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Volcán Aracar

Aracar

Estratovolcán · Argentina · 6095 m

Aracar volcano in Argentina has a 1.5-km-wide summit crater in the center of this May 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 22 km across). Lobate lava flows with pressure ridges are exposed along the lower southern flanks, and lava flows have been emplaced around topographic highs on the W, E, and S.
Aracar volcano in Argentina has a 1.5-km-wide summit crater in the center of this May 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 22 km across). Lobate lava flows with pressure ridges are exposed along the lower southern flanks, and lava flows have been emplaced around topographic highs on the W, E, and S. · Foto: Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/). · Wikimedia Commons
Tipo
Estratovolcán
País
Argentina
Región
South America Volcanic Regions / Central Andean Volcanic Arc
Altitud
6095 m
Coordenadas
-24.290, -67.783
Última erupción
Desconocido
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

Aracar is a steep-sided stratovolcano with a youthful-looking summit crater 1-1.5 km in diameter that contains a small lake. It is located just east of the Argentina-Chile border. The volcano was constructed during three eruptive cycles dating back to the Pliocene. The andesitic stratovolcano overlies dacitic lava domes. Lava flows found at the base of the volcano below 4500 m elevation are relatively well preserved, but upper-flank lavas, often an indication of youthful activity, are not present (de Silva, 2007 pers. comm.). There were reports of possible ash columns from the summit in 1993, but it is not known whether these were rockfall dust or eruption plumes.

Resumen de Wikipedia

El Aracar es un estratovolcán ubicado en Argentina, cerca del límite con Chile. Presenta un cráter juvenil de 1,5 km de diámetro, el cual contiene una pequeña laguna. El cono volcánico se generó en tres ciclos eruptivos antes del Plioceno. El estratovolcán andesítico subyace sobre domos de lava dacítica. Se ven flujos de lava conservados en su base, por debajo de los 4500 m s. n. m. La primera ascensión fue realizada el 1.º de abril de 1958, por la cordada integrada por Jorge Cvitanic, del Club Andino del Norte (Salta) y los austriacos Gustav Lanschner y Emo Henrich.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1993~1993 · 1 erupciones · VEI máx. 219931993199419941994

Línea de tiempo detallada

  1. 1993VEI 2Estimación geológica
    1993-03-28 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.