What is Koryaksky?

Information about Koryaksky

Koryaksky

Koryaksky volcano towers over Avacha Bay
Elevation3,456 metres (11,340 feet)
LocationKamchatka, Russia
Coordinates
TypeStratovolcano
Last eruption1957
Easiest routebasic rock/snow climb


Koryaksky or Koryakskaya Sopka (Russian: Коря́кская со́пка) is a volcano on the Kamchatka Peninsula in the far east of Russia. It lies within sight of Kamchatka Krai's administrative center, Petropavlovsk-Kamchatsky. Together with neighbouring Avachinsky, it has been designated a Decade Volcano, worthy of particular study in light of its history of explosive eruptions and proximity to populated areas.

Geological history

Koryaksky lies on the Pacific Ring of Fire, at a point where the Pacific Plate is sliding underneath the Eurasian Plate at a rate of about 80 mm/year. A wedge of mantle material lies between the subducting Pacific Plate and the overlying Eurasian Plate is the source of dynamic volcanism over the whole Kamchatka Peninsula.

The volcano has probably been active for tens of thousands of years. Geological records indicate that there have been three major eruptions in the last 10,000 years, at 5500 BC, 1950 BC and 1550 BC. These three eruptions seem to have been mainly effusive, generating extensive lava flows.

Recent activity

Enlarge picture
Clouds forming over Koryakasky


Koryaksky erupted for the first time in recorded history in 1890, in an eruption characterised by the emission of lava from fissures which opened up on the south western flank of the volcano, and phreatic explosions. It was thought to have erupted again five years later, but it was later shown that no eruption had occurred; what was thought to be an eruption column was simply steam generated by strong fumarolic activity.

Another brief, moderately explosive eruption occurred in 1926, after which the volcano was dormant until 1956. The 1956 eruption was more explosive than the previous known eruptions, with VEI=3, and generated pyroclastic flows and lahars. The eruption continued until June 1957.

Since then, the volcano has seen no further eruptions, but occasional seismic activity and ongoing fumarolic activity has indicated that the volcano is still active. In light of its proximity to Petropavlovsk-Kamchatsky, Koryaksky was designated a Decade Volcano in 1996 as part of the United Nations' International Decade for Natural Disaster Reduction, together with the nearby Avachinsky volcano.

References

Enlarge picture
Koryaksky seen from neighbouring Avachinsky's peak
  1. Droznin D., Levin V., Park J., Gordeev E. (2002), Detailed Mapping of Seismic Anisotropy Indicators in Southeastern Kamchatka, American Geophysical Union, Fall Meeting 2002
  2. Levin V., Park J., Gordeev E., Droznin D. (2002), Complex Anisotropic Structure of the Mantle Wedge Beneath Kamchatka Volcanoes, American Geophysical Union, Fall Meeting 2002
  3. Taran Y.A., Connor C.B., Shapar V.N., Ovsyannikov A.A., Bilichenko A.A. (1997), Fumarolic activity of Avachinsky and Koryaksky volcanoes, Kamchatka, from 1993 to 1994, Bulletin of Volcanology, v. 58, p. 441-448

External links

Avacha Bay (Russian: Авачинская губа, Авачинская бухта
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summit is a point on a surface which is higher in elevation than all points immediately adjacent to it. Mathematically speaking, a summit is a local maximum in elevation.
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Kamchatka Peninsula (Russian: полуо́стров Камча́тка
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Anthem
Hymn of the Russian Federation


Capital
(and largest city) Moscow

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geographic coordinate system enables every location on the earth to be specified by the three coordinates of a spherical coordinate system aligned with the spin axis of the Earth.
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Mountains can be characterized in several ways. Some mountains are volcanoes and can be characterized by the type of lava and eruptive history. Other mountains are shaped by glacial processes and can be characterized by their shape.
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stratovolcano, also called a composite volcano, is a tall, conical volcano composed of many layers of hardened lava, tephra, and volcanic ash. These volcanoes are characterized by a steep profile and periodic, explosive eruptions.
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Volcano:
1. Large magma chamber
2. Bedrock
3. Conduit (pipe)
4. Base
5. Sill
6. Branch pipe
7. Layers of ash emitted by the volcano
8. Flank 9. Layers of lava emitted by the volcano
10. Throat
11. Parasitic cone
12. Lava flow
13. Vent
14.
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19th century - 20th century - 21st century
1920s  1930s  1940s  - 1950s -  1960s  1970s  1980s
1954 1955 1956 - 1957 - 1958 1959 1960

