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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 AT 20170712/0050Z FL170 EXTD SSE REPORTED OBS VA DTG: 12/0150Z

Wednesday Jul 12, 2017 02:30 AM |

Satellite image of Klyuchevskoy volcano on 12 Jul 2017
Satellite image of Klyuchevskoy volcano on 12 Jul 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report:

FVFE01 at 02:23 UTC, 12/07/17 from RJTD
VA ADVISORY
DTG: 20170712/0223Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2017/251
INFO SOURCE: HIMAWARI-8 KVERT
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: VA AT 20170712/0050Z FL170 EXTD SSE REPORTED
OBS VA DTG: 12/0150Z
OBS VA CLD: SFC/FL170 N5609 E16043 - N5535 E16112 - N5530 E16103 -
N5607 E16039 MOV SE 20KT
FCST VA CLD +6 HR: 12/0750Z SFC/FL140 N5424 E16111 - N5243 E16140 -
N5253 E16041 - N5332 E16036
FCST VA CLD +12 HR: 12/1350Z SFC/FL120 N4959 E16222 - N5045 E16031 -

N5143 E15953 - N5245 E16121
FCST VA CLD +18 HR: 12/1950Z SFC/FL110 N5036 E16133 - N4816 E16422 -

N4810 E16356 - N5003 E16054 - N5056 E16015 - N5151 E16028 - N5206
E16157
RMK: T+0 CONFIDENCE HIGH.
NXT ADVISORY: 20170712/0600Z=

Vorig nieuws
Tuesday, Jul 11, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Friday, Jul 07, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  7 Jul 2017
Friday, Jul 07, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Thursday, Jul 06, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  6 Jul 2017
Thursday, Jul 06, 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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