Вулкан Karymsky: Консультативный центр по вулканическому пеплу: VA CONTINUOUSLY OBS IN SATELLITE IMAGERY OBS VA DTG: 08/1720Z

Вс, 8 ноя 2020, 18:15
18:15 PM | ПЇЅПЇЅПЇЅПЇЅПЇЅ: VN
Спутниковое изображение вулкана Karymsky  8 Nov 2020
Спутниковое изображение вулкана Karymsky 8 Nov 2020
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 15 узлов в NE направлении.
Полный отчет выглядит следующим образом:

FVFE01 at 18:00 UTC, 08/11/20 from RJTD
VA ADVISORY
DTG: 20201108/1800Z
VAAC: TOKYO
VOLCANO: KARYMSKY 300130
PSN: N5403 E15927
AREA: RUSSIA
SUMMIT ELEV: 1513M
ADVISORY NR: 2020/108
INFO SOURCE: HIMAWARI-8
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: VA CONTINUOUSLY OBS IN SATELLITE IMAGERY
OBS VA DTG: 08/1720Z
OBS VA CLD: SFC/FL200 N5414 E15935 - N5454 E16018 - N5444 E16032 -
N5416 E16033 - N5406 E16000 MOV NE 15KT
FCST VA CLD +6 HR: 08/2320Z SFC/FL210 N5435 E16246 - N5407 E16203 -
N5348 E16015 - N5352 E15948 - N5440 E16016 - N5534 E16140
FCST VA CLD +12 HR: 09/0520Z SFC/FL210 N5431 E16528 - N5357 E16446 -

N5324 E15942 - N5436 E16036 - N5600 E16251
FCST VA CLD +18 HR: NO VA EXP
RMK: NIL
NXT ADVISORY: 20201109/0000Z=

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Background:

Karymsky, the most active volcano of  Kamchatka's eastern volcanic zone, is a symmetrical stratovolcano constructed within a 5-km-wide caldera that formed during the early Holocene.  The caldera cuts the south side of the Pleistocene Dvor volcano and is located outside the north margin of the large mid-Pleistocene Polovinka caldera, which contains the smaller Akademia Nauk and Odnoboky calderas. 
Most seismicity preceding Karymsky eruptions originated beneath Akademia Nauk caldera, which is located immediately south of Karymsky volcano.  The caldera enclosing Karymsky volcano formed about 7600-7700 radiocarbon years ago; construction of the Karymsky stratovolcano began about 2000 years later.  The latest eruptive period began about 500 years ago, following a 2300-year quiescence.  Much of the cone is mantled by lava flows less than 200 years old.  Historical eruptions have been vulcanian or vulcanian-strombolian with moderate explosive activity and occasional lava flows from the summit crater.


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Source: GVP, Smithsonian Institution


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