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	<title>Gill Bluff - Revision history</title>
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	<updated>2026-05-05T13:25:43Z</updated>
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		<id>https://www.westarctica.wiki/index.php?title=Gill_Bluff&amp;diff=7908&amp;oldid=prev</id>
		<title>Westarctica: Created page with &quot;Map of Mount Takahe showing the location of Gill Bluff '''Gill Bluff''' (76°14′S 112°33′W) is a rock bluff on the northwest side of [...&quot;</title>
		<link rel="alternate" type="text/html" href="https://www.westarctica.wiki/index.php?title=Gill_Bluff&amp;diff=7908&amp;oldid=prev"/>
		<updated>2019-12-01T22:05:48Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;&lt;a href=&quot;/index.php?title=File:Gill-Bluff.jpg&quot; title=&quot;File:Gill-Bluff.jpg&quot;&gt;350px|thumb|Map of Mount Takahe showing the location of Gill Bluff&lt;/a&gt; &amp;#039;&amp;#039;&amp;#039;Gill Bluff&amp;#039;&amp;#039;&amp;#039; (76°14′S 112°33′W) is a rock bluff on the northwest side of [...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Gill-Bluff.jpg|350px|thumb|Map of Mount Takahe showing the location of Gill Bluff]]&lt;br /&gt;
'''Gill Bluff''' (76°14′S 112°33′W) is a rock bluff on the northwest side of [[Mount Takahe]] in [[Westarctica]].&lt;br /&gt;
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==Paleological ice levels==&lt;br /&gt;
In 1999, a team from Albion College and the New Mexico Bureau of Mines conducted an extensive survey of Mount Takahe in an attempt to determine if the [[West Antarctic Ice Sheet]] was higher in the past than it is in modern time. They determined that vertical expansions of the West Antarctic Ice Sheet up to 575 meters above the present [[ice]] level are recorded in three volcanic passage zones around Mt. Takahe. The horizontal passage zones at Stauffer Bluff, Gill Bluff and [[Möll Spur]] formed where the late-stage lower flank eruptions emerged above the level of ice-magma interaction. The passage zones are inferred to represent approximate paleo-ice-levels at the time of eruptions.&lt;br /&gt;
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Descending and climbing passage zone sequences at Gill Bluff may indicate the draining and refilling of an ice-marginal lake during the eruption interval. In addition to glaciovolcanic deposits, an ablation till at Roper Point, located 292 meters above the present ice-sheet level, overlies an in-situ lava deposit.&lt;br /&gt;
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==Discovery and name==&lt;br /&gt;
Gill Bluff, with the rest of Mount Takahe, was mapped by the United States Geological Survey utilizing ground surveys and [[U.S. Navy]] air photos collected during the 1959–66 seasons. The bluff was named by the Advisory Committee on [[Antarctic]] Names in honor of Allan Gill, an aurora researcher at [[Byrd Station]] in 1963.&lt;br /&gt;
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==External links==&lt;br /&gt;
* [https://www.researchgate.net/publication/330183703_Higher_inland_ice_levels_of_the_West_Antarctic_Ice_Sheet_at_Mt_Takahe_volcano_during_Early_and_late_Wisconsinan_times Research paper on Gill Bluff]&lt;br /&gt;
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[[Category: Geography of Westarctica]]&lt;/div&gt;</summary>
		<author><name>Westarctica</name></author>
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