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Klyuchevskoy vulkaan
Stratovulkaan 4835 m (15,863 ft)
Kamchatka, 56.06°N / 160.64°E
Current status: restless (2 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
Satelite Image by (c) Google & NASA
Satelite Image by (c) Google & NASA
 

Klyuchevsky volcano news & activity updates

Klyuchevskoy volcano Volcanic Ash Advisory: ERUPTION AT 20171204/2125Z FL200 EXTD E-NE REPORTED

Monday Dec 04, 2017 22:00 PM |

Satellite image of Klyuchevskoy volcano on  4 Dec 2017
Satellite image of Klyuchevskoy volcano on 4 Dec 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report:

FVFE01 at 21:49 UTC, 04/12/17 from RJTD
VA ADVISORY
DTG: 20171204/2149Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2017/376
INFO SOURCE: HIMAWARI-8 KBGS
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: ERUPTION AT 20171204/2125Z FL200 EXTD E-NE REPORTED

OBS VA DTG: 04/2120Z
OBS VA CLD: SFC/FL200 N5605 E16037 - N5633 E16100 - N5632 E16145 -
N5620 E16139 - N5619 E16059 MOV NE 10KT
FCST VA CLD +6 HR: 05/0320Z SFC/FL210 N5701 E16215 - N5609 E16215 -
N5559 E16043 - N5652 E16055
FCST VA CLD +12 HR: 05/0920Z SFC/FL210 N5732 E16206 - N5537 E16236 -

N5537 E16043 - N5735 E16050
FCST VA CLD +18 HR: 05/1520Z SFC/FL210 N5714 E16308 - N5620 E16128 -

N5533 E16235 - N5531 E16002 - N5852 E16002 - N5838 E16155
RMK: NIL
NXT ADVISORY: 20171205/0000Z=

Vorig nieuws
Satellite image of Klyuchevskoy volcano on 18 Sep 2017
Monday, Sep 18, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 13 Sep 2017
Wednesday, Sep 13, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  7 Sep 2017
Thursday, Sep 07, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  3 Sep 2017
Sunday, Sep 03, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  2 Sep 2017
Saturday, Sep 02, 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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