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	<title>Deep Field</title>
	<updated>2008-08-20T23:19:51Z</updated>
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		<title>And so we begin...</title>
		<link rel="alternate" href="http://blog.deepfieldantarctica.com/2008/04/30/and-so-we-begin-3.aspx" />
		<id>tag:blog.deepfieldantarctica.com,2008-04-30:bb3168ac-370c-4b35-94d8-86b5a74cb7c5</id>
		<author>
			<name>Ed Stump</name>
		</author>
		<updated>2008-06-09T12:15:09Z</updated>
		<published>2008-04-30T17:05:00Z</published>
		<content type="html"><![CDATA[<p style="margin-bottom: 0in;">	My first season on the Ice was
1970-71, as a grad student at Ohio State, working on a
helicopter-supported project in the Queen Maud Mountains.  I came
into the Antarctic program just after what I like to think of as the
“Post-IGY Heroic Era”.  The real Heroic Era had ended with Byrd
in the 30’s (you might say earlier than that), and the several
expeditions between 1934 and the IGY never touched ground in the
Transantarctic Mountains (hereafter the TAM). The Post-IGY Heroic Era
was the period when the TAM were mapped in their entirety, both
topographically and geologically. 
</p>
<p style="text-indent: 0.5in; margin-bottom: 0in;">With the onset of
the International Geophysical Year (IGY), 1957-58, the U. S.
established McMurdo Station, the Kiwis, Scott Base.  With the air
capability to fly the length of the TAM and land on glaciers in the
open field, the U. S. and New Zealand fielded a succession of
independent ground parties that systematically mapped at a
reconnaissance level both the terrain and the geology. The stories
that these guys have to tell should fill a book some day, ought to be
in the oral history archives.  They completed huge traverses using
rickety, primitive snowmobiles, made surveys, collected rocks, mapped
contacts, and basically put together the geological history of the
TAM.  Topographic quadrangles at a scale of 1:250,000 for the
entirely of the TAM had been published by the USGS by 1965.  In 1969,
the year before I got my start, Folio 12 of the Antarctic Map Folio
Series was published by the American Geographical Society.  It
contained geological maps of the entire TAM (as well as all other
rocky areas of Antarctica) at a scale of 1:1,000,000.  This is <u><b>the</b></u>
benchmark publication for the geology of the TAM.  Essentially the
entire map of the TAM had color. Henceforth it has not been a matter
of filling in the spaces; it has been a matter of adding detail.</p>
<p style="text-indent: 0.5in; margin-bottom: 0in;">Actually, this is a
bit of an overstatement. At the time of the printing of Folio 12
there were in fact two places on the maps that lacked color, at the
northern end of northern Victoria Land (hereafter NVL) and a pocket
between Axel Heiberg Glacier and Amundsen Glacier.  Much of the area
from lower Scott Glacier out along the Watson Escarpment to Reedy
Glacier was mapped in a dark brown color, which the legend called
“Undifferentiated Basement Complex.” Blackburn had been up Scott
Glacier in 1933-34 and had noted mostly granite, and a single helo
landing had been made on Mt. Webster in 1962-63, where fossil
trilobites of Cambrian age had been found in some limestones, but
beyond that the lower Scott Glacier and Leverett Glacier areas were
uncharted. These unmapped areas were what drew me in the early years of my
career.</p>
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