2021
DOI: 10.3390/su13041714
|View full text |Cite
|
Sign up to set email alerts
|

Community Perception and Communication of Volcanic Risk from the Cotopaxi Volcano in Latacunga, Ecuador

Abstract: The inhabitants of Latacunga living in the surrounding of the Cotopaxi volcano (Ecuador) are exposed to several hazards and related disasters. After the last 2015 volcanic eruption, it became evident once again how important it is for the exposed population to understand their own social, physical, and systemic vulnerability. Effective risk communication is essential before the occurrence of a volcanic crisis. This study integrates quantitative risk and semi-quantitative social risk perceptions, aiming for ris… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
8
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
5
1

Relationship

0
6

Authors

Journals

citations
Cited by 14 publications
(13 citation statements)
references
References 93 publications
0
8
0
Order By: Relevance
“…The most recent notable activity began with the eruptions of Tungurahua and Guagua Pichincha in September and October 1999, respectively, and since then three additional volcanoes (El Reventador, Cotopaxi, Sangay) have erupted in continental Ecuador [Hall and Mothes 2008;Robin et al 2008;Hidalgo et al 2018;Almeida et al 2019;Ortiz et al 2020;Valverde et al 2021]. These volcanoes showed different eruptive styles and eruption durations and led to different impacts on the population: Guagua Pichin-cha's eruption mainly resulted in ashfall on the capital city of Quito and the consequences (especially on the younger population) lasted for a few months [Naumova et al 2007]; Tungurahua's eruption lasted 16 years with explosions that occasionally caused significant ash emissions and pyroclastic density currents (PDC) that impacted local communities in various forms [Few et al 2017]; El Reventador and Sangay volcanoes continue to erupt almost without interruption to this day, with outbursts of explosions and small to medium PDCs and a relatively rapid landscape change [Ortiz et al 2021;Valverde et al 2021]; Cotopaxi volcano's brief reactivation in 2015 lasted for a few months with a paroxysm with a volcano explosivity index (VEI) of 2 and a lowlevel ash plume that caused social distress in nearby (∼14 km) communities [Hidalgo et al 2018;Gomez-Zapata et al 2021]. The high spatial density of active Holocene volcanoes and associated volcanic hazards has impacted pre-Columbian populations [Isaacson and Zeidler 1999;Hall and Mothes 2008;Vallego Vargas 2011;Le Pennec 2013] and continues to impact contemporary populations [Le Pennec et al 2008;Biass et al 2012;Le Pennec et al 2012] in the region.…”
Section: Geological Context Of Ecuadormentioning
confidence: 99%
See 4 more Smart Citations
“…The most recent notable activity began with the eruptions of Tungurahua and Guagua Pichincha in September and October 1999, respectively, and since then three additional volcanoes (El Reventador, Cotopaxi, Sangay) have erupted in continental Ecuador [Hall and Mothes 2008;Robin et al 2008;Hidalgo et al 2018;Almeida et al 2019;Ortiz et al 2020;Valverde et al 2021]. These volcanoes showed different eruptive styles and eruption durations and led to different impacts on the population: Guagua Pichin-cha's eruption mainly resulted in ashfall on the capital city of Quito and the consequences (especially on the younger population) lasted for a few months [Naumova et al 2007]; Tungurahua's eruption lasted 16 years with explosions that occasionally caused significant ash emissions and pyroclastic density currents (PDC) that impacted local communities in various forms [Few et al 2017]; El Reventador and Sangay volcanoes continue to erupt almost without interruption to this day, with outbursts of explosions and small to medium PDCs and a relatively rapid landscape change [Ortiz et al 2021;Valverde et al 2021]; Cotopaxi volcano's brief reactivation in 2015 lasted for a few months with a paroxysm with a volcano explosivity index (VEI) of 2 and a lowlevel ash plume that caused social distress in nearby (∼14 km) communities [Hidalgo et al 2018;Gomez-Zapata et al 2021]. The high spatial density of active Holocene volcanoes and associated volcanic hazards has impacted pre-Columbian populations [Isaacson and Zeidler 1999;Hall and Mothes 2008;Vallego Vargas 2011;Le Pennec 2013] and continues to impact contemporary populations [Le Pennec et al 2008;Biass et al 2012;Le Pennec et al 2012] in the region.…”
Section: Geological Context Of Ecuadormentioning
confidence: 99%
“…tentially devastating primary lahars or mudflows [Mothes et al 2004]. People in the vicinity of Cotopaxi even consider the occurrence of lahars to be impossible within their lifetimes while still acknowledging the volcano as the major local hazard [Gomez-Zapata et al 2021]. Others are unaware that the volcanoes in the Galapagos pose little hazard to the population as they have mostly effusive eruptions with lava flows that extend for a few kilometres from the volcanoes [Naumann and Geist 2000].…”
Section: The Hazard As a Sourcementioning
confidence: 99%
See 3 more Smart Citations