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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
Klyuchevskoy vulkaan boeken | Tours
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: VA EMISSIONS CONTINUING OBS VA DTG: 28/2320Z

Wednesday Mar 29, 2017 00:15 AM |

Satellite image of Klyuchevskoy volcano on 29 Mar 2017
Satellite image of Klyuchevskoy volcano on 29 Mar 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report:

FVFE01 at 00:03 UTC, 29/03/17 from RJTD
VA ADVISORY
DTG: 20170329/0003Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2017/51
INFO SOURCE: HIMAWARI-8
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: VA EMISSIONS CONTINUING
OBS VA DTG: 28/2320Z
OBS VA CLD: SFC/FL230 N5613 E16038 - N5612 E16053 - N5525 E16034 -
N5529 E16003 MOV SW 5KT
FCST VA CLD +6 HR: 29/0520Z SFC/FL240 N5552 E16110 - N5440 E15959 -
N5459 E15910 - N5553 E15925 - N5612 E16002
FCST VA CLD +12 HR: 29/1120Z SFC/FL240 N5523 E16100 - N5348 E15910 -

N5503 E15758 - N5543 E15754 - N5554 E16030
FCST VA CLD +18 HR: 29/1720Z SFC/FL240 N5457 E16039 - N5348 E15939 -

N5302 E15807 - N5542 E15700 - N5558 E15953
RMK: T+0 CONFIDENCE HIGH.
NXT ADVISORY: 20170329/0600Z=

Vorig nieuws
Satellite image of Klyuchevskoy volcano on 28 Mar 2017
Tuesday, Mar 28, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 27 Mar 2017
Monday, Mar 27, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 10 Mar 2017
Friday, Mar 10, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  9 Mar 2017
Thursday, Mar 09, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Thursday, Mar 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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