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Klyuchevskoy вулкан
Стратовулкан 4835 m (15,863 ft)
Kamchatka, 56.06°N / 160.64°E
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Klyuchevsky volcano news & activity updates

Klyuchevskoy volcano (Kamchatka, Russia): ongoing strombolian activity from the summit crater

Вторник фев 25, 2020 10:37 | АВТОР: MARTIN

Glow from Klyuchevskoy volcano (image: KVERT)
Glow from Klyuchevskoy volcano (image: KVERT)
An ash plume from Klyuchevskoy volcano drifted towards the E direction (image: KVERT)
An ash plume from Klyuchevskoy volcano drifted towards the E direction (image: KVERT)
KVERT recorded a moderate explosions at the volcano that generated an ash plumes which reached approx. 16,400 ft-23,000 ft (5,000 m-7,000 m) altitude and drifted 84 km away towards the E direction. Strombolian activity continues from the summit crater.
Ongoing activity could affect low-flying aircrafts.
The Aviation Color Code remains orange.
Source: Kamchatka Volcanic Eruption Response Team volcano activity update 25 February 2020
Предыдущие новости

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

Background:

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.


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Source: Klyuchevsky information by the GVP (Smithsonian Institution)



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