<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>Serra, Elena</dc:creator>
  <dc:creator>Valla, Pierre G.</dc:creator>
  <dc:creator>Gribenski, Natacha</dc:creator>
  <dc:creator>Guedes Magrani, Fabio</dc:creator>
  <dc:creator>Carcaillet, Julien</dc:creator>
  <dc:creator>Delaloye, Reynald</dc:creator>
  <dc:creator>Grobéty, Bernard</dc:creator>
  <dc:creator>Braillard, Luc</dc:creator>
  <dc:date>2020-10-29</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Several palaeoclimatic archives have documented the pronounced climatic and  environmental change associated with the Lateglacial–Holocene transition in the  European Alps. However, the geomorphic response to this major environmental  transition has only been punctually investigated. In this study, we propose a detailed  reconstruction of post‐Last Glacial Maximum palaeoenvironmental conditions and  geomorphic connectivity in the Sanetsch Pass area (2252 m a.s.l., western Swiss  Alps) based on a multi‐method approach combining geomorphological and  sedimentological field investigations with quantitative sedimentology and  geochronology. Samples for sediment characterization (grain size, micromorphology  and X‐ray diffraction) and geochronology (optically stimulated luminescence and 10Be  surface exposure dating) were collected from three representative landforms of the  study area: a high‐elevation silty deposit covered by patterned ground, an alluvial fan,  and a hummocky moraine covered by rockfall deposits. Our results reveal the  geomorphic history of the three deposits and their connectivity through sediment  cascade. These results highlight the development of rapid and most probably  transient landscape changes in high Alpine regions during the Lateglacial–Holocene  transition, with an increase in sediment flux and the establishment of paraglacial and  periglacial geomorphic processes.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/308898</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/bra_grl.pdf</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S1.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S2.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S3.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S4.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S5.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S6A.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S6B.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/Table_S7.txt</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308898/files/bra_grl_sm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/bor.12480</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Boreas. - 2020, p. bor.12480</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Geomorphic response to the lateglacial–holocene transition in high alpine regions (Sanetsch pass, Swiss alps)</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>