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<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:creator>Elaine S. McGee</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>The Colorado Yule marble, quarried in Marble, Colo.,&#13;
is a very pure white marble, and it has been widely&#13;
acclaimed for its quality and purity. This marble has been&#13;
used for many prominent buildings; one of the most notable&#13;
is the Lincoln Memorial in Washington, D.C., built nearly&#13;
80 years ago. Although most of the marble in the memorial&#13;
appears to be in very good condition, some of the stones&#13;
have developed pronounced surficial roughness and show a&#13;
significant loss of carved details and rounded edges&#13;
compared with adjacent stones. Because adjacent blocks of&#13;
marble receive nearly identical exposure to weathering&#13;
agents that cause deterioration of the marble, it seems very&#13;
likely that this pronounced difference in durability of&#13;
adjacent stones arises from some inherent characteristic of&#13;
the marble.&#13;
The Colorado Yule marble is a nearly pure calcite marble&#13;
with minor inclusions of mica, quartz, and feldspar.&#13;
Compositions of the calcite and the inclusion phases in the&#13;
marble are typical for those phases. The calcite grains that&#13;
compose the marble are irregularly shaped and range from&#13;
100 to 600 micrometers in diameter. The texture of the marble&#13;
is even, with a slight preferred directional elongation&#13;
that is visible when the marble is cut in certain directions.&#13;
Physical tests of the marble show that its strength is comparable&#13;
to that of other marbles typically used in buildings.&#13;
Variations in the durability of the marble, like those&#13;
seen at the Lincoln Memorial, are not related to variations in&#13;
calcite composition or to the presence of inclusions in the&#13;
marble. Most likely, the variations arise from differences in&#13;
the calcite grain boundaries and the degree to which the&#13;
grains interlock with one another. Weak grain boundaries&#13;
that permit water or solutions to penetrate into the marble&#13;
and dissolve the calcite grains at their edges cause the marble&#13;
to disaggregate or ?sugar.? Subtle differences in texture&#13;
that occur in the marble from various parts of the quarry&#13;
probably cause some stones to be more susceptible to this&#13;
form of deterioration. These differences may not be readily&#13;
visible when the stone is freshly quarried.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/b2162</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Dept. of the Interior, U.S. Geological Survey ; Information Services [distributor],</dc:publisher>
  <dc:title>Colorado Yule Marble; building stone of the Lincoln Memorial</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>