Mount Armaghan
Ghegham Volcanic Ridge
Medan gunung api · Armenia · 3597 m

- Tipe
- Medan gunung api
- Negara
- Armenia
- Wilayah
- Arabia-Central Asia Volcanic Regions / Caucasus Volcanic Province
- Ketinggian
- 3597 m
- Koordinat
- 40.283, 45.000
- Letusan terakhir
- -1900
- Kondisi tektonik
- Intraplate / Continental crust (> 25 km)
- Bentuk lahan
- Cluster
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisThe 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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Riwayat letusan
Garis waktu rinci
- 1900 SM (±750 tahun)VEI 0Perkiraan geologiBCE 1900 – BerlangsungNorth part of eastern cone cluster
Tautan eksternal
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