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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
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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 (Kamchatka): new strombolian-type eruption

Thursday Mar 02, 2017 17:23 PM | DOOR: T

Ash emission from Klyuchevskoy volcano last evening (KVERT webcam)
Ash emission from Klyuchevskoy volcano last evening (KVERT webcam)
The activity of the volcano has again increased into a new eruptive phase. KVERT raised the Aviation Color Code to orange.
After more than a month of relative calm, with only degassing and sporadic weak ash emissions, the volcano began a more sustained phase of strombolian activity shortly after midnight (local time) between yesterday and today (1-2 March). So far, this activity has been accompanied by mild to moderate ash emissions, but no lava flow (as typical for most eruptions at the volcano). This could change quickly if the effusion rate increases.
The most recent eruptive phase from Klyuchevskoy took place between April-November last year and was characterized by both lava flows and mild to moderate explosive activity at the summit, at fluctuating intensity. It was followed by a period with sporadic weak ash emissions followed during December and January, showing that the activity at the volcano never really stopped completely.
Vorig nieuws
Thursday, Mar 02, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on  1 Mar 2017
Wednesday, Mar 01, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Friday, Feb 17, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Monday, Jan 23, 2017
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [meer...]
Satellite image of Klyuchevskoy volcano on 22 Jan 2017
Sunday, Jan 22, 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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