Vasconez F. J. auteur aut IRD Samaniego Pablo auteur aut IRD Phillips J. auteur aut IRD Andrade S. D. auteur aut IRD Simbana E. auteur aut IRD Nogales V. auteur aut IRD Roman-Carrion J. L. auteur aut IRD Muller A. V. auteur aut IRD Vasquez M. A. auteur aut IRD text journalArticle eng text/pdf reformatted digital access 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. specialized Debris flow Pre-Hispanic settlements Caranqui culture Cayambe Non-volcanic Post-eruptive ÉQUATEUR ANDES 112 064 066 634 65-80 2022 1040-6182 https://www.documentation.ird.fr/hor/fdi:010086313 10.1016/j.quaint.2022.06.006 1040-6182 [F B010086313] https://www.documentation.ird.fr/hor/fdi:010086313 https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2022-11/010086313.pdf IRD - Base Horizon / Pleins textes 2022-11-09 2025-02-24 fdi:010086313 fre