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Klyuchevskoy vulkaan
Stratovulkaan 4835 m (15,863 ft)
Kamchatka, 56.06°N / 160.64°E
Current status: normal or dormant (1 out of 5)
Klyuchevskoy webcams / Live-gegevens | Reports
Klyuchevskoy vulkaan video 's
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Klyuchevskoy vulkaanuitbarstingen:
1697-98, 1720-21, 1727-31, 1737, 1740, 1762, 1767, 1770, 1772, 1785, 1787, 1788, 1789-90, 1791, 1807, 1812, 1813, 1819-22, 1829, 1840, 1848, 1852, 1853-54, 1865, 1877, 1878, 1879, 1882, 1883, 1890, 1896-97, 1890, 1896-97, 1898, 1904, 1907, 1909, 1910, 1911, 1913, 1915, 1922, 1923, 1925, 1926, 1929, 1931, 1932, 1935-36, 1937-39, 1944-1945, 1946, 1948, 1949, 1951, 1953, 1954, 1956, 1957, 1958, 1959, 1960-63, 1963-64, 1965-1966, 1967, 1968, 1969, 1970, 1971, 1971-73, 1974, 1977-80, 1981, 1982, 1982-83, 1984-85, 1986, 1986-90, 1991, 1992, 1992-93, 1994-95, 1996-97, 1998, 1999, 2000, 2002, 2002-04, 2005 - ongoing
Typical eruption style:
Dominantly explosive, strombolian and vulcanian activity, sometimes lava flows from fissure vents. At present in a phase of near-persistant activity.
Laatste aardbevingen in de omgeving
Meest recente satellietbeelden

Sentinel hub | Landsat 8
Satelite Image by (c) Google & NASA
Satelite Image by (c) Google & NASA
 

Klyuchevsky volcano news & activity updates

Klyuchevskoy volcano Volcanic Ash Advisory: POSS ERUPTION OBS AT 20170902/2000Z FL190 EXTD SW OBS VA DTG: 02/2130Z

Saturday Sep 02, 2017 22:15 PM |

Satellite image of Klyuchevskoy volcano on  2 Sep 2017
Satellite image of Klyuchevskoy volcano on 2 Sep 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report:

FVFE01 at 22:03 UTC, 02/09/17 from RJTD
VA ADVISORY
DTG: 20170902/2203Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2017/366
INFO SOURCE: HIMAWARI-8
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: POSS ERUPTION OBS AT 20170902/2000Z FL190 EXTD SW
OBS VA DTG: 02/2130Z
OBS VA CLD: SFC/FL190 N5550 E16013 - N5604 E16038 - N5602 E16041 -
N5540 E16017 MOV SW 5KT
FCST VA CLD +6 HR: 03/0330Z SFC/FL170 N5608 E16115 - N5527 E16059 -
N5510 E16016 - N5553 E16029
FCST VA CLD +12 HR: 03/0930Z SFC/FL160 N5626 E16214 - N5612 E16216 -

N5501 E16111 - N5452 E16008 - N5602 E16104
FCST VA CLD +18 HR: 03/1530Z SFC/FL140 N5637 E16253 - N5607 E16154 -

N5502 E16032 - N5506 E15857 - N5621 E16116
RMK: NIL
NXT ADVISORY: 20170903/0000Z=

Vorig nieuws
Satellite image of Klyuchevskoy volcano on 30 Aug 2017
Wednesday, Aug 30, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Friday, Aug 25, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 25 Aug 2017
Friday, Aug 25, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 24 Aug 2017
Thursday, Aug 24, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 23 Aug 2017
Wednesday, Aug 23, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]

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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