<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">445365080</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180317142927.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170323e20110301xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s11001-011-9128-y</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s11001-011-9128-y</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Flash-flood hyperpycnal flows generating shallow-water landslides at Fiumara mouths in Western Messina Strait (Italy)</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[D. Casalbore, F. Chiocci, G. Scarascia Mugnozza, P. Tommasi, A. Sposato]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">On October 1, 2009, a small area along the Sicilian coast between the villages of Scaletta Zanclea and Giampilieri was struck by intense and concentrated rainfall causing countless small landslides widespread over the catchment area of steep subaerial creeks, locally known as Fiumara. Dense and quick debris flows were channelized within the Fiumara and destructively hit the villages and entered the sea, where they likely transformed into hyperpycnal flows. The availability of pre- and post-flood high-resolution bathymetry allows us to recognize the main features and the most significant morphological variations related to the impact of the flows on the seafloor. The passage of hyperpycnal flows on the seafloor possibly produced a suite of mass-wasting events, encompassing sheet landslides (i.e. erosive scours), retrogressive slope failure on loose sediment at the canyon headwall and rock-falls on the conglomeratic bedrock along canyon sidewall. The possible causes of these events are discussed on the basis of available morphological evidence and geotechnical considerations. Finally, the widespread occurrence of mass-wasting features (i.e. submarine landslide scars) morphologically similar to those generated by the 2009 flash flood allows us to hypothesize, from one side, a strong correlation between this catastrophic event and the evolution of submarine canyons, and from the other side, the possible use of these features for the assessment of flash-flood occurrence.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer Science+Business Media B.V., 2011</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Seafloor mapping</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Bathymetric residual</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Submarine instability</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Hyperpycnal flow</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Sicily</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Casalbore</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">CNR, Istituto di Geologia Ambientale e Geoingegneria, Rome, Via Salaria km 29.300, Monterotondo Stazione, 00016, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Chiocci</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Dip. Scienze della Terra, University of Rome Sapienza, P.le Aldo Moro 5, 00185, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Scarascia Mugnozza</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Dip. Scienze della Terra, University of Rome Sapienza, P.le Aldo Moro 5, 00185, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Tommasi</subfield>
   <subfield code="D">P.</subfield>
   <subfield code="u">CNR, Istituto di Geologia Ambientale e Geoingegneria, Rome, Via Salaria km 29.300, Monterotondo Stazione, 00016, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Sposato</subfield>
   <subfield code="D">A.</subfield>
   <subfield code="u">CNR, Istituto di Geologia Ambientale e Geoingegneria, Rome, Via Salaria km 29.300, Monterotondo Stazione, 00016, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Marine Geophysical Research</subfield>
   <subfield code="d">Springer Netherlands</subfield>
   <subfield code="g">32/1-2(2011-03-01), 257-271</subfield>
   <subfield code="x">0025-3235</subfield>
   <subfield code="q">32:1-2&lt;257</subfield>
   <subfield code="1">2011</subfield>
   <subfield code="2">32</subfield>
   <subfield code="o">11001</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s11001-011-9128-y</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/s11001-011-9128-y</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Casalbore</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">CNR, Istituto di Geologia Ambientale e Geoingegneria, Rome, Via Salaria km 29.300, Monterotondo Stazione, 00016, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Chiocci</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Dip. Scienze della Terra, University of Rome Sapienza, P.le Aldo Moro 5, 00185, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Scarascia Mugnozza</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Dip. Scienze della Terra, University of Rome Sapienza, P.le Aldo Moro 5, 00185, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Tommasi</subfield>
   <subfield code="D">P.</subfield>
   <subfield code="u">CNR, Istituto di Geologia Ambientale e Geoingegneria, Rome, Via Salaria km 29.300, Monterotondo Stazione, 00016, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Sposato</subfield>
   <subfield code="D">A.</subfield>
   <subfield code="u">CNR, Istituto di Geologia Ambientale e Geoingegneria, Rome, Via Salaria km 29.300, Monterotondo Stazione, 00016, Rome, Italy</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Marine Geophysical Research</subfield>
   <subfield code="d">Springer Netherlands</subfield>
   <subfield code="g">32/1-2(2011-03-01), 257-271</subfield>
   <subfield code="x">0025-3235</subfield>
   <subfield code="q">32:1-2&lt;257</subfield>
   <subfield code="1">2011</subfield>
   <subfield code="2">32</subfield>
   <subfield code="o">11001</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
