Middle–to–late Holocene explosive eruptions of Lonquimay volcano (Southern Andes of Chile): Stratigraphy, tephra dispersal, and pre-eruptive conditions

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F25%3A10513882" target="_blank" >RIV/00216208:11310/25:10513882 - isvavai.cz</a>

Výsledek na webu

<a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=bB_6IRGSZ_" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=bB_6IRGSZ_</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.jvolgeores.2025.108457" target="_blank" >10.1016/j.jvolgeores.2025.108457</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Middle–to–late Holocene explosive eruptions of Lonquimay volcano (Southern Andes of Chile): Stratigraphy, tephra dispersal, and pre-eruptive conditions

Popis výsledku v původním jazyce

The Lonquimay-Tolguaca Volcanic Complex (LTVC), located in Chile&apos;s Andean Southern Volcanic Zone (40°S), experienced its last eruption in 1988-90, profoundly affecting neighbouring rural communities. Yet, more than twenty explosive eruptions have been recognised and described at Lonquimay volcano from its Holocene tephra records. Knowing its eruptive past is one of the main concerns of the residents of Malalcahuello, 11 km E-SE from the LTVC. In this contribution, we aim to decipher the behaviour of Lonquimay, focusing on its most recent (i.e., Middle-to-Late Holocene, &lt;5.5 ka) explosive history to address community-based questions with renewed scientific knowledge. We studied proximal-to-medial (i.e., 2-15 km) tephra sequences east-southeast from the LTVC. Seventeen tephra units were described. These are mainly formed by rhythmic alternations of both grey to white pumice beds, and black to brown scoria beds. Pyroclast textures consisting of scoria, dense juvenile fragments and pumices display compositions ranging from basalts to dacites. The study of tephra deposits suggests Strombolian to Sub-Plinian eruptive styles, whereas isopach-based volume estimates on the order of 10(7) m3 from four individual deposits support a Volcanic Explosivity Index (VEI) of 3. This type of events has a 27-61 % probability of occurrence within the next 100 years. The studied tephra deposits were fed by mafic (basaltic and basaltic andesitic, 1050-1100 °C) and silicic (andesites and dacites, 890-940 °C) magma batches stored between ~2 to ~7.5 kbar. Magma evolution was mostly controlled by fractional crystallisation and occasional mixing events. Assessing tephra fall deposits simultaneously at multiple scales offers clues on the eruptive scenarios, magma processes and sources, as well as potential hazards of their parent volcanic systems. Along with contributing to scientific knowledge, these elements can enhance risk reduction strategies by integrating community questions about active volcanism into hazard research.

Název v anglickém jazyce

Middle–to–late Holocene explosive eruptions of Lonquimay volcano (Southern Andes of Chile): Stratigraphy, tephra dispersal, and pre-eruptive conditions

Popis výsledku anglicky

The Lonquimay-Tolguaca Volcanic Complex (LTVC), located in Chile&apos;s Andean Southern Volcanic Zone (40°S), experienced its last eruption in 1988-90, profoundly affecting neighbouring rural communities. Yet, more than twenty explosive eruptions have been recognised and described at Lonquimay volcano from its Holocene tephra records. Knowing its eruptive past is one of the main concerns of the residents of Malalcahuello, 11 km E-SE from the LTVC. In this contribution, we aim to decipher the behaviour of Lonquimay, focusing on its most recent (i.e., Middle-to-Late Holocene, &lt;5.5 ka) explosive history to address community-based questions with renewed scientific knowledge. We studied proximal-to-medial (i.e., 2-15 km) tephra sequences east-southeast from the LTVC. Seventeen tephra units were described. These are mainly formed by rhythmic alternations of both grey to white pumice beds, and black to brown scoria beds. Pyroclast textures consisting of scoria, dense juvenile fragments and pumices display compositions ranging from basalts to dacites. The study of tephra deposits suggests Strombolian to Sub-Plinian eruptive styles, whereas isopach-based volume estimates on the order of 10(7) m3 from four individual deposits support a Volcanic Explosivity Index (VEI) of 3. This type of events has a 27-61 % probability of occurrence within the next 100 years. The studied tephra deposits were fed by mafic (basaltic and basaltic andesitic, 1050-1100 °C) and silicic (andesites and dacites, 890-940 °C) magma batches stored between ~2 to ~7.5 kbar. Magma evolution was mostly controlled by fractional crystallisation and occasional mixing events. Assessing tephra fall deposits simultaneously at multiple scales offers clues on the eruptive scenarios, magma processes and sources, as well as potential hazards of their parent volcanic systems. Along with contributing to scientific knowledge, these elements can enhance risk reduction strategies by integrating community questions about active volcanism into hazard research.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Volcanology and Geothermal Research

ISSN

0377-0273

e-ISSN

1872-6097

Svazek periodika

468

Číslo periodika v rámci svazku

December

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

18

Strana od-do

108457

Kód UT WoS článku

001588806100001

EID výsledku v databázi Scopus

2-s2.0-105017237632