 000 m&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; na 60 000 m&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;.&amp;lt;ref name=&amp;quot;Thompson2002&amp;quot;/&amp;gt; Do 2018. veličina se smanjila na 11,000 m&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;.&amp;lt;ref&amp;gt;[http://kilimanjaro.bplaced.net/wiki/index.php?title=Furtw%C3%A4ngler_Gletscher Das Mount-Kilimanjaro-Wiki (DE)] - Furtwängler Gletscher - Ermittlung der aktuellen Gletschergröße 2018. Retrieved 2019-04-16&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Izvori ==&lt;br /&gt;
{{izvori|refs=&lt;br /&gt;
&amp;lt;ref name=&amp;quot;Retreat&amp;quot;&amp;gt;&lt;br /&gt;
  {{cite journal | url = http://www.the-cryosphere.net/7/419/2013/tc-7-419-2013.pdf &lt;br /&gt;
   | title = A century of ice retreat on Kilimanjaro: the mapping reloaded | journal = The Cryosphere&lt;br /&gt;
   | authors = N. J. Cullen, P. Sirguey, T. Ölg, G. Kaser, M. Winkler, and S. J. Fitzsimons&lt;br /&gt;
   | volume = 7 | pages = 419–31 | date = 2013 | accessdate = 2014-10-08 | doi=10.5194/tc-7-419-2013| doi-access = free }}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&amp;lt;ref name=&amp;quot;Stedman&amp;quot;&amp;gt;&lt;br /&gt;
  {{cite web | url = http://www.climbmountkilimanjaro.com/the-history-of-kilimanjaro/history-of-kilimanjaro-after-meyer/index.html&lt;br /&gt;
   | title = History of Kilimanjaro: After Meyer | work = Excerpt from &amp;quot;Kilimanjaro&amp;quot; | author = Stedman, Henry&lt;br /&gt;
   | publisher = Climb Mount Kilimanjaro | accessdate = 2007-05-03&lt;br /&gt;
   | archiveurl = https://web.archive.org/web/20080908035210/http://www.climbmountkilimanjaro.com/the-history-of-kilimanjaro/history-of-kilimanjaro-after-meyer/index.html&lt;br /&gt;
   | archivedate= 2008-09-08}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&amp;lt;ref name=&amp;quot;T&amp;amp;D&amp;quot;&amp;gt;&lt;br /&gt;
  {{cite web | url = http://research.bpcrc.osu.edu/Icecore/publications/Thompson_and_Davis_Ice_Cores_Africa_2013.pdf &lt;br /&gt;
   | title = Ice Core Records | author1 = Thompson, L. G. | author2 = Davis, M. E. | publisher = The Ohio State University&lt;br /&gt;
   | date = 2013 | accessdate = 2016-03-07}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&amp;lt;ref name=&amp;quot;Thompson2002&amp;quot;&amp;gt;&lt;br /&gt;
  {{cite web | last = Thompson | first = Lonnie G. | authorlink =&lt;br /&gt;
   | url = http://www.geo.umass.edu/climate/doug/pubs/thompson_etal_sci02.pdf&lt;br /&gt;
   | title = Kilimanjaro Ice Core Records: Evidence of Holocene Climate Change in Tropical Africa | format = pdf | work =&lt;br /&gt;
   | publisher = Science | date = October 2002 | accessdate = 2006-08-31 | display-authors=etal}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[[Kategorija:Ledenjaci]]&lt;br /&gt;
[[Kategorija:Zemljopis Tanzanije]]&lt;/div&gt;</summary>
		<author><name>WikiSysop</name></author>
	</entry>
</feed>