<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>Schneuwly, Dominique M.</dc:creator>
  <dc:creator>Stoffel, Markus</dc:creator>
  <dc:date>2008-06-05</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Tree-ring series have been used to reconstruct 50 years of rockfall behavior on a slope near Saas Balen (Swiss Alps). A total of 796 cores and 141 cross sections from 191 severely injured conifer trees (&lt;i&gt;Larix decidua&lt;/i&gt; Mill., &lt;i&gt;Picea abies&lt;/i&gt; (L.) Karst. and &lt;i&gt;Pinus cembra&lt;/i&gt; L.), combined with a series of aerial photographs, were used to investigate the evolution of the forest stand so as (i) to reconstruct past rockfall rates; (ii) to analyze the spatial behavior of maximum bounce heights; and (iii) to analyze the spatial comportment of rockfall activity over the last five decades.Tree-ring analysis permitted the reconstruction of the age distribution at the study site; results were in perfect agreement with the afforestation process shown in the aerial photographs. The oldest are located in the lower, central part of the study site; the youngest individuals at its uppermost lateral boundaries. Reconstructed rockfall rates reveal strong interannual variations and single event years with increased activity, namely in 1960/1961 and 1995. Spatial analysis of the maximum bounce heights indicate highest values at the lateral boundaries and lowest heights in the lower central part of the forest stand, where a big boulder seems to shield trees growing below it. The spatial analysis of past rockfall activity shows high active zones at the uppermost north-facing boundaries of the forest and least active zones in the lowermost central part of the studied stand. The high rockfall activity at the slope is expressed by a mean rockfall rate of &gt; 1 event m&lt;sup&gt;− 1&lt;/sup&gt; y&lt;sup&gt;− 1&lt;/sup&gt;.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/300969</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/300969/files/stoffel_sar.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geomorph.2008.05.043</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Geomorphology. - 2008, vol. 102, no. 3-4, p. 522-531</dc:source>
  <dc:subject xmlns:ns1="xml" ns1:lang="en">Dendrogeomorphology</dc:subject>
  <dc:subject xmlns:ns2="xml" ns2:lang="en">tree-ring</dc:subject>
  <dc:subject xmlns:ns3="xml" ns3:lang="en">rockfall</dc:subject>
  <dc:subject xmlns:ns4="xml" ns4:lang="en">spatial analysis</dc:subject>
  <dc:subject xmlns:ns5="xml" ns5:lang="en">frequency</dc:subject>
  <dc:subject xmlns:ns6="xml" ns6:lang="en">GIS</dc:subject>
  <dc:subject>info:eu-repo/classification/udc/551</dc:subject>
  <dc:title xmlns:ns7="xml" ns7:lang="en">Spatial analysis of rockfall activity, bounce heights and geomorphic changes over the last 50 years – A case study using dendrogeomorphology</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
