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アララト山

Ararat

成層火山 · Turkiye · 5165m

Snow-capped Mount Ararat is seen from the Khor Virap monastery in Armenia, NE of the volcano. Ararat, also known as Agri Dagi, is Turkey's highest and easternmost volcano, lying near the border with Armenia. Ararat appears to have been active during the 3rd millennium BCE; pyroclastic flow deposits overlie early Bronze Age artifacts and human remains.
Snow-capped Mount Ararat is seen from the Khor Virap monastery in Armenia, NE of the volcano. Ararat, also known as Agri Dagi, is Turkey's highest and easternmost volcano, lying near the border with Armenia. Ararat appears to have been active during the 3rd millennium BCE; pyroclastic flow deposits overlie early Bronze Age artifacts and human remains. · 写真: Photo by Andrew Behesnilian (Wikimedia Commons). · Wikimedia Commons
タイプ
成層火山
Turkiye
地域
Arabia-Central Asia Volcanic Regions / Central Anatolian Volcanic Province
標高
5165m
座標
39.700, 44.300
最終噴火
1840年
テクトニクス環境
Intraplate / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Andesite / Basaltic Andesite
地質学的概要

Mount Ararat, also known as Agri Dagi, is Turkey's highest and largest volume volcano. The overall massif extends ~25 km NW-SE, and 18 km NE-SW, with another large volcano, Kucuk Ararat (or Lesser Ararat), ~11 km SE. Construction of the Greater and Lesser Ararat volcanoes was followed by a period of extensive flank eruptions, many erupted along N-S fissures. The initial stage of flank eruptions produced a cluster of cinder cones and dacitic-rhyolitic lava domes surrounding Greater Ararat and a series of pyroclastic cones and domes on the W flank of Lesser Ararat. There are also large pyroclastic cones lower on the flanks of the two volcanoes. A small cone ~8 km SW of Lesser Ararat appears to be the source of a dark lava-flow field covering ~80 km2 towards the S. Ararat appears to have been active during the 3rd millennium BCE; pyroclastic-flow deposits overlie early Bronze Age artifacts and human remains. Karakhanian et al. (2002) reported historical evidence for a phreatic eruption and pyroclastic flow at the time of a July 1840 earthquake and landslide.

Wikipedia の要約

要約が短いです。詳細は記事全文をご覧ください。

アララト山 またはアール山 は、トルコ共和国の東端にある標高5,137mの山であり成層火山である。

Wikipedia · CC BY-SA · 記事全文を読む

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
2450 BCE~2255 BCE · 1件 · 最大 VEI ?695 BCE~500 BCE · 1件 · 最大 VEI ?1450~1645 · 1件 · 最大 VEI ?1645~1840 · 2件 · 最大 VEI 32450 BCE1475 BCE305 BCE6701645

詳細タイムライン

  1. 1840年VEI 3観測記録
    1840-07-02 ~ 進行中
    Upper northern flank
  2. 1783年VEI ?地質学的推定
    1783 ~ 進行中
  3. 1450年VEI ?地質学的推定
    1450 ~ 進行中
  4. 紀元前 550年VEI ?地質学的推定
    BCE 550 ~ 進行中
    Summit (?) and north flank
  5. 紀元前 2450年 (±50年)VEI ?地質学的推定
    BCE 2450 ~ 進行中
    NW flank

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。