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Tres Vírgenes

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area of 0.46 km and averages a height of 0.06 km. These scoria cones consist of massive grain supported poorly sorted fallout beds. It also consists of 6 andesite lava being the Cueva de Gel, Lower Pintos, Upper Pintos, Lower Virgen, Pintos dacite, and Upper Virgen andesite lava. Adding to the andesites has one neck which serves as a feeding vent of the volcano and is almost entirely covered by younger deposits of the volcano. The Virgen dacite lava cone is the only cone and represents the main structure of the La Virgen stratocone. As well as there being many andesite lavas there are 4 lava domes. The Mezquital dacite lava dome is made up of two and they are located on the southern apron of the Virgen volcano. El Virgen is by far the most complex of the three volcanoes as you can see by everything that it consists of such as the lavas, cones, and domes.
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thick lobe-like lava. The dome has light gray lava with mottled structure due to the abundance of enclaves which are dark gray aphanitic that come in different shapes. The puerta dacite is well exposed compared to the other two domes. The dome is covered by a blocky lava surface with a crumble breccia at the base. It is 0.19 km thick and the lava contains sub-rounded 10 cm enclaves. The last dome being the youngest is the Upper Viejo dacite and this dome has a blocky surface as well and it contains sub-rounded enclaves. The average thickness of the dome is 0.26 km.
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Formation is beneath this volcanic cover which consists of shallow-water marine deposits identified by fossiliferous sandstone. Above all these layers, the region consists of a variety of pyroclastic particles from different stages of its most recent volcanic activity. These rocks produced at Las Tres Vírgenes volcanic region have characteristics like those of the calc–alkaline magma series. The volcanic complex has also emitted andesitic to dacitic magmas from 300 to 22ka.
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El Viejo is the oldest from the volcanoes that make up the Tres Virgenes. It is made up of three lava domes which are in oldest to youngest : the lower viejo dacite, puerta dacite, and the upper viejo dacite. The Lower Viejo dacite dome is overlain by the puerta dacite dome and has a 0.1 km
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This complex of three stratovolcanoes began as mostly dacitic lava flows and domes which resulted in the formation of El Viejo (300 Ka). Volcanic activity later shifted southwest forming El Azufre (173 Ka). Finally, at about 112 Ka, volcanism migrated southwest yet again beginning the creation of El
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The ground floor of Las Tres Vírgenes volcano holds the oldest rock in the region which is a granitic rock of the Cretaceous era. Above this intrusive rock layer is a volcanic cover from the late Cenozoic era that includes andesite from the Santa Lucía Range, and Esperanza basalt. The Santa Rosalia
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El Virgen is by far the most conspicuous of the three. It is made up of at least 6 scoria cones all spread out around the Virgen volcano. Three of these cones are on the southern flank of El Azufre and they have elongated and coalesced shapes and are crudely aligned in N-S direction. They cover an
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This volcano has block and ash flow which pyroclastic fans that are dissected by radial drainage and at the fan toe is limited by volcaniclastic deposits. The average thickness is 0.1 km and it covers an area of 7.5 km. Then it also consists of a dacite central dome which is located atop
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Volcán Las Tres Vírgenes is part of a cluster that includes the central vent structure of El Azufre and El Viejo. The off-shore volcanic ridges extend from Tres Vírgenes–Aguajito–La Reforma towards sea-floor spreading centers in the Guayamas basin. It is located within the Gulf of California rift
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contains a reference to an eruption in 1746. Radiometric datings, however, do not agree with this. A charcoal fragment found in a volcanic deposit was dated at approximately 6515 years before present. A basaltic lava flow, which must be younger than the actual eruption, was dated at
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Avellán, Denis Ramón; Macías, José Luis; Arce, José Luis; Saucedo-Girón, Ricardo; Garduño-Monroy, Víctor Hugo; Jiménez-Haro, Adrian; Sosa-Ceballos, Giovanni; Cisneros, Guillermo; Bernal, Juan Pablo; Layer, Paul W.; García-Sánchez, Laura (2019-07-03).
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Avellán, Denis Ramón; Macías, José Luis; Arce, José Luis; Jiménez-Haro, Adrian; Saucedo-Girón, Ricardo; Garduño-Monroy, Víctor Hugo; Sosa-Ceballos, Giovanni; Bernal, Juan Pablo; López-Loera, Hector; Cisneros, Guillermo; Layer, Paul W. (2018-07-01).
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the Azufre Volcano. It has a height of 0.3 km and an exposed area of 0.78 km. The lava varies from dark-gray to pinkish-gray and the dome shows sub-rounded lava blocks with dark gray enclaves.
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It is composed of three volcanoes, aligned northeast–southwest, with El Viejo, the oldest, to the northeast, El Azufre in the middle, and the youngest, El Vírgen, to the southwest.
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Virgen. Up until 22Ka, El Virgen initially had the largest cone of the three volcanoes at 31.2 km3. The next largest was El Viejo at 4.2 km3 and lastly, El Azufre at 3.8 km3.
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zone. It is a part of a volcanic ridge that extends from the eastern coast of Baja California towards active sea floor spreading in the Guaymas basin.
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Eruption and magma crystallization ages of Las Tres Vírgenes (Baja California) constrained by combined 230Th/238U and (U–Th)/He dating of zircon,
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The last eruption of the volcanoes in the complex was of El Vírgen, but the date is disputed. A map drawn by the
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Schmitt, Axel K.; Stockli, Daniel F.; Niedermann, Samuel; Lovera, Oscar M.; Hausback, Brian P. (2010-10-01).
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fragments from El Vírgen that yielded an age of approximately 36 thousand years B.P. for the eruption.
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El Vírgen, being by far the most conspicuous of the three, is commonly known as "Las Tres Vírgenes".
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Plinian eruption of La Virgen Tephra, Volcán Las Tres Virgenes, Baja California Sur, Mexico
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Dating of the 1746 Eruption of Tres Virgenes Volcano, Baja California Del Sur, Mexico,
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Journal of Volcanology and Geothermal Research, Issue 158, pp. 281–295, 2006.
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Journal of Volcanology and Geothermal Research, Issue 80 pp. 239–266, 1998.
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Holocene plinian eruption of La Virgen Volcano, Baja California, Mexico,
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Schmitt, Axel K.; Stockli, Daniel F.; Hausback, Brian P. (2006-11-15).
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Geological Society of America Bulletin, v. 73, pp. 647–648, May 1962.
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approximately 24 thousand years B.P., which agrees with a dating of
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Complex of volcanoes located Mulegé Municipality, Mexico
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Index


Elevation
Prominence
Listing
North America isolated peaks
Ultra prominent peak
Coordinates
27°28′12″N 112°35′30″W / 27.47000°N 112.59167°W / 27.47000; -112.59167
Volcán Las Tres Vírgenes is located in Mexico
Baja California Sur
Mexico
Mountain type
Stratovolcano
Last eruption
volcanoes
Mulegé Municipality
Baja California Sur
Baja California Peninsula
Mexico
Croatian
Ferdinand Konščak
tephra
Volcanoes of east-central Baja California
List of volcanoes in Mexico
List of Ultras of Mexico
List of mountain peaks of Mexico
"Tres Vírgenes"
Global Volcanism Program
Smithsonian Institution
Tres Virgenes Volcanic Complex

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