<?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:creator>Water Resources Division, U.S. Geological Survey</dc:creator>
  <dc:date>1994</dc:date>
  <dc:description>The world's glaciers react to and interact 
with changes in global and regional climates. 
Most mountain glaciers worldwide have been 
retreating since the latter part of the 19th 
century; global sea level has risen about 10 
centimeters during the past century. Glaciers 
vary in size as a result of several factors, of 
which climate variation is probably the most 
important. The reasons we are interested in 
glacier variation include its connection to climate 
change and to global sea level.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/fs00994</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Satellite image atlas of glaciers of the world</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>