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Dar-Alages

Vaiyots-Sar

火砕丘 · Armenia · 2575m

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. · 写真: Satellite image courtesy of Planet Labs Inc., 2020 (https://www.planet.com/).
タイプ
火砕丘
Armenia
地域
Arabia-Central Asia Volcanic Regions / Caucasus Volcanic Province
標高
2575m
座標
39.797, 45.497
最終噴火
-2000年
テクトニクス環境
Intraplate / Continental crust (> 25 km)
火山地形
Minor (Basaltic)
主要岩石
Andesite / Basaltic Andesite
地質学的概要

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).

Wikipedia の要約

英語版の要約

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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噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
2000 BCE~1803 BCE · 1件 · 最大 VEI ?556~753 · 1件 · 最大 VEI ?2000 BCE1410 BCE623 BCE34 BCE556

詳細タイムライン

  1. 753年VEI ?地質学的推定
    753 ~ 進行中
  2. 紀元前 2000年 (±1000年)VEI ?地質学的推定
    BCE 2000 ~ 進行中
    Vaiyots-Sar

外部リンク

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