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Montañas de Geghama

Ghegham Volcanic Ridge

Campo volcánico · Armenia · 3597 m

The snow-capped cones of the Ghegam Ridge volcanic field rise across Lake Sevan from a fishing village on its NE shore. This volcanic field in west-central Armenia covers a 35-km-wide area between the capital city of Yerevan and Lake Sevan. Morphologically youthful lava flows from the central and eastern portions of Ghegam Ridge flowed into Lake Sevan.
The snow-capped cones of the Ghegam Ridge volcanic field rise across Lake Sevan from a fishing village on its NE shore. This volcanic field in west-central Armenia covers a 35-km-wide area between the capital city of Yerevan and Lake Sevan. Morphologically youthful lava flows from the central and eastern portions of Ghegam Ridge flowed into Lake Sevan. · Foto: Photo by Ivan Savov, 2002 (Smithsonian Institution). · Wikimedia Commons
Tipo
Campo volcánico
País
Armenia
Región
Arabia-Central Asia Volcanic Regions / Caucasus Volcanic Province
Altitud
3597 m
Coordenadas
40.283, 45.000
Última erupción
-1900
Contexto tectónico
Intraplate / Continental crust (> 25 km)
Forma volcánica
Cluster
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Ghegham Volcanic Ridge, located in west-central Armenia between the capital city of Yerevan and Lake Sevan, contains as many as 127 volcanic centers, lava domes and pyroclastic cones, of Pleistocene-to-Holocene age. The volcanoes and associated lava flows cover a 65-km-long, 35-km-wide area west of Lake Sevan and south of the Hrazdan River and are concentrated along three NNW-SSE-trending alignments. Lava flows from the central and eastern clusters flowed into Lake Sevan. Initial explosive eruptions in the volcanic field were followed by the extrusion of rhyolitic obsidian lava domes and flows. The latest activity produced a series of andesitic and basaltic andesite cinder cones and lava flows. The central and eastern portions of the field contain large areas of Holocene eruptions with morphologically fresh lava flows devoid of vegetation.

Resumen de Wikipedia

Las montañas de Geghama o Sierra de Geghama son una cadena de montañas en Armenia, entre el lago Sevan, al este, y la llanura de Ararat, al oeste. Por el norte limita con el valle del río Hrazdan, y por el sur con un pequeño cinturón de picos volcánicos, Hadis, Gutanasar, Menakasar, entre otros, y el paso de Vanderyats, donde se encuentra el Caravanserai de Orbelian. Toda la vertiente oriental se encuentra en la provincia de Geghark'unik'; la occidental se encuentra dividida entre las provincias de Kotayk', al norte y Ararat, al sur, y la meridional limita con la provincia de Vayots' Dzor.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1900 BCE~1900 BCE · 1 erupciones · VEI máx. 01900 BCE1900 BCE1899 BCE1899 BCE1899 BCE

Línea de tiempo detallada

  1. 1900 a. C. (±750 años)VEI 0Estimación geológica
    BCE 1900 – En curso
    North part of eastern cone cluster

Enlaces externos

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