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Armenia · Cono piroclástico

Dar-Alages

Vaiyots-Sar

Tipo
Cono piroclástico
Altitud
2575 m
Última erupción
-2000
The Vaiyots-Sar scoria cone has a roughly 500-m-wide summit crater, seen in this August 2020 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 15 km across). Lavas with visible flow boundaries and levees are to the NW and S to SW of the cone, with some long, linear flows and some much broader flow fronts with pressure ridges.
The Vaiyots-Sar scoria cone has a roughly 500-m-wide summit crater, seen in this August 2020 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 15 km across). Lavas with visible flow boundaries and levees are to the NW and S to SW of the cone, with some long, linear flows and some much broader flow fronts with pressure ridges. · Foto: Satellite image courtesy of Planet Labs Inc., 2020 (https://www.planet.com/).
Tipo
Cono piroclástico
País
Armenia
Región
Arabia y Asia Central / Caucasus Volcanic Province
Altitud
2575 m
Coordenadas
39.797, 45.497
Última erupción
-2000
Contexto tectónico
Intraplaca / Corteza continental (> 25 km)
Forma volcánica
Menor (basáltico)
Roca principal
Andesita / Andesita basáltica
Resumen geológico

The Vaiyots-Sar pyroclastic cone is located in the southern Armenia province of Vayots Dzor in the western Vardenis Volcanic Highland south of Lake Sevan (Karakhanian et al., 2002); previous names such as Dar-Alages or Daly-Tapa are of Russian origin. Near the north end of the approximately 5 x 8 km flow field the 1.5-km-diameter cone rises about 300 m above the surrounding lavas, identified by Sviatlovsky (1959) as post-glacial. Oswald (1906) noted that steep escarpments of Nummulitic limestones were ~6 km NE of the cone across an lava-flow field. At the southern end of the flow field a fissure-fed lava flow several thousand years ago dammed the Arpah River near the town of Vyke and then flowed NW for 6 km; the flows overlie a late Pleistocene terrace and have little soil development (Karakhanian et al., 2002). The youthful-looking Smbatassar cinder cone, 17 km NW of Vaiyots-Sar, appears to be the source vent for Holocene lava flows that traveled 11 km N and 17 km S down two valleys (Karakhanian et al., 2002).

Resumen de Wikipedia

Resumen en inglés

Dar-Alages is a group of six cinder lava cones south of Lake Sevan in Armenia. Fissure eruptions from Vaiyots-Sar dammed the Arpa river at Vayk and continued down the valley for 6 km. These lava flows are considered Holocene in age given the lack of a soil cover and their placement above a Pleistocene river terrace. Smbatassar cinder cones likewise generated two lava flows of 11 and 17 km length that overlie Pleistocene Yeheghis river terraces, thus also dating to the Holocene. Legends of the destruction of the towns Yegheghis and Moz in 735 AD may be linked to activity in these volcanoes.

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Historial de erupciones

2 registradasGlosario
Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales · Usa las flechas para moverte entre barras y Enter para abrir
2000 a. C.~1803 a. C. · 1 erupciones · VEI máx. ?556~753 · 1 erupciones · VEI máx. ?2000 a. C.1410 a. C.623 a. C.34 a. C.556

Línea de tiempo detallada

  1. 753VEI ?Método no indicado
    753 – fin desconocido
  2. 2000 a. C. (±1000 años)VEI ?Estimación geológica
    2000 a. C. – fin desconocido
    Vaiyots-Sar

Volcanes cercanos

Enlaces externos

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