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Eyewitness, stratigraphy, chemistry, and eruptive dynamics of the 1913 Plinian eruption of Volcán de Colima, México
related by: authorship_15301
date time value: article date 2596
related by: authorship_15300
type: Generically Dependent Continuant
crisid: 2596
origen: scopus
has funding vehicle: Consejo Nacional de Ciencia y Tecnología, CONACYT: PromeP UASLP-PTC-56, 45843, FAI C05-FAI-1012.33, 47226, 45894
related by: authorship_15303
doi: 10.1016/j.jvolgeores.2010.01.011
type: Continuant
page end: 166
related by: authorship_15302
abstract: Based on the stratigraphic record of the deposits, analysis of previous works, historic archives, and eyewitness accounts the 1913 eruption of Volcán de Colima was reconstructed. The eruption started in 17 January and peaked in 20 January, 1913. It occurred in three main phases: 1) An opening phase with the generation of Merapi-type pyroclastic flows (units F1, F2, F3) and a pyroclastic surge (S1), 2) A vent-clearing phase with strong explosions that produced Vulcanian-Soufriere-type pyroclastic flows (F4) and a pyroclastic surge (S2) which destroyed the summit dome decompressing the magma system, and 3) a Plinian phase with the establishment of a ~23km high column dispersing a fallout (C1) to the NE followed by the collapse of the column that generated a pyroclastic surge (S3) and 15-km long pumice-rich pyroclastic flows (F5). After the eruption, remobilization of the pyroclastic material generated lahars in main gullies around the crater. Fallout C1 blanketed an area of ~191,318km2 covering the cities of Guzman, Guadalajara, and Saltillo (Coahuila) located at 725km from the source. It had a volume of 1.4km3 (0.57km3 DRE= Dense Rock Equivalent). The total volume of pyroclastic flow and surge deposits was 0.26km3 (0.07km3 DRE) giving a total volume of the eruption of 1.66km3 (0.64km3 DRE). The Plinian column lasted 4.6h with a total mass of 1.5×1012kg and a mass eruption rate of 9.02×107kg/s. The column height and the ejected magma volume indicate that the 1913 eruption had a VEI=5 being the largest event in the historical record of Colima Volcano. Juvenile scoria and pumice consisted of Pl>Opx>Cpx>Hbl accessory titanomagnetite Ap and Ol with reaction rims. Chemistry of juvenile scoria and pumice samples is andesitic very homogeneous (58.3±0.5wt.%25 SiO2) and similar to the 1818 juvenile products (58.9±0.2wt.%25 SiO2). The presence of banded scoria, olivine phenocrysts with reaction rims, and trace element variations strongly suggest that the 1913 eruption was cause…
related by: authorship_15305
type: Entity
type: Article
type: Thing
page start: 149
volume: 191
has funding vehicle: National Science Foundation, NSF: EAR-0711043, EAR-0408896
related by: authorship_15304
abstract: Based on the stratigraphic record of the deposits, analysis of previous works, historic archives, and eyewitness accounts the 1913 eruption of Volcán de Colima was reconstructed. The eruption started in 17 January and peaked in 20 January, 1913. It occurred in three main phases: 1) An opening phase with the generation of Merapi-type pyroclastic flows (units F1, F2, F3) and a pyroclastic surge (S1), 2) A vent-clearing phase with strong explosions that produced Vulcanian-Soufriere-type pyroclastic flows (F4) and a pyroclastic surge (S2) which destroyed the summit dome decompressing the magma system, and 3) a Plinian phase with the establishment of a ~23km high column dispersing a fallout (C1) to the NE followed by the collapse of the column that generated a pyroclastic surge (S3) and 15-km long pumice-rich pyroclastic flows (F5). After the eruption, remobilization of the pyroclastic material generated lahars in main gullies around the crater. Fallout C1 blanketed an area of ~191,318km2 covering the cities of Guzman, Guadalajara, and Saltillo (Coahuila) located at 725km from the source. It had a volume of 1.4km3 (0.57km3 DRE= Dense Rock Equivalent). The total volume of pyroclastic flow and surge deposits was 0.26km3 (0.07km3 DRE) giving a total volume of the eruption of 1.66km3 (0.64km3 DRE). The Plinian column lasted 4.6h with a total mass of 1.5×1012kg and a mass eruption rate of 9.02×107kg/s. The column height and the ejected magma volume indicate that the 1913 eruption had a VEI=5 being the largest event in the historical record of Colima Volcano. Juvenile scoria and pumice consisted of Pl>Opx>Cpx>Hbl%2baccessory titanomagnetite%2bAp and Ol with reaction rims. Chemistry of juvenile scoria and pumice samples is andesitic very homogeneous (58.3±0.5wt.%25 SiO2) and similar to the 1818 juvenile products (58.9±0.2wt.%25 SiO2). The presence of banded scoria, olivine phenocrysts with reaction rims, and trace element variations strongly suggest that the 1913 eruption was c…
e iscopus: 2-s2.0-77950520875
most specific type: Document
type: Document
related by: authorship_15306
estado: published
issue: 3-4
has publication venue: Journal of Volcanology and Geothermal Research
most specific type: Article
freetext keyword: 1913; Colima Volcano; Eruption dynamics; Magma mixing; Mexico; Plinian eruption 1913; Magma mixing; Me-xico; Plinian eruption; Volcano eruptions; Deposits; Fallout; Olivine; Silicate minerals; Silicon compounds; Stratigraphy; Trace elements; Volcanoes; Compressible flow; explosive volcanism; geological record; magma; magmatic differentiation; plinian eruption; pumice; pyroclastic flow; volcanic eruption; Basse Terre; Coahuila; Colima; Colima Volcano; Guadalajara [Jalisco]; Guadeloupe; Jalisco; Leeward Islands [Lesser Antilles]; Mexico [North America]; Saltillo; Soufriere; Plinia
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Journal of Volcanology and Geothermal Research
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National Science Foundation, NSF: EAR-0711043, EAR-0408896
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funding vehicle for: Eyewitness, stratigraphy, chemistry, and eruptive dynamics of the 1913 Plinian eruption of Volcán de Colima, México

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Consejo Nacional de Ciencia y Tecnología, CONACYT: PromeP UASLP-PTC-56, 45843, FAI C05-FAI-1012.33, 47226, 45894
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