Year 1957 (MCMLVII
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climbing route is a path by which a climber reaches the top of a mountain, rock, or ice wall. Routes can vary dramatically in difficulty and, once committed to that ascent, can be difficult to stop or return. So, choice of route can be critically important.
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Russian 
Writing system: Cyrillic (Russian variant)  
Official status
Official language of:  Abkhazia (Georgia)
 Belarus
 Commonwealth of Independent States (working)
 Crimea (de facto; Ukraine)
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Volcano:
1. Large magma chamber
2. Bedrock
3. Conduit (pipe)
4. Base
5. Sill
6. Branch pipe
7. Layers of ash emitted by the volcano
8. Flank 9. Layers of lava emitted by the volcano
10. Throat
11. Parasitic cone
12. Lava flow
13. Vent
14.
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Kamchatka Peninsula (Russian: полуо́стров Камча́тка
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Anthem
Hymn of the Russian Federation


Capital
(and largest city) Moscow

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Камчатский кра?
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Петропавловск-Камчатски?
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Avachinsky (also known as Avacha or Avacha Volcano or Avachinskaya Sopka) (Russian: Авачинская сопка,
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Decade Volcanoes are 16 volcanoes identified by the International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI) as being worthy of particular study in light of their history of large, destructive eruptions and proximity to populated areas.
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Pacific Ring of Fire is an area of frequent earthquakes and volcanic eruptions encircling the basin of the Pacific Ocean. In a 40,000 km horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and/or plate
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Pacific Plate is an oceanic tectonic plate beneath the Pacific Ocean.

To the north the easterly side is a divergent boundary with the Explorer Plate, the Juan de Fuca Plate and the Gorda Plate forming respectively the Explorer Ridge, the Juan de Fuca Ridge and the Gorda
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Eurasian Plate is a tectonic plate covering Eurasia (a landmass consisting of the traditional continents of Europe and Asia) except that it does not cover the Indian subcontinent, the Arabian subcontinent, and the area east of the Verkhoyansk Range in East Siberia.
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mantle is a ~2,900 km thick rocky shell comprising approximately 70% of Earth's volume. It is predominantly solid and overlies the Earth's iron-rich core, which occupies about 30% of Earth's volume.
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subduction zone is an area on Earth where two tectonic plates meet and move towards one another, with one sliding underneath the other and moving down into the mantle, at rates typically measured in centimeters per year.
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7th millennium BC - 6th millennium BC - 5th millennium BC During the 6th millennium BC, agriculture spreads from the Balkans to Italy and Eastern Europe and from Mesopotamia to Egypt. World population is essentially stable at ca. 5 million people.
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and

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16th century BC - 15th century BC

1580s BC 1570s BC 1560s BC - 1550s BC - 1540s BC 1530s BC 1520s BC
1559 BC 1558 BC 1557 BC 1556 BC 1555 BC
1554 BC 1553 BC 1552 BC 1551 BC 1550 BC

- - State leaders - Sovereign states
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Events and trends


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    Lava is molten rock expelled by a volcano during an eruption. When first expelled from a volcanic vent, it is a liquid at temperatures from 700 °C to 1,200 °C (1,300 °F to 2,200 °F).
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    18th century - 19th century - 20th century
    1860s  1870s  1880s  - 1890s -  1900s  1910s  1920s
    1887 1888 1889 - 1890 - 1891 1892 1893

    :
    Subjects:     Archaeology - Architecture -
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    In anatomy, fissure (Latin fissura, Plural fissurae) is a groove, natural division, deep furrow, cleft, or tear in various parts of the body.

    Natural fissure

    Various types of fissure are:
    • Auricular fissure: found in the temporal bone

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    Phreatic eruptions, also called ultravulcanian eruptions, occur when rising magma makes contact with ground or surface water. The extreme temperature of the magma (anywhere from 600 Â°C to 1,170 Â°C (1110–2140 Â°F)) causes near-instantaneous evaporation to
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