<?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>D.J. Harding</dc:contributor>
  <dc:contributor>S. Y. Johnson</dc:contributor>
  <dc:contributor>J.L. Harless</dc:contributor>
  <dc:contributor>C.S. Weaver</dc:contributor>
  <dc:contributor>B.L. Sherrod</dc:contributor>
  <dc:creator>R. A. Haugerud</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>More than 10,000 km2 of high-resolution, public-domain topography acquired by the Puget Sound Lidar Consortium is revolutionizing investigations of active faulting, continental glaciation, landslides, and surficial processes in the seismically active Puget Lowland. The Lowland-the population and economic center of the Pacific Northwest-presents special problems for hazards investigations, with its young glacial topography, dense forest cover, and urbanization. Lidar mapping during leaf-off conditions has led to a detailed digital model of the landscape beneath the forest canopy. The surface thus revealed contains a rich and diverse record of previously unknown surface-rupturing faults, deep-seated landslides, uplifted Holocene and Pleistocene beaches, and subglacial and periglacial features. More than half a dozen suspected postglacial fault scarps have been identified to date. Five scarps that have been trenched show evidence of large, Holocene, surface-rupturing earthquakes.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/1052-5173(2003)13&lt;0004:HLTOTP&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>High-resolution lidar topography of the Puget Lowland, Washington - A bonanza for earth science</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>