Klyuchevskoy volcano (Kamchatka): new ash emissions

Вс, 26 янв 2014, 12:16
Steam/ash plume from Klyuchevskoy volcano today (KVERT webcam)
Steam/ash plume from Klyuchevskoy volcano today (KVERT webcam)
Новый этап Эруптивной, по-видимому, начали на вулкан. VAAC Токио сообщили выбросов непрерывной золы и пепла шлейф, дрейфующих Север на высоте примерно 16 000 футов (5 км).
Веб-камеры изображения показывают значительное увеличение паром произошло сегодня, которая подготовила впечатляющий шлейфа, который скорее всего содержит золы. Пока KVERT не прокомментировал новый вид деятельности и кодекс авиации цвет до сих пор хранится в зеленый (но это может измениться, если продолжается деятельность или новое извержение подтверждается). Следующее видео показывает сегодняшней деятельности:

Предыдущие новости

Thu, 2 Jan 2014, 15:52
Взрывчатое вещество эффузивные извержения вулкана закончил 20 декабря, согласно KVERT, который сегодня разместил кодекс авиации цвет на зеленый. 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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