<?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>K.A. Kastens</dc:contributor>
  <dc:contributor>A. Maldonado</dc:contributor>
  <dc:contributor>A. Malinverno</dc:contributor>
  <dc:contributor>C.H. Nelson</dc:contributor>
  <dc:contributor>S. O'Connell</dc:contributor>
  <dc:contributor>A. Palanques</dc:contributor>
  <dc:contributor>William B. F. Ryan</dc:contributor>
  <dc:creator>B. Alonso</dc:creator>
  <dc:date>1985</dc:date>
  <dc:description>The northern continental slope off the Ebro Delta has a badland topography indicating major slope erosion and mass movement of material that deposits sediment into a ponded lobe. The southern slope has a low degree of mass movement activity and slope valleys feed channel levee-complexes on a steep continental rise. The last active fan valley is V-shaped with little meandering and its thalweg merges downstream with the Valencia Valley. The older and larger inactive channel-levee complex is smoother, U-shaped, and meanders more than the active fan valley. ?? 1985 Springer-Verlag New York Inc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02281631</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Morphology of the Ebro fan valleys from SeaMARC and sea beam profiles</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>