Montañas de Geghama
Ghegham Volcanic Ridge
Campo volcánico · Armenia · 3597 m

- Tipo
- Campo volcánico
- País
- Armenia
- Región
- Arabia y Asia Central / 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
Resumen en inglésThe Gegham mountains are a range of mountains in Armenia. The range is a tableland-type watershed basin of Sevan Lake from east, inflows of rivers Araks and Hrazdan from north and west, Azat and Vedi rivers from south-west and Arpachai river from south. The average elevation of the Gegham mountain range is near 2500m. The range is of volcanic origin including many extinct volcanoes. The range is 70 km length and 48 km width, and stretch between Lake Sevan and the Ararat plain. The highest peak of the Gegham mountains is the Azhdahak, at 3597m. They are formed by a volcanic field, containing Pleistocene-to-Holocene lava domes and cinder cones. The highland reaches a height of 1800–2000m up to 3000m in the dividing ridge.
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Historial de erupciones
Línea de tiempo detallada
- 1900 a. C. (±750 años)VEI 0Estimación geológicaBCE 1900 – En cursoNorth part of eastern cone cluster
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.