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Klyuchevskoy volcano
Stratovolcano 4835 m (15,863 ft)
Kamchatka, 56.06°N / 160.64°E
Current status: normal or dormant (1 out of 5)
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Klyuchevskoy volcano eruptions:
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.
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Satelite Image by (c) Google & NASA
Satelite Image by (c) Google & NASA
 

Klyuchevsky volcano news & activity updates

Klyuchevskoy volcano (Kamchatka): continuing activity, lava flow on SE flank

Wednesday Apr 27, 2016 21:23 PM | BY: T
Klyuchevskoi volcano early morning 28 April 2016
Klyuchevskoi volcano early morning 28 April 2016
As had been previously suggested, the volcano's most recent eruptive phase had become both effusive and explosive: in addition to ash-generating strombolian explosions from the summit vent, a new, but short-lived lava flow appeared during 23 or 24 April and descended approx. 800 m on the south-eastern flank of the volcano (along the Apakhonchich ravine).
It seems that the lava flow remained active at least until Tue (26 April) according to KVERT's daily reports and images from the local observatory, but seems to have stopped by now; glow is no longer visible on clear webcam imagery from yesterday and today.
A significant, continuous steam plume suggests that mild explosive activity continues.
Previous news
Sunday, Apr 24, 2016
Klyuchevskoi volcano this morning with what is likely a new lava flow (KVERT webcam)
The activity of the volcano has intensified, in particular during the past 24-36 hours. KVERT reported that strong strombolian explosions produced an ash plume that rose to 8-9 km altitude that drifted more than 400 km to the SW. ... read all
Wednesday, Apr 20, 2016
Strombolian activity at Klyuchevskoy volcano on 16 April (image: Yury Demyanchuk)
The volcano continues to be in mild to moderate strombolian activity. ... read all
Thursday, Apr 07, 2016
Steam plume from Klyuchevskoy volcano yesterday morning
According to KVERT new phase of (so far) mild strombolian activity seems to have started at the volcano on around 4 April. read all
Monday, May 11, 2015
Glow and ash plume from Klyuchevskoy volcano 9 May 2015 (KVERT webcam)
Mild strombolian activity and associated ash emissions continue from the summit crater of the volcano. read all
Sunday, May 03, 2015
Steam and ash plume from Klyuchevskoy volcano today
Activity at the volcano, probably strombolian-type explosions from the summit vent, has increased during the past days. read all

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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