Klyuchevskoy volcano (Kamchatka): continuing mild strombolian activity

Пт, 30 янв 2015, 12:11
Lava flow or incandescent avalanche on Klyuchevskoy this morning (evening in Kamchatka)
Lava flow or incandescent avalanche on Klyuchevskoy this morning (evening in Kamchatka)
Активность вулкана сегодня состояла из продолжения легкой до умеренной Стромболианская деятельности. Вероятно поток лавы на его верхнем склоне по-прежнему активен, но кажется уменьшилось. Частые накаливания лавины произошел, сопровождается мягкой золы выбросов.
Токио VAAC выдается предупреждение о возможной пепла шлейф, поднимаясь до высоты 34 000 футов (10 км) 02:57 UTC, хотя он заявил, что без пепла был виден на спутниковых снимков, и нет такого шлейфа видна на веб-камеры изображения, только довольно разбавленный пепла шлейф на гораздо более низкой высоте.
Промежуток времени видео сегодняшней деятельности:

Предыдущие новости

Wed, 28 Jan 2015, 18:46
Ash cloud rising from the pyroclastic flow on Klyuchevskoy volcano yesterday
Извержение продолжается и лавовый поток активен на юго-востоке Верхняя фланге. Крах лавы от потока и насильственных снег лавы взаимодействия производится Пирокластический поток, который спустился на базе крутые горные вчера вечером около 17:40 местное время. Read all
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NASA photo of the eruption of Klyuchevsky volcano on 30 September, 1994, the volcano's largest explosion in 40 years. The large
NASA photo of the eruption of Klyuchevsky volcano on 30 September, 1994, the volcano's largest explosion in 40 years. The large


Kliuchevskoi is Kamchatka's highest and most active volcano.  Since its origin about 6000 years ago, the beautifully symmetrical, 4835-m-high basaltic stratovolcano has produced frequent moderate-volume explosive and effusive eruptions without major periods of inactivity.  Kliuchevskoi rises above a saddle NE of sharp-peaked Kamen volcano and lies SE of the broad Ushkovsky massif.  More than 100 flank eruptions have occurred at Kliuchevskoi during the past roughly 3000 years, with most lateral craters and cones occurring along radial fissures between the unconfined NE-to-SE flanks of the conical volcano between 500 m and 3600 m elevation.  The morphology of its 700-m-wide summit crater has been frequently modified by historical eruptions, which have been recorded since the late-17th century.  Historical eruptions have originated primarily from the summit crater, but have also included numerous major explosive and effusive eruptions from flank craters.


Source: Klyuchevsky information by the GVP (Smithsonian Institution)

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