<?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>Sara G. Bangen</dc:contributor>
  <dc:contributor>Daniel D. Buscombe</dc:contributor>
  <dc:contributor>Joshua Caster</dc:contributor>
  <dc:contributor>Amy E. East</dc:contributor>
  <dc:contributor>Paul E. Grams</dc:contributor>
  <dc:contributor>Joel B. Sankey</dc:contributor>
  <dc:creator>Alan Kasprak</dc:creator>
  <dc:date>2017</dc:date>
  <dc:description>&lt;p&gt;In river valleys, fluvial and upland landscapes are intrinsically linked through sediment exchange between the active channel, near-channel fluvial deposits, and higher elevation upland deposits. During floods, sediment is transferred from channels to low-elevation nearchannel deposits [Schmidt and Rubin, 1995]. Particularly in dryland river valleys, subsequent aeolian reworking of these flood deposits redistributes sediment to higher elevation upland sites, thus maintaining naturallyoccurring aeolian landscapes [Draut, 2012]. &lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>University of Trento - Italy</dc:publisher>
  <dc:title>Linking fluvial and aeolian morphodynamics in the Grand Canyon, USA</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>