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Случайные фотографии
Klyuchevskoy вулкан
Стратовулкан 4835 m (15,863 ft)
Kamchatka, 56.06°N / 160.64°E
Текущее состояние: незначительные действия или извержения предупреждение (3 из 5)
Klyuchevskoy Веб-камеры / данные в реальном времени | Reports
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Klyuchevskoy Вулкан-извержения:
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
Типичный извержения стиль:
Преимущественно взрывчатого вещества, Стромболианская и извержение активности, иногда потоки лавы из жерла трещина. В настоящее время в фазе вблизи Персистирующая активность.
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Latest satellite images
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: 20/1420Z

Вторник дек 20, 2016 15:15 |

Satellite image of Klyuchevskoy volcano on 20 Dec 2016
Satellite image of Klyuchevskoy volcano on 20 Dec 2016
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report:

FVFE01 at 15:00 UTC, 20/12/16 from RJTD
VA ADVISORY
DTG: 20161220/1500Z
VAAC: TOKYO
VOLCANO: KLYUCHEVSKOY 300260
PSN: N5603 E16039
AREA: RUSSIA
SUMMIT ELEV: 4754M
ADVISORY NR: 2016/482
INFO SOURCE: HIMAWARI-8
AVIATION COLOUR CODE: NIL
ERUPTION DETAILS: VA EMISSIONS CONTINUING
OBS VA DTG: 20/1420Z
OBS VA CLD: SFC/FL220 N5607 E16036 - N5702 E16019 - N5703 E16026 -
N5609 E16040 MOV N 20KT
FCST VA CLD +6 HR: 20/2020Z SFC/FL230 N5856 E15943 - N5751 E16054 -
N5656 E16052 - N5842 E15904
FCST VA CLD +12 HR: 21/0220Z SFC/FL220 N5832 E16033 - N5722 E16111 -

N5942 E15711 - N6000 E15754 - N5925 E15923
FCST VA CLD +18 HR: 21/0820Z SFC/FL220 N5903 E16004 - N5754 E16138 -

N5747 E16117 - N5936 E15538 - N6023 E15413 - N6038 E15529
RMK: NIL
NXT ADVISORY: 20161220/1800Z=

Предыдущие новости
Вторник, дек 20, 2016
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [подробнее]
Klyuchevskoy's steam plume this morning
Понедельник, дек 19, 2016
По словам KVERT недавние эффузивные фугасные извержения вулкана прекратилось в середине ноября. Небольшая термальная аномалия сохраняется из района саммита. ... [подробнее]
Понедельник, дек 19, 2016
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [подробнее]
Satellite image of Klyuchevskoy volcano on 26 Nov 2016
Суббота, ноя 26, 2016
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [подробнее]
Satellite image of Klyuchevskoy volcano on 17 Nov 2016
Четверг, ноя 17, 2016
Volcanic Ash Advisory Center Tokyo (VAAC) issued the following report: ... [подробнее]

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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