<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>John F. Splettstoesser</dc:contributor>
  <dc:creator>Damien Gildea</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>The highest peak in Antarctica, the Vinson Massif (78º35’S, 85º25’W), is at an elevation of 4892 m (16,046 
ft), as determined in 2004. Measurements of the elevation have fluctuated over the years, from its earliest surveyed 
elevation of 5140 m (16,859 ft), to its present height. Vinson Massif and three of its near neighbors in the Sentinel 
Range of the Ellsworth Mountains are the highest peaks in Antarctica, making them a favorite objective of 
mountaineers. Well over 1,100 people have climbed Vinson since the first ascent by a team in the 1966-67 austral 
summer. The range is composed of Crashsite quartzite, making the Sentinel’s very resistant to erosion. Very accurate 
elevations have been achieved annually by GPS mapping done by a climbing team sponsored by the Omega 
Foundation, active in Antarctica since 1998. The Craddock Massif now includes Mt. Craddock, the ninth highest peak 
in Antarctica, at 4368 m (14,327 ft). Both are named for Campbell Craddock*, a U.S. geologist active in Antarctic 
research beginning in 1959-60.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20071047SRP069</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Craddock Massif and Vinson Massif remeasured</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>