Вулкан Klyuchevskoy: Консультативный центр по вулканическому пеплу: VA EMISSIONS CONTINUING OBS VA DTG: 29/0520Z

Пт, 29 янв 2021, 06:15
06:15 AM | ПЇЅПЇЅПЇЅПЇЅПЇЅ: VN
Спутниковое изображение вулкана Klyuchevskoy 29 Jan 2021
Спутниковое изображение вулкана Klyuchevskoy 29 Jan 2021
Эруптивная активность продолжается. Консультативный центр по вулканическому пеплу (VAAC) в Tokyo предупредил о шлейфе вулканического пепла, который поднялся на высоту 20000 футов (6100 m) и движется со скоростью 30 узлов в NE направлении.
Полный отчет выглядит следующим образом:

FVFE01 at 06:00 UTC, 29/01/21 from RJTD
VA ADVISORY
DTG: 20210129/0600Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2021/63
INFO SOURCE: HIMAWARI-8
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: VA EMISSIONS CONTINUING
OBS VA DTG: 29/0520Z
OBS VA CLD: SFC/FL200 N5606 E16037 - N5617 E16048 - N5616 E16051 -
N5603 E16040 MOV NE 30KT
FCST VA CLD +6 HR: 29/1120Z SFC/FL210 N5815 E16433 - N5604 E16038 -
N5732 E16106
FCST VA CLD +12 HR: 29/1720Z SFC/FL200 N6015 E17149 - N5910 E16555 -

N5603 E16037 - N5838 E16016 - N5958 E16526
FCST VA CLD +18 HR: NO VA EXP
RMK: NIL
NXT ADVISORY: 20210129/1200Z=

Предыдущие новости

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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

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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