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Willekeurige foto 's
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: VA IS NOT IDENTIFIABLE ON SATELLITE IMAGERY.

Tuesday Jun 27, 2017 12:00 PM |

Satellite image of Klyuchevskoy volcano on 27 Jun 2017
Satellite image of Klyuchevskoy volcano on 27 Jun 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report:

FVFE01 at 11:50 UTC, 27/06/17 from RJTD
VA ADVISORY
DTG: 20170627/1150Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2017/216
INFO SOURCE: HIMAWARI-8
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: VA IS NOT IDENTIFIABLE ON SATELLITE IMAGERY.
OBS VA DTG: 27/1120Z
OBS VA CLD: VA NOT IDENTIFIABLE FM SATELLITE DATA WIND FL180 320/44KT

FCST VA CLD +6 HR: NOT AVBL
FCST VA CLD +12 HR: NOT AVBL
FCST VA CLD +18 HR: NOT AVBL
RMK: T+0 CONFIDENCE LOW. VA IS NOT IDENTIFIABLE DUE TO MET CLOUD OR

DISSIPATED. WE WILL ISSUE FURTHER ADVISORY IF VA DETECTED ON
SATELLITE IMAGERY.
NXT ADVISORY: NO FURTHER ADVISORIES=

Vorig nieuws
Monday, Jun 26, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 26 Jun 2017
Monday, Jun 26, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 24 Jun 2017
Saturday, Jun 24, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Klyuchevskoy volcano with a small steam plume this morning
Friday, Jun 23, 2017
Mild, strombolian-type eruptions continue to occur at the summit vent of the volcano. ... [meer...]
Satellite image of Klyuchevskoy volcano on 22 Jun 2017
Friday, Jun 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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