<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" 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:title>Evidence of destructive debris flows at (pre-) Hispanic Cayambe settlements, Ecuador</dc:title>
  <dc:creator>Vasconez, F. J.</dc:creator>
  <dc:creator>/Samaniego, Pablo</dc:creator>
  <dc:creator>Phillips, J.</dc:creator>
  <dc:creator>Andrade, S. D.</dc:creator>
  <dc:creator>Simbana, E.</dc:creator>
  <dc:creator>Nogales, V.</dc:creator>
  <dc:creator>Roman-Carrion, J. L.</dc:creator>
  <dc:creator>Muller, A. V.</dc:creator>
  <dc:creator>Vasquez, M. A.</dc:creator>
  <dc:subject>Debris flow</dc:subject>
  <dc:subject>Pre-Hispanic settlements</dc:subject>
  <dc:subject>Caranqui culture</dc:subject>
  <dc:subject>Cayambe</dc:subject>
  <dc:subject>Non-volcanic</dc:subject>
  <dc:subject>Post-eruptive</dc:subject>
  <dc:description>In Ecuador, a country with numerous potentially active volcanoes, recurrent large earthquakes, and regular climate-related events, it is surmised that phenomena such as debris flows have affected pre-Hispanic pop-ulations since their settlement in-5000 cal BC. Here, using a multidisciplinary approach, we studied the most recent debris flow events that affected the Cayambe city area, located 15 km west of the active glacier-clad Cayambe volcano. Based on detailed characterization of the deposits, including sedimentological, archaeolog-ical, and paleontological analyses, as well as radiocarbon dating. We found that two debris flow (i.e., Rio Blanco I and II) destroyed Caranqui settlements in 665-775 cal AD and 774-892 cal AD, respectively, while another event impacted a Spanish colonial farm in 1590-1620 cal AD (Rio Blanco III). The grain size distribution of these deposits indicates a gravel-rich flow for Rio Blanco I and clay-rich flow for Rio Blanco II and III, whilst com-ponentry suggests low juvenile volcanic content for all three deposits. Juvenile components include pumice and lustrous dense dacites, while accidental clasts are dull dense dacites, oxidized and hydrothermally-altered ma-terial, as well as archaeological artifacts. These results, in addition to radiocarbon ages, suggest that the debris flows could either be post-eruptive or not related to volcanic eruptions. Potential non-volcanic trigger mecha-nisms for these events include rainfall and/or earthquakes, which implies that they can occur at any time and without forecast. Currently, the city of Cayambe is rapidly expanding and, consequently, our findings are rele-vant for creating impact scenarios for future debris flows forming in the Rio Blanco headwaters and descending to the city.</dc:description>
  <dc:date>2022</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010086313</dc:identifier>
  <dc:identifier>fdi:010086313</dc:identifier>
  <dc:identifier>Vasconez F. J., Samaniego Pablo, Phillips J., Andrade S. D., Simbana E., Nogales V., Roman-Carrion J. L., Muller A. V., Vasquez M. A.. Evidence of destructive debris flows at (pre-) Hispanic Cayambe settlements, Ecuador. 2022, 634, 65-80</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>&#xC9;QUATEUR</dc:coverage>
  <dc:coverage>ANDES</dc:coverage>
</oai_dc:dc>
