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The Global Volcanism Program has no activity reports for Quilotoa.
The Global Volcanism Program has no Weekly Reports available for Quilotoa.
The Global Volcanism Program has no Bulletin Reports available for Quilotoa.
Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|[ 1797 Feb 4 ]||[ Unknown ]||Uncertain|
|[ 1759 ]||[ Unknown ]||Uncertain||2|
|[ 1740 Dec ]||[ Unknown ]||Uncertain||2|
|[ 1725 ]||[ Unknown ]||Uncertain||2|
|[ 1660 Nov 28 ]||[ Unknown ]||Discredited|
|1280 (?)||Unknown||Confirmed||6||Radiocarbon (corrected)|
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Quirotoa | Quilatoa|
|Quilotoa is a truncated, forested dacitic cone containing a steep-walled, 3-km-wide caldera filled by a 250-m-deep lake. Lava domes form the caldera's perimeter and occupy its floor. Its most recent large eruption about 800 years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes. Reports of historical eruptions from the caldera lake are somewhat ambiguous. Fumaroles are present on the lake floor and hot springs occur on the eastern flank.
Photo by Minard Hall, 1973 (Escuela Politécnica Nacional, Quito).
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.
Di Muro A, Rosi M, Aguilera E, Barbieri R, Massa G, Mundula F, Pieri F, 2008. Transport and sedimentation dynamics of transitional explosive eruption columns: the example of the 800 BP Quilotoa plinian eruption (Ecuador). J Volc Geotherm Res, 174: 307-324.
Hall M L, 1977. El Volcanismo en El Ecuador. Quito: Biblioteca Ecuador, 120 p.
Hall M L, Mothes P A, 2008a. Quilotoa volcano--Ecuador: an overview of young dacitic volcanism in a lake-filled caldera. J Volc Geotherm Res, 176: 44-55.
Hantke G, Parodi I, 1966. Colombia, Ecuador and Peru. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 19: 1-73.
Mothes P A, Hall M L, 2008. The plinian fallout associated with Quilotoa's 800 yr BP eruption, Ecuadorian Andes. J Volc Geotherm Res, 176: 56-69.
Rosi M, Di Muro A, Aguilera E, 2006. Eruptive dynamics during the 800 yr BP Quilotoa eruption. IAVCEI Commission on Explosive Volcanism Field Workshop, Cities on Volcanoes 4, Quito, Ecuador 23-27 Jan, 2006, 30 p.
Rosi M, Landi P, Polacci M, Di Muro A, Zandomeneghi D, 2004. Role of conduit shear on ascent of the crystal-rich magma feeding the 800-year-B.P. Plinian eruption of Quilotoa volcano (Ecuador). Bull Volc, 66: 307-321.
Sapper K, 1917. Katalog der Geschichtlichen Vulkanausbruche. Strasbourg: Karl J Trubner, 358 p.
|Large Eruptions of Quilotoa||Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).|
|WOVOdat||WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.|
|EarthChem||EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).|
|Smithsonian Collections||Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.